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authorRoger Frank <rfrank@pglaf.org>2025-10-15 04:55:49 -0700
committerRoger Frank <rfrank@pglaf.org>2025-10-15 04:55:49 -0700
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+<div lang="en" class="tei tei-text" style="margin-bottom: 2.00em; margin-top: 2.00em" xml:lang="en">
+ <div class="tei tei-front" style="margin-bottom: 6.00em; margin-top: 2.00em">
+ <div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+ <div id="pgheader" class="tei tei-div" style="margin-bottom: 4.00em; margin-top: 4.00em"><div class="tei tei-div" style="margin-bottom: 3.00em; margin-top: 3.00em"><p class="tei tei-p" style="margin-bottom: 2.00em">The Project Gutenberg EBook of Draining for Profit, and Draining for Health by George E. Waring</p></div><div class="tei tei-div" style="margin-bottom: 3.00em; margin-top: 3.00em"><p class="tei tei-p" style="margin-bottom: 1.00em">This eBook is for the use of anyone anywhere at no cost
+ and with almost no restrictions whatsoever. You may copy it,
+ give it away or re-use it under the terms of the Project
+ Gutenberg License <a href="#pglicense" class="tei tei-ref">included with this
+ eBook</a> or online at <a href="http://www.gutenberg.org/license" class="tei tei-xref">http://www.gutenberg.org/license</a></p></div><pre class="pre tei tei-div" style="margin-bottom: 3.00em; margin-top: 3.00em">Title: Draining for Profit, and Draining for Health
+
+Author: George E. Waring
+
+Release Date: October 4, 2006 [Ebook #19465]
+
+Language: English
+
+Character set encoding: UTF-8
+
+
+***START OF THE PROJECT GUTENBERG EBOOK DRAINING FOR PROFIT, AND DRAINING FOR HEALTH***
+</pre></div>
+ </div>
+
+ <div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+
+ </div>
+
+ <hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+ <div class="block tei tei-docTitle"><div class="block tei tei-titlePart" style="text-align: left; margin-bottom: 3.46em"><span style="font-size: 173%">Draining for Profit, and Draining for Health</span></div></div><div class="block tei tei-byline" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">by </span><span class="inline tei tei-docAuthor" style="text-align: left"><span style="font-size: 173%">George E. Waring</span></span></div><div class="tei tei-div" style="text-align: left; margin-bottom: 5.76em; margin-top: 5.76em"><span class="tei tei-docEdition" style="text-align: left"><span class="tei tei-edition" style="text-align: left"><span style="font-size: 144%">Edition 1</span></span></span><span style="font-size: 144%">, (</span><span class="tei tei-docDate" style="text-align: left"><span class="tei tei-date" style="text-align: left"><span style="font-size: 144%">October 4, 2006</span></span></span><span style="font-size: 144%">)</span></div>
+ </div>
+
+ <hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+ <p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em">New York<br />
+ Orange Judd &amp; Company,<br />
+ 245 Broadway.</p>
+ </div>
+
+ <hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+ <p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em">Entered according to Act of Congress, in the year 1867, by<br />
+ORANGE JUDD &amp; CO.</p>
+ <p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em">At the Clerk's Office of the District Court of the United States for this
+Southern District of New-York.</p>
+<p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em">Lovejoy &amp; Son,<br />
+Electrotypers and Stereotypers.<br />
+15 Vandewater street N.Y.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page003">[pg 003]</span><a name="Pg003" id="Pg003" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In presenting this book to the public the writer desires
+to say that, having in view the great importance of thorough
+work in land draining, and believing it advisable to
+avoid every thing which might be construed into an approval
+of half-way measures, he has purposely taken the
+most radical view of the whole subject, and has endeavored
+to emphasize the necessity for the utmost thoroughness in
+all draining operations, from the first staking of the lines
+to the final filling-in of the ditches.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">That it is sometimes necessary, because of limited means,
+or limited time, or for other good reasons, to drain partially
+or imperfectly, or with a view only to temporary results,
+is freely acknowledged. In these cases the occasion for
+less completeness in the work must determine the extent
+to which the directions herein laid down are to be disregarded;
+but it is believed that, even in such cases, the
+principles on which those directions are founded should
+be always borne in mind.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-variant: small-caps">Newport, R.I.</span></span>, 1867.</p>
+</div>
+
+ <hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+ <h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">Illustrations</span></h1>
+ <ul class="tei tei-index tei-index-fig"><li><a href="#fig3">Fig. 1 - A DRY SOIL.</a></li><li><a href="#fig4">Fig. 2 - A WET SOIL.</a></li><li><a href="#fig5">Fig. 3 - A DRAINED SOIL.</a></li><li><a href="#fig10">Fig. 4 - MAP OF LAND, WITH SWAMPS, ROCKS, SPRINGS AND TREES. INTENDED TO REPRESENT A FIELD OF TEN ACRES BEFORE DRAINING.</a></li><li><a href="#fig11">Fig. 5 - MAP WITH 50-FOOT SQUARES, AND CONTOUR LINES.</a></li><li><a href="#fig12">Fig. 6 - LEVELLING INSTRUMENT.</a></li><li><a href="#fig13">Fig. 7 - LEVELLING ROD.</a></li><li><a href="#fig14">Fig. 8 - MAP WITH CONTOUR LINES.</a></li><li><a href="#fig15">Fig. 9 - WELL'S CLINOMETER.</a></li><li><a href="#fig16">Fig. 10 - STONE PIT TO CONNECT SPRING WITH DRAIN.</a></li><li><a href="#fig17">Fig. 11 - STONE AND TILE BASIN FOR SPRING WITH DRAIN.</a></li><li><a href="#fig18">Fig. 12 - LINE OF SATURATION BETWEEN DRAINS.</a></li><li><a href="#fig19">Fig. 13 - HORSE-SHOE TILE.</a></li><li><a href="#fig20">Fig. 14 - SOLE TILE.</a></li><li><a href="#fig21">Fig. 15 - DOUBLE-SOLE TILE.</a></li><li><a href="#fig22">Fig. 16 - ROUND TILE AND COLLAR, AND THE SAME AS LAID.</a></li><li><a href="#fig23">Fig. 19 - THREE PROFILES OF DRAINS, WITH DIFFERENT INCLINATIONS.</a></li><li><a href="#fig24">Fig. 20 - MAP WITH DRAINS AND CONTOUR LINES.</a></li><li><a href="#fig25">Fig. 21 - PROFILE OF DRAIN C.</a></li><li><a href="#fig28">Fig. 22 - SET OF TOOLS.</a></li><li><a href="#fig29">Fig. 23 - OUTLET, SECURED WITH MASONRY AND GRATING.</a></li><li><a href="#fig30">Fig. 24 - SILT-BASIN, BUILT TO THE SURFACE.</a></li><li><a href="#fig31">Fig. 25 - FINISHING SPADE.</a></li><li><a href="#fig32">Fig. 26 - FINISHING SCOOP.</a></li><li><a href="#fig33">Fig. 27 - BRACING THE SIDES IN SOFT LAND.</a></li><li><a href="#fig34">Fig. 28 - MEASURING STAFF.</a></li><li><a href="#fig35">Fig. 29 - BONING ROD.</a></li><li><a href="#fig36">Fig. 30 - POSITION OF WORKMAN AND USE OF FINISHING SCOOP.</a></li><li><a href="#fig37">Fig. 31 - SIGHTING BY THE BONING-RODS.</a></li><li><a href="#fig38">Fig. 32 - PICK FOR DRESSING AND PREFORATING TILE.</a></li><li><a href="#fig39">Fig. 33 - LATERAL DRAIN ENTERING AT TOP.</a></li><li><a href="#fig40">Fig. 34 - SECTIONAL VIEW OF JOINT.</a></li><li><a href="#fig41">Fig. 35 - SQUARE BRICK SILT-BASIN.</a></li><li><a href="#fig42">Fig. 36 - SILT-BASIN OF VITRIFIED PIPE.</a></li><li><a href="#fig43">Fig. 37 - TILE SILT-BASIN.</a></li><li><a href="#fig44">Fig. 38 - MAUL FOR RAMMING.</a></li><li><a href="#fig45">Fig. 39 - BOARD SCRAPER FOR FILLING DITCHES.</a></li><li><a href="#fig46">Fig. 40 - CROSS-SECTION OF DITCH (FILLED), WITH FURROW AT EACH SIDE.</a></li><li><a href="#fig51">Fig. 41 - FOOT PICK.</a></li><li><a href="#fig56">Fig. 42 - PUG-MILL.</a></li><li><a href="#fig57">Fig. 43 - PLATE OF DIES.</a></li><li><a href="#fig58">Fig. 44 - CHEAP WOODEN MACHINE.</a></li><li><a href="#fig59">Fig. 45 - MANDRIL FOR CARRYING TILES FROM MACHINE.</a></li><li><a href="#fig60">Fig. 46 - CLAY-KILN.</a></li><li><a href="#fig63">Fig. 47 - DYKE AND DITCH.</a></li><li><a href="#fig68">Fig. 48 - OLD STYLE HOUSE DRAINAGE AND SEWERAGE.</a></li><li><a href="#fig69">Fig. 49 - MODERN HOUSE DRAINAGE AND SEWERAGE.</a></li></ul>
+ </div>
+
+ <hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+ <h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">Contents</span></h1>
+ <ul class="tei tei-index tei-index-toc"><li><a href="#toc1">CHAPTER I. - LAND TO BE DRAINED AND THE REASONS WHY.</a></li><li><a href="#toc6">CHAPTER II. - HOW DRAINS ACT, AND HOW THEY AFFECT THE SOIL</a></li><li><a href="#toc8">CHAPTER III. - HOW TO GO TO WORK TO LAY OUT A SYSTEM OF DRAINS.</a></li><li><a href="#toc26">CHAPTER IV. - HOW TO MAKE THE DRAINS.</a></li><li><a href="#toc47">CHAPTER V. - HOW TO TAKE CARE OF DRAINS AND DRAINED LAND.</a></li><li><a href="#toc49">CHAPTER VI. - WHAT DRAINING COSTS.</a></li><li><a href="#toc52">CHAPTER VII. - "WILL IT PAY?"</a></li><li><a href="#toc54">CHAPTER VIII. - HOW TO MAKE DRAINING TILES.</a></li><li><a href="#toc61">CHAPTER IX. - THE RECLAIMING OF SALT MARSHES.</a></li><li><a href="#toc64">CHAPTER X. - MALARIAL DISEASES.</a></li><li><a href="#toc66">CHAPTER XI. - HOUSE DRAINAGE AND TOWN SEWERAGE IN
+THEIR RELATIONS TO THE PUBLIC HEALTH.</a></li><li><a href="#toc70">INDEX</a></li></ul>
+ </div>
+
+</div>
+
+<div class="tei tei-body" style="margin-bottom: 6.00em; margin-top: 6.00em">
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page007">[pg 007]</span><a name="Pg007" id="Pg007" class="tei tei-anchor"></a>
+<a name="toc1" id="toc1"></a>
+<a name="pdf2" id="pdf2"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER I. - LAND TO BE DRAINED AND THE REASONS WHY.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Land which requires draining hangs out a sign of its
+condition, more or less clear, according to its circumstances,
+but always unmistakable to the practiced eye. Sometimes
+it is the broad banner of standing water, or dark, wet streaks
+in plowed land, when all should be dry and of even color;
+sometimes only a fluttering rag of distress in curling corn,
+or wide-cracking clay, or feeble, spindling, shivering grain,
+which has survived a precarious winter, on the ice-stilts
+that have stretched its crown above a wet soil; sometimes
+the quarantine flag of rank growth and dank miasmatic fogs.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">To recognize these indications is the first office of the
+drainer; the second, to remove the causes from which they
+arise.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If a rule could be adopted which would cover the varied
+circumstances of different soils, it would be somewhat as
+follows: All lands, of whatever texture or kind, in which
+<span class="tei tei-hi"><span style="font-style: italic">the spaces between the particles of soil</span></span> are filled with water,
+(whether from rain or from springs,) within less than four
+feet of the surface of the ground, except during and
+<span class="tei tei-hi"><span style="font-style: italic">immediately</span></span> after heavy rains, require draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of course, the <span class="tei tei-hi"><span style="font-style: italic">particles</span></span> of the soil cannot be made dry,
+nor should they be; but, although they should be moist
+themselves, they should be surrounded with air, not with
+water. To illustrate this: suppose that water be poured
+into a barrel filled with chips of wood until it runs over at
+the top. The spaces between the chips will be filled with<span class="tei tei-pb" id="page008">[pg 008]</span><a name="Pg008" id="Pg008" class="tei tei-anchor"></a>
+water, and the chips themselves will absorb enough to become
+thoroughly wet;—this represents the worst condition
+of a wet soil. If an opening be made at the bottom of the
+barrel, the water which fills the spaces between the chips
+will be drawn off, and its place will be taken by air, while
+the chips themselves will remain wet from the water which
+they hold by absorption. A drain at the bottom of a wet
+field draws away the water from the free spaces between
+its particles, and its place is taken by air, while the particles
+hold, by attraction, the moisture necessary to a healthy
+condition of the soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There are vast areas of land in this country which do
+not need draining. The whole range of sands, gravels,
+light loams and moulds allow water to pass freely through
+them, and are sufficiently drained by nature, <span class="tei tei-hi"><span style="font-style: italic">provided</span></span>,
+they are as open at the bottom as throughout the mass.
+A sieve filled with gravel will drain perfectly; a basin filled
+with the same gravel will not drain at all. More than this,
+a sieve filled with the stiffest clay, if not "puddled,"<a id="noteref_1" name="noteref_1" href="#note_1"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">1</span></span></a>
+will drain completely, and so will heavy clay soils on porous
+and well drained subsoils. Money expended in draining
+such lands as do not require the operation is, of course,
+wasted; and when there is doubt as to the requirement,<span class="tei tei-pb" id="page009">[pg 009]</span><a name="Pg009" id="Pg009" class="tei tei-anchor"></a>
+tests should be made before the outlay for so
+costly work is encountered.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There is, on the other hand, much land which only by
+thorough-draining can be rendered profitable for cultivation,
+or healthful for residence, and very much more, described
+as "ordinarily dry land," which draining would
+greatly improve in both productive value and salubrity.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Surface Indications</span></span> of the necessity for draining
+are various. Those of actual swamps need no description;
+those of land in cultivation are more or less evident at
+different seasons, and require more or less care in their examination,
+according to the circumstances under which
+they are manifested.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If a plowed field show, over a part or the whole of its
+surface, a constant appearance of dampness, indicating that,
+as fast as water is dried out from its upper parts, more
+is forced up from below, so that after a rain it is much
+longer than other lands in assuming the light color of dry
+earth, it unmistakably needs draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A pit, sunk to the depth of three or four feet in the
+earth, may collect water at its bottom, shortly after a
+rain;—this is a sure sign of the need of draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">All tests of the condition of land as to water,—such as
+trial pits, etc.,—should be made, when practicable, during
+the wet spring weather, or at a time when the springs and
+brooks are running full. If there be much water in the
+soil, even at such times, it needs draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the water of heavy rains stands for some time on the
+surface, or if water collects in the furrow while plowing,
+draining is necessary to bring the land to its full fertility.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Other indications may be observed in dry weather;—wide
+cracks in the soil are caused by the drying of clays, which,
+by previous soaking, have been pasted together; the curling
+of corn often indicates that in its early growth it has
+been prevented, by a wet subsoil, from sending down its
+roots below the reach of the sun's heat, where it would find,<span class="tei tei-pb" id="page010">[pg 010]</span><a name="Pg010" id="Pg010" class="tei tei-anchor"></a>
+even in the dryest weather, sufficient moisture for a healthy
+growth; any <span class="tei tei-hi"><span style="font-style: italic">severe</span></span> effect of drought, except on poor
+sands and gravels, may be presumed to result from the
+same cause; and a certain wiryness of grass, together with
+a mossy or mouldy appearance of the ground, also indicate
+excessive moisture during some period of growth. The
+effects of drought are, of course, sometimes manifested on
+soils which do not require draining,—such as those poor
+gravels, which, from sheer poverty, do not enable plants
+to form vigorous and penetrating roots; but any soil of
+ordinary richness, which contains a fair amount of clay,
+will withstand even a severe drought, without great injury
+to its crop, if it is thoroughly drained, and is kept loose at
+its surface.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Poor crops are, when the cultivation of the soil is reasonably
+good, caused either by inherent poverty of the
+land, or by too great moisture during the season of early
+growth. Which of these causes has operated in a particular
+case may be easily known. Manure will correct the difficulty
+in the former case, but in the latter there is no real remedy
+short of such a system of drainage as will thoroughly relieve
+the soil of its surplus water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Sources of the Water</span></span> in the soil are various.
+Either it falls directly upon the land as rain; rises into it
+from underlying springs; or reaches it through, or over,
+adjacent land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">rain water</span></span> belongs to the field on which it falls, and
+it would be an advantage if it could all be made to pass
+down through the first three or four feet of the soil, and be
+removed from below. Every drop of it is freighted with
+fertilizing matters washed out from the air, and in its descent
+through the ground, these are given up for the use
+of plants; and it performs other important work among
+the vegetable and mineral parts of the soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">spring water</span></span> does not belong to the field,—not a<span class="tei tei-pb" id="page011">[pg 011]</span><a name="Pg011" id="Pg011" class="tei tei-anchor"></a>
+drop of it,—and it ought not to be allowed to show itself
+within the reach of the roots of ordinary plants. It has
+fallen on other land, and, presumably, has there done its
+appointed work, and ought not to be allowed to convert
+our soil into a mere outlet passage for its removal.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">ooze water</span></span>,—that which soaks out from adjoining
+land,—is subject to all the objections which hold against
+spring water, and should be rigidly excluded.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">But the <span class="tei tei-hi"><span style="font-style: italic">surface water</span></span> which comes over the surface of
+higher ground in the vicinity, should be allowed every
+opportunity, which is consistent with good husbandry, to
+work its slow course over our soil,—not to run in such
+streams as will cut away the surface, nor in such quantities
+as to make the ground inconveniently wet, but to spread
+itself in beneficent irrigation, and to deposit the fertilizing
+matters which it contains, then to descend through a well-drained
+subsoil, to a free outlet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">From whatever source the water comes, it cannot remain
+stagnant in any soil without permanent injury to its fertility.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Objection to too much Water in the Soil</span></span> will
+be understood from the following explanation of the process
+of germination, (sprouting,) and growth. Other grave
+reasons why it is injurious will be treated in their proper
+order.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The first growth of the embryo plant, (in the seed,) is
+merely a change of form and position of the material which
+the seed itself contains. It requires none of the elements
+of the soil, and would, under the same conditions, take place
+as well in moist saw-dust as in the richest mold. The
+conditions required are, the exclusion of light; a certain
+degree of heat; and the presence of atmospheric air, and
+moisture. Any material which, without entirely excluding
+the air, will shade the seed from the light, yield
+the necessary amount of moisture, and allow the accumulation
+of the requisite heat, will favor the chemical<span class="tei tei-pb" id="page012">[pg 012]</span><a name="Pg012" id="Pg012" class="tei tei-anchor"></a>
+changes which, under these circumstances, take place in the
+living seed. In proportion as the heat is reduced by the
+chilling effect of evaporation, and as atmospheric air is excluded,
+will the germination of the seed be retarded; and,
+in case of complete saturation for a long time, absolute
+decay will ensue, and the germ will die.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The accompanying illustrations, (Figures 1, 2 and 3,) from
+the "Minutes of Information" on Drainage, submitted by
+the General Board of Health to the British Parliament in
+1852, represent the different conditions of the soil as to
+moisture, and the effect of these conditions on the germination
+of seeds. The figures are thus explained by Dr.
+Madden, from whose lecture they are taken:</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"Soil, examined mechanically, is found to consist entirely
+of particles of all shapes and sizes, from stones and pebbles
+down to the finest powder; and, on account of their
+extreme irregularity of shape, they cannot lie so close to
+one another as to prevent there being passages between
+them, owing to which circumstance soil in the mass is
+always more or less </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">porous</span></span><span style="font-size: 90%">. If, however, we proceed to
+examine one of the smallest particles of which soil is
+made up, we shall find that even this is not always solid,
+but is much more frequently porous, like soil in the mass.
+A considerable proportion of this finely-divided part of
+soil, </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">the impalpable matter</span></span><span style="font-size: 90%">, as it is generally called, is
+found, by the aid of the microscope, to consist of </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">broken
+down vegetable tissue</span></span><span style="font-size: 90%">, so that when a small portion of
+the finest dust from a garden or field is placed under the
+microscope, we have exhibited to us particles of every
+variety of shape and structure, of which a certain part is
+evidently of vegetable origin.</span></p>
+
+<a name="fig3" id="fig3"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 1.80em"><img src="images/image01.png" width="640" height="546" alt="Illustration: Fig. 1 - A DRY SOIL." title="Fig. 1 - A DRY SOIL." /><div class="tei tei-head" style="text-align: center; margin-bottom: 0.90em; margin-top: 0.90em"><span style="font-size: 90%">Fig. 1 - A DRY SOIL.</span></div></div>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"In these figures I have given a very rude representation
+of these particles; and I must beg you particularly to
+remember that they are not meant to represent by any
+means accurately what the microscope exhibits, but are</span><span class="tei tei-pb" id="page013">[pg 013]</span><a name="Pg013" id="Pg013" class="tei tei-anchor"></a><span style="font-size: 90%">
+only designed to serve as a plan by which to illustrate
+the mechanical properties of the soil. On referring to
+Fig. 1, we perceive that there are two distinct classes of
+pores,—first, the large ones, which exist </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">between</span></span><span style="font-size: 90%"> the particles
+of soil, and second, the very minute ones, which
+occur in the particles themselves; and you will at the
+same time notice that,
+whereas all the larger
+pores,—those between the
+particles of soil,—communicate
+most freely with
+each other, so that they
+form canals, the small
+pores, however freely they
+may communicate with
+one another in the interior
+of the particle in which
+they occur, have no direct
+connection with the pores of the surrounding particles.
+Let us now, therefore, trace the effect of this arrangement.
+In Fig. 1 we perceive that
+these canals and pores are
+all empty, the soil being
+</span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">perfectly dry</span></span><span style="font-size: 90%">; and the
+canals communicating freely
+at the surface with the
+surrounding atmosphere,
+the whole will of course
+be filled with air. If in
+this condition a seed be
+placed in the soil, at </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">a</span></span><span style="font-size: 90%">,
+you at once perceive that
+it is freely supplied with air, </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">but there is no moisture</span></span><span style="font-size: 90%">;
+therefore, when soil is </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">perfectly dry</span></span><span style="font-size: 90%">, a seed cannot grow.</span></p>
+
+<a name="fig4" id="fig4"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 1.80em"><img src="images/image02.png" width="640" height="546" alt="Illustration: Fig. 2 - A WET SOIL." title="Fig. 2 - A WET SOIL." /><div class="tei tei-head" style="text-align: center; margin-bottom: 0.90em; margin-top: 0.90em"><span style="font-size: 90%">Fig. 2 - A WET SOIL.</span></div></div>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"Let us turn our attention now to Fig. 2. Here we</span><span class="tei tei-pb" id="page014">[pg 014]</span><a name="Pg014" id="Pg014" class="tei tei-anchor"></a><span style="font-size: 90%">
+perceive that both the pores and canals are no longer
+represented white, but black, this color being used to indicate
+water; in this instance, therefore, water has taken
+the place of air, or, in other words, the soil is </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">very wet</span></span><span style="font-size: 90%">.
+If we observe our seed </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">a</span></span><span style="font-size: 90%"> now, we find it abundantly
+supplied with water, but </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">no air</span></span><span style="font-size: 90%">. Here again, therefore,
+germination cannot take place. It may be well to state
+here that this can never occur </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">exactly</span></span><span style="font-size: 90%"> in nature, because,
+water having the power of dissolving air to a certain
+extent, the seed </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">a</span></span><span style="font-size: 90%"> in Fig. 2 is, in fact, supplied with a
+</span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">certain</span></span><span style="font-size: 90%"> amount of this necessary substance; and, owing
+to this, germination does take place, although by no
+means under such advantageous circumstances as it would
+were the soil in a better condition.</span></p>
+
+<a name="fig5" id="fig5"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 1.80em"><img src="images/image03.png" width="640" height="544" alt="Illustration: Fig. 3 - A DRAINED SOIL." title="Fig. 3 - A DRAINED SOIL." /><div class="tei tei-head" style="text-align: center; margin-bottom: 0.90em; margin-top: 0.90em"><span style="font-size: 90%">Fig. 3 - A DRAINED SOIL.</span></div></div>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"We pass on now to Fig. 3. Here we find a different
+state of matters. The canals are open and freely supplied
+with air, while the pores are filled with water; and,
+consequently, you perceive
+that, while the seed </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">a</span></span><span style="font-size: 90%"> has
+quite enough of air from
+the canals, it can never be
+without moisture, as every
+particle of soil which
+touches it is well supplied
+with this necessary ingredient.
+This, then, is
+the proper condition of soil
+for germination, and in
+fact for every period of the
+plant's development; and this condition occurs when the
+soil is </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">moist</span></span><span style="font-size: 90%">, but not </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">wet</span></span><span style="font-size: 90%">,—that is to say, when it has the
+color and appearance of being well watered, but when it
+is still capable of being crumbled to pieces by the hands,
+without any of its particles adhering together in the
+familiar form of mud."</span></p>
+</div>
+
+<span class="tei tei-pb" id="page015">[pg 015]</span><a name="Pg015" id="Pg015" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As plants grow under the same conditions, as to soil,
+that are necessary for the germination of seeds, the foregoing
+explanation of the relation of water to the particles
+of the soil is perfectly applicable to the whole period of
+vegetable growth. The soil, to the entire depth occupied
+by roots, which, with most cultivated plants is, in drained
+land, from two to four feet, or even more, should be maintained,
+as nearly as possible, in the condition represented
+in Fig. 3,—that is, the particles of soil should hold water
+by attraction, (absorption,) and the spaces between the
+particles should be filled with air. Soils which require
+drainage are not in this condition. When they are not
+saturated with water, they are generally dried into lumps
+and clods, which are almost as impenetrable by roots as so
+many stones. The moisture which these clods contain is
+not available to plants, and their surfaces are liable to be
+dried by the too free circulation of air among the wide
+fissures between them. It is also worthy of incidental remark,
+that the cracking of heavy soils, shrinking by
+drought, is attended by the tearing asunder of the smaller
+roots which may have penetrated them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Injurious Effects of Standing Water in the Subsoil</span></span>
+may be best explained in connection with the description
+of a soil which needs under-draining. It would
+be tedious, and superfluous, to attempt to detail the various
+geological formations and conditions which make the soil
+unprofitably wet, and render draining necessary. Nor,—as
+this work is intended as a hand-book for practical use,—is
+it deemed advisable to introduce the geological charts and
+sections, which are so often employed to illustrate the
+various sources of under-ground water; interesting as
+they are to students of the theories of agriculture, and
+important as the study is, their consideration here would
+consume space, which it is desired to devote only to the
+reasons for, and the practice of, thorough-draining.</p>
+
+<span class="tei tei-pb" id="page016">[pg 016]</span><a name="Pg016" id="Pg016" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">To one writing in advocacy of improvements, of any
+kind, there is always a temptation to throw a tub to the
+popular whale, and to suggest some make-shift, by which
+a certain advantage may be obtained at half-price. It is
+proposed in this essay to resist that temptation, and to adhere
+to the rule that "whatever is worth doing, is worth
+doing well," in the belief that this rule applies in no
+other department of industry with more force than in the
+draining of land, whether for agricultural or for sanitary
+improvement. Therefore, it will not be recommended that
+draining be ever confined to the wettest lands only; that, in
+the pursuance of a penny-wisdom, drains be constructed
+with stones, or brush, or boards; that the antiquated
+horse-shoe tiles be used, because they cost less money; or
+that it will, in any case, be economical to make only such
+drains as are necessary to remove the water of large springs.
+The doctrine herein advanced is, that, so far as draining
+is applied at all, it should be done in the most thorough
+and complete manner, and that it is better that, in
+commencing this improvement, a single field be really well
+drained, than that the whole farm be half drained.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of course, there are some farms which suffer from too
+much water, which are not worth draining at present;
+many more which, at the present price of frontier lands,
+are only worth relieving of the water which stands on the
+surface; and not a few on which the quantity of stone to
+be removed suggests the propriety of making wide ditches,
+in which to hide them, (using the ditches, incidentally, as
+drains). A hand-book of draining is not needed by the
+owners of these farms; their operations are simple, and they
+require no especial instruction for their performance. This
+work is addressed especially to those who occupy lands of
+sufficient value, from their proximity to market, to make
+it cheaper to cultivate well, than to buy more land for the
+sake of getting a larger return from poor cultivation.<span class="tei tei-pb" id="page017">[pg 017]</span><a name="Pg017" id="Pg017" class="tei tei-anchor"></a>
+Wherever Indian corn is worth fifty cents a bushel, on the
+farm, it will pay to thoroughly drain every acre of land
+which needs draining. If, from want of capital, this cannot
+be done at once, it is best to first drain a portion of the
+farm, doing the work thoroughly well, and to apply the
+return from the improvement to its extension over other
+portions afterward.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In pursuance of the foregoing declaration of principles,
+it is left to the sagacity of the individual operator, to decide
+when the full effect desired can be obtained, on particular
+lands, without applying the regular system of depth
+and distance, which has been found sufficient for the worst
+cases. The directions of this book will be confined to the
+treatment of land which demands thorough work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Such land is that which, at some time during the period
+of vegetation, contains stagnant water, at least in its sub-soil,
+within the reach of the roots of ordinary crops; in
+which there is not a free outlet <span class="tei tei-hi"><span style="font-style: italic">at the bottom</span></span> for all the
+water which it receives from the heavens, from adjoining
+land, or from springs; and which is more or less in the condition
+of standing in a great, water-tight box, with openings
+to let water in, but with no means for its escape, except
+by evaporation at the surface; or, having larger inlets
+than outlets, and being at times "water-logged," at
+least in its lower parts. The subsoil, to a great extent, consists
+of clay or other compact material, which is not <span class="tei tei-hi"><span style="font-style: italic">impervious</span></span>,
+in the sense in which india-rubber is impervious,
+(else it could not have become wet,) but which is sufficiently
+so to prevent the free escape of water. The surface
+soil is of a lighter or more open character, in consequence
+of the cultivation which it has received, or of the decayed
+vegetable matter and the roots which it contains.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In such land the subsoil is wet,—almost constantly wet,—and
+the falling rain, finding only the surface soil in a condition
+to receive it, soon fills this, and often more than fills it,
+and stands on the surface. After the rain, come wind and<span class="tei tei-pb" id="page018">[pg 018]</span><a name="Pg018" id="Pg018" class="tei tei-anchor"></a>
+sun, to dry off the standing water,—to dry out the free water
+in the surface soil, and to drink up the water of the
+subsoil, which is slowly drawn from below. If no spring,
+or ooze, keep up the supply, and if no more rain fall,
+the subsoil may be dried to a considerable depth, cracking
+and gaping open, in wide fissures, as the clay loses its
+water of absorption, and shrinks. After the surface soil has
+become sufficiently dry, the land may be plowed, seeds will
+germinate, and plants will grow. If there be not too much
+rain during the season, nor too little, the crop may be a
+fair one,—if the land be rich, a very good one. It is not impossible,
+nor even very uncommon, for such soils to produce
+largely, but they are always precarious. To the labor
+and expense of cultivation, which fairly earn a secure return,
+there is added the anxiety of chance; success is greatly
+dependent on the weather, and the weather may be bad:
+Heavy rains, after planting, may cause the seed to rot in the
+ground, or to germinate imperfectly; heavy rains during
+early growth may give an unnatural development, or a
+feeble character to the plants; later in the season, the want
+of sufficient rain may cause the crop to be parched by
+drought, for its roots, disliking the clammy subsoil below,
+will have extended within only a few inches of the surface,
+and are subject, almost, to the direct action of the sun's
+heat; in harvest time, bad weather may delay the gathering
+until the crop is greatly injured, and fall and spring
+work must often be put off because of wet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The above is no fancy sketch. Every farmer who cultivates
+a retentive soil will confess, that all of these inconveniences
+conspire, in the same season, to lessen his returns,
+with very damaging frequency; and nothing is more common
+than for him to qualify his calculations with the proviso,
+"if I have a good season." He prepares his ground,
+plants his seed, cultivates the crop, "does his best,"—thinks
+he does his best, that is,—and trusts to Providence
+to send him good weather. Such farming is attended with<span class="tei tei-pb" id="page019">[pg 019]</span><a name="Pg019" id="Pg019" class="tei tei-anchor"></a>
+too much uncertainty,—with too much <span class="tei tei-hi"><span style="font-style: italic">luck</span></span>,—to be satisfactory;
+yet, so long as the soil remains in its undrained
+condition, the element of luck will continue to play a very
+important part in its cultivation, and bad luck will often
+play sad havoc with the year's accounts.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Land of this character is usually kept in grass, as long
+as it will bring paying crops, and is, not unfrequently, only
+available for pasture; but, both for hay and for pasture, it
+is still subject to the drawback of the uncertainty of the
+seasons, and in the best seasons it produces far less than it
+might if well drained.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The effect of this condition of the soil on the health of animals
+living on it, and on the health of persons living near
+it, is extremely unfavorable; the discussion of this branch
+of the question, however, is postponed to a later chapter.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Thus far, there have been considered only the <span class="tei tei-hi"><span style="font-style: italic">effects</span></span> of
+the undue moisture in the soil. The manner in which these
+effects are produced will be examined, in connection with
+the manner in which draining overcomes them,—reducing
+to the lowest possible proportion, that uncertainty which
+always attaches to human enterprises, and which is falsely
+supposed to belong especially to the cultivation of the soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Why is it that the farmer believes, why should any
+one believe, in these modern days, when the advancement
+of science has so simplified the industrial processes
+of the world, and thrown its light into so many corners,
+that the word "mystery" is hardly to be applied to any
+operation of nature, save to that which depends on the
+always mysterious Principle of Life,—when the effect of any
+combination of physical circumstances may be foretold,
+with almost unerring certainty,—why should we believe
+that the success of farming must, after all, depend
+mainly on chance? That an intelligent man should submit
+the success of his own patient efforts to the operation of
+"luck;" that he should deliberately <span class="tei tei-hi"><span style="font-style: italic">bet</span></span> his capital, his toil,<span class="tei tei-pb" id="page020">[pg 020]</span><a name="Pg020" id="Pg020" class="tei tei-anchor"></a>
+and his experience on having a good season, or a bad one,—this
+is not the least of the remaining mysteries. Some
+chance there must be in all things,—more in farming
+than in mechanics, no doubt; but it should be made to
+take the smallest possible place in our calculations, by a
+careful avoidance of every condition which may place our
+crops at the mercy of that most uncertain of all things—the
+weather; and especially should this be the case, when
+the very means for lessening the element of chance in our
+calculations are the best means for increasing our crops, even
+in the most favorable weather.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page021">[pg 021]</span><a name="Pg021" id="Pg021" class="tei tei-anchor"></a>
+<a name="toc6" id="toc6"></a>
+<a name="pdf7" id="pdf7"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER II. - HOW DRAINS ACT, AND HOW THEY AFFECT THE SOIL</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For reasons which will appear, in the course of this work,
+the only sort of drain to which reference is here made is that
+which consists of a conduit of burned clay, (tile,) placed at a
+considerable depth in the subsoil, and enclosed in a compacted
+bed of the stiffest earth which can conveniently be found.
+Stone-drains, brush-drains, sod-drains, mole-plow tracks,
+and the various other devices for forming a conduit for the
+conveying away of the soakage-water of the land, are not
+without the support of such arguments as are based on the
+expediency of make-shifts, and are, perhaps, in rare cases,
+advisable to be used; but, for the purposes of permanent
+improvement, they are neither so good nor so economical as
+tile-drains. The arguments of this book have reference to
+the latter, (as the most perfect of all drains thus far invented,)
+though they will apply, in a modified degree, to all
+underground conduits, so long as they remain free from obstructions.
+Concerning stone-drains, attention may properly
+be called to the fact that, (contrary to the general
+opinion of farmers,) they are very much more expensive
+than tile-drains. So great is the cost of cutting the ditches
+to the much greater size required for stone than for tiles, of
+handling the stones, of placing them properly in the ditches,
+and of covering them, after they are laid, with a suitable barrier
+to the rattling down of loose earth among them, that,
+as a mere question of first cost, it is far cheaper to buy
+tiles than to use stones, although these may lie on the surface<span class="tei tei-pb" id="page022">[pg 022]</span><a name="Pg022" id="Pg022" class="tei tei-anchor"></a>
+of the field, and only require to be placed in the
+trenches. In addition to this, the great liability of stone-drains
+to become obstructed in a few years, and the certainty
+that tile-drains will, practically, last forever, are
+conclusive arguments in favor of the use of the latter.
+If the land is stony, it must be cleared; this is a proposition
+by itself, but if the sole object is to make drains, the
+best material should be used, and this material is not stone.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A well laid tile-drain has the following essential characteristics:—1.
+It has a free outlet for the discharge of all
+water which may run through it. 2. It has openings, at its
+joints, sufficient for the admission of all the water which
+may rise to the level of its floor. 3. Its floor is laid on a
+well regulated line of descent, so that its current may
+maintain a flow of uniform, or, at least, never decreasing
+rapidity, throughout its entire length.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Land which requires draining, is that which, at some
+time during the year, (either from an accumulation of the
+rains which fall upon it, from the lateral flow, or soakage,
+from adjoining land, from springs which open within it, or
+from a combination of two or all of these sources,) becomes
+filled with water, that does not readily find a natural
+outlet, but remains until removed by evaporation. Every
+considerable addition to its water wells up, and soaks its
+very surface; and that which is added after it is already
+brim full, must flow off over the surface, or lie in puddles
+upon it. Evaporation is a slow process, and it becomes
+more and more slow as the level of the water recedes from
+the surface, and is sheltered, by the overlying earth, from the
+action of sun and wind. Therefore, at least during the
+periods of spring and fall preparation of the land, during
+the early growth of plants, and often even in midsummer,
+the <span class="tei tei-hi"><span style="font-style: italic">water-table</span></span>,—the top of the water of saturation,—is
+within a few inches of the surface, preventing the natural
+descent of roots, and, by reason of the small space to receive<span class="tei tei-pb" id="page023">[pg 023]</span><a name="Pg023" id="Pg023" class="tei tei-anchor"></a>
+fresh rains, causing an interruption of work for some
+days after each storm.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If such land is properly furnished with tile-drains, (having
+a clear and sufficient outfall, offering sufficient means
+of entrance to the water which reaches them, and carrying
+it, by a uniform or increasing descent, to the outlet,)
+its water will be removed to nearly, or quite, the level
+of the floor of the drains, and its water-table will be at the
+distance of some feet from the surface, leaving the spaces
+between the particles of all of the soil above it filled with
+air instead of water. The water below the drains stands
+at a level, like any other water that is dammed up. Rain
+water falling on the soil will descend by its own weight to
+this level, and the water will rise into the drains, as it
+would flow over a dam, until the proper level is again attained.
+Spring water entering from below, and water oozing
+from the adjoining land, will be removed in like manner,
+and the usual condition of the soil, above the water-table,
+will be that represented in Fig. 3, the condition which
+is best adapted to the growth of useful plants.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the heaviest storms, some water will flow over the
+surface of even the dryest beach-sand; but, in a well
+drained soil the water of ordinary rains will be at once
+absorbed, will slowly descend toward the water-table, and
+will be removed by the drains, so rapidly, even in heavy
+clays, as to leave the ground fit for cultivation, and in a
+condition for steady growth, within a short time after the
+rain ceases. It has been estimated that a drained soil has
+room between its particles for about one quarter of its bulk
+of water;—that is, four inches of drained soil contains free
+space enough to receive a rain-fall one inch in depth, and, by
+the same token, four feet of drained soil can receive twelve
+inches of rain,—-more than is known to have ever fallen in
+twenty-four hours, since the deluge, and more than one
+quarter of the <span class="tei tei-hi"><span style="font-style: italic">annual</span></span> rain-fall in the United States.</p>
+
+<span class="tei tei-pb" id="page024">[pg 024]</span><a name="Pg024" id="Pg024" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As was stated in the previous chapter, the water which
+reaches the soil may be considered under two heads:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1st—That which reaches its surface, whether directly by
+rain, or by the surface flow of adjoining land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2d—That which reaches it below the surface, by springs
+and by soakage from the lower portions of adjoining land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The first of these is beneficial, because it contains fresh
+air, carbonic acid, ammonia, nitric acid, and heat, obtained
+from the atmosphere; and the flowage water contains, in
+addition, some of the finer or more soluble parts of the
+land over which it has passed. The second, is only so much
+dead water, which has already given up, to other soil, all
+that ours could absorb from it, and its effect is chilling and
+hurtful. This being the case, the only interest we can have
+in it, is to keep it down from the surface, and remove it as
+rapidly as possible.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The water of the first sort, on the other hand, should be
+arrested by every device within our reach. If the land is
+steep, the furrows in plowing should be run horizontally
+along the hill, to prevent the escape of the water over the
+surface, and to allow it to descend readily into the ground.
+Steep grass lands may have frequent, small, horizontal
+ditches for the same purpose. If the soil is at all heavy, it
+should not, when wet, be trampled by animals, lest it be
+puddled, and thus made less absorptive. If in cultivation,
+the surface should be kept loose and open, ready to receive
+all of the rain and irrigation water that reaches it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In descending through the soil, this water, in summer,
+gives up heat which it received from the air and from the
+heated surface of the ground, and thus raises the temperature
+of the lower soil. The fertilizing matters which it has
+obtained from the air,—carbonic acid, ammonia and nitric
+acid,—are extracted from it, and held for the use of growing
+plants. Its fresh air, and the air which follows the descent
+of the water-table, carries oxygen to the organic and<span class="tei tei-pb" id="page025">[pg 025]</span><a name="Pg025" id="Pg025" class="tei tei-anchor"></a>
+mineral parts of the soil, and hastens the rust and decay
+by which these are prepared for the uses of vegetation.
+The water itself supplies, by means of their power of absorption,
+the moisture which is needed by the particles of
+the soil; and, having performed its work, it goes down to
+the level of the water below, and, swelling the tide above
+the brink of the dam, sets the drains running, until it is
+all removed. In its descent through the ground, this water
+clears the passages through which it flows, leaving a
+better channel for the water of future rains, so that, in
+time, the heaviest clays, which will drain but imperfectly
+during the first one or two years, will pass water, to a
+depth of four or five feet, almost as readily as the lighter
+loams.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Now, imagine the drains to be closed up, leaving no outlet
+for the water, save at the surface. This amounts to a
+raising of the dam to that height, and additions to the water
+will bring the water-table even with the top of the soil.
+No provision being made for the removal of spring and
+soakage water, this causes serious inconvenience, and
+even the rain-fall, finding no room in the soil for its
+reception, can only lie upon, or flow over, the surface,—not
+yielding to the soil the fertilizing matters which it contains,
+but, on the contrary, washing away some of its finer
+and looser parts. The particles of the soil, instead of being
+furnished, by absorption, with a healthful amount of
+moisture, are made unduly wet; and the spaces between
+them, being filled with water, no air can enter, whereby the
+chemical processes by which the inert minerals, and the
+roots and manure, in the soil are prepared for the use of
+vegetation, are greatly retarded.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Instead of carrying the heat of the air, and of the surface
+of the ground, to the subsoil, the rain only adds so
+much to the amount of water to be evaporated, and increases,
+by so much, the chilling effect of evaporation.</p>
+
+<span class="tei tei-pb" id="page026">[pg 026]</span><a name="Pg026" id="Pg026" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Instead of opening the spaces of the soil for the more
+free passage of water and air, as is done by descending
+water, that which ascends by evaporation at the surface
+brings up soluble matters, which it leaves at the point
+where it becomes a vapor, forming a crust that prevents
+the free entrance of air at those times when the soil is dry
+enough to afford it space for circulation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Instead of crumbling to the fine condition of a loam, as
+it does, when well drained, by the descent of water
+through it, heavy clay soil, being rapidly dried by evaporation,
+shrinks into hard masses, separated by wide cracks.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In short, in wet seasons, on such land, the crops will be
+greatly lessened, or entirely destroyed, and in dry seasons,
+cultivation will always be much more laborious, more hurried,
+and less complete, than if it were well drained.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The foregoing general statements, concerning the action
+of water in drained, and in undrained land, and of the effects
+of its removal, by gravitation, and by evaporation, are based
+on facts which have been developed by long practice, and
+on a rational application of well know principles of science.
+These facts and principles are worthy of examination, and
+they are set forth below, somewhat at length, especially
+with reference to <span class="tei tei-hi"><span style="font-style: italic">Absorption</span></span> and <span class="tei tei-hi"><span style="font-style: italic">Filtration</span></span>; <span class="tei tei-hi"><span style="font-style: italic">Evaporation</span></span>;
+<span class="tei tei-hi"><span style="font-style: italic">Temperature</span></span>; <span class="tei tei-hi"><span style="font-style: italic">Drought</span></span>; <span class="tei tei-hi"><span style="font-style: italic">Porosity</span></span> or <span class="tei tei-hi"><span style="font-style: italic">Mellowness;</span></span>
+and <span class="tei tei-hi"><span style="font-style: italic">Chemical Action</span></span>.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-variant: small-caps">Absorption and Filtration.</span></span>—The process of under-draining
+is a process of absorption and filtration, as distinguished
+from surface-flow and evaporation. The completeness
+with which the latter are prevented, and the
+former promoted, is the measure of the completeness of the
+improvement. If water lie on the surface of the ground
+until evaporated, or if it flow off over the surface, it will
+do harm; if it soak away through the soil, it will do good.
+The rapidity and ease with which it is absorbed, and, therefore,
+the extent to which under-draining is successful, depend<span class="tei tei-pb" id="page027">[pg 027]</span><a name="Pg027" id="Pg027" class="tei tei-anchor"></a>
+on the physical condition of the soil, and on the
+manner in which its texture is affected by the drying action
+of sun and wind, and by the downward passage of water
+through it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In drying, all soils, except pure sands, shrink, and occupy
+less space than when they are saturated with water. They
+shrink more or less, according to their composition, as will
+be seen by the following table of results obtained in the
+experiments of Schuebler:</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="4"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell">1,000 Parts of</td><td class="tei tei-cell">Will Contract Parts.</td><td class="tei tei-cell">1,000 Parts of</td><td class="tei tei-cell">Will Contract Parts.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Strong Limey Soil</td><td class="tei tei-cell">50.</td><td class="tei tei-cell">Pure Clay</td><td class="tei tei-cell">183.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Heavy Loam</td><td class="tei tei-cell">60.</td><td class="tei tei-cell">Peat</td><td class="tei tei-cell">200.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Brick Maker's Clay</td><td class="tei tei-cell">85.</td><td class="tei tei-cell"></td><td class="tei tei-cell"></td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Professor Johnson estimates that peat and heavy clay
+shrink one-fifth of their bulk.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If soil be dried suddenly, from a condition of extreme
+wetness, it will be divided into large masses, or clods, separated
+by wide cracks. A subsequent wetting of the clods,
+which is not sufficient to expand it to its former condition,
+will not entirely obliterate the cracks, and the next drying
+will be followed by new fissures within the clods themselves;
+and a frequent repetition of this process will make
+the network of fissures finer and finer, until the whole mass
+of the soil is divided to a pulverulent condition. This is the
+process which follows the complete draining of such lands
+as contain large proportions of clay or of peat. It is retarded,
+in proportion to the amount of the free water in the
+soil which is evaporated from the surface, and in proportion
+to the trampling of the ground, when very wet. It is
+greatly facilitated by frost, and especially by deep frost.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The fissures which are formed by this process are, in time,
+occupied by the roots of plants, which remain and decay,
+when the crop has been removed, and which prevent the
+soil from ever again closing on itself so completely as before
+their penetration; and each season's crop adds new roots<span class="tei tei-pb" id="page028">[pg 028]</span><a name="Pg028" id="Pg028" class="tei tei-anchor"></a>
+to make the separation more complete and more universal;
+but it is only after the water of saturation, which occupies
+the lower soil for so large a part of the year, has been removed
+by draining, that roots can penetrate to any considerable
+depth, and, in fact, the cracking of undrained
+soils, in drying, never extends beyond the separation into
+large masses, because each heavy rain, by saturating the
+soil and expanding it to its full capacity, entirely obliterates
+the cracks and forms a solid mass, in which the operation
+has to be commenced anew with the next drying.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Mr. Gisborne, in his capital essay on "Agricultural
+Drainage," which appeared in the <span class="tei tei-hi"><span style="font-style: italic">Quarterly Review</span></span>, No.
+CLXXI, says: "We really thought that no one was so ignorant
+as not to be aware that clay lands always shrink
+and crack with drought, and the stiffer the clay the
+greater the shrinking, as brickmakers well know. In the
+great drought, 36 years ago, we saw in a very retentive
+soil in the Vale of Belvoir, cracks which it was not
+very pleasant to ride among. This very summer, on land
+which, with reference to this very subject, the owner
+stated to be impervious, we put a walking stick three
+feet into a sun-crack, without finding a bottom, and the
+whole surface was what Mr. Parkes, not inappropriately,
+calls a network of cracks. When heavy rain comes
+upon a soil in this state, of course the cracks fill, the clay
+imbibes the water, expands, and the cracks are abolished.
+But if there are four or five feet parallel drains in the
+land, the water passes at once into them and is carried
+off. In fact, when heavy rain falls upon clay lands in this
+cracked state, it passes off too quickly, without adequate
+filtration. Into the fissures of the undrained soil the roots
+only penetrate to be perished by the cold and wet of the
+succeeding winter; but in the drained soil the roots follow
+the threads of vegetable mold which have been
+washed into the cracks, and get an abiding tenure. Earth<span class="tei tei-pb" id="page029">[pg 029]</span><a name="Pg029" id="Pg029" class="tei tei-anchor"></a>
+worms follow either the roots or the mold. Permanent
+schisms are established in the clay, and its whole character
+is changed. An old farmer in a midland county began
+with 20-inch drains across the hill, and, without ever
+reading a word, or, we believe, conversing with any one
+on the subject, poked his way, step by step, to four or
+five feet drains, in the line of steepest descent. Showing
+us his drains this spring, he said: 'They do better year
+by year; the water gets a habit of coming to them '—a very
+correct statement of fact, though not a very philosophical
+explanation."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Alderman Mechi, of Tiptree Hall, says: "Filtration
+may be too sudden, as is well enough shown by our hot
+sands and gravels; but I apprehend no one will ever
+fear rendering strong clays too porous and manageable.
+The object of draining is to impart to such soils the
+mellowness and dark color of self drained, rich and friable
+soil. That perfect drainage and cultivation will do
+this, is a well known fact. I know it in the case of my
+own garden. How it does so I am not chemist enough
+to explain in detail; but it is evident the effect is produced
+by the fibers of the growing crop intersecting
+every particle of the soil, which they never could do before
+draining; these, with their excretions, decompose on
+removal of the crop, and are acted on by the alternating
+air and water, which also decompose and change, in a
+degree, the inorganic substances of the soil. Thereby
+drained land, which was, before, impervious to air and
+water, and consequently unavailable to air and roots,
+to worms, or to vegetable or animal life, becomes, by
+drainage, populated by both, and is a great chemical
+laboratory, as our own atmosphere is subject to all the
+changes produced by animated nature."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Experience proves that the descent of water through the
+soil renders it more porous, so that it is easier for the<span class="tei tei-pb" id="page030">[pg 030]</span><a name="Pg030" id="Pg030" class="tei tei-anchor"></a>
+water falling afterward to pass down to the drains, but no
+very satisfactory reason for this has been presented, beyond
+that which is connected with the cracking of the soil. The
+fact is well stated in the following extract from a letter to
+the <span class="tei tei-hi"><span style="font-style: italic">Country Gentleman</span></span>:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"A simple experiment will convince any farmer that the
+best means of permanently deepening and mellowing the
+soil is by thorough drainage, to afford a ready exit for all
+surplus moisture. Let him take in spring, while wet, a
+quantity of his hardest soil,—such as it is almost impossible
+to plow in summer,—such as presents a baked and
+brick-like character under the influence of drought,—and
+place it in a box or barrel, open at the bottom, and frequently
+during the season let him saturate it with water.
+He will find it gradually becoming more and more porous
+and friable,—holding water less and less perfectly as the
+experiment proceeds, and in the end it will attain a state
+best suited to the growth of plants from its deep and
+mellow character."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is equally a fact that the ascent of water in the soil,
+together with its evaporation at the surface, has the effect
+of making the soil impervious to rains, and of covering the
+land with a crust of hard, dry earth, which forms a barrier
+to the free entrance of air. So far as the formation of crust
+is concerned, it is doubtless due to the fact that the water
+in the soil holds in solution certain mineral matters, which
+it deposits at the point of evaporation, the collection of
+these finely divided matters serving to completely fill the
+spaces between the particles of soil at the surface,—pasting
+them together, as it were. How far below the surface this
+direct action extends, cannot be definitely determined; but
+the process being carried on for successive years, accumulating
+a quantity of these fine particles, each season, they
+are, by cultivation, and by the action of heavy showers
+falling at a time when the soil is more or less dry, distributed
+through a certain depth, and ordinarily, in all<span class="tei tei-pb" id="page031">[pg 031]</span><a name="Pg031" id="Pg031" class="tei tei-anchor"></a>
+probability, are most largely deposited at the top of the
+subsoil. It is found in practice that the first foot in depth
+of retentive soils is more retentive than that which lies
+below. If this opinion as to the cause of this greater imperviousness
+is correct, it will be readily seen how water,
+descending to the drains, by carrying these soluble and
+finer parts downward and distributing them more equally
+through the whole, should render the soil more porous.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Another cause of the retention of water by the surface
+soil, often a very serious one, is the puddling which
+clayey lands undergo by working them, or feeding cattle
+upon them, when they are wet. This is always injurious.
+By draining, land is made fit for working much earlier in
+the spring, and is sooner ready for pasturing after a rain,
+but, no matter how thoroughly the draining has been done,
+if there is much clay in the soil, the effect of the improvement
+will be destroyed by plowing or trampling, while
+very wet; this impervious condition will be removed in
+time, of course, but while it lasts, it places us as completely
+at the mercy of the weather as we were before a
+ditch was dug.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In connection with the use of the word <span class="tei tei-hi"><span style="font-style: italic">impervious</span></span>, it
+should be understood that it is not used in its strict sense,
+for no substance which can be wetted by water is really
+impervious and the most retentive soil will become wet.
+Gisborne states the case clearly when he says: "Is your
+subsoil moister after the rains of mid-winter, than it is
+after the drought of mid-summer? If it is, it will drain."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The proportion of the rain-fall which will filtrate
+through the soil to the level of the drains, varies with the
+composition of the soil, and with the effect that the
+draining has had upon them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In a very loose, gravelly, or sandy soil, which has a perfect
+outlet for water below, all but the heaviest falls of
+rain will sink at once, while on a heavy clay, no matter
+<span class="tei tei-pb" id="page032">[pg 032]</span><a name="Pg032" id="Pg032" class="tei tei-anchor"></a>
+how well it is drained, the process of filtration will be
+much more slow, and if the land be steeply inclined, some
+of the water of ordinarily heavy rains must flow off over
+the surface, unless, by horizontal plowing, or catch drains
+on the surface, its flow be retarded until it has time to
+enter the soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The power of drained soils to hold water, by absorption,
+is very great. A cubic foot of very dry soil, of favorable
+character, has been estimated to absorb within its particles,—holding
+no free water, or water of drainage,—about one-half
+its bulk of water; if this is true, the amount required
+to <span class="tei tei-hi"><span style="font-style: italic">moisten</span></span> a dry soil, four feet deep, giving no excess to be
+drained away, would amount to a rain fall of from 20 to 30
+inches in depth. If we consider, in addition to this, the
+amount of water drained away, we shall see that the soil
+has sufficient capacity for the reception of all the rain water
+that falls upon it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In connection with the question of absorption and filtration,
+it is interesting to investigate the movements of
+water in the ground. The natural tendency of water, in the
+soil as well as out of it, is to descend perpendicularly
+toward the center of the earth. If it meet a flat layer of
+gravel lying upon clay, and having a free outlet, it will
+follow the course of the gravel,—laterally,—and find the
+outlet; if it meet water which is dammed up in the soil,
+and which has an outlet at a certain elevation, as at the
+floor of a drain, it will raise the general level of the water,
+and force it out through the drain; if it meet water which
+has no outlet, it will raise its level until the soil is filled, or
+until it accumulates sufficient pressure, (head,) to force its
+way through the adjoining lands, or until it finds an outlet
+at the surface.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The first two cases named represent the condition which
+it is desirable to obtain, by either natural or artificial
+drainage; the third case is the only one which makes<span class="tei tei-pb" id="page033">[pg 033]</span><a name="Pg033" id="Pg033" class="tei tei-anchor"></a>
+drainage necessary. It is a fixed rule that water, descending
+in the soil, will find the <span class="tei tei-hi"><span style="font-style: italic">lowest</span></span> outlet to which there
+exists a channel through which it can flow, and that if, after
+heavy rains, it rise too near the surface of the ground, the
+proper remedy is to tap it at a lower level, and thus remove
+the water table to the proper distance from the surface.
+This subject will be more fully treated in a future
+chapter, in considering the question of the depth, and the
+intervals, at which drains should be placed.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Evaporation.</span></span>—By evaporation is meant the process by
+which a liquid assumes the form of a gas or vapor, or
+"dries up." Water, exposed to the air, is constantly undergoing
+this change. It is changed from the liquid form, and
+becomes a vapor in the air. Water in the form of vapor
+occupies nearly 2000 times the space that it filled as a
+liquid. As the vapor at the time of its formation is of the
+same temperature with the water, and, from its highly expanded
+condition, requires a great <span class="tei tei-hi"><span style="font-style: italic">amount</span></span> of heat to maintain
+it as vapor, it follows that a given quantity of water
+contains, in the vapory form, many times as much heat as
+in the liquid form. This heat is taken from surrounding
+substances,—from the ground and from the air,—which are
+thereby made much cooler. For instance, if a shower
+moisten the ground, on a hot summer day, the drying up
+of the water will cool both the ground and the air. If we
+place a wet cloth on the head, and hasten the evaporation
+of the water by fanning, we cool the head; if we wrap
+a wet napkin around a pitcher of water, and place it in a
+current of air, the water in the pitcher is made cooler,
+by giving up its heat to the evaporating water of the
+napkin; when we sprinkle water on the floor of a room,
+its evaporation cools the air of the room.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">So great is the effect of evaporation, on the temperature
+of the soil, that Dr. Madden found that the soil of a
+drained field, in which most of the water was removed<span class="tei tei-pb" id="page034">[pg 034]</span><a name="Pg034" id="Pg034" class="tei tei-anchor"></a>
+from below, was 6-1/2° Far. warmer than a similar soil undrained,
+from which the water had to be removed by
+evaporation. This difference of 6-1/2° is equal to a difference
+of elevation of 1,950 feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It has been found, by experiments made in England, that
+the average evaporation of water from wet soils is equal
+to a depth of <span class="tei tei-hi"><span style="font-style: italic">two inches per month</span></span>, from May to August,
+inclusive; in America it must be very much greater than
+this in the summer months, but this is surely enough for
+the purposes of illustration, as two inches of water, over an
+acre of land, would weigh about <span class="tei tei-hi"><span style="font-style: italic">two hundred tons</span></span>. The
+amount of heat required to evaporate this is immense, and
+a very large part of it is taken from the soil, which, thereby,
+becomes cooler, and less favorable for a rapid growth. It
+is usual to speak of heavy, wet lands as being "cold," and
+it is now seen why they are so.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If none of the water which falls on a field is removed by
+drainage, (natural or artificial,) and if none runs off from
+the surface, the whole rain-fall of a year must be removed
+by evaporation, and the cooling of the soil will be proportionately
+great. The more completely we withdraw this
+water from the surface, and carry it off in underground
+drains, the more do we reduce the amount to be removed
+by evaporation. In land which is well drained, the amount
+evaporated, even in summer, will not be sufficient to so
+lower the temperature of the soil as to retard the growth
+of plants; the small amount dried out of the particles of
+the soil, (water of absorption,) will only keep it from being
+raised to too great a heat by the mid-summer sun.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">An idea of the amount of heat lost to the soil, in the
+evaporation of water, may be formed from the fact that to
+evaporate, by artificial heat, the amount of water contained
+in a rain-fall of two inches on an acre, (200 tons,) would
+require over 20 tons of coal. Of course a considerable—probably
+by far the larger,—part of the heat taken up in<span class="tei tei-pb" id="page035">[pg 035]</span><a name="Pg035" id="Pg035" class="tei tei-anchor"></a>
+the process of evaporation is furnished by the air; but the
+amount abstracted from the soil is great, and is in direct
+proportion to the amount of water removed by this process;
+hence, the more we remove by draining, the more
+heat we retain in the ground.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The season of growth is lengthened by draining, because,
+by avoiding the cooling effects of evaporation, germination
+is more rapid, and the young plant grows steadily
+from the start, instead of struggling against the retarding
+influence of a cold soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Temperature.</span></span>—The temperature of the soil has great
+effect on the germination of seeds, the growth of plants,
+and the ripening of the crops.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Gisborne says: "The evaporation of 1 lb. of water
+lowers the temperature of 100 lbs. of soil 10°,—that is
+to say, that, if to 100 lbs. of soil, holding all the water
+it can by attraction, but containing no water of drainage,
+is added 1 lb. of water which it has no means of
+discharging, except by evaporation, it will, by the time
+that it has so discharged it, be 60° colder than it would
+have been, if it had the power of discharging this 1 lb.
+by filtration; or, more practically, that, if rain, entering
+in the proportion of 1 lb. to 100 lbs. into a retentive
+soil, which is saturated with water of attraction, is discharged
+by evaporation, it lowers the temperature of
+that soil 10°. If the soil has the means of discharging
+that 1 lb. of water by filtration, no effect is produced beyond
+what is due to the relative temperatures of the
+rain and of the soil."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It has been established by experiment that four times
+as much heat is required to evaporate a certain quantity
+of water, as to raise the same quantity from the freezing
+to the boiling point.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is, probably, in consequence of this cooling effect
+of evaporation, that wet lands are warmest when shaded,<span class="tei tei-pb" id="page036">[pg 036]</span><a name="Pg036" id="Pg036" class="tei tei-anchor"></a>
+because, under this condition, evaporation is less active.
+Such lands, in cloudy weather, form an unnatural growth,
+such as results in the "lodging" of grain crops, from the
+deficient strength of the straw which this growth produces.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In hot weather, the temperature of the lower soil is, of
+course, much lower than that of the air, and lower than
+that of the water of warm rains. If the soil is saturated
+with water, the water will, of course, be of an even temperature
+with the soil in which it lies, but if this be drained
+off, warm air will enter from above, and give its heat to
+the soil, while each rain, as it falls, will also carry its heat
+with it. Furthermore, the surface of the ground is sometimes
+excessively heated by the summer sun, and the heat
+thus contained is carried down to the lower soil by the
+descending water of rains, which thus cool the surface and
+warm the subsoil, both beneficial.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Mr. Josiah Parkes, one of the leading draining engineers
+of England, has made some experiments to test the
+extent to which draining affects the temperature of the
+soil. The results of his observations are thus stated by
+Gisborne: "Mr. Parkes gives the temperature on a
+Lancashire flat moss, but they only commence 7 inches
+below the surface, and do not extend to mid-summer.
+At that period of the year the temperature, at 7 inches,
+never exceeded 66°, and was generally from 10° to 15°
+below the temperature of the air in the shade, at 4 feet
+above the earth. Mr. Parkes' experiments were made
+simultaneously, on a drained, and on an undrained portion
+of the moss; and the result was, that, on a mean
+of 35 observations, the drained soil at 7 inches in depth
+was 10° warmer than the undrained, at the same depth.
+The undrained soil never exceeded 47°, whereas, after a
+thunder storm, the drained reached 66° at 7 inches, and
+48° at 31 inches. Such were the effects, at an early
+period of the year, on a black bog. They suggest some<span class="tei tei-pb" id="page037">[pg 037]</span><a name="Pg037" id="Pg037" class="tei tei-anchor"></a>
+idea of what they were, when, in July or August, thunder
+rain at 60° or 70° falls on a surface heated to 130°, and
+carries down with it, into the greedy fissures of the earth,
+its augmented temperature. These advantages, porous
+soils possess by nature, and retentive ones only acquire
+them by drainage."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Drained land, being more open to atmospheric circulation,
+and having lost the water which prevented the temperature
+of its lower portions from being so readily
+affected by the temperature of the air as it is when dry,
+will freeze to a greater depth in winter and thaw out earlier
+in the spring. The deep freezing has the effect to
+greatly pulverize the lower soil, thus better fitting it for
+the support of vegetation; and the earlier thawing makes
+it earlier ready for spring work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Drought.</span></span>—At first thought, it is not unnatural to suppose
+that draining will increase the ill effect of too dry
+seasons, by removing water which might keep the soil
+moist. Experience has proven, however, that the result
+is exactly the opposite of this. Lands which suffer most
+from drought are most benefited by draining,—more in
+their greater ability to withstand drought than in any
+other particular.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The reasons for this action of draining become obvious,
+when its effects on the character of the soil are examined.
+There is always the same amount of water in, and about,
+the surface of the earth. In winter there is more in the
+soil than in summer, while in summer, that which has
+been dried out of the soil exists in the atmosphere in the
+form of a <span class="tei tei-hi"><span style="font-style: italic">vapor</span></span>. It is held in the vapory form by <span class="tei tei-hi"><span style="font-style: italic">heat</span></span>,
+which may be regarded as <span class="tei tei-hi"><span style="font-style: italic">braces</span></span> to keep it distended.
+When vapor comes in contact with substances sufficiently
+colder than itself, it gives up its heat,—thus losing its
+braces,—contracts, becomes liquid water, and is deposited
+as dew.</p>
+
+<span class="tei tei-pb" id="page038">[pg 038]</span><a name="Pg038" id="Pg038" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Many instances of this operation are familiar to all.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For instance, a cold pitcher in the summer robs the
+vapor in the air of its heat, and causes it to be deposited
+on its own surface,—of course the water comes from the
+atmosphere, not through the wall of the pitcher; if we
+breathe on a knife blade, it condenses, in the same manner,
+the moisture of the breath, and becomes covered with a
+film of-water; stone-houses are damp in summer, because
+the inner surface of their walls, being cooler than the
+atmosphere, causes its moisture to be deposited in the
+manner described;<a id="noteref_2" name="noteref_2" href="#note_2"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">2</span></span></a> nearly every night, in summer, the
+cold earth receives moisture from the atmosphere in the
+form of dew; a single large head of cabbage, which at
+night is very cold, often condenses water to the amount of
+a gill or more.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The same operation takes place in the soil. When the
+air is allowed to circulate among its lower and cooler,
+(because more shaded,) particles, they receive moisture by
+the same process of condensation. Therefore, when, by
+the aid of under-drains, the lower soil becomes sufficiently
+loose and open, to allow a circulation of air, the deposit of
+atmospheric moisture will keep it supplied with water, at
+a point easily accessible to the roots of plants.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If we wish to satisfy ourselves that this is practically
+correct, we have only to prepare two boxes of finely pulverized
+soil,—one three or four inches deep,—and the other
+fifteen or twenty inches deep, and place them in the sun, at
+midday, in summer. The thinner soil will soon be completely
+dried, while the deeper one, though it may have
+been previously dried in an oven, will soon accumulate a<span class="tei tei-pb" id="page039">[pg 039]</span><a name="Pg039" id="Pg039" class="tei tei-anchor"></a>
+large amount of water on those particles which, being
+lower and better sheltered from the sun's heat than the
+particles of the thin soil, are made cooler.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">We have seen that even the most retentive soil,—the
+stiffest clay,—is made porous by the repeated passage of
+water from the surface to the level of the drains, and that
+the ability to admit air, which plowing gives it, is maintained
+for a much longer time than if it were usually saturated
+with water which has no other means of escape
+than by evaporation at the surface. The power of dry
+soils to absorb moisture from the air may be seen by an
+examination of the following table of results obtained by
+Schuebler, who exposed 1,000 grains of dried soil of the
+various kinds named to the action of the air:</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="2"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell">Kind of Soil.</td><td class="tei tei-cell">Amount of Water Absorbed in 24 Hours.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Common Soil</td><td class="tei tei-cell">22 grains.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Loamy Clay</td><td class="tei tei-cell">26 grains.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Garden Soil</td><td class="tei tei-cell">45 grains.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Brickmakers' Clay</td><td class="tei tei-cell">30 grains.</td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The effect of draining in overcoming drought, by admitting
+atmospheric vapor will, of course, be very much increased
+if the land be thoroughly loosened by cultivation,
+and especially if the surface be kept in an open and mellow
+condition.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In addition to the moisture received from the air, as
+above described, water is, in a porous soil, drawn up from
+the wetter subsoil below, by the same attractive force
+which acts to wet the whole of a sponge of which only the
+lower part touches the water;—as a hard, dry, compact
+sponge will absorb water much less readily than one
+which is loose and open, so the hard clods, into which undrained
+clay is dried, drink up water much less freely than
+they will do after draining shall have made them more
+friable.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The source of this underground moisture is the "water
+table,"—the level of the soil below the influence of the<span class="tei tei-pb" id="page040">[pg 040]</span><a name="Pg040" id="Pg040" class="tei tei-anchor"></a>
+drains,—and this should be so placed that, while its water
+will easily rise to a point occupied by the feeding roots of
+the crop, it should yield as little as possible for evaporation
+at the surface.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Another source of moisture, in summer, is the deposit of
+dew on the surface of the ground. The amount of this is
+very difficult to determine, and accurate American experiments
+on the subject are wanting. Of course the amount
+of dew is greater here than in England, where Dr. Dalton,
+a skillful examiner of atmospheric phenomena, estimates
+the annual deposit of dew to equal a depth of five inches,
+or about one-fifth of the rain-fall. Water thus deposited
+on the soil is absorbed more or less completely, in proportion
+to the porosity of the ground.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The extent to which plants will be affected by drought
+depends, other things being equal, on the depth to which
+they send their roots. If these lie near the surface, they
+will be parched by the heat of the sun. If they strike
+deeply into the damper subsoil, the sun will have less effect
+on the source from which they obtain their moisture.
+Nothing tends so much to deep rooting, as the thorough
+draining of the soil. If the <span class="tei tei-hi"><span style="font-style: italic">free</span></span> water be withdrawn to
+a considerable distance from the surface, plants,—even
+without the valuable aid of deep and subsoil plowing,—will
+send their roots to great depths. Writers on this
+subject cite many instances in which the roots of ordinary
+crops "not mere hairs, but strong fibres, as large as pack-thread,"
+sink to the depth of 4, 6, and in some instances
+12 or 14 feet. Certain it is that, in a healthy, well aerated
+soil, any of the plants ordinarily cultivated in the garden
+or field will send their roots far below the parched surface
+soil; but if the subsoil is wet, cold, and soggy, at the
+time when the young crop is laying out its plan of future
+action, it will perforce accommodate its roots to the
+limited space which the comparatively dry surface soil
+affords.</p>
+
+<span class="tei tei-pb" id="page041">[pg 041]</span><a name="Pg041" id="Pg041" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is well known among those who attend the meetings
+of the Farmers' Club of the American Institute, in New
+York, that the farm of Professor Mapes, near Newark, N.J.,
+which maintains its wonderful fertility, year after year,
+without reference to wet or dry weather, has been rendered
+almost absolutely indifferent to the severest drought,
+by a course of cultivation which has been rendered possible
+only by under-draining. The lawns of the Central
+Park, which are a marvel of freshness, when the lands about
+the Park are burned brown, owe their vigor mainly to the
+complete drainage of the soil. What is true of these thoroughly
+cultivated lands, it is practicable to attain on all
+soils, which, from their compact condition, are now almost
+denuded of vegetation in dry seasons.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Porosity or Mellowness.</span></span>—An open and mellow condition
+of the soil is always favorable for the growth of
+plants. They require heat, fresh air and moisture, to enable
+them to take up the materials on which they live, and
+by which they grow. We have seen that the heat of retentive
+soils is almost directly proportionate to the completeness
+with which their free water is removed by underground
+draining, and that, by reason of the increased
+facility with which air and water circulate within them,
+their heat is more evenly distributed among all those parts
+of the soil which are occupied by roots. The word <span class="tei tei-hi"><span style="font-style: italic">moisture</span></span>,
+in this connection, is used in contradistinction to <span class="tei tei-hi"><span style="font-style: italic">wetness</span></span>,
+and implies a condition of freshness and dampness,—not
+at all of saturation. In a saturated, a soaking-wet soil,
+every space between the particles is filled with water to
+the entire exclusion of the atmosphere, and in such a soil
+only aquatic plants will grow. In a <span class="tei tei-hi"><span style="font-style: italic">dry</span></span> soil, on the other
+hand, when the earth is contracted into clods and baked,
+almost as in an oven,—one of the most important conditions
+for growth being wanting,—nothing can thrive, save
+those plants which ask of the earth only an anchoring
+place, and seek their nourishment from the air. Both air<span class="tei tei-pb" id="page042">[pg 042]</span><a name="Pg042" id="Pg042" class="tei tei-anchor"></a>
+plants and water plants have their wisely assigned places
+in the economy of nature, and nature provides them with
+ample space for growth. Agriculture, however, is directed
+to the production of a class of plants very different from
+either of these,—to those which can only grow to their
+greatest perfection in a soil combining, not one or two
+only, but all three of the conditions named above. While
+they require heat, they cannot dispense with the moisture
+which too great heat removes; while they require moisture,
+they cannot abide the entire exclusion of air, nor the
+dissipation of heat which too much water causes. The
+interior part of the pellets of a well pulverized soil should
+contain all the water that they can hold by their own absorptive
+power, just as the finer walls of a damp sponge
+hold it; while the spaces between these pellets, like the
+pores of the sponge, should be filled with air.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In such a soil, roots can extend in any direction, and to
+considerable depth, without being parched with thirst, or
+drowned in stagnant water, and, other things being equal,
+plants will grow to their greatest possible size, and all
+their tissues will be of the best possible texture. On
+rich land, which is maintained in this condition of porosity
+and mellowness, agriculture will produce its best results,
+and will encounter the fewest possible chances of failure.
+Of course, there are not many such soils to be found, and
+such absolute balance between warmth and moisture in the
+soil cannot be maintained at all times, and under all circumstances,
+but the more nearly it is maintained, the more
+nearly perfect will be the results of cultivation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Chemical Action in the Soil.</span></span>—Plants receive certain of
+their constituents from the soil, through their roots. The
+raw materials from which these constituents are obtained
+are the minerals of the soil, the manures which are artificially
+applied, water, and certain substances which are
+taken from the air by the absorptive action of the soil,<span class="tei tei-pb" id="page043">[pg 043]</span><a name="Pg043" id="Pg043" class="tei tei-anchor"></a>
+or are brought to it by rains, or by water flowing over the
+surface from other land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The mineral matters, which constitute the ashes of
+plants, when burned, are not mere accidental impurities
+which happen to be carried into their roots in solution in
+the water which supplies the sap, although they vary in
+character and proportion with each change in the mineral
+composition of the soil. It is proven by chemical
+analysis, that the composition of the ashes, not only of
+different species of plants, but of different parts of the
+same plant, have distinctive characters,—some being rich
+in phosphates, and others in silex; some in potash, and others
+in lime,—and that these characters are in a measure
+the same, in the same plants or parts of plants, without
+especial reference to the soil on which they grow. The
+minerals which form the ashes of plants, constitute but a
+very small part of the soil, and they are very sparsely distributed
+throughout the mass; existing in the interior of
+its particles, as well as upon their surfaces. As roots cannot
+penetrate to the interior of pebbles and compact particles
+of earth, in search of the food which they require,
+but can only take that which is exposed on their surfaces,
+and, as the oxydizing effect of atmospheric air is useful in
+preparing the crude minerals for assimilation, as well as in
+decomposing the particles in which they are bound up,—a
+process which is allied to the <span class="tei tei-hi"><span style="font-style: italic">rusting</span></span> of metals,—the more
+freely atmospheric air is allowed, or induced, to circulate
+among the inner portions of the soil, the more readily are
+its fertilizing parts made available for the use of roots.
+By no other process, is air made to enter so deeply, nor to
+circulate so readily in the soil, as by under-draining, and
+the deep cultivation which under-draining facilitates.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of the manures which are applied to the land, those of
+a mineral character are affected by draining, in the same
+manner as the minerals which are native to the soil;<span class="tei tei-pb" id="page044">[pg 044]</span><a name="Pg044" id="Pg044" class="tei tei-anchor"></a>
+while organic, or animal and vegetable, manures, (especially
+when applied, as is usual, in an incompletely fermented
+condition,) absolutely require fresh supplies of
+atmospheric air, to continue the decomposition which
+alone can prepare them for their proper effect on vegetation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If kept saturated with water, so that the air is excluded,
+animal manures lie nearly inert, and vegetable matters
+decompose but incompletely,—yielding acids which are injurious
+to vegetation, and which would not be formed in
+the presence of a sufficient supply of air. An instance is
+cited by H. Wauer where sheep dung was preserved, for
+five years, by excessive moisture, which kept it from the
+air. If the soil be saturated with water in the spring, and,
+in summer, (by the compacting of its surface, which is
+caused by evaporation,) be closed against the entrance of
+air, manures will be but slowly decomposed, and will act
+but imperfectly on the crop,—if, on the other hand, a
+complete system of drainage be adopted, manures, (and
+the roots which have been left in the ground by the previous
+crop,) will be readily decomposed, and will exercise
+their full influence on the soil, and on the plants growing
+in it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Again, manures are more or less effective, in proportion
+as they are more or less thoroughly mixed with the soil.
+In an undrained, retentive soil, it is not often possible to
+attain that perfect <span class="tei tei-hi"><span style="font-style: italic">tilth</span></span>, which is best suited for a proper
+admixture, and which is easily given after thorough
+draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The soil must be regarded as the laboratory in which
+nature, during the season of growth, is carrying on those
+hidden, but indispensable chemical separations, combinations,
+and re-combinations, by which the earth is made to
+bear its fruits, and to sustain its myriad life. The chief
+demand of this laboratory is for free ventilation. The<span class="tei tei-pb" id="page045">[pg 045]</span><a name="Pg045" id="Pg045" class="tei tei-anchor"></a>
+raw material for the work is at hand,—as well in the wet
+soil as in the dry; but the door is sealed, the damper is
+closed, and only a stray whiff of air can, now and then,
+gain entrance,—only enough to commence an analysis, or a
+combination, which is choked off when half complete,
+leaving food for sorrel, but making none for grass. We
+must throw open door and window, draw away the water
+in which all is immersed, let in the air, with its all destroying,
+and, therefore, all re-creating oxygen, and leave
+the forces of nature's beneficent chemistry free play,
+deep down in the ground. Then may we hope for the
+full benefit of the fertilizing matters which our good soil
+contains, and for the full effect of the manures which we
+add.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">With our land thoroughly improved, as has been described,
+we may carry on the operations of farming with
+as much certainty of success, and with as great immunity
+from the ill effects of unfavorable weather, as can be expected
+in any business, whose results depend on such a
+variety of circumstances. We shall have substituted certainty
+for chance, as far as it is in our power to do so, and
+shall have made farming an art, rather than a venture.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page046">[pg 046]</span><a name="Pg046" id="Pg046" class="tei tei-anchor"></a>
+<a name="toc8" id="toc8"></a>
+<a name="pdf9" id="pdf9"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER III. - HOW TO GO TO WORK TO LAY OUT A SYSTEM OF DRAINS.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">How to lay out the drains; where to place the outlet;
+where to locate the main collecting lines; how to arrange
+the laterals which are to take the water from the soil and
+deliver it at the mains; how deep to go; at what intervals;
+what fall to give; and what sizes of tile to use,—these
+are all questions of great importance to one who is
+about to drain land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">On the proper adjustment of these points, depend the
+<span class="tei tei-hi"><span style="font-style: italic">economy</span></span> and <span class="tei tei-hi"><span style="font-style: italic">effectiveness</span></span> of the work. Time and attention
+given to them, before commencing actual operations, will
+prevent waste and avoid failure. Any person of ordinary
+intelligence may qualify himself to lay out under-drains
+and to superintend their construction,—but the knowledge
+which is required does not come by nature. Those
+who have not the time for the necessary study and practice
+to make a plan for draining their land, will find it
+economical to employ an engineer for the purpose. In
+this era of railroad building, there is hardly a county in
+America which has not a practical surveyor, who may
+easily qualify himself, by a study of the principles and
+directions herein set forth, to lay out an economical plan
+for draining any ordinary agricultural land, to stake the
+lines, and to determine the grade of the drains, and the
+sizes of tile with which they should be furnished.</p>
+
+<span class="tei tei-pb" id="page047">[pg 047]</span><a name="Pg047" id="Pg047" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">On this subject Mr. Gisborne says: "If we should give
+a stimulus to amateur draining, we shall do a great deal
+of harm. We wish we could publish a list of the moneys
+which have been squandered in the last 40 years in amateur
+draining, either ineffectually or with very imperfect efficiency.
+Our own name would be inscribed in the list for a
+very respectable sum. Every thoughtless squire supposes
+that, with the aid of his ignorant bailiff, he can effect a perfect
+drainage of his estate; but there is a worse man behind
+the squire and the bailiff,—the draining conjuror. * * * * * *
+These fellows never go direct about their
+work. If they attack a spring, they try to circumvent
+it by some circuitous route. They never can learn that
+nature shows you the weakest point, and that you should
+assist her,—that <span class="tei tei-hi"><span style="font-style: italic">hit him straight in the eye</span></span> is as good a
+maxim in draining as in pugilism. * * * * * *
+If you wish to drain, we recommend you to take advice.
+We have disposed of the quack, but there is a faculty,
+not numerous but extending, and whose extension appears
+to us to be indispensable to the satisfactory
+progress of improvements by draining,—a faculty of
+draining engineers. If we wanted a profession for a lad
+who showed any congenial talent, we would bring him
+up to be a draining engineer." He then proceeds to
+speak of his own experience in the matter, and shows that,
+after more than thirty years of intelligent practice, he
+employed Mr. Josiah Parkes to lay out and superintend
+his work, and thus effected a saving, (after paying all professional
+charges,) of fully twelve per cent. on the cost of
+the draining, which was, at the same time, better executed
+than any that he had previously done.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is probable that, in nearly all amateur draining, the
+unnecessary frequency of the lateral drains; the extravagant
+size of the pipes used; and the number of useless
+angles which result from an unskillful arrangement, would
+amount to an expense equal to ten times the cost of the<span class="tei tei-pb" id="page048">[pg 048]</span><a name="Pg048" id="Pg048" class="tei tei-anchor"></a>
+proper superintendence, to say nothing of the imperfect
+manner in which the work is executed. A common impression
+seems to prevail, that if a 2-inch pipe is good, a
+3-inch pipe must be better, and that, generally, if draining
+is worth doing at all, it is worth overdoing; while
+the great importance of having perfectly fitting connections
+is not readily perceived. The general result is, that
+most of the tile-draining in this country has been too expensive
+for economy, and too careless for lasting efficiency.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is proposed to give, in this chapter, as complete a
+description of the preliminary engineering of draining as
+can be concentrated within a few pages, and a hope is entertained,
+that it will, at least, convey an idea of the importance
+of giving a full measure of thought and ingenuity
+to the maturing of the <span class="tei tei-hi"><span style="font-style: italic">plan</span></span>, before the execution of
+the work is commenced. "Farming upon paper" has
+never been held in high repute, but draining upon paper
+is less a subject for objection. With a good map of the
+farm, showing the comparative levels of outlet, hill, dale,
+and plain, and the sizes and boundaries of the different
+in closures, a profitable winter may be passed,—with pencil
+and rubber,—in deciding on a plan which will do the
+required work with the least possible length of drain, and
+which will require the least possible extra deep cutting;
+and in so arranging the main drains as to require the
+smallest possible amount of the larger and more costly
+pipes; or, if only a part of the farm is to be drained during
+the coming season, in so arranging the work that it will
+dovetail nicely with future operations. A mistake in actual
+work is costly, and, (being buried under the ground,) is
+not easily detected, while errors in drawing upon paper
+are always obvious, and are remedied without cost.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For the purpose of illustrating the various processes
+connected with the laying out of a system of drainage,
+the mode of operating on a field of ten acres will be detailed,<span class="tei tei-pb" id="page049">[pg 049]</span><a name="Pg049" id="Pg049" class="tei tei-anchor"></a>
+in connection with a series of diagrams showing
+the progress of the work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">A Map of the Land</span></span> is first made, from a careful survey.
+This should be plotted to a scale of 50 or 100 feet
+to the inch,<a id="noteref_3" name="noteref_3" href="#note_3"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">3</span></span></a> and should exhibit the location of obstacles
+which may interfere with the regularity of the
+drains,—such as large trees, rocks, etc., and the existing
+swamps, water courses, springs, and open drains. (Fig. 4.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The next step is to locate the contour lines of the land,
+or the lines of equal elevation,—also called the <span class="tei tei-hi"><span style="font-style: italic">horizontal
+lines</span></span>,—which serve to show the shape of the surface. To do
+this, stake off the field into squares of 50 feet, by first running
+a base line through the center of the greatest length of the
+field, marking it with stakes at intervals of 50 feet, then stake
+other lines, also at intervals of 50 feet, perpendicular to the
+base line, and then note the position of the stakes on the
+maps; next, by the aid of an engineer's level and staff, ascertain
+the height, (above an imaginary plain below the lowest
+part of the field,) of the surface of the ground at each stake,
+and note this elevation at its proper point on the map. This
+gives a plot like Fig. 5. The best instrument with which to
+take these levels, is the ordinary telescope-level used by railroad
+engineers, shown in Fig. 6, which has a telescope with
+cross hairs intersecting each other in the center of the line
+of sight, and a "bubble" placed exactly parallel to this
+line. The instrument, fixed on a tripod, and so adjusted
+that it will turn to any point of the compass without disturbing
+the position of the bubble, will, (as will its "line of
+sight,") revolve in a perfectly horizontal plane. It is so
+placed as to command a view of a considerable stretch of
+the field, and its height above the imaginary plane is
+measured, an attendant places next to one of the stakes
+a levelling rod, (Fig. 7,) which is divided into feet and<span class="tei tei-pb" id="page052">[pg 052]</span><a name="Pg052" id="Pg052" class="tei tei-anchor"></a>
+fractions of a foot, and is furnished with a movable target,
+so painted that its center point may be plainly seen.
+The attendant raises and lowers the target, until it comes
+exactly in the line of sight; its height on the rod denotes
+the height of the instrument above the level of the
+ground at that stake, and, as the height of the instrument
+above the imaginary plane has been reached, by subtracting
+one elevation from the other, the operator determines
+the height of the ground at that stake above the imaginary
+plane,—which is called the "<span class="tei tei-hi"><span style="font-style: italic">datum line</span></span>."</p>
+
+<a name="fig10" id="fig10"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image04.png" width="640" height="812" alt="Illustration: Fig. 4 - MAP OF LAND, WITH SWAMPS, ROCKS, SPRINGS AND TREES. INTENDED TO REPRESENT A FIELD OF TEN ACRES BEFORE DRAINING." title="Fig. 4 - MAP OF LAND, WITH SWAMPS, ROCKS, SPRINGS AND TREES. INTENDED TO REPRESENT A FIELD OF TEN ACRES BEFORE DRAINING." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 4 - MAP OF LAND, WITH SWAMPS, ROCKS, SPRINGS AND TREES. INTENDED TO REPRESENT A FIELD OF TEN ACRES BEFORE DRAINING.</div></div>
+
+<a name="fig11" id="fig11"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image05.png" width="640" height="811" alt="Illustration: Fig. 5 - MAP WITH 50-FOOT SQUARES, AND CONTOUR LINES." title="Fig. 5 - MAP WITH 50-FOOT SQUARES, AND CONTOUR LINES." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 5 - MAP WITH 50-FOOT SQUARES, AND CONTOUR LINES.</div></div>
+
+<a name="fig12" id="fig12"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image06.png" width="640" height="521" alt="Illustration: Fig. 5 - MAP WITH 50-FOOT SQUARES, AND CONTOUR LINES." title="Fig. 6 - LEVELLING INSTRUMENT.44The instrument from which this cut was taken, (as also Fig. 7) was made by Messrs. Blunt &amp; Nichols, Water st., N. Y." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 6 - LEVELLING INSTRUMENT.<a id="noteref_4" name="noteref_4" href="#note_4"><span class="tei tei-noteref" style="text-align: center"><span style="font-size: 60%; vertical-align: super">4</span></span></a></div></div>
+
+<a name="fig13" id="fig13"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image07.png" width="70" height="600" alt="Illustration: Fig. 7 - LEVELLING ROD." title="Fig. 7 - LEVELLING ROD." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 7 - LEVELLING ROD.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The next operation is to trace, on the plan, lines following
+the same level, wherever the land is of the proper
+height for its surface to meet them. For the purpose of
+illustrating this operation, lines at intervals of elevation of<span class="tei tei-pb" id="page053">[pg 053]</span><a name="Pg053" id="Pg053" class="tei tei-anchor"></a>
+one foot are traced on the plan in Fig. 8. And these lines
+show, with sufficient accuracy for practical purposes, the
+elevation and rate of inclination of all parts
+of the field,—where it is level or nearly so,
+where its rise is rapid, and where slight. As
+the land rises one foot from the position of
+one line to the position of the line next above
+it, where the distance from one line to the
+next is great, the land is more nearly level,
+and when it is short the inclination is steeper.
+For instance, in the southwest corner of the
+plan, the land is nearly level to the 2-foot
+line; it rises slowly to the center of the field,
+and to the eastern side about one-fourth of
+the distance from the southern boundary,
+while an elevation coming down between
+these two valleys, and others skirting the
+west side of the former one and the southern
+side of the latter, are indicated by the greater
+nearness of the lines. The points at which
+the contour lines cross the section lines are
+found in the following manner: On the
+second line from the west side of the field we
+find the elevations of the 4th, 5th and 6th
+stakes from the southern boundary to be 1.9,
+3.3, and 5.1. The contour lines, representing
+points of elevation of 2, 3, 4, and 5 feet above
+the <span class="tei tei-hi"><span style="font-style: italic">datum line</span></span>, will cross the 50-foot lines at
+their intersections, only where these intersections
+are marked in even feet. When they are
+marked with fractions of a foot, the lines must
+be made to cross at points between two intersections,—nearer
+to one or the other, according
+to their elevations,—thus between 1.9
+and 3.3, the 2-foot and 3-foot contour lines
+must cross. The total difference of elevation, between the<span class="tei tei-pb" id="page055">[pg 055]</span><a name="Pg055" id="Pg055" class="tei tei-anchor"></a>
+two points is 3.3—1.9=1.4; 10/14 of the space must be given
+to the even foot between the lines, and the 2-foot line should
+be 1/14 of the space above the point 1.9;—the 3-foot line
+will then come 3/14 below the point 3.3. In the same manner,
+the line from 3.3 to 5.1 is divided into 18 parts, of
+which 10 go to the space between the 4. and 5. lines, 7 are
+between 3.3 and the 4-foot line, and 1 between the 5-foot
+line and 5.1.</p>
+
+<a name="fig14" id="fig14"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image08.png" width="640" height="809" alt="Illustration: Fig. 8 - MAP WITH CONTOUR LINES." title="Fig. 8 - MAP WITH CONTOUR LINES." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 8 - MAP WITH CONTOUR LINES.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">With these maps, made from observations taken in the
+field, we are prepared to lay down, on paper, our system
+of drainage, and to mature a plan which shall do the necessary
+work with the least expenditure of labor and material.
+The more thoroughly this plan is considered, the
+more economical and effective will be the work. Having
+already obtained the needed information, and having it all
+before us, we can determine exactly the location and size of
+each drain, and arrange, before hand, for a rapid and satisfactory
+execution of the work. The only thing that may
+interfere with the perfect application of the plan, is the
+presence of masses of underground rock, within the depth
+to which the drains are to be laid.<a id="noteref_5" name="noteref_5" href="#note_5"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">5</span></span></a> Where these are supposed
+to exist, soundings should be made, by driving a
+3/4-inch pointed iron rod to the rock, or to a depth of <span class="tei tei-hi"><span style="font-style: italic">five</span></span>
+feet where the rock falls away. By this means, measuring
+the distance from the soundings to the ranges of the
+stakes, we can denote on the map the shape and depth of
+sunken rocks. The shaded spot on the east side of the
+map, (Fig. 8,) indicates a rock three feet from the surface,
+which will be assumed to have been explored by sounding.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In most cases, it will be sufficient to have contour lines
+taken only at intervals of two feet, and, owing to the
+smallness of the scale on which these maps are engraved,
+and to avoid complication in the finished plan, where so<span class="tei tei-pb" id="page056">[pg 056]</span><a name="Pg056" id="Pg056" class="tei tei-anchor"></a>
+much else must be shown, each alternate line is omitted.
+Of course, where drains are at once staked out on the
+land, by a practiced engineer, no contour lines are taken,
+as by the aid of the level and rod for the flatter portions,
+and by the eye alone for the steeper slopes, he will be able
+at once to strike the proper locations and directions; but
+for one of less experience, who desires to thoroughly
+mature his plan before commencing, they are indispensable;
+and their introduction here will enable the novice to
+understand, more clearly than would otherwise be possible,
+the principles on which the plan should be made.</p>
+
+<a name="fig15" id="fig15"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image09.png" width="640" height="329" alt="Illustration: Fig. 9 - WELL'S CLINOMETER." title="Fig. 9 - WELL'S CLINOMETER." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 9 - WELL'S CLINOMETER.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For preliminary examinations, and for all purposes in
+which great accuracy is not required, the little instrument
+shown in Fig. 9,—"Wells' Clinometer,"—is exceedingly
+simple and convenient. Its essential parts are a flat side,
+or base, on which it stands, and a hollow disk just half
+filled with some heavy liquid. The glass face of the disk is
+surrounded by a graduated scale that marks the angle at
+which the surface of the liquid stands, with reference to
+the flat base. The line 0.——0. being parallel to the
+base, when the liquid stands on that line, the flat side is
+horizontal; the line 90.——90. being perpendicular to<span class="tei tei-pb" id="page057">[pg 057]</span><a name="Pg057" id="Pg057" class="tei tei-anchor"></a>
+the base, when the liquid stands on that line, the flat side
+is perpendicular or <span class="tei tei-hi"><span style="font-style: italic">plumb</span></span>. In like manner, the intervening
+angles are marked, and, by the aid of the following tables,
+the instrument indicates the rate of fall per hundred feet
+of horizontal measurement, and per hundred feet measured
+upon the sloping line.<a id="noteref_6" name="noteref_6" href="#note_6"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">6</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Table No. 1 shows the rise of the slope for 100 feet of
+the horizontal measurement. Example: If the horizontal
+distance is 100 feet, and the slope is at an angle of 15°,
+the rise will be 17-633/1000 feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Table No. 2 shows the rise of the slope for 100 feet of
+its own length. If the sloping line, (at an angle of 15°,)
+is 100 feet long, it rises 25.882 feet.</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="2"></colgroup><thead><tr><th colspan="2" class="tei tei-head tei-head-table" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em"><span style="font-weight: 700">TABLE No. 1.</span></th></tr></thead><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Deg.</span></span></td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Feet.</span></span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">5</td><td class="tei tei-cell">8.749</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">10</td><td class="tei tei-cell">17.663</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">15</td><td class="tei tei-cell">26.795</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">20</td><td class="tei tei-cell">36.397</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">25</td><td class="tei tei-cell">46.631</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">30</td><td class="tei tei-cell">57.735</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">35</td><td class="tei tei-cell">70.021</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">40</td><td class="tei tei-cell">83.910</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">45</td><td class="tei tei-cell">100.—</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">50</td><td class="tei tei-cell">119.175</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">55</td><td class="tei tei-cell">142.815</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">60</td><td class="tei tei-cell">173.205</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">65</td><td class="tei tei-cell">214.451</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">70</td><td class="tei tei-cell">274.748</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">75</td><td class="tei tei-cell">373.205</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">80</td><td class="tei tei-cell">567.128</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">85</td><td class="tei tei-cell">1143.01</td>
+</tr></tbody></table>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="2"></colgroup><thead><tr><th colspan="2" class="tei tei-head tei-head-table" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em"><span style="font-weight: 700">TABLE No. 2</span></th></tr></thead><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Deg.</span></span></td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Feet.</span></span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">5</td><td class="tei tei-cell">8.716</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">10</td><td class="tei tei-cell">17.365</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">15</td><td class="tei tei-cell">25.882</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">20</td><td class="tei tei-cell">34.202</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">25</td><td class="tei tei-cell">42.262</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">30</td><td class="tei tei-cell">50.—</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">35</td><td class="tei tei-cell">57.358</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">40</td><td class="tei tei-cell">64.279</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">45</td><td class="tei tei-cell">70.711</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">50</td><td class="tei tei-cell">76.604</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">55</td><td class="tei tei-cell">81.915</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">60</td><td class="tei tei-cell">86.602</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">65</td><td class="tei tei-cell">90.631</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">70</td><td class="tei tei-cell">93.969</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">75</td><td class="tei tei-cell">96.593</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">80</td><td class="tei tei-cell">98.481</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">85</td><td class="tei tei-cell">99.619</td>
+</tr></tbody></table>
+
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">With the maps before him, showing the surface features
+of the field, and the position of the under-ground rock,
+the drainer will have to consider the following points:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1. Where, and at what depth, shall the outlet be
+placed?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2. What shall be the location, the length and the depth
+of the main drain?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">3. What subsidiary mains,—or collecting drains,—shall
+connect the minor valleys with the main?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">4. What may best be done to collect the water of large
+springs and carry it away?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">5. What provision is necessary to collect the water
+that flows over the surface of out-cropping rock, or<span class="tei tei-pb" id="page058">[pg 058]</span><a name="Pg058" id="Pg058" class="tei tei-anchor"></a>
+along springy lines on side hills or under banks?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">6. What should be the depth, the distance apart, the
+direction, and the rate of <span class="tei tei-hi"><span style="font-style: italic">fall</span></span>, of the lateral drains?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">7. What kind and sizes of tile should be used to form
+the conduits?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">8. What provision should be made to prevent the obstruction
+of the drains, by an accumulation of silt or sand,
+which may enter the tiles immediately after they are laid,
+and before the earth becomes compacted about them; and
+from the entrance of vermin?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1. The outlet should be at the lowest point of the boundary,
+unless, (for some especial reason which does not
+exist in the case under consideration, nor in any usual
+case,) it is necessary to seek some other than the natural
+outfall; and it should be deep enough to take the water of
+the main drain, and laid on a sufficient inclination for a free
+flow of the water. It should, where sufficient fall can be
+obtained without too great cost, deliver this water over a
+step of at least a few inches in height, so that the action of
+the drain may be seen, and so that it may not be liable to
+be clogged by the accumulation of silt, (or mud,) in the
+open ditch into which it flows.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2. The main drain should, usually, be run as nearly in
+the lowest part of the principal valley as is consistent with
+tolerable straightness. It is better to cut across the point
+of a hill, to the extent of increasing the depth for a few
+rods, than to go a long distance out of the direct course
+to keep in the valley, both because of the cost of
+the large tile used in the main, and of the loss of fall
+occasioned by the lengthening of the line. The main should
+be continued from the outlet to the point at which it is
+most convenient to collect the more remote sub-mains,
+which bring together the water of several sets of laterals.
+As is the case in the tract under consideration, the depth
+of the main is often restricted, in nearly level land, toward
+the upper end of the flat which lies next to the outlet,<span class="tei tei-pb" id="page059">[pg 059]</span><a name="Pg059" id="Pg059" class="tei tei-anchor"></a>
+by the necessity for a fall and the difficulty which often
+exists in securing a sufficiently low outlet. In such case,
+the only rule is to make it as deep as possible. When the
+fall is sufficient, it should be placed at such depth as will
+allow the laterals and sub-mains which discharge into it
+to enter at its top, and discharge above the level of the
+water which flows through it.</p>
+
+<a name="fig16" id="fig16"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image10.png" width="640" height="624" alt="Illustration: Fig. 10 - STONE PIT TO CONNECT SPRING WITH DRAIN." title="Fig. 10 - STONE PIT TO CONNECT SPRING WITH DRAIN." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 10 - STONE PIT TO CONNECT SPRING WITH DRAIN.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">3. Subsidiary mains, or <span class="tei tei-hi"><span style="font-style: italic">sub-mains</span></span>, connecting with the
+main drains, should be run up the minor valleys of the
+land, skirting the
+bases of the hills.
+Where the valley is
+a flat one, with rising
+ground at each side,
+there should be a
+sub-main, to receive
+the laterals from
+<span class="tei tei-hi"><span style="font-style: italic">each</span></span> hill side. As a
+general rule, it may
+be stated, that the
+collecting drain at
+the foot of a slope
+should be placed on
+the line which is first
+reached by the water
+flowing directly
+down over its surface, before it commences its lateral
+movement down the valley; and it should, if possible, be
+so arranged that it shall have a uniform descent for its
+whole distance. The proper arrangement of these collecting
+drains requires more skill and experience than
+any other branch of the work, for on their disposition
+depends, in a great measure, the economy and success of
+the undertaking.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">4. Where springs exist, there should be some provision
+made for collecting their water in pits filled with loose<span class="tei tei-pb" id="page060">[pg 060]</span><a name="Pg060" id="Pg060" class="tei tei-anchor"></a>
+stone, gravel, brush or other rubbish, or furnished with
+several lengths of tile set on end, one above the other, or
+with a barrel or other vessel; and a line of tile of proper
+size should be run directly
+to a main, or sub-main
+drain. The manner of
+doing this by means of a
+pit filled with stone is
+shown in Fig. 10. The
+collection of spring water
+in a vertical tile basin is
+shown in Fig. 11.</p>
+
+<a name="fig17" id="fig17"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image11.png" width="640" height="860" alt="Illustration: Fig. 11 - STONE AND TILE BASIN FOR SPRING WITH DRAIN." title="Fig. 11 - STONE AND TILE BASIN FOR SPRING WITH DRAIN." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 11 - STONE AND TILE BASIN FOR SPRING WITH DRAIN.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">5. Where a ledge of
+shelving rock, of considerable
+size, occurs on land
+to be drained, it is best to
+make some provision for
+collecting, at its base, the
+water flowing over its surface,
+and taking it at once
+into the drains, so that it
+may not make the land
+near it unduly wet. To
+effect this, a ditch should be dug along the base of the rock,
+and <span class="tei tei-hi"><span style="font-style: italic">quite down to it</span></span>, considerably deeper than the level of
+the proposed drainage; and this should be filled with small
+stones to that level, with a line of tile laid on top of the
+stones, a uniform bottom for the tile to rest upon being
+formed of cheap strips of board. The tile and stone should
+then be covered with inverted sods, with wood shavings,
+or with other suitable material, which will prevent the entrance
+of earth, (from the covering of the drain,) to choke
+them. The water, following down the surface of the rock,
+will rise through the stone work and, entering the tile, will
+flow off. This method may be used for springy hill sides.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">6. The points previously considered relate only to the<span class="tei tei-pb" id="page061">[pg 061]</span><a name="Pg061" id="Pg061" class="tei tei-anchor"></a>
+collection of unusual quantities of water, (from springs
+and from rock surfaces,) and to the removal from the land
+of what is thus collected, and of that which flows from
+the minor or lateral drains.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">lateral drains</span></span> themselves constitute the real drainage
+of the field, for, although main lines take water from
+the land on each side, their action in this regard is not
+usually considered, in determining either their depth or
+their location, and they play an exceedingly small part in
+the more simple form of drainage,—that in which a large
+tract of land, of perfectly uniform slope, is drained by parallel
+lines of equal length, all discharging into a single
+main, running across the foot of the field. The land would
+be equally well drained, if the parallel lines were continued
+to an open ditch beyond its boundary,—the main tile drain
+is only adopted for greater convenience and security. It
+will simplify the question if, in treating the <span class="tei tei-hi"><span style="font-style: italic">theory</span></span> of lateral
+drains, it be assumed that our field is of this uniform
+inclination, and admits of the use of long lines of parallel
+drains. In fact, it is best in practice to approximate as
+nearly as possible to this arrangement, because deviations
+from it, though always necessary in broken land, are
+always more expensive, and present more complicated
+engineering problems. If all the land to be drained had
+a uniform fall, in a single direction, there would be but
+little need of engineering skill, beyond that which is required
+to establish the depth, fall, and distance apart, at
+which the drains should be laid. It is chiefly when the
+land pitches in different directions, and with varying inclination,
+that only a person skilled in the arrangement of
+drains, or one who will give much consideration to the
+subject, can effect the greatest economy by avoiding unnecessary
+complication, and secure the greatest efficiency
+by adjusting the drains to the requirements of the land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Assuming the land to have an unbroken inclination, so
+as to require only parallel drains, it becomes important to<span class="tei tei-pb" id="page062">[pg 062]</span><a name="Pg062" id="Pg062" class="tei tei-anchor"></a>
+know how these parallel drains, (corresponding to the
+<span class="tei tei-hi"><span style="font-style: italic">lateral drains</span></span> of an irregular system,) should be made.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The history of land draining is a history of the gradual
+progress of an improvement, from the accomplishment of
+a single purpose, to the accomplishment of several purposes,
+and most of the instruction which modern agricultural
+writers have given concerning it, has shown too
+great dependence upon the teachings of their predecessors,
+who considered well the single object which they sought
+to attain, but who had no conception that draining was to
+be so generally valuable as it has become. The effort, (probably
+an unconscious one,) to make the theories of modern
+thorough-draining conform to those advanced by the early
+practitioners, seems to have diverted attention from some
+more recently developed principles, which are of much
+importance. For example, about a hundred years ago,
+Joseph Elkington, of Warwickshire, discovered that, where
+land is made too wet by under-ground springs, a skillful
+tapping of these,—drawing off their water through suitable
+conduits,—would greatly relieve the land, and for
+many years the Elkington System of drainage, being a
+great improvement on every thing theretofore practiced,
+naturally occupied the attention of the agricultural world,
+and the Board of Agriculture appointed a Mr. Johnstone
+to study the process, and write a treatise on the subject.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Catch-water drains, made so as to intercept a flow of
+surface water, have been in use from immemorial time, and
+are described by the earliest writers. Before the advent
+of the Draining Tile, covered drains were furnished with
+stones, boards, brush, weeds, and various other rubbish,
+and their good effect, very properly, claimed the attention
+of all improvers of wet land. When the tile first made
+its appearance in general practice, it was of what is called
+the "horse-shoe" form, and,—imperfect though it was,—it
+was better than anything that had preceded it, and was
+received with high approval, wherever it became known.<span class="tei tei-pb" id="page063">[pg 063]</span><a name="Pg063" id="Pg063" class="tei tei-anchor"></a>
+The general use of all these materials for making drains
+was confined to a system of <span class="tei tei-hi"><span style="font-style: italic">partial</span></span> drainage, until the
+publication of a pamphlet, in 1833, by Mr. Smith, of Deanston,
+who advocated the drainage of the whole field, without
+reference to springs. From this plan, but with important
+modifications in matters of detail, the modern system
+of tile draining has grown. Many able men have
+aided its progress, and have helped to disseminate a
+knowledge of its processes and its effects, yet there are
+few books on draining, even the most modern ones, which
+do not devote much attention to Elkington's discovery;
+to the various sorts of stone and brush drains; and to the
+manufacture and use of horse-shoe tile;—not treating them
+as matters of antiquarian interest, but repeating the instructions
+for their application, and allowing the reasoning
+on which their early use was based, to influence, often to a
+damaging extent, their general consideration of the modern
+practice of tile draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">These processes are all of occasional use, even at this
+day, but they are based on no fixed rules, and are so much
+a matter of traditional knowledge, with all farmers, that
+instruction concerning them is not needed. The kind of
+draining which is now under consideration, has for its object
+the complete removal of all of the surplus water that
+reaches the soil, from whatever source, and the assimilation
+of all wet soils to a somewhat uniform condition, as to
+the ease with which water passes through them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There are instances, as has been shown, where a large
+spring, overflowing a considerable area, or supplying the
+water of an annoying brook, ought to be directly connected
+with the under-ground drainage, and its flow neatly
+carried away; and, in other cases, the surface flow over
+large masses of rock should be given easy entrance into
+the tile; but, in all ordinary lands, whether swamps,
+springy hill sides, heavy clays, or light soils lying on retentive
+subsoil, all ground, in fact, which needs under-draining<span class="tei tei-pb" id="page064">[pg 064]</span><a name="Pg064" id="Pg064" class="tei tei-anchor"></a>
+at all, should be laid dry above the level to which
+it is deemed best to place the drains;—not only secured
+against the wetting of springs and soakage water, but
+rapidly relieved of the water of heavy rains. The water
+table, in short, should be lowered to the proper depth, and,
+by permanent outlets at that depth, be prevented from
+ever rising, for any considerable time, to a higher level.
+This being accomplished, it is of no consequence to know
+whence the water comes, and Elkington's system need
+have no place in our calculations. As round pipes, with collars,
+are far superior to the "horse-shoe" tiles, and are
+equally easy to obtain, it is not necessary to consider the
+manner in which these latter should be used,—only to say
+that they ought not to be used at all.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The water which falls upon the surface is at once absorbed,
+settles through the ground, until it reaches a
+point where the soil is completely saturated, and raises the
+general water level. When this level reaches the floor of
+the drains, the water enters at the joints and is carried
+off. That which passes down through the land lying
+between the drains, bears down upon that which has already
+accumulated in the soil, and forces it to seek an outlet
+by rising into the drains.<a id="noteref_7" name="noteref_7" href="#note_7"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">7</span></span></a> For example, if a barrel,
+standing on end, be filled with earth which is saturated
+with water, and its bung be removed, the water of saturation,
+(that is, all which is not held by attraction <span class="tei tei-hi"><span style="font-style: italic">in</span></span> the particles
+of earth,) will be removed from so much of the
+mass as lies above the bottom of the bung-hole. If a
+bucket of water be now poured upon the top, it will not all
+run diagonally toward the opening; it will trickle down to
+the level of the water remaining in the barrel, and this level
+will rise and water will run off at the bottom of the orifice.
+In this manner, the water, even below the drainage level,<span class="tei tei-pb" id="page065">[pg 065]</span><a name="Pg065" id="Pg065" class="tei tei-anchor"></a>
+is changed with each addition at the surface. In a barrel
+filled with coarse pebbles, the water of saturation would
+maintain a nearly level surface; if the material were more
+compact and retentive, a true level would be attained only
+after a considerable time. Toward the end of the flow,
+the water would stand highest at the points furthest distant
+from the outlet. So, in the land, after a drenching
+rain, the water is first removed to the full depth, near the
+line of the drain, and that midway between two drains
+settles much more slowly, meeting more resistance from
+below, and, for a long time, will remain some inches
+higher than the floor of the drain. The usual condition
+of the soil, (except in very dry weather,) would be somewhat
+as represented in the accompanying cut, (Fig. 12.)</p>
+
+<a name="fig18" id="fig18"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image12.png" width="640" height="168" alt="Illustration: Fig. 12 - LINE OF SATURATION BETWEEN DRAINS." title="Fig. 12 - LINE OF SATURATION BETWEEN DRAINS." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 12 - LINE OF SATURATION BETWEEN DRAINS.</div><p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em"><span class="tei tei-hi" style="text-align: center"><span style="font-style: italic">YY are the draings. The curved line b is the line of saturation, which has descended from a, and is approaching c.</span></span></p></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">To provide for this deviation of the line of saturation,
+in practice, drains are placed deeper than would be necessary
+if the water sunk at once to the level of the drain
+floor, the depth of the drains being increased with the increasing
+distance between them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Theoretically, every drop of water which falls on a field
+should sink straight down to the level of the drains, and
+force a drop of water below that level to rise into the drain
+and flow off. How exactly this is true in nature cannot
+be known, and is not material. Drains made in pursuance
+of this theory will be effective for any actual condition.</p>
+
+<span class="tei tei-pb" id="page066">[pg 066]</span><a name="Pg066" id="Pg066" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">depth</span></span> to which the water table should be withdrawn
+depends, not at all on the character of the soil,
+but on the requirements of the crops which are to be
+grown upon it, and these requirements are the same in all
+soils,—consequently the depth should be the same in all.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">What, then, shall that depth be? The usual practice
+of the most experienced drainers seems to have fixed four
+feet as about the proper depth, and the arguments against
+anything less than this, as well as some reasons for supposing
+that to be sufficient, are so clearly stated by Mr.
+Gisborne that it has been deemed best to quote his own
+words on the subject:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Take a flower-pot a foot deep, filled with dry soil.
+Place it in a saucer containing three inches of water.
+The first effect will be, that the water will rise through
+the hole in the bottom of the pot till the water which
+fills the interstices between the soil is on a level with the
+water in the saucer. This effect is by gravity. The
+upper surface of this water is our water-table. From it
+water will ascend by attraction through the whole
+body of soil till moisture is apparent at the surface. Put
+in your soil at 60°, a reasonable summer heat for nine
+inches in depth, your water at 47°, the seven inches'
+temperature of Mr. Parke's undrained bog; the attracted
+water will ascend at 47°, and will diligently occupy
+itself in attempting to reduce the 60° soil to its own
+temperature. Moreover, no sooner will the soil hold
+water of attraction, than evaporation will begin to carry
+it off, and will produce the cold consequent thereon.
+This evaporated water will be replaced by water of attraction
+at 47°, and this double cooling process will go
+on till all the water in the water-table is exhausted.
+Supply water to the saucer as fast as it disappears, and
+then the process will be perpetual. The system of saucer-watering
+is reprobated by every intelligent gardener; it
+is found by experience to chill vegetation; besides which,<span class="tei tei-pb" id="page067">[pg 067]</span><a name="Pg067" id="Pg067" class="tei tei-anchor"></a>
+scarcely any cultivated plant can dip its roots into stagnant
+water with impunity. Exactly the process which
+we have described in the flower-pot is constantly in
+operation on an undrained retentive soil; the water-table
+may not be within nine inches of the surface, but
+in very many instances it is within a foot or eighteen
+inches, at which level the cold surplus oozes into some
+ditch or other superficial outlet. At eighteen inches,
+attraction will, on the average of soils, act with considerable
+power. Here, then, you have two obnoxious
+principles at work, both producing cold, and the one
+administering to the other. The obvious remedy is, to
+destroy their <span class="tei tei-hi"><span style="font-style: italic">united</span></span> action; to break through their line
+of communication. Remove your water of attraction
+to such a depth that evaporation cannot act upon it, or
+but feebly. What is that depth? In ascertaining this
+point we are not altogether without data. No doubt
+depth diminishes the power of evaporation rapidly. Still,
+as water taken from a 30-inch drain is almost invariably
+two or three degrees colder than water taken from four
+feet, and as this latter is generally one or two degrees
+colder than water from a contiguous well several feet
+below, we can hardly avoid drawing the conclusion that
+the cold of evaporation has considerable influence at 30
+inches, a much-diminished influence at four feet, and little
+or none below that depth. If the water-table is removed
+to the depth of four feet, when we have allowed 18
+inches of attraction, we shall still have 30 inches of defence
+against evaporation; and we are inclined to believe
+that any prejudicial combined action of attraction
+and evaporation is thereby well guarded against. The
+facts stated seem to prove that less will not suffice.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"So much on the score of temperature; but this is not
+all. Do the roots of esculents wish to penetrate into
+the earth—at least, to the depth of some feet? We believe
+that they do. We are sure of the brassica tribe,<span class="tei tei-pb" id="page068">[pg 068]</span><a name="Pg068" id="Pg068" class="tei tei-anchor"></a>
+of grass, and clover. All our experience and observation
+deny the doctrine that roots only ramble when they are
+stinted of food; that six inches well manured is quite
+enough, better than more. Ask the Jerseyman; he
+will show you a parsnip as thick as your thigh, and as
+long as your leg, and will tell you of the advantages of
+14 feet of dry soil. You will hear of parsnips whose
+roots descend to unsearchable depths. We will not
+appeal to the Kentucky carrot, which was drawn out
+by its roots at the antipodes; but Mr. Mechi's, if we
+remember right, was a dozen feet or more. Three years
+ago, in a midland county, a field of good land, in good
+cultivation, and richly manured, produced a heavy crop
+of cabbages. In November of that year we saw that
+field broken into in several places, and at the depth of
+four feet the soil (a tenacious marl, fully stiff enough for
+brick-earth) was occupied by the roots of cabbage, not
+sparingly—not mere capillæ—but fibres of the size of
+small pack-thread. A farmer manures a field of four or
+five inches of free soil reposing on a retentive clay, and
+sows it with wheat. It comes up, and between the kernel
+and the manure, it looks well for a time, but anon it
+sickens. An Irish child looks well for five or six years,
+but after that time potato-feeding, and filth, and hardship,
+begin to tell. You ask what is amiss with the
+wheat, and you are told that when its roots reach the
+clay, they are poisoned. This field is then thorough-drained,
+deep, at least four feet. It receives again from
+the cultivator the previous treatment; the wheat comes
+up well, maintains throughout a healthy aspect, and
+gives a good return. What has become of the poison?
+We have been told that the rain water filtered through
+the soil has taken it into solution or suspension, and has
+carried it off through the drains; and men who assume
+to be of authority put forward this as one of the advantages
+of draining. If we believed it, we could not<span class="tei tei-pb" id="page069">[pg 069]</span><a name="Pg069" id="Pg069" class="tei tei-anchor"></a>
+advocate draining. We really should not have the face
+to tell our readers that water, passing through soils containing
+elements prejudicial to vegetation, would carry
+them off, but would leave those which are beneficial behind.
+We cannot make our water so discriminating; the
+general merit of water of deep drainage is, that it contains
+very little. Its perfection would be that it should
+contain nothing. We understand that experiments are
+in progress which have ascertained that water, charged
+with matters which are known to stimulate vegetation,
+when filtered through four feet of retentive soil, comes
+out pure. But to return to our wheat. In the first case,
+it shrinks before the cold of evaporation and the cold of
+water of attraction, and it sickens because its feet are
+never dry; it suffers the usual maladies of cold and wet.
+In the second case, the excess of cold by evaporation
+is withdrawn; the cold water of attraction is removed
+out of its way; the warm air from the surface, rushing
+in to supply the place of the water which the drains remove,
+and the warm summer rains, bearing down with
+them the temperature which they have acquired from
+the upper soil, carry a genial heat to its lowest roots.
+Health, vigorous growth, and early maturity are the
+natural consequences. * * * * * * * * *</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The practice so derided and maligned referring to
+deep draining has advanced with wonderful strides.
+We remember the days of 15 inches; then a step to 20; a
+stride to 30; and the last (and probably final) jump to 50, a
+few inches under or over. We have dabbled in them all,
+generally belonging to the deep section of the day. We
+have used the words 'probably final,' because the first
+advances were experimental, and, though they were justified
+by the results obtained, no one attempted to explain
+the principle on which benefit was derived from
+them. The principles on which the now prevailing
+depth is founded, and which we believe to be true, go<span class="tei tei-pb" id="page070">[pg 070]</span><a name="Pg070" id="Pg070" class="tei tei-anchor"></a>
+far to show that we have attained all the advantages
+which can be derived from the removal of water in
+ordinary agriculture. We do not mean that, even in the
+most retentive soil, water would not get into drains
+which were laid somewhat deeper; but to this there
+must be a not very distant limit, because pure clay, lying
+below the depth at which wet and drought applied at
+surface would expand and contract it, would certainly
+part with its water very slowly. We find that, in coal
+mines and in deep quarries, a stratum of clay of only a
+few inches thick interposed between two strata of pervious
+stone will form an effectual bar to the passage of
+water; whereas, if it lay within a few feet of the surface,
+it would, in a season of heat and drought become
+as pervious as a cullender. But when we have got rid
+of the cold arising from the evaporation of free water,
+have given a range of several feet to the roots of grass
+and cereals, and have enabled retentive land to filter
+through itself all the rain which falls upon its surface,
+we are not, in our present state of knowledge, aware of
+any advantage which would arise from further lowering
+the surface of water in agricultural land. Smith, of
+Deanston, first called prominent attention to the fertilizing
+effects of rain filtered through land, and to evils produced
+by allowing it to flow off the surface. Any one
+will see how much more effectually this benefit will be
+attained, and this evil avoided, by a 4-foot than a 2-foot
+drainage. The latter can only prepare two feet of soil
+for the reception and retention of rain, which two feet,
+being saturated, will reject more, and the surplus must
+run off the surface, carrying whatever it can find with it.
+A 4-foot drainage will be constantly tending to have four
+feet of soil ready for the reception of rain, and it will
+take much more rain to saturate four feet than two.
+Moreover, as a gimlet-hole bored four feet from the surface
+of a barrel filled with water will discharge much<span class="tei tei-pb" id="page071">[pg 071]</span><a name="Pg071" id="Pg071" class="tei tei-anchor"></a>
+more in a given time than a similar hole bored at the
+depth of two feet, so will a 4-foot drain discharge in a
+given time much more water than a drain of two feet.
+One is acted on by a 4-foot, and the other by a 2-foot
+pressure."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If any single fact connected with tile-drainage is established,
+beyond all possible doubt, it is that in the stiffest
+clay soils ever cultivated, drains four feet deep will act
+effectually; the water will find its way to them, more and
+more freely and completely, as the drying of successive
+years, and the penetration and decay of the roots of successive
+crops, modify the character of the land, and they
+will eventually be practically so porous that,—so far as
+the ease of drainage is concerned,—no distinction need, in
+practice, be made between them and the less retentive
+loams. For a few years, the line of saturation between
+the drains, as shown in Fig. 11, may stand at all seasons
+considerably above the level of the bottom of the tile, but
+it will recede year by year, until it will be practically
+level, except immediately after rains.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Mr. Josiah Parkes recommends drains to be laid</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"</span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">At a minimum depth of four feet</span></span><span style="font-size: 90%">, designed with the two-fold object of
+not only freeing the active soil from stagnant and injurious water, but
+of converting the water falling on the surface into an agent for fertilizing;
+no drainage being deemed efficient that did not both remove the
+water falling on the surface, and 'keep down the subterranean water at
+a depth exceeding the power of capillary attraction to elevate it near the
+surface.'"</span></p>
+</div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Alderman Mechi says:</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"Ask nineteen farmers out of twenty, who hold strong clay land, and
+they will tell you it is of no use placing deep four-foot drains in such soils—the
+water cannot get in; a horse's foot-hole (without an opening
+under it) will hold water like a basin; and so on. Well, five minutes
+after, you tell the same farmers you propose digging a cellar, well
+bricked, six or eight feet deep; what is their remark? 'Oh! it's of no
+use your making an underground cellar in our soil, you </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">can't keep the
+water</span></span> <span class="tei tei-hi"><span style="font-size: 90%; font-variant: small-caps">out</span></span><span style="font-size: 90%">!' Was there ever such an illustration of prejudice as this?
+What is a drain pipe but a small cellar full of air? Then, again, common
+sense tells us, you can't keep a light fluid under a heavy one. You might
+as well try to keep a cork under water, as to try and keep air under</span><span class="tei tei-pb" id="page072">[pg 072]</span><a name="Pg072" id="Pg072" class="tei tei-anchor"></a><span style="font-size: 90%">
+water. 'Oh! but then our soil isn't porous.' If not, how can it hold
+water so readily? I am led to these observations by the strong controversy
+I am having with some Essex folks, who protest that I am mad, or
+foolish, for placing 1-inch pipes, at four-foot depth, in strong clays. It
+is in vain I refer to the numerous proofs of my soundness, brought forward
+by Mr. Parkes, engineer to the Royal Agricultural Society, and
+confirmed by Mr. Pusey. They still dispute it. It is in vain I tell them
+</span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">I cannot keep the rainwater out of</span></span><span style="font-size: 90%"> socketed pipes, twelve feet deep, that
+convey a spring to my farm yard. Let us try and convince this large
+class of doubters; for it is of </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">national</span></span><span style="font-size: 90%"> importance. Four feet of good
+porous clay would afford a far better meal to some strong bean, or other
+tap roots, than the usual six inches; and a saving of $4 to $5 per acre,
+in drainage, is no trifle.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"The shallow, or non-drainers, assume that tenacious subsoils are impervious
+or non-absorbent. This is entirely an erroneous assumption.
+If soils were impervious, how could they get wet?</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"I assert, and pledge my agricultural reputation for the fact, that there
+are no earths or clays in this kingdom, be they ever so tenacious, that
+will not readily receive, filter, and transmit rain water to drains placed
+five or more feet deep.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"A neighbor of mine drained twenty inches deep in strong clay; the
+ground cracked widely; the contraction destroyed the tiles, and the
+rains washed the surface soils into the cracks and choked the drains. He
+has since abandoned shallow draining.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"When I first began draining, I allowed myself to be overruled by
+my obstinate man, Pearson, who insisted that, for top water, two feet
+was a sufficient depth in a veiny soil. I allowed him to try the experiment
+on two small fields; the result was, that nothing prospered; and
+I am redraining those fields at </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">one-half</span></span><span style="font-size: 90%"> the cost, five and six feet deep,
+at intervals of 70 and 80 feet.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"I found iron-sand rocks, strong clay, silt, iron, etc., and an enormous
+quantity of water, all </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">below</span></span><span style="font-size: 90%"> the 2-foot drains. This accounted at
+once for the sudden check the crops always met with in May, when they
+wanted to send their roots down, but could not, without going into stagnant
+water."</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"There can be no doubt that it is the </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">depth</span></span><span style="font-size: 90%"> of the drain which regulates
+the escape of the surface water in a given time; regard being had,
+as respects extreme distances, to the nature of the soil, and a due capacity
+of the pipe. </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">The deeper the drain, even in the strongest soils, the quicker
+the water escapes.</span></span><span style="font-size: 90%"> This is an astounding but certain fact.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"That deep and distant drains, where a sufficient fall can be obtained,
+are by far the most profitable, by affording to the roots of the plants a
+greater range for food."</span></p>
+</div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of course, where the soil is underlaid by rock, less than
+four feet from the surface; and where an outlet at that
+depth cannot be obtained, we must, per force, drain less<span class="tei tei-pb" id="page073">[pg 073]</span><a name="Pg073" id="Pg073" class="tei tei-anchor"></a>
+deeply, but where there exists no such obstacle, drains
+should be laid at a <span class="tei tei-hi"><span style="font-style: italic">general</span></span> depth of four-feet,—general,
+not uniform, because the drain should have a uniform inclination,
+which the surface of the land rarely has.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Distance between the Drains.</span></span>—Concerning this,
+there is less unanimity of opinion among engineers, than
+prevails with regard to the question of depth.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In tolerably porous soils, it is generally conceded that 40
+or even 50 feet is sufficiently near for 4-foot drains, but, for
+the more retentive clays, all distances from 18 feet to 50
+feet are recommended, though those who belong to the
+more narrow school are, as a rule, extending the limit,
+as they see, in practice, the complete manner in which
+drains at wider intervals perform their work. A careful
+consideration of the experience of the past twenty years,
+and of the arguments of writers on drainage, leads to the
+belief that there are few soils, which need draining at all,
+on which it will be safe to place 4-foot drains at much
+wider intervals than 40 feet. In the lighter loams there
+are many instances of the successful application of
+Professor Mapes' rule, that "3-foot drains should be
+placed 20 feet apart, and for each additional foot in
+depth the distance may be doubled; for instance, 4-foot
+drains should be 40 feet apart, and 5-foot drains 80 feet
+apart." But, with reference to the greater distance,
+(80 feet,) it is not to be recommended in stiff clays, for
+any depth of drain. Where it is necessary, by reason of
+insufficient fall, or of underground rock, to go only three
+feet deep, the drains should be as near together as 20 feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">At first thought, it may seem akin to quackery to recommend
+a uniform depth and distance, without reference
+to the character of the land to be drained; and it is unquestionably
+true that an exact adaptation of the work to
+the varying requirements of different soils would be beneficial,
+though no system can be adopted which will make<span class="tei tei-pb" id="page074">[pg 074]</span><a name="Pg074" id="Pg074" class="tei tei-anchor"></a>
+clay drain as freely as sand. The fact is, that the adjustment
+of the distances between drains is very far from
+partaking of the nature of an exact science, and there is
+really very little known, by any one, of the principles on
+which it should be based, or of the manner in which the
+bearing of those principles, in any particular case, is affected
+by several circumstances which vary with each
+change of soil, inclination and exposure.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the essays on drainage which have been thus far
+published, there is a vagueness in the arguments on this
+branch of the subject, which betrays a want of definite
+conviction in the minds of the writers; and which tends
+quite as much to muddle as to enlighten the ideas of the
+reader. In so far as the directions are given, whether fortified
+by argument or not, they are clearly empirical, and
+are usually very much qualified by considerations which
+weigh with unequal force in different cases.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In laying out work, any skillful drainer will be guided,
+in deciding the distance between the lines, by a judgment
+which has grown out of his former experience; and which
+will enable him to adapt the work, measurably, to the
+requirements of the particular soil under consideration;
+but he would probably find it impossible to so state the
+reasons for his decision, that they would be of any general
+value to others.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Probably it will be a long time before rules on this subject,
+based on well sustained <span class="tei tei-hi"><span style="font-style: italic">theory</span></span>, can be laid down with distinctness,
+and, in the mean time, we must be guided by
+the results of practice, and must confine ourselves to a
+distance which repeated trial, in various soils, has proven
+to be safe for all agricultural land. In the drainage of
+the Central Park, after a mature consideration of all that
+had been published on the subject, and of a considerable
+previous observation and experience, it was decided to
+adopt a general depth of four feet, and to adhere as closely
+as possible to a uniform distance of forty feet. No instance<span class="tei tei-pb" id="page075">[pg 075]</span><a name="Pg075" id="Pg075" class="tei tei-anchor"></a>
+was known of a failure to produce good results by draining
+at that distance, and several cases were recalled where
+drains at fifty and sixty feet had proved so inefficient that
+intermediate lines became necessary. After from seven
+to ten years' trial, the Central Park drainage, by its results,
+has shown that,—although some of the land is of a
+very retentive character,—this distance is not too great;
+and it is adopted here for recommendation to all who have
+no especial reason for supposing that greater distances
+will be fully effective in their more porous soils.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As has been before stated, drains at that distance, (or
+at any distance,) will not remove all of the water of saturation
+from heavy clays so rapidly as from more porous
+soil; but, although, in some cases, the drainage may be
+insufficient during the first year, and not absolutely perfect
+during the second and third years, the increased porosity
+which drainage causes, (as the summer droughts
+make fissures in the earth, as decayed roots and other
+organic deposits make these fissures permanent, and as
+chemical action in the aërated soil changes its character,)
+will finally bring clay soils to as perfect a condition as they
+are capable of attaining, and will invariably render them
+excellent for cultivation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Direction of the Laterals</span></span> should be <span class="tei tei-hi"><span style="font-style: italic">right up and
+down the slope of the land</span></span>, in the line of steepest descent.
+For a long time after the general adoption of thorough-draining,
+there was much discussion of this subject, and
+much variation in practice. The influence of the old rules
+for making surface or "catch-water" drains lasted for a
+long time, and there was a general tendency to make tile
+drains follow the same directions. An important requirement
+of these was that they should not take so steep an
+inclination as to have their bottoms cut out and their
+banks undermined by the rapid flow of water, and that
+they should arrest and carry away the water flowing
+down over the surface of hill sides. The arguments for the<span class="tei tei-pb" id="page076">[pg 076]</span><a name="Pg076" id="Pg076" class="tei tei-anchor"></a>
+line of steepest descent were, however, so clear, and
+drains laid on that line were so universally successful in
+practice, that it was long ago adopted by all,—save those
+novices who preferred to gain their education in draining
+in the expensive school of their own experience.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The more important reasons why this direction is the
+best are the following: First, it is the quickest way to
+get the water off. Its natural tendency is to run straight
+down the hill, and nothing is gained by diverting it from
+this course. Second, if the drain runs obliquely down the
+hill, the water will be likely to run out at the joints of the
+tile and wet the ground below it; even if it do not,
+mainly, run past the drain from above into the land below,
+instead of being forced into the tile. Third, a drain
+lying obliquely across a hillside will not be able to draw
+the water from below up the hill toward it, and the
+water of nearly the whole interval will have to seek its
+outlet through the drain below it. Fourth, drains running
+directly down the hill will tap any porous water
+bearing strata, which may crop out, at regular intervals, and
+will thus prevent the spewing out of the water at the surface,
+as it might do if only oblique drains ran for a long
+distance just above or just below them. Very steep, and
+very springy hill sides, sometimes require very frequent
+drains to catch the water which has a tendency to flow to
+the surface; this, however, rarely occurs.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In laying out a plan for draining land of a broken surface,
+which inclines in different directions, it is impossible
+to make the drains follow the line of steepest descent, and
+at the same time to have them all parallel, and at uniform
+distances. In all such cases a compromise must be made
+between the two requirements. The more nearly the parallel
+arrangement can be preserved, the less costly will
+the work be, while the more nearly we follow the steepest
+slope of the ground, the more efficient will each drain be.
+No rule for this adjustment can be given, but a careful<span class="tei tei-pb" id="page077">[pg 077]</span><a name="Pg077" id="Pg077" class="tei tei-anchor"></a>
+study of the plan of the ground, and of its contour lines,
+will aid in its determination. On all irregular ground it
+requires great skill to secure the greatest efficiency consistent
+with economy.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">fall</span></span> required in well made tile drains is very much
+less than would be supposed, by an inexperienced person,
+to be necessary. Wherever practicable, without too great
+cost, it is desirable to have a fall of one foot in one hundred
+feet, but more than this in ordinary work is not especially
+to be sought, although there is, of course, no
+objection to very much greater inclination.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">One half of that amount of fall, or six inches in one
+hundred feet, is quite sufficient, if the execution of the
+work is carefully attended to.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The least rate of fall which it is prudent to give to a
+drain, in using ordinary tiles, is 2.5 in 1,000, or three inches
+in one hundred feet, and even this requires very careful
+work.<a id="noteref_8" name="noteref_8" href="#note_8"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">8</span></span></a> A fall of six inches in one hundred feet is recommended
+whenever it can be easily obtained—not as being
+more effective, but as requiring less precision, and consequently
+less expense.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Kinds and Sizes of Tiles.</span></span>—Agricultural drain-tiles are
+made of clay similar to that which is used for brick.
+When burned, they are from twelve inches to fourteen
+inches long, with an interior diameter of from one to
+eight inches, and with a thickness of wall, (depending on
+the strength of the clay, and the size of the bore,) of from
+one-quarter of an inch to more than an inch. They are
+porous, to the extent of absorbing a certain amount of
+water, but their porosity has nothing to do with their use
+for drainage,—for this purpose they might as well be of
+glass. The water enters them, not through their walls,<span class="tei tei-pb" id="page078">[pg 078]</span><a name="Pg078" id="Pg078" class="tei tei-anchor"></a>
+but at their joints, which cannot be made so tight that
+they will not admit the very small amount of water that
+will need to enter at each space. Gisborne says:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"If an acre of land be intersected with parallel drains
+twelve yards apart, and if on that acre should fall the
+very unusual quantity of one inch of rain in twelve
+hours, in order that every drop of this rain may be discharged
+by the drains in forty-eight hours from the commencement
+of the rain—(and in a less period that quantity
+neither will, not is it desirable that it should, filter
+through an agricultural soil)—the interval between two
+pipes will be called upon to pass two-thirds of a tablespoonful
+of water per minute, and no more. Inch pipes,
+lying at a small inclination, and running only half-full,
+will discharge more than double this quantity of water
+in forty-eight hours."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Tiles may be made of any desired form of section,—the
+usual forms are the "horse-shoe," the "sole," the "double-sole,"
+and the "round." The latter may be used with
+collars, and they constitute the "pipes and collars," frequently
+referred to in English books on drainage.</p>
+
+<a name="fig19" id="fig19"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image13.png" width="640" height="127" alt="Illustration: Fig. 13 - HORSE-SHOE TILE." title="Fig. 13 - HORSE-SHOE TILE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 13 - HORSE-SHOE TILE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Horse-shoe tiles</span></span>, Fig. 13, are condemned by all modern
+engineers. Mr. Gisborne disposes of them by an argument
+of some length, the quotation
+of which in these pages is
+probably advisable, because
+they form so much better conduits
+than stones, and to that extent have been so successfully
+employed, that they are still largely used in this country
+by "amateurs."</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"We shall shock some and surprise many of our readers, when we
+state confidently that, in average soils, and, still more, in those which
+are inclined to be tender, horse shoe tiles form the weakest and most
+failing conduit which has ever been used for a deep drain. It is so, however;
+and a little thought, even if we had no experience, will tell us
+that it must be so. A doggrel song, quite destitute of humor, informs
+us that tiles of this sort were used in 1760 at Grandesburg Hall, in Suffolk,</span><span class="tei tei-pb" id="page079">[pg 079]</span><a name="Pg079" id="Pg079" class="tei tei-anchor"></a><span style="font-size: 90%">
+by Mr. Charles Lawrence, the owner of the estate. The earliest of
+which we had experience were of large area and of weak form. Constant
+failures resulted from their use, and the cause was investigated; many
+of the tiles were found to be choked up with clay, and many to be broken
+longitudinally through the crown. For the first evil, two remedies
+were adopted; a sole of slate, of wood, or of its own material, was
+sometimes placed under the tile, but the more usual practice was to form
+them with club-feet. To meet the case of longitudinal fracture, the tiles
+were reduced in size, and very much thickened in proportion to their
+area. The first of these remedies was founded on an entirely mistaken,
+and the second on no conception at all of the cause of the evil to which
+they were respectively applied. The idea was, that this tile, standing on
+narrow feet, and pressed by the weight of the refilled soil, sank into the
+floor of the drain; whereas, in fact, the floor of the drain rose into the
+tile. Any one at all conversant with collieries is aware that when a </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">strait</span></span><span style="font-size: 90%">
+work (which is a small subterranean tunnel six feet high and four feet
+wide or thereabouts) is driven in coal, the rising of the floor is a more
+usual and far more inconvenient occurrence than the falling of the roof:
+the weight of the two sides squeezes up the floor. We have seen it
+formed into a very decided arch without fracture. Exactly a similar
+operation takes place in the drain. No one had till recently dreamed of
+forming a tile drain, the bottom of which a man was not to approach
+personally within twenty inches or two feet. To no one had it then occurred
+that width at the bottom of the drain was a great evil. For the
+convenience of the operator the drain was formed with nearly perpendicular
+sides, of a width in which he could stand and work conveniently,
+shovel the bottom level with his ordinary spade, and lay the tiles by his
+hand; the result was a drain with nearly perpendicular sides, and a wide
+bottom. No sort of clay, particularly when softened by water standing
+on it or running over it, could fail to rise under such circumstances; and
+the deeper the drain the greater the pressure and the more certain the
+rising. A horse-shoe tile, which may be a tolerable secure conduit in a
+drain of two feet, in one of four feet becomes an almost certain failure.
+As to the longitudinal fracture—not only is the tile subject to be broken
+by one of those slips which are so troublesome in deep draining, and to
+which the lightly-filled material, even when the drain is completed,
+offers an imperfect resistance, but the constant pressure together of the
+sides, even when it does not produce a fracture of the soil, catches hold
+of the feet of the tile, and breaks it through the crown. Consider the
+case of a drain formed in clay when dry, the conduit a horse-shoe tile.
+When the clay expands with moisture, it necessarily presses on the tile
+and breaks it through the crown, its weakest part.</span><a id="noteref_9" name="noteref_9" href="#note_9"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">9</span></span></a><span style="font-size: 90%"> When the Regent's</span><span class="tei tei-pb" id="page080">[pg 080]</span><a name="Pg080" id="Pg080" class="tei tei-anchor"></a><span style="font-size: 90%">
+Park was first drained, large conduits were in fashion, and they were
+made circular by placing one horse-shoe tile upon another. It would be
+difficult to invent a weaker conduit. On re-drainage, innumerable instances
+were found in which the upper tile was broken through the
+crown, and had dropped into the lower. Next came the D form, tile and
+sole in one, and much reduced in size—a great advance; and when some
+skillful operator had laid this tile bottom upwards we were evidently on
+the eve of pipes. For the D tile a round pipe moulded with a flat-bottomed
+solid sole is now generally substituted, and is an improvement;
+but is not equal to pipes and collars, nor generally cheaper than they
+are."</span></p>
+</div>
+
+<a name="fig20" id="fig20"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image14.png" width="640" height="108" alt="Illustration: Fig. 14 - SOLE TILE." title="Fig. 14 - SOLE TILE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 14 - SOLE TILE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">One chief objection to the <span class="tei tei-hi"><span style="font-style: italic">Sole-tiles</span></span> is, that, in the drying
+which they undergo, preparatory to the burning, the
+upper side is contracted, by
+the more rapid drying, and
+they often require to be trimmed
+off with a hatchet before
+they will form even tolerable joints; another is, that they
+cannot be laid with collars, which form a joint so perfect
+and so secure, that their use, in the smaller drains, should
+be considered indispensable.</p>
+
+<a name="fig21" id="fig21"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image15.png" width="640" height="119" alt="Illustration: Fig. 15 - DOUBLE-SOLE TILE." title="Fig. 15 - DOUBLE-SOLE TILE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 15 - DOUBLE-SOLE TILE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">double-sole tiles</span></span>, which can be laid either side up
+give a much better joint,
+but they are so heavy as to
+make the cost of transporation
+considerably greater.
+They are also open to the grave objection that they cannot
+be fitted with collars.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Experience, in both public and private works in this
+country, and the cumulative testimony of English and
+French engineers, have demonstrated that the only tile
+which it is economical to use, is the <span class="tei tei-hi"><span style="font-style: italic">best</span></span> that can be found,
+and that the best,—much the best—thus far invented, is
+the "pipe, or round tile, and collar,"—and these are unhesitatingly
+recommended for use in all cases. Round
+tiles of small sizes should not be laid without collars, as the
+ability to use these constitutes their chief advantage;
+holding them perfectly in place, preventing the rattling<span class="tei tei-pb" id="page081">[pg 081]</span><a name="Pg081" id="Pg081" class="tei tei-anchor"></a>
+in of loose dirt in laying, and giving twice the space for
+the entrance of water at the joints. A chief advantage
+of the larger sizes is, that they may be laid on any side
+and thus made to fit closely. The usual sizes of these
+tiles are 1-1/4 inches, 2-1/4 inches, and 3-1/2 inches in interior diameter.
+Sections of the 2-1/4 inch make collars for the 1-1/4
+inch, and sections of the 3-1/2 inch make collars for the 2-1/4
+inch. The 3-1/2 inch size does not need collars, as it is easily
+secured in place, and is only used where the flow of water
+would be sufficient to wash out the slight quantity of foreign
+matters that might enter at the joints.</p>
+
+<a name="fig22" id="fig22"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image16.png" width="640" height="130" alt="Illustration: Fig. 16 - ROUND TILE AND COLLAR, AND THE SAME AS LAID." title="Fig. 16 - ROUND TILE AND COLLAR, AND THE SAME AS LAID." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 16 - ROUND TILE AND COLLAR, AND THE SAME AS LAID.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The size of tile</span></span> to be used is a question of consequence.
+In England, 1-inch pipes are frequently used, but 1-1/4 inch<a id="noteref_10" name="noteref_10" href="#note_10"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">10</span></span></a>
+are recommended for the smallest drains. Beyond this
+limit, the proper size to select is, <span class="tei tei-hi"><span style="font-style: italic">the smallest that can convey
+the water which will ordinarily reach it after a heavy
+rain</span></span>. The smaller the pipe, the more concentrated the
+flow, and, consequently, the more thoroughly obstructions
+will be removed, and the occasional flushing of the pipe,
+when it is taxed, for a few hours, to its utmost capacity,
+will insure a thorough cleansing. No inconvenience can
+result from the fact that, on rare occasions, the drain is
+unable, for a short time, to discharge all the water that
+reaches it, and if collars are used, or if the clay be well
+packed about the pipes, there need be no fear of the tile
+being displaced by the pressure. An idea of the drying
+capacity of a 1-1/4-inch tile may be gained from observing
+its <span class="tei tei-hi"><span style="font-style: italic">wetting</span></span> capacity, by connecting a pipe of this size with<span class="tei tei-pb" id="page082">[pg 082]</span><a name="Pg082" id="Pg082" class="tei tei-anchor"></a>
+a sufficient body of water, at its surface, and discharging,
+over a level dry field, all the water which it will carry.
+A 1-1/4-inch pipe will remove all the water which would fall
+on an acre of land in a very heavy rain, in 24 hours,—much
+less time than the water would occupy in getting to
+the tile, in any soil which required draining; and tiles of
+this size are ample for the draining of two acres. In like
+manner, 2-1/2-inch tile will suffice for eight, and 3-1/2-inch tile
+for twenty acres. The foregoing estimates are, of course,
+made on the supposition that only the water which falls
+on the land, (storm water,) is to be removed. For main
+drains, when greater capacity is required, two tiles may be
+laid, (side by side,) or in such cases the larger sizes of
+sole tiles may be used, being somewhat cheaper. Where
+the drains are laid 40 feet apart, about 1,000 tiles per acre
+will be required, and, in estimating the quantity of tiles of
+the different sizes to be purchased, reference should be
+had to the following figures; the first 2,000 feet of drains
+require a collecting drain of 2-1/4-inch tile, which will take
+the water from 7,000 feet; and for the outlet of from
+7,000 to 20,000 feet 3-1/2-inch tile may be used. Collars,
+being more subject to breakage, should be ordered in somewhat
+larger quantities.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of course, such guessing at what is required, which is
+especially uncertain if the surface of the ground is so
+irregular as to require much deviation from regular parallel
+lines, is obviated by the careful preparation of a plan
+of the work, which enables us to measure, beforehand, the
+length of drain requiring the different sizes of conduit,
+and, as tiles are usually made one or two inches more than
+a foot long, a thousand of them will lay a thousand feet,—leaving
+a sufficient allowance for breakage, and for such
+slight deviations of the lines as may be necessary to pass
+around those stones which are too large to remove. In very
+stony ground, the length of lines is often materially increased,
+but in such ground, there is usually rock enough<span class="tei tei-pb" id="page083">[pg 083]</span><a name="Pg083" id="Pg083" class="tei tei-anchor"></a>
+or such accumulations of boulders in some parts, to reduce
+the length of drain which it is possible to lay, at
+least as much as the deviations will increase it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is always best to make a contract for tile considerably
+in advance. The prices which are given in the advertisements
+of the makers, are those at which a single thousand,—or
+even a few hundred,—can be purchased, and
+very considerable reductions of price may be secured on
+large orders. Especially is this the case if the land is so
+situated that the tile may be purchased at either one of
+two tile works,—for the prices of all are extravagantly
+high, and manufacturers will submit to large discounts
+rather than lose an important order.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is especially recommended, in making the contract,
+to stipulate that every tile shall be hard-burned, and that
+those which will not give a <span class="tei tei-hi"><span style="font-style: italic">clear ring</span></span> when struck with
+a metallic instrument, shall be rejected, and the cost of
+their transportation borne by the maker. The tiles used
+in the Central Park drainage were all tested with the aid
+of a bit of steel which had, at one end, a cutting edge.
+With this instrument each tile was "sounded," and its
+hardness was tested by scraping the square edge of the
+bore. If it did not "ring" when struck, or if the edge
+was easily cut, it was rejected. From the first cargo there
+were many thrown out, but as soon as the maker saw that
+they were really inspected, he sent tile of good quality
+only. Care should also be taken that no <span class="tei tei-hi"><span style="font-style: italic">over-burned</span></span>
+tile,—such as have been melted and warped, or very much
+contracted in size by too great heat,—be smuggled into
+the count.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A little practice will enable an ordinary workman to
+throw out those which are imperfect, and, as a single tile
+which is so underdone that it will not last, or which, from
+over-burning, has too small an orifice, may destroy a long
+drain, or a whole system of drains, the inspection should
+be thorough.</p>
+
+<span class="tei tei-pb" id="page084">[pg 084]</span><a name="Pg084" id="Pg084" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The collars should be examined with equal care. Concerning
+the use of these, Gisborne says:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"To one advantage which is derived from the use of
+collars we have not yet adverted—the increased facility
+with which free water existing in the soil can find entrance
+into the conduit. The collar for a 1-1/2-inch pipe
+has a circumference of three inches. The whole space
+between the collar and the pipe on each side of the
+collar is open, and affords no resistance to the entrance
+of water; while at the same time the superincumbent
+arch of the collar protects the junction of two
+pipes from the intrusion of particles of soil. We confess
+to some original misgivings that a pipe resting only
+on an inch at each end, and lying hollow, might prove
+weak and liable to fracture by weight pressing on it
+from above; but the fear was illusory. Small particles
+of soil trickle down the sides of every drain, and the
+first flow of water will deposit them in the vacant space
+between the two collars. The bottom, if at all soft, will
+also swell up into any vacancy. Practically, if you reopen
+a drain well laid with pipes and collars, you will
+find them reposing in a beautiful nidus, which, when they
+are carefully removed, looks exactly as if it had been
+moulded for them."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The cost of collars should not be considered an objection
+to their use; because, without collars it would not be
+safe, (as it is difficult to make the orifices of two pieces
+come exactly opposite to each other,) to use less than 2-inch
+tiles, while, with collars, 1-1/4-inch are sufficient for the
+same use, and, including the cost of collars, are hardly
+more expensive.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is usual, in all works on agricultural drainage, to insert
+tables and formulæ for the guidance of those who
+are to determine the size of tile required to discharge the
+water of a certain area. The practice is not adopted here,<span class="tei tei-pb" id="page085">[pg 085]</span><a name="Pg085" id="Pg085" class="tei tei-anchor"></a>
+for the reason that all such tables are without practical
+value. The smoothness and uniformity of the bore; the
+rate of fall; the depth of the drain, and consequent
+"head," or pressure, of the water; the different effects of
+different soils in retarding the flow of the water to the
+drain; the different degrees to which angles in the line of
+tile affect the flow; the degree of acceleration of the flow
+which is caused by greater or less additions to the stream
+at the junction of branch drains; and other considerations,
+arising at every step of the calculation, render it
+impossible to apply delicate mathematical rules to work
+which is, at best, rude and unmathematical in the extreme.
+In sewerage, and the water supply of towns, such tables
+are useful,—though, even in the most perfect of these
+operations, engineers always make large allowances for
+circumstances whose influence cannot be exactly measured,—but
+in land drainage, the ordinary rules of hydraulics
+have to be considered in so many different bearings,
+that the computations of the books are not at all reliable.
+For instance, Messrs. Shedd &amp; Edson, of Boston, have
+prepared a series of tables, based on Smeaton's experiments,
+for the different sizes of tile, laid at different inclinations,
+in which they state that 1-1/2-inch tile, laid with a
+fall of one foot in a length of one hundred feet, will discharge
+12,054.81 gallons of water in 24 hours. This is
+equal to a rain-fall of over 350 inches per year on an acre
+of land. As the average annual rain-fall in the United
+States is about 40 inches, at least one-half of which is removed
+by evaporation, it would follow, from this table,
+that a 1-1/2-inch pipe, with the above named fall, would
+serve for the drainage of about 17 acres. But the calculation
+is again disturbed by the fact that the rain-fall is
+not evenly distributed over all the days of the year,—as
+much as six inches having been known to fall in a single
+24 hours, (amounting to about 150,000 gallons per acre,)
+and the removal of this water in a single day would require<span class="tei tei-pb" id="page086">[pg 086]</span><a name="Pg086" id="Pg086" class="tei tei-anchor"></a>
+a tile nearly five inches in diameter, laid at the
+given fall, or a 3-inch tile laid at a fall of more than 7-1/2 feet
+in 100 feet. But, again, so much water could not reach a
+drain four feet from the surface, in so short a time, and
+the time required would depend very much on the character
+of the soil. Obviously, then, these tables are worthless
+for our purpose. Experience has fully shown that the sizes
+which are recommended below are ample for practical
+purposes, and probably the areas to be drained by the
+given sizes might be greatly increased, especially with reference
+to such soils as do not allow water to percolate very
+freely through them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In connection with this subject, attention is called to the
+following extract from the Author's Report on the Drainage,
+which accompanies the "Third Annual Report of the
+Board of Commissioners of the Central Park:"</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In order to test the efficiency of the system of drainage
+employed on the Park, I have caused daily observations
+to be taken of the amount of water discharged from the
+principal drain of 'the Green,' and have compared it
+with the amount of rain-fall. A portion of the record of
+those observations is herewith presented.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In the column headed 'Rain-Fall,' the amount of
+water falling on one acre during the entire storm, is given
+in gallons. This is computed from the record of a rain-gauge
+kept on the Park.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Under the head of 'Discharge,' the number of gallons
+of water drained from one acre during 24 hours is given.
+This is computed from observations taken, once a day or
+oftener, and supposes the discharge during the entire
+day to be the same as at the time of taking the observations.
+It is, consequently, but approximately correct:</p>
+
+<span class="tei tei-pb" id="page087">[pg 087]</span><a name="Pg087" id="Pg087" class="tei tei-anchor"></a>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="5"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell">Date.</td><td class="tei tei-cell">Hour.</td><td class="tei tei-cell">Rain-fall.</td><td class="tei tei-cell">Discharge.</td><td class="tei tei-cell">Remarks.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 13.</td><td class="tei tei-cell">10 a.m.</td><td class="tei tei-cell">49,916 galls.</td><td class="tei tei-cell">184 galls.</td><td class="tei tei-cell">Ground dry. No rain since 3d inst.; 2 inches rain fell between 5.15 and 5.45 p.m. and 1-5th of an inch between 5.45 and 7.15.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 14.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">4,968 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 15.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">1,325 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 16.</td><td class="tei tei-cell">8 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">1,104 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 16.</td><td class="tei tei-cell">6 p.m.</td><td class="tei tei-cell">33,398 "</td><td class="tei tei-cell">7,764 "</td><td class="tei tei-cell">Ground saturated at a depth of 2 feet when this rain commenced.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 17.</td><td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell">4,319 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 18.</td><td class="tei tei-cell">9 a.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">2,208 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 19.</td><td class="tei tei-cell">7 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">1,325 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 20.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">993 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 21.</td><td class="tei tei-cell">11 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">662 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 22.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">560 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 23.</td><td class="tei tei-cell">10 "</td><td class="tei tei-cell">1,698 "</td><td class="tei tei-cell">515 "</td><td class="tei tei-cell">This slight rain only affected the ratio of decrease.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">July 24.</td><td class="tei tei-cell">7 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">442 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell">Nothing worthy of note until Aug. 3.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 3.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell">8,490 "</td><td class="tei tei-cell">191 "</td><td class="tei tei-cell">Rain from 3 p.m. to 3.30 p.m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 4.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell">13,018 "</td><td class="tei tei-cell">184 "</td><td class="tei tei-cell">" 4.45 p.m. to 12 m.n.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 5.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell">45,288 "</td><td class="tei tei-cell">368 "</td><td class="tei tei-cell">" 12 m. to 6 p.m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 5.</td><td class="tei tei-cell">6 p.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">8,280 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 6.</td><td class="tei tei-cell">9 a.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">3,954 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 7.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">2,208 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 8.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">828 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 9.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">662 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 12.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">368 "</td><td class="tei tei-cell">Rain 12 m. Aug. 12 to 7 a.m. Aug. 13.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 13.</td><td class="tei tei-cell">7 "</td><td class="tei tei-cell">19,244 "</td><td class="tei tei-cell">1,104 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 14.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">736 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 24.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">1,132 "</td><td class="tei tei-cell">191 "</td><td class="tei tei-cell">" 3 a.m. to 4.15 a.m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 25.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">5,547 "</td><td class="tei tei-cell">9,936 "</td><td class="tei tei-cell">" 3.30 p.m. 24th, to 7 a.m. 25th.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 25.</td><td class="tei tei-cell">7 p.m.</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">7,740 "</td><td class="tei tei-cell">" 7 a.m. to 12 m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 26.</td><td class="tei tei-cell">6-1/2 a.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">3,974 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 26.</td><td class="tei tei-cell">6 p.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">2,208 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 27.</td><td class="tei tei-cell">6-1/2 a.m.</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">1,529 "</td><td class="tei tei-cell">" 4 p.m. to 6 p.m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Aug. 28.</td><td class="tei tei-cell">7 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">993 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 11.</td><td class="tei tei-cell">7 "</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">165 "</td><td class="tei tei-cell">" 12 m.n. (10th) to 7 a.m. (11th.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 12.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">5,094 "</td><td class="tei tei-cell">147 "</td><td class="tei tei-cell">" 12 m. (11th) to 7 a.m. (12th.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 13.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">132 "</td><td class="tei tei-cell">" 4 p.m. to 6 p.m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 16.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">15,848 "</td><td class="tei tei-cell">110 "</td><td class="tei tei-cell">" 12 m. to 12 m.n.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 17.</td><td class="tei tei-cell">7 "</td><td class="tei tei-cell">27,552 "</td><td class="tei tei-cell">1,104 "</td><td class="tei tei-cell">Rain continued until 12 m.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 17.</td><td class="tei tei-cell">5 p.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">6,624 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 18.</td><td class="tei tei-cell">8 a.m.</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">4,968 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 19.</td><td class="tei tei-cell">6-1/2 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">2,208 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 19.</td><td class="tei tei-cell">4 p.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">1,805 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 20.</td><td class="tei tei-cell">9 a.m.</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">1,324 "</td><td class="tei tei-cell">Rain f'm 12 m. (19th) to 7 a.m. (20th.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 21.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">5,094 "</td><td class="tei tei-cell">945 "</td><td class="tei tei-cell">" 3.20 p.m. (20th) to 6 a.m. (21st.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 22.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">10,185 "</td><td class="tei tei-cell">1,656 "</td><td class="tei tei-cell">" 12 m. (21st) to 7 a.m. (22d.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 23.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">40,756 "</td><td class="tei tei-cell">7,948 "</td><td class="tei tei-cell">Rain continued until 7 a.m. (23d.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 24.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">4,968 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 25.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">566 "</td><td class="tei tei-cell">2,984 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Sep. 26.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">2,484 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Oct. 1.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">828 "</td><td class="tei tei-cell">There was not enough rain during this period to materially affect the flow of water.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 18.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">83 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 19.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">1,132 "</td><td class="tei tei-cell">184 "</td><td class="tei tei-cell">Rain 4.50 p.m. (18th) to 8 a.m. (19th.)</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 20.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">119 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 22.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell">29,336 "</td><td class="tei tei-cell">6,624 "</td><td class="tei tei-cell">Rain all of the previous night.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 22.</td><td class="tei tei-cell">2 p.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">6,624 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 23.</td><td class="tei tei-cell">9 a.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">4,968 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 24.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">1,711 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Nov. 24.</td><td class="tei tei-cell">2 p.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">1,417 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Dec. 17.</td><td class="tei tei-cell">9 a.m.</td><td class="tei tei-cell"></td><td class="tei tei-cell">552 "</td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Dec. 18.</td><td class="tei tei-cell">9 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">4,968 "</td><td class="tei tei-cell">Rain during the previous night.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Dec. 30.</td><td class="tei tei-cell">10 "</td><td class="tei tei-cell"></td><td class="tei tei-cell">581 "</td><td class="tei tei-cell"></td>
+</tr></tbody></table>
+
+<span class="tei tei-pb" id="page088">[pg 088]</span><a name="Pg088" id="Pg088" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The tract drained by this system, though very swampy,
+before being drained, is now dry enough to walk upon,
+almost immediately after a storm, except when underlaid
+by a stratum of frozen ground."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The area drained by the main at which these gaugings
+were made, is about ten acres, and, in deference to the
+prevailing mania for large conduits, it had been laid with
+6-inch sole-tile. The greatest recorded discharge in 24
+hours was (August 25th,) less than 100,000 gallons from
+the ten acres,—an amount of water which did not half fill
+the tile, but which, according to the tables referred to,
+would have entirely filled it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In view of all the information that can be gathered
+on the subject, the following directions are given as perfectly
+reliable for drains four feet or more in depth, laid
+on a well regulated fall of even three inches in a hundred
+feet:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For 2 acres 1-1/4 inch pipes (with collars.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For 8 acres 2-1/4 inch pipes (with collars.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For 20 acres 3-1/2 inch pipes</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For 40 acres 2 3-1/2 inch pipes or one 5-inch sole-tile.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For 50 acres 6 inch pipes sole-tile.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For 100 acres 8 inch pipes or two 6-inch sole-tiles.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is not pretended that these drains will immediately
+remove all the water of the heaviest storms, but they will
+always remove it fast enough for all practical purposes,
+and, if the pipes are securely laid, the drains will only be
+benefited by the occasional cleansing they will receive
+when running "more than full." In illustration of this
+statement, the following is quoted from a paper communicated
+by Mr. Parkes to the Royal Agricultural Society of
+England in 1843:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Mr. Thomas Hammond, of Penshurst, (Kent,) now
+uses no other size for the parallel drains than the inch
+tile in the table, (No. 5,) having commenced with No.<span class="tei tei-pb" id="page089">[pg 089]</span><a name="Pg089" id="Pg089" class="tei tei-anchor"></a>
+4,<a id="noteref_11" name="noteref_11" href="#note_11"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">11</span></span></a> and it may be here stated, that the opinion of all the
+farmers who have used them in the Weald, is that a bore
+of an inch area is abundantly large. A piece of 9 acres,
+now sown with wheat, was observed by the writer, 36
+hours after the termination of a rain which fell heavily
+and incessantly during 12 hours on the 7th of November.
+This field was drained in March, 1842, to the depth
+of 30 to 36 inches, at a distance of 24 feet asunder, the
+length of each drain being 235 yards.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Each, drain emptied itself through a fence bank into
+a running stream in a road below it; the discharge
+therefore was distinctly observable. Two or three of
+the pipes had now ceased running; and, with the exception
+of one which tapped a small spring and gave a
+stream about the size of a tobacco pipe, the run from
+the others did not exceed the size of a wheat straw.
+The greatest flow had been observed by Mr. Hammond
+at no time to exceed half the bore of the pipes. The
+fall in this field is very great, and the drains are laid in
+the direction of the fall, which has always been the practice
+in this district. The issuing water was transparently
+clear; and Mr. Hammond states that he has
+never observed cloudiness, except for a short time after
+very heavy flushes of rain, when the drains are quickly
+cleared of all sediment, in consequence of the velocity
+and force of the water passing through so small a channel.
+Infiltration through the soil and into the pipes, must,
+in this case, be considered to have been perfect; and
+their observed action is the more determinate and valuable
+as regards time and effect, as the land was saturated
+with moisture previous to this particular fall of rain,
+and the pipes had ceased to run when it commenced.
+This piece had, previous to its drainage, necessarily
+been cultivated in narrow stretches, with an open water<span class="tei tei-pb" id="page090">[pg 090]</span><a name="Pg090" id="Pg090" class="tei tei-anchor"></a>
+furrow between them; but it was now laid quite plain,
+by which one-eighth of the continuation of acreage has
+been saved. Not, however, being confident as to the
+soil having already become so porous as to dispense entirely
+with surface drains, Mr. Hammond had drawn
+two long water furrows diagonally across the field. On
+examining these, it appeared that very little water had
+flowed along any part of them during these 12 hours of
+rain,—no water had escaped at their outfall; the entire
+body of rain had permeated the mass of the bed, and
+passed off through the inch pipes; no water perceptible
+on the surface, which used to carry it throughout. The
+subsoil is a brick clay, but it appears to crack very
+rapidly by shrinkage consequent to drainage."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Obstructions.</span></span>—The danger that drains will become
+obstructed, if not properly laid out and properly made, is
+very great, and the cost of removing the obstructions,
+(often requiring whole lines to be taken up, washed, and
+relaid with the extra care that is required in working in
+old and soft lines,) is often greater than the original cost
+of the improvement. Consequently, the possibility of tile
+drains becoming stopped up should be fully considered
+at the outset, and every precaution should be taken to
+prevent so disastrous a result.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The principal causes of obstruction are <span class="tei tei-hi"><span style="font-style: italic">silt, vermin</span></span>, and
+<span class="tei tei-hi"><span style="font-style: italic">roots</span></span>.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Silt</span></span> is earth which is washed into the tile with the
+water of the soil, and which, though it may be carried
+along in suspension in the water, when the fall is good,
+will be deposited in the eddies and slack-water, which
+occur whenever there is a break in the fall, or a defect in
+the laying of the tile.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Whenever it is possible to avoid it, no drain should
+have a decreasing rate of fall as it approaches its outlet.</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the first hundred feet from the upper end of the<span class="tei tei-pb" id="page091">[pg 091]</span><a name="Pg091" id="Pg091" class="tei tei-anchor"></a>
+drain has a fall of three inches, the next hundred feet
+should not have less than three inches, lest the diminished
+velocity cause silt, which required the speed which that
+fall gives for its removal, to be deposited and to choke
+the tile. This defect of grade is shown in Fig. 17. If the
+second hundred feet has an inclination of <span class="tei tei-hi"><span style="font-style: italic">more</span></span> than
+three inches, (Fig. 18,) the removal of silt will be even better
+secured than if the fall continued at the original rate.
+Some silt will enter newly made drains, in spite of our
+utmost care, but the amount should be very slight, and
+if it is evenly deposited throughout the whole length of
+the drain, (as it sometimes is when the rate of fall is very
+low,) it will do no especial harm; but it becomes dangerous
+when it is accumulated within a short distance, by a
+decreasing fall, or by a single badly laid tile, or imperfect
+joint, which, by arresting the flow, may cause as much
+mischief as a defective grade.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Owing to the general conformation of the ground, it is
+sometimes absolutely necessary to adopt such a grade as
+is shown in Fig. 19,—even to the extent of bringing the
+drain down a rapid slope, and continuing it with the least
+possible fall through level ground. When such changes
+must be made, they should be effected by angles, and not
+by curves. In <span class="tei tei-hi"><span style="font-style: italic">increasing</span></span> the fall, curves in the grade are
+always advisable, in <span class="tei tei-hi"><span style="font-style: italic">decreasing</span></span> it they are always objectionable,
+except when the decreased fall is still considerable,—say,
+at least 2 feet in 100 feet. The reason for making
+an absolute angle at the point of depression is, that it
+enables us to catch the silt at that point in a silt basin,
+from which it may be removed as occasion requires.</p>
+
+<a name="fig23" id="fig23"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image19.png" width="640" height="257" alt="Illustration: Fig. 19 - THREE PROFILES OF DRAINS, WITH DIFFERENT INCLINATIONS." title="Fig. 19 - THREE PROFILES OF DRAINS, WITH DIFFERENT INCLINATIONS." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 19 - THREE PROFILES OF DRAINS, WITH DIFFERENT INCLINATIONS.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">A Silt Basin</span></span> is a chamber, below the grade of the drain,
+into which the water flows, becomes comparatively quiet,
+and deposits its silt, instead of carrying it into the tile
+beyond. It may be large or small, in proportion to the
+amount of drain above, which it has to accommodate. For
+a few hundred feet of the smallest tile, it may be only a<span class="tei tei-pb" id="page093">[pg 093]</span><a name="Pg093" id="Pg093" class="tei tei-anchor"></a>
+6-inch tile placed on end and sunk so as to receive and
+discharge the water at its top. For a large main, it may
+be a brick reservoir with a capacity of 2 or 3 cubic feet.
+The position of a silt basin is shown in Fig. 19.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The quantity of silt which enters the drain depends very
+much on the soil. Compact clays yield very little, and
+wet, running sands, (quicksands,) a great deal. In a soil
+of the latter sort, or one having a layer of running sand at
+the level of the drain, the ditch should be excavated a little
+below the grade of the drain, and then filled to that
+level with a retentive clay, and rammed hard. In all cases
+when the tile is well laid, (especially if collars are used,)
+and a stiff earth is well packed around the tile, silt will
+not enter the drain to an injurious extent, after a few
+months' operation shall have removed the loose particles
+about the joints, and especially after a few very heavy
+rains, which, if the tiles are small, will sometimes wash
+them perfectly clean, although they may have been half
+filled with dirt.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Vermin</span></span>,—field mice, moles, etc.,—sometimes make
+their nests in the tile and thus choke them, or, dying
+in them, stop them up with their carcases. Their entrance
+should be prevented by placing a coarse wire cloth
+or grating in front of the outlets, which afford the only
+openings for their entrance.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Roots.</span></span>—The roots of many water-loving trees,—especially
+willows,—will often force their entrance into the
+joints of the tile and fill the whole bore with masses of
+fibre which entirely prevent the flow of water. Collars
+make it more difficult for them to enter, but even these
+are not a sure preventive. Gisborne says:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"My own experience as to roots, in connection with
+deep pipe draining, is as follows: I have never known
+roots to obstruct a pipe through which there was not a
+perennial stream. The flow of water in summer and
+early autumn appears to furnish the attraction. I have<span class="tei tei-pb" id="page094">[pg 094]</span><a name="Pg094" id="Pg094" class="tei tei-anchor"></a>
+never discovered that the roots of any esculent vegetable
+have obstructed a pipe. The trees which, by my own
+personal observation, I have found to be most dangerous,
+have been red willow, black Italian poplar, alder,
+ash, and broad-leaved elm. I have many alders in close
+contiguity with important drains, and, though I have
+never convicted one, I cannot doubt that they are dangerous.
+Oak, and black and white thorns, I have not
+detected, nor do I suspect them. The guilty trees have
+in every instance been young and free growing; I have
+never convicted an adult. These remarks apply solely
+to my own observation, and may of course be much
+extended by that of other agriculturists. I know an instance
+in which a perennial spring of very pure and (I
+believe) soft water is conveyed in socket pipes to a
+paper mill. Every junction of two pipes is carefully
+fortified with cement. The only object of cover being
+protection from superficial injury and from frost, the
+pipes are laid not far below the sod. Year by year these
+pipes are stopped by roots. Trees are very capricious in
+this matter. I was told by the late Sir R. Peel that he
+sacrificed two young elm trees in the park at Drayton
+Manor to a drain which had been repeatedly stopped by
+roots. The stoppage was nevertheless repeated, and
+was then traced to an elm tree far more distant than
+those which had been sacrificed. Early in the autumn
+of 1850 I completed the drainage of the upper part of a
+boggy valley, lying, with ramifications, at the foot of
+marly banks. The main drains converge to a common
+outlet, to which are brought one 3-inch pipe and three of 4
+inches each. They lie side by side, and water flows perennially
+through each of them. Near to this outlet did
+grow a red willow. In February, 1852, I found the
+water breaking out to the surface of the ground about
+10 yards above the outlet, and was at no loss for the
+cause, as the roots of the red willow showed themselves<span class="tei tei-pb" id="page095">[pg 095]</span><a name="Pg095" id="Pg095" class="tei tei-anchor"></a>
+at the orifice of the 3-inch and of two of the 4-inch pipes.
+On examination I found that a root had entered a joint
+between two 3-inch pipes, and had traveled 5 yards to
+the mouth of the drain, and 9 yards up the stream,
+forming a continuous length of 14 yards. The root which
+first entered had attained about the size of a lady's little
+finger; and its ramifications consisted of very fine and
+almost silky fibres, and would have cut up into half a
+dozen comfortable boas. The drain was completely
+stopped. The pipes were not in any degree displaced.
+Roots from the same willow had passed over the 3-inch
+pipes, and had entered and entirely stopped the first
+4-inch drain, and had partially stopped the second. At
+a distance of about 50 yards a black Italian poplar,
+which stood on a bank over a 4-inch drain, had completely
+stopped it with a bunch of roots. The whole of
+this had been the work of less than 18 months, including
+the depth of two winters. A 3-inch branch of the same
+system runs through a little group of black poplars.
+This drain conveys a full stream in plashes of wet, and
+some water generally through the winter months, but
+has not a perennial flow. I have perceived no indication
+that roots have interfered with this drain. I draw
+no general conclusions from these few facts, but they
+may assist those who have more extensive experience in
+drawing some, which may be of use to drainers."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Having considered some of the principles on which our
+work should be based, let us now return to the map of the
+field, and apply those principles in planning the work to be
+done to make it dry.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Outlet</span></span> should evidently be placed at the present
+point of exit of the brook which runs from the springs,
+collects the water of the open ditches, and spreads over
+the flat in the southwest corner of the tract, converting
+it into a swamp. Suppose that, by going some distance
+into the next field, we can secure an outlet of 3 feet and<span class="tei tei-pb" id="page096">[pg 096]</span><a name="Pg096" id="Pg096" class="tei tei-anchor"></a>
+9 inches (3.75) below the level of the swamp, and that we
+decide to allow 3 inches drop between the bottom of the
+tile at that point, and the reduced level of the brook to
+secure the drain against the accumulation of sand, which
+might result from back water in time of heavy rain. This
+fixes the depth of drain at the outlet at 3-1/2 (3.50) feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">At that side of the swamp which lies nearest to the
+main depression of the up-land, (See Fig. 21,) is the proper
+place at which to collect the water from so much of
+the field as is now drained by the main brook, and at that
+point it will be well to place a <span class="tei tei-hi"><span style="font-style: italic">silt basin</span></span> or well, built up
+to the surface, which may, at any time, be uncovered for
+an observation of the working of the drains. The land
+between this point and the outlet is absolutely level, requiring
+the necessary fall in the drain which connects the
+two, to be gained by raising the upper end of it. As the
+distance is nearly 200 feet, and as it is advisable to give a
+fall at least five-tenths of a foot per hundred feet to so important
+an outlet as this, the drain at the silt basin may
+be fixed at only 2-1/2 feet. The basin being at the foot of
+a considerable rise in the ground, it will be easy, within a
+short distance above, to carry the drains which come to it
+to a depth of 4 feet,—were this not the case, the fall between
+the basin and the outlet would have to be very
+much reduced.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Main Drains.</span></span>—The valley through which the brook
+now runs is about 80 feet wide, with a decided rise in the
+land at each side. If one main drain were laid in the center
+of it, all of the laterals coming to the main would first
+run down a steep hillside, and then across a stretch of
+more level land, requiring the grade of each lateral to be
+broken at the foot of the hill, and provided with a silt
+basin to collect matters which might be deposited when
+the fall becomes less rapid. Consequently, it is best to
+provide two mains, or collecting drains, (<span class="tei tei-hi"><span style="font-style: italic">A</span></span> and <span class="tei tei-hi"><span style="font-style: italic">C</span></span>,) one
+lying at the foot of each hill, when they will receive the<span class="tei tei-pb" id="page097">[pg 097]</span><a name="Pg097" id="Pg097" class="tei tei-anchor"></a>
+laterals at their greatest fall; but, as these are too far
+apart to completely drain the valley between them, and
+are located on land higher than the center of the valley, a
+drain, (<span class="tei tei-hi"><span style="font-style: italic">B</span></span>,) should be run up, midway between them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The collecting drain, <span class="tei tei-hi"><span style="font-style: italic">A</span></span>, will receive the laterals from the
+hill to the west of it, as far up as the 10-foot contour line,
+and, above that point,—running up a branch of the valley,—it
+will receive laterals from both sides. The drain, <span class="tei tei-hi"><span style="font-style: italic">B</span></span>,
+may be continued above the dividing point of the valley,
+and will act as one of the series of laterals. The drain, <span class="tei tei-hi"><span style="font-style: italic">C</span></span>,
+will receive the laterals and sub-mains from the rising
+ground to the east of it, and from both sides of the minor
+valley which extends in that direction.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Most of the valley which runs up from the easterly side
+of the swamp must be drained independently by the drain
+<span class="tei tei-hi"><span style="font-style: italic">E</span></span>, which might be carried to the silt basin, did not its
+continuation directly to the outlet offer a shorter course
+for the removal of its water. This drain will receive laterals
+from the hill bordering the southeasterly side of the
+swamp, and, higher up, from both sides of the valley in
+which it runs.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In laying out these main drains, more attention should
+be given to placing them where they will best receive the
+water of the laterals, and on lines which offer a good and
+tolerably uniform descent, than to their use for the immediate
+drainage of the land through which they pass.
+Afterward, in laying out the laterals, the use of these lines
+as local drains should, of course, be duly considered.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Lateral Drains</span></span> should next receive attention, and
+in their location and arrangement the following rules
+should be observed:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1st. They should run down the steepest descent of the
+land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2d. They should be placed at intervals proportionate to
+their depth;—if 4 feet deep, at 40 feet intervals; if 3 feet
+deep, at 20 feet intervals.</p>
+
+<a name="fig24" id="fig24"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image20.png" width="640" height="832" alt="Illustration: Fig. 20 - MAP WITH DRAINS AND CONTOUR LINES." title="Fig. 20 - MAP WITH DRAINS AND CONTOUR LINES." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 20 - MAP WITH DRAINS AND CONTOUR LINES.</div></div>
+
+<span class="tei tei-pb" id="page099">[pg 099]</span><a name="Pg099" id="Pg099" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">3d. They should, as nearly as possible, run parallel to
+each other.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">On land of perfectly uniform character, (all sloping in
+the same direction,) all of these requirements may be
+complied with, but on irregular land it becomes constantly
+necessary to make a compromise between them. Drains
+running down the line of steepest descent cannot be parallel,—and,
+consequently, the intervals between them cannot
+be always the same; those which are farther apart at
+one end than at the other cannot be always of a depth
+exactly proportionate to their intervals.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the adjustment of the lines, so as to conform as nearly
+to these requirements as the shape of the ground will
+allow, there is room for the exercise of much skill, and on
+such adjustment depend, in a great degree, the success and
+economy of the work. Remembering that on the map, the
+line of steepest descent is exactly perpendicular to the contour
+lines of the land, it will be profitable to study carefully
+the system of drains first laid out, erasing and making
+alterations wherever it is found possible to simplify
+the arrangement.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Strictly speaking, all <span class="tei tei-hi"><span style="font-style: italic">angles</span></span> are, to a certain extent,
+wasteful, because, if two parallel drains will suffice to drain
+the land between them, no better drainage will be effected
+by a third drain running across that land. Furthermore,
+the angles are practically supplied with drains at less intervals
+than are required,—for instance, at <span class="tei tei-hi"><span style="font-style: italic">C 7 a</span></span> on the
+map the triangles included within the dotted line <span class="tei tei-hi"><span style="font-style: italic">x</span></span>, <span class="tei tei-hi"><span style="font-style: italic">y</span></span>,
+will be doubly drained. So, also, if any point of a
+4-foot drain will drain the land within 20 feet of it,
+the land included within the dotted line forming a
+semi-circle about the point <span class="tei tei-hi"><span style="font-style: italic">C 14</span></span>, might drain into the
+end of the lateral, and it no more needs the action of
+the main drain than does that which lies between the
+laterals. Of course, angles and connecting lines are indispensable,
+except where the laterals can run independently<span class="tei tei-pb" id="page100">[pg 100]</span><a name="Pg100" id="Pg100" class="tei tei-anchor"></a>
+across the entire field, and discharge beyond it.
+The longer the laterals can be made, and the more angles
+can be avoided, the more economical will the arrangement
+be; and, until the arrangement of the lines has been made
+as nearly perfect as possible, the time of the drainer can
+be in no way so profitably spent as in amending his plan.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The series of laterals which discharge through the
+mains <span class="tei tei-hi"><span style="font-style: italic">A</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, <span class="tei tei-hi"><span style="font-style: italic">D</span></span> and <span class="tei tei-hi"><span style="font-style: italic">E</span></span>, on the accompanying map, have
+been very carefully considered, and are submitted to the
+consideration of the reader, in illustration of what has
+been said above.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">At one point, just above the middle of the east side of
+the field, the laterals are placed at a general distance of
+20 feet, because, as will be seen by reference to Fig. 4, a
+ledge of rock, underground, will prevent their being made
+more than 3 feet deep.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The line from <span class="tei tei-hi"><span style="font-style: italic">H</span></span> to <span class="tei tei-hi"><span style="font-style: italic">I</span></span>, (Fig. 20,) at the north side of
+the field, connecting the heads of the laterals, is to be a
+stone and tile drain, such as is described on page 60, intended
+to collect the water which follows the surface of
+the rock. (See Fig. 4.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The swamp is to be drained by itself, by means of two
+series of laterals discharging into the main lines <span class="tei tei-hi"><span style="font-style: italic">F</span></span> and <span class="tei tei-hi"><span style="font-style: italic">G</span></span>,
+which discharge at the outlet, by the side of the main
+drain from the silt-basin. By this arrangement, these
+laterals, especially at the north side of the swamp, being
+accurately laid, with very slight inclinations, can be placed
+more deeply than if they ran in an east and west direction,
+and discharged into the main, which has a greater inclination,
+and is only two and a half feet deep at the basin.
+Being 3-1/2 (3.50) feet deep at the outlet, they may
+be made fully 3 feet deep at their upper ends, and, being
+only 20 feet apart, they will drain the land as well as is
+possible. The drains being now laid out, over the whole
+field, the next thing to be attended to is</p>
+
+<span class="tei tei-pb" id="page101">[pg 101]</span><a name="Pg101" id="Pg101" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Ordering of the Tile.</span></span>—The main line from the outlet
+up to the silt-basin, should be of 3-1/2-inch tiles, of which
+about 190 feet will be required. The main drain <span class="tei tei-hi"><span style="font-style: italic">A</span></span> should
+be laid with 2-1/4-inch tiles to the point marked <span class="tei tei-hi"><span style="font-style: italic">m</span></span>, near its
+upper end, as the lateral entering there carries the water
+of a spring, which is supposed to fill a 1-1/4-inch tile. The
+length of this drain, from the silt-basin to that point is
+575 feet. The main drain <span class="tei tei-hi"><span style="font-style: italic">C</span></span> will require 2-1/4 inch tiles from
+the silt-basin to the junction with the lateral, which is
+marked <span class="tei tei-hi"><span style="font-style: italic">C</span></span> 10, above which point there is about 1,700 feet
+of drain discharging into it, a portion of which, being a
+stone-and-tile drain at the foot of a rock, may be supposed
+to receive more water than that which lies under the rest
+of the land;—distance 450 feet. The main drain <span class="tei tei-hi"><span style="font-style: italic">E</span></span> requires
+2-1/4-inch tiles from the outlet to the point marked <span class="tei tei-hi"><span style="font-style: italic">o</span></span>, a distance
+of 380 feet. This tile will, in addition to its other
+work, carry as much water from the spring, on the line of
+its fourth lateral, as would fill a 1-1/4-inch pipe.<a id="noteref_12" name="noteref_12" href="#note_12"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">12</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The length of the main drains above the points indicated,
+and of all the laterals, amounts to about 12,250 feet.
+These all require 1-1/4-inch tiles.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Allowing about five per cent. for breakage, the order in
+round numbers, will be as follows:<a id="noteref_13" name="noteref_13" href="#note_13"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">13</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">3-1/2-inch round tiles 200 feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2-1/4-inch round tiles 1,500 feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1-1/4-inch round tiles 13,000 feet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">3-1/2-inch round tiles 1,600</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2-1/4-inch round tiles 13,250</p>
+
+<span class="tei tei-pb" id="page102">[pg 102]</span><a name="Pg102" id="Pg102" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Order, also, 25 6-inch sole-tiles, to be used in making
+small silt-basins.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It should be arranged to have the tiles all on the ground
+before the work of ditching commences, so that there may
+be no delay and consequent danger to the stability of the
+banks of the ditches, while waiting for them to arrive. As
+has been before stated, it should be especially agreed with
+the tile-maker, at the time of making the contract, that
+every tile should be perfect;—of uniform shape, and
+neither too much nor too little burned.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Staking Out.</span></span>—Due consideration having been given to
+such preliminaries as are connected with the mapping of
+the ground, and the arrangement, on paper, of the drains
+to be made, the drainer may now return to his field, and,
+while awaiting the arrival of his tiles, make the necessary
+preparation for the work to be done. The first step is to
+fix certain prominent points, which will serve to connect
+the map with the field, by actual measurements, and this
+will very easily be done by the aid of the stakes which
+are still standing at the intersections of the 50-foot lines,
+which were used in the preliminary levelling.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Commencing at the southwest corner of the field, and
+measuring toward the east a distance of 34 feet, set a pole
+to indicate the position of the outlet. Next, mark the
+center of the silt-basin at the proper point, which will be
+found by measuring 184 feet up the western boundary, and
+thence toward the east 96 feet, on a line parallel with the
+nearest row of 50-foot stakes. Then, in like manner, fix
+the points <span class="tei tei-hi"><span style="font-style: italic">C1</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C6</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C9</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C10</span></span>, and <span class="tei tei-hi"><span style="font-style: italic">C17</span></span>, and the angles
+of the other main lines, marking the stakes, when placed,
+to correspond with the same points on the map. Then
+stake the angles and the upper ends of the laterals, and
+mark these stakes to correspond with the map.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It will greatly facilitate this operation, if the plan of
+the drains which is used in the field, from which the horizontal<span class="tei tei-pb" id="page103">[pg 103]</span><a name="Pg103" id="Pg103" class="tei tei-anchor"></a>
+lines should be omitted, have the intersecting 50-foot
+lines drawn upon it, so that the measurements may
+be made from the nearest points of intersection.<a id="noteref_14" name="noteref_14" href="#note_14"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">14</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Having staked these guiding points of the drains, it is
+advisable to remove all of the 50-foot stakes, as these are
+of no further use, and would only cause confusion. It
+will now be easy to set the remaining stakes,—placing one
+at every 50 feet of the laterals, and at the intersections
+of all the lines.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A system for marking the stakes is indicated on the
+map, (in the <span class="tei tei-hi"><span style="font-style: italic">C</span></span> series of drains,) which, to avoid the confusion
+which would result from too much detail on such a
+small scale, has been carried only to the extent necessary
+for illustration. The stakes of the line <span class="tei tei-hi"><span style="font-style: italic">C</span></span> are marked <span class="tei tei-hi"><span style="font-style: italic">C1</span></span>,
+<span class="tei tei-hi"><span style="font-style: italic">C2</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C3</span></span>, etc. The stakes of the sub-main <span class="tei tei-hi"><span style="font-style: italic">C7</span></span>, are marked
+<span class="tei tei-hi"><span style="font-style: italic">C7a</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C7b</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C7c</span></span>, etc. The stakes of the lateral which
+enters this drain at <span class="tei tei-hi"><span style="font-style: italic">C7a</span></span>, are marked <span class="tei tei-hi"><span style="font-style: italic">C7a/1</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C7a/2</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C7a/3,</span></span> etc.
+etc. This system, which connects the lettering of each
+lateral with its own sub-main and main, is perfectly simple,
+and avoids the possibility of confusion. The position
+of the stakes should all be lettered on the map, at the
+original drawing, and the same designating marks put on
+the stakes in the field, as soon as set.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Grade Stakes</span></span>, (pegs about 8 or 10 inches long,) should
+be placed close at the sides of the marked stakes, and
+driven nearly their full length into the ground. The tops
+of these stakes furnish fixed points of elevation from
+which to take the measurements, and to make the computations
+necessary to fix the depth of the drain at each
+stake. If the measurements were taken from the surface
+of the ground, a slight change of position in placing the
+instrument, would often make a difference of some inches
+in the depth of the drain.</p>
+
+<span class="tei tei-pb" id="page104">[pg 104]</span><a name="Pg104" id="Pg104" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Taking the Levels.</span></span>—For accurate work, it is necessary
+to ascertain the comparative levels of the tops of all of
+the grade stakes; or the distance of each one of them
+below an imaginary horizontal plane. This plane, (in which
+we use only such lines as are directly above the drains,)
+may be called the "Datum Line." Its elevation should
+be such that it will be above the highest part of the land,
+and, for convenience, it is fixed at the elevation of the levelling
+instrument when it is so placed as to look over the
+highest part of the field.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Levelling Instruments</span></span> are of various kinds. The best
+for the work in hand, is the common railroad level, which
+is shown in Fig. 6. This is supported on three legs, which
+bring it to about the level of the eye. Its essential parts
+are a telescope, which has two cross-hairs intersecting each
+other in the line of sight, and which may be turned on its
+pivot toward any point of the horizon; a bubble glass
+placed exactly parallel to the line of sight, and firmly
+secured in its position so as to turn with the telescope;
+and an apparatus for raising or depressing any side of the
+instrument by means of set-screws. The instrument is
+firmly screwed to the tripod, and placed at a point convenient
+for looking over a considerable part of the highest
+land. By the use of the set-screws, the plane in which the
+instrument revolves is brought to a level, so that in whatever
+direction the instrument is pointed, the bubble will be
+in the center of the glass. The line of sight, whichever
+way it is turned, is now in our imaginary plane. A convenient
+position for the instrument in the field under consideration,
+would be at the point, east of the center, marked
+<span class="tei tei-hi"><span style="font-style: italic">K</span></span>, which is about 3 feet below the level of the highest
+part of the ground. The telescope should stand about 5
+feet above the surface of the ground directly under it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">The Levelling-Rod</span></span>, (See Fig. 7,) is usually 12 feet long,
+is divided into feet and hundredths of a foot, and has a<span class="tei tei-pb" id="page105">[pg 105]</span><a name="Pg105" id="Pg105" class="tei tei-anchor"></a>
+movable target which may be placed at any part of its
+entire length. This is carried by an attendant, who holds
+it perpendicularly on the top of the grade-stake, while the
+operator, looking through the telescope, directs him to
+move the target up and down until its center is exactly in
+the line of sight. The attendant then reads the elevation,
+and the operator records it as the distance below the
+<span class="tei tei-hi"><span style="font-style: italic">datum-line</span></span> of the top of the grade-stake. For convenience,
+the letterings of the stakes should be systematically
+entered in a small field book, before the work commences,
+and this should be accompanied by such a sketch of the
+plan as will serve as a guide to the location of the lines on
+the ground.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The following is the form of the field book for the main
+drain <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, with the levels recorded:</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="2"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Lettering of the Stake</span></span>.</td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Depth from Datum Line</span></span>.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Silt Basin</td><td class="tei tei-cell">18.20</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 1</td><td class="tei tei-cell">15.44</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 2</td><td class="tei tei-cell">14.36</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 3</td><td class="tei tei-cell">12.85</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 4</td><td class="tei tei-cell">12.18</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 5</td><td class="tei tei-cell">11.79</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 6</td><td class="tei tei-cell">11.69</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 7</td><td class="tei tei-cell">11.55</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 8</td><td class="tei tei-cell">11.37</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 9</td><td class="tei tei-cell">11.06</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 10</td><td class="tei tei-cell">8.94</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 11</td><td class="tei tei-cell">8.52</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 12</td><td class="tei tei-cell">7.86</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 13</td><td class="tei tei-cell">7.70</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 14</td><td class="tei tei-cell">7.39</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 15</td><td class="tei tei-cell">7.06</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C 16</td><td class="tei tei-cell">6.73</td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The levelling should be continued in this manner, until
+the grades of all the points are recorded in the field book.</p>
+
+<a name="fig25" id="fig25"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image21.png" width="640" height="354" alt="Illustration: Fig. 21 - PROFILE OF DRAIN C." title="Fig. 21 - PROFILE OF DRAIN C." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 21 - PROFILE OF DRAIN C.</div><p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em">Horizontal Scale, 66 ft. to the inch.<br />
+Vertical Scale, 15 ft. to the inch.<br /><br />
+1 to 17. Numbers of Stakes.<br />
+(82) etc. Distances between Stakes.<br />
+18.20 etc. Depths from <span class="tei tei-hi" style="text-align: center"><span style="font-style: italic">datum-line</span></span> to surface.<br />
+2.50 etc. Depths of ditch.<br />
+20.70 etc. Depths from <span class="tei tei-hi" style="text-align: center"><span style="font-style: italic">datum-line</span></span> to drain.</p></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If, from too great depression of the lower parts of the
+field, or too great distances for observation, it becomes
+necessary to take up a new position with the instrument,
+the new level should be connected, by measurement, with<span class="tei tei-pb" id="page107">[pg 107]</span><a name="Pg107" id="Pg107" class="tei tei-anchor"></a>
+the old one, and the new observations should be computed
+to the original plane.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is not necessary that these levels should be noted on
+the map,—they are needed only for computing the depth
+of cutting, and if entered on the map, might be mistaken
+for the figures indicating the depth, which it is more important
+to have recorded in their proper positions, for convenience
+of reference during the work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Depth and Grade of the Drains.</span></span>—Having now
+staked out the lines upon the land, and ascertained and
+recorded the elevations at the different stakes, it becomes
+necessary to determine at what depth the tile shall be
+placed at each point, so as to give the proper fall to each
+line, and to bring all of the lines of the system into accord.
+As the simplest means of illustrating the principle on
+which this work should be done, it will be convenient to
+go through with the process with reference to the main
+drain <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, of the plan under consideration. A profile of this
+line is shown in Fig. 21, where the line is broken at stake
+No. 7, and continued in the lower section of the diagram.
+The topmost line, from "Silt Basin" to "17," is the horizontal
+datum-line. The numbers above the vertical lines indicate
+the stakes; the figures in brackets between these, the
+number of feet between the stakes; and the heavy figures
+at the left of the vertical lines, the recorded measurements
+of depth from the datum-line to the surface of the ground,
+which is indicated by the irregular line next below the
+datum-line. The vertical measurements are, of course,
+very much exaggerated, to make the profile more marked,
+but they are in the proper relation to each other.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The depth at the silt-basin is fixed at 2-1/2 feet (2.50.)
+The rise is rapid to stake 3, very slight from there to stake
+7, very rapid from there to stake 10, a little less rapid from
+there to stake 11, and still less rapid from there to
+stake 17.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">To establish the grade by the profile alone, the proper<span class="tei tei-pb" id="page108">[pg 108]</span><a name="Pg108" id="Pg108" class="tei tei-anchor"></a>
+course would be to fix the depth at the stakes at which
+the inclination is to be changed, to draw straight lines between
+the points thus found, and then to measure the
+vertical distance from these lines to the line indicating the
+surface of the ground at the different stakes; thus, fixing
+the depth at stake 3, at 4 feet and 13 hundredths,<a id="noteref_15" name="noteref_15" href="#note_15"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">15</span></span></a> the line
+drawn from that point to the depth of 2.50, at the silt-basin,
+will be 3 feet and 62 hundredths (3.62) below stake
+1, and 3 feet and 92 hundredths (3.92) below stake 2. At
+stake 7 it is necessary to go sufficiently deep to pass from 7
+to 10, without coming too near the surface at 9, which is at
+the foot of a steep ascent. A line drawn straight from
+4.59 feet below stake 10 to 4.17 feet at stake 17, would be
+unnecessarily deep at 11, 12, 13, and 14; and, consequently
+it is better to rise to 4.19 feet at 11. So far as
+this part of the drain is concerned, it would be well to
+continue the same rise to 12, but, in doing so, we would
+come too near the surface at 13, 14, and 15; or must considerably
+depress the line at 16, which would either make
+a bad break in the fall at that point, or carry the drain
+too deep at 17.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">By the arrangement adopted, the grade is broken at 3,
+7, 10, and 11. Between these points, it is a straight line, with
+the rate of fall indicated in the following table, which
+commences at the upper end of the drain and proceeds toward
+its outlet:</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="6"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">From Stake, Depth.</span></span></td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">To Stake, Depth.</span></span></td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Distance</span></span>.</td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Total Fall</span></span>.</td><td class="tei tei-cell"><span class="tei tei-hi"><span style="font-variant: small-caps">Rate of Fall. Per 100 Ft.</span></span></td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">No. 17...4.17 ft.</td><td class="tei tei-cell">No. 11...4.19 ft.</td><td class="tei tei-cell">246 ft.</td><td class="tei tei-cell">2.46 ft.</td><td class="tei tei-cell">1.09 ft.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">No. 11...4.19 ft.</td><td class="tei tei-cell">No. 10...4.59 ft.</td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell">82 ft.</td><td class="tei tei-cell">2.00 ft.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">No. 10...4.59 ft.</td><td class="tei tei-cell">No. 7...4.47 ft.</td><td class="tei tei-cell">91 ft.</td><td class="tei tei-cell">2.49 ft.</td><td class="tei tei-cell">2.83 ft.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">No. 7...4.47 ft.</td><td class="tei tei-cell">No. 3...4.13 ft.</td><td class="tei tei-cell">173 ft.</td><td class="tei tei-cell">96 ft.</td><td class="tei tei-cell">56 ft.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">No. 3...4.13 ft.</td><td class="tei tei-cell">S. Basin 2.25 ft.</td><td class="tei tei-cell">186 ft.</td><td class="tei tei-cell">3.47 ft.</td><td class="tei tei-cell">1.87 ft.</td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It will be seen that the fall becomes more rapid as we
+ascend from stake 7, but below this point it is very much<span class="tei tei-pb" id="page109">[pg 109]</span><a name="Pg109" id="Pg109" class="tei tei-anchor"></a>
+reduced, so much as to make it very likely that silt will
+be deposited, (see page 91), and the drain, thereby, obstructed.
+To provide against this, a silt-basin must be
+placed at this point which will collect the silt and prevent
+its entrance into the more nearly level tile below. The
+construction of this silt-basin is more particularly described
+in the next chapter. From stake 7 to the main silt-basin
+the fall is such that the drain will clear itself.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The drawing of regular profiles, for the more important
+drains, will be useful for the purpose of making the beginner
+familiar with the method of grading, and with the
+principles on which the grade and depth are computed;
+and sometimes, in passing over very irregular surfaces, this
+method will enable even a skilled drainer to hit upon the
+best adjustment in less time than by computation. Ordinarily,
+however, the form of computation given in the following
+table, which refers to the same drain, (<span class="tei tei-hi"><span style="font-style: italic">C</span></span>,) will be
+more expeditious, and its results are mathematically more
+correct.<a id="noteref_16" name="noteref_16" href="#note_16"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">16</span></span></a></p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="8"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell">Fall. Feet and Decimals.</td><td class="tei tei-cell"></td><td class="tei tei-cell">Depth from Datum Line.</td><td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">No. of Stake.</td><td class="tei tei-cell">Distance Between Stakes.</td><td class="tei tei-cell">Per 100 Feet.</td><td class="tei tei-cell">Between Stakes.</td><td class="tei tei-cell">To Drain.</td><td class="tei tei-cell">To Surface.</td><td class="tei tei-cell">Depth of Drain.</td><td class="tei tei-cell">Remarks.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Silt Basin.</td><td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell"></td><td class="tei tei-cell">20.70 ft.</td><td class="tei tei-cell">18.20 ft.</td><td class="tei tei-cell">2.50 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 1. </td><td class="tei tei-cell"> 82 ft. </td><td class="tei tei-cell"> 2 ft.</td><td class="tei tei-cell">1.64 ft.</td><td class="tei tei-cell">19.06 "</td><td class="tei tei-cell">15.44 "</td><td class="tei tei-cell">3.48 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 2. </td><td class="tei tei-cell">39 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .78 ft. </td><td class="tei tei-cell">18.28 "</td><td class="tei tei-cell">14.36 "</td><td class="tei tei-cell">3.83 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 3. </td><td class="tei tei-cell">65 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell">1.30 ft. </td><td class="tei tei-cell">16.98 "</td><td class="tei tei-cell">12.85 "</td><td class="tei tei-cell">4.13 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 4. </td><td class="tei tei-cell">51 ft.</td><td class="tei tei-cell">.56 </td><td class="tei tei-cell"> .28 ft. </td><td class="tei tei-cell">16.70 "</td><td class="tei tei-cell">12.18 "</td><td class="tei tei-cell">4.52 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 5. </td><td class="tei tei-cell">43 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .24 ft. </td><td class="tei tei-cell">16.46 "</td><td class="tei tei-cell">11.79 "</td><td class="tei tei-cell">4.67 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 6. </td><td class="tei tei-cell">47 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .26 ft. </td><td class="tei tei-cell">16.20 "</td><td class="tei tei-cell">11.69 "</td><td class="tei tei-cell">4.51 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 7. </td><td class="tei tei-cell">32 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .18 ft. </td><td class="tei tei-cell">16.02 "</td><td class="tei tei-cell">11.55 "</td><td class="tei tei-cell">4.47 ft </td><td class="tei tei-cell">Silt-Basin here. Made deep at Nos. 7 and 10 to pass a depression of the surface at No. 9.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 8. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell"> 2.83 </td><td class="tei tei-cell">1.16 ft. </td><td class="tei tei-cell">14.86 "</td><td class="tei tei-cell">11.37 "</td><td class="tei tei-cell">3.49 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C. 9. </td><td class="tei tei-cell">12 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .34 ft. </td><td class="tei tei-cell">14.52 "</td><td class="tei tei-cell">11.06 "</td><td class="tei tei-cell">3.46 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.10. </td><td class="tei tei-cell">38 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .99 ft. </td><td class="tei tei-cell">13.53 "</td><td class="tei tei-cell"> 8.94 "</td><td class="tei tei-cell">4.59 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.11. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell"> 2.00 </td><td class="tei tei-cell"> .82 ft. </td><td class="tei tei-cell">12.61 "</td><td class="tei tei-cell"> 8.52 "</td><td class="tei tei-cell">4.19 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.12. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell"> 1.09 </td><td class="tei tei-cell"> .44 ft. </td><td class="tei tei-cell">12.27 "</td><td class="tei tei-cell"> 7.86 "</td><td class="tei tei-cell">4.41 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.13. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .44 ft. </td><td class="tei tei-cell">11.83 "</td><td class="tei tei-cell"> 7.70 "</td><td class="tei tei-cell">4.13 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.14. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .44 ft. </td><td class="tei tei-cell">11.39 "</td><td class="tei tei-cell"> 7.39 "</td><td class="tei tei-cell">4.00 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.15. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .44 ft. </td><td class="tei tei-cell">10.95 "</td><td class="tei tei-cell"> 7.06 "</td><td class="tei tei-cell">3.89 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.16. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .44 ft. </td><td class="tei tei-cell">10.51 "</td><td class="tei tei-cell"> 6.73 "</td><td class="tei tei-cell">3.88 ft </td><td class="tei tei-cell"></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">C.17. </td><td class="tei tei-cell">41 ft.</td><td class="tei tei-cell">do. </td><td class="tei tei-cell"> .44 ft. </td><td class="tei tei-cell">10.07 "</td><td class="tei tei-cell"> 5.90 "</td><td class="tei tei-cell">4.17 ft </td><td class="tei tei-cell"></td>
+</tr></tbody></table>
+
+<span class="tei tei-pb" id="page110">[pg 110]</span><a name="Pg110" id="Pg110" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-variant: small-caps">Note.</span></span>—The method of making the foregoing computation
+is this:</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">1st. Enter the lettering of the stakes in the first column, commencing
+at the lower end of the drain.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">2d. Enter the distances between each two stakes in the second column,
+placing the measurement on the line with the number of the
+</span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">upper</span></span><span style="font-size: 90%"> stake of the two.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">3d. In the next to the last column enter, on the line with each stake,
+its depth below the datum-line, as recorded in the field book of levels,
+(See page 105.)</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">4th. On the first line of the last column, place the depth of the lower
+end of the drain, (this is established by the grade of the main or other
+outlet at which it discharges.)</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">5th. Add this depth to the first number of the line next preceding it,
+and enter the sum obtained on the first line of the fifth column, as the
+depth of the </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">drain</span></span><span style="font-size: 90%"> below the datum-line.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">6th. Having reference to the grade of the surface, (as shown by the
+figures in the sixth column,) as well as to any necessity for placing the
+drain at certain depths at certain places, enter the desired depth, </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">in pencil,</span></span><span style="font-size: 90%">
+in the last column, opposite the stakes marking those places. Then add
+together this depth and the corresponding surface measurement in the
+column next preceding, and enter the sum, </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">in pencil</span></span><span style="font-size: 90%">, in the fifth column,
+as the depth from the datum-line to the desired position of the drain.
+(In the example in hand, these points are at Nos. 3, 7, 10, 11, and 17.)</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">7th. Subtract the second amount in the fifth column from the first
+amount for the total fall between the two points—in the example, "3"
+from "Silt-Basin." Divide this total fall, (in feet and hundredths,) by
+one hundredth of the total number of feet between them. The result
+will be the rate of fall per 100 feet, and this should be entered, in the
+third column, opposite each of the intermediate distances between the
+points.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">Example:</span></p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 0.90em"><colgroup span="2"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Depth of the Drain at the Silt-Basin</span></td><td class="tei tei-cell"><span style="font-size: 90%">20.45 feet.</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Depth of the Drain at the Stake No. 3</span></td><td class="tei tei-cell"><span style="font-size: 90%">16.98 feet.</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"></td><td class="tei tei-cell"><span style="font-size: 90%">——</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Difference</span></td><td class="tei tei-cell"><span style="font-size: 90%">3.47 feet.</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Distance between the two</span></td><td class="tei tei-cell"><span style="font-size: 90%">186.— feet.</span></td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">1.86)3.47(1.865 or 1.87</span></p>
+<p class="tei tei-p" style="text-align: right; margin-bottom: 0.90em"><span style="font-size: 90%">1 86</span><br /><span style="font-size: 90%">
+——</span><br /><span style="font-size: 90%">
+1 610</span><br /><span style="font-size: 90%">
+1 488</span><br /><span style="font-size: 90%">
+——</span><br /><span style="font-size: 90%">
+1 220</span><br /><span style="font-size: 90%">
+1 116</span><br /><span style="font-size: 90%">
+——</span><br /><span style="font-size: 90%">
+1 040</span><br /><span style="font-size: 90%">
+930</span><br /><span style="font-size: 90%">
+——</span><br /><span style="font-size: 90%">
+110</span></p>
+
+<span class="tei tei-pb" id="page111">[pg 111]</span><a name="Pg111" id="Pg111" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">8th. Multiply the numbers of the second column by those of the third
+and divide the product by 100. The result will be the amount of fall between
+the stakes, (fourth column.)—Example: 1.87×82=153÷100=1.53.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">9th. Subtract the first number of the fourth column from the first
+number of the fifth column, (on the line above it,) and place the remainder
+on the next line of the fifth column.—Example: 20.70-1.64=
+19.06.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">Then, from this new amount, subtract the second number of the
+fourth column, for the next number of the fifth, and so on, until, in
+place of the entry in pencil, (Stake 3,) we place the exact result of the
+computation.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">Proceed in like manner with the next interval,—3 to 7.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">10th. Subtract the numbers in the sixth column from those in the
+fifth, and the remainders will be the depths to be entered in the last.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">Under the head of "Remarks," note any peculiarity of the drain
+which may require attention in the field.</span></p>
+</div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The main lines <span class="tei tei-hi"><span style="font-style: italic">A</span></span>, <span class="tei tei-hi"><span style="font-style: italic">D</span></span>, and <span class="tei tei-hi"><span style="font-style: italic">E</span></span>, and the drain <span class="tei tei-hi"><span style="font-style: italic">B</span></span>, should
+next be graded on the plan set forth for <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, and their laterals,
+all of which have considerable fall, and being all so
+steep as not to require silt-basins at any point,—can, by
+a very simple application of the foregoing principles, be
+adjusted at the proper depths. In grading the stone and
+tile drain, (<span class="tei tei-hi"><span style="font-style: italic">H, I</span></span>,) it is only necessary to adopt the depth of
+the last stakes of the laterals, with which it is connected,
+as it is immaterial in which direction the water flows. The
+ends of this drain,—from H to the head of the drain <span class="tei tei-hi"><span style="font-style: italic">C10</span></span>,
+and from <span class="tei tei-hi"><span style="font-style: italic">I</span></span> to the head of <span class="tei tei-hi"><span style="font-style: italic">C17</span></span>,—should, of course, have a
+decided fall toward the drains.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The laterals which are placed at intervals of 20 feet,
+over the underground rock on the east side of the field,
+should be continued at a depth of about 3 feet for nearly
+their whole length, dropping in a distance of 8 or 10 feet
+at their lower ends to the top of the tile of the main. The
+intervals between the lower ends of <span class="tei tei-hi"><span style="font-style: italic">C7c</span></span>, <span class="tei tei-hi"><span style="font-style: italic">C7d</span></span>, and <span class="tei tei-hi"><span style="font-style: italic">C7e</span></span>,
+being considerably more than 20 feet, the drains may be
+gradually deepened, throughout their whole length from 3
+feet at the upper ends to the depth of the top of the main
+at the lower ends.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The main drains <span class="tei tei-hi"><span style="font-style: italic">F</span></span> and <span class="tei tei-hi"><span style="font-style: italic">G</span></span>, being laid in flat land, their<span class="tei tei-pb" id="page112">[pg 112]</span><a name="Pg112" id="Pg112" class="tei tei-anchor"></a>
+outlets being fixed at a depth of 3.50, (the floor of the
+main outlet,) and it being necessary to have them as deep
+as possible throughout their entire length, should be
+graded with great care on the least admissible fall. This,
+in ordinary agricultural drainage, may be fixed at .25, or
+3 inches, per 100 feet. Their laterals should commence
+with the top of their 1/4 tile even with the top of the 2-1/2 collar
+of the main,—or .15 higher than the grade of the main,—and
+rise, at a uniform inclination of .25, to the upper end.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Having now computed the depth at which the tile is to
+lie, at each stake, and entered it on the map, we are ready
+to mark these depths on their respective stakes in the field,
+when the preliminary engineering of the work will be
+completed.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It has been deemed advisable in this chapter to consider
+the smallest details of the work of the draining engineer.
+Those who intend to drain in the best manner will find
+such details important. Those who propose to do their
+work less thoroughly, may still be guided by the principles
+on which they are based. Any person who will
+take the pains to mature the plans of his work as closely
+as has been here recommended, will as a consequence
+commence his operations in the field much more understandingly.
+The advantage of having everything decided
+beforehand,—so that the workmen need not be delayed for
+want of sufficient directions, and of making, on the map,
+such alterations as would have appeared necessary in the
+field, thus saving the cost of cutting ditches in the wrong
+places, will well repay the work of the evenings of a
+whole winter.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page113">[pg 113]</span><a name="Pg113" id="Pg113" class="tei tei-anchor"></a>
+<a name="toc26" id="toc26"></a>
+<a name="pdf27" id="pdf27"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER IV. - HOW TO MAKE THE DRAINS.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Knowing, now, precisely what is to be done; having
+the lines all staked out, and the stakes so marked as to be
+clearly designated; knowing the precise depth at which
+the drain is to be laid, at every point; having the requisite
+tiles on the ground, and thoroughly inspected, the operator
+is prepared to commence actual work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">He should determine how many men he will employ,
+and what tools they will require to work to advantage. It
+may be best that the work be done by two or three
+men, or it may be advisable to employ as many as can
+work without interfering with each other. In most cases,—especially
+where there is much water to contend with,—the
+latter course will be the most economical, as the ditches
+will not be so liable to be injured by the softening of their
+bottoms, and the caving in of their sides.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Tools Required</span></span> are a subsoil plow, two garden
+lines, spades, shovels, and picks; narrow finishing spades,
+a finishing scoop, a tile pick, a scraper for filling the
+ditches, a heavy wooden maul for compacting the bottom
+filling, half a dozen boning-rods, a measuring rod, and a
+plumb rod. These should all be on hand at the outset, so
+that no delay in the work may result from the want of
+them.</p>
+
+<a name="fig28" id="fig28"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image22.png" width="640" height="832" alt="Illustration: Fig. 22 - SET OF TOOLS." title="Fig. 22 - SET OF TOOLS." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 22 - SET OF TOOLS.</div><p class="tei tei-p" style="text-align: center; margin-bottom: 1.00em">Flat Spades of
+various lengths
+and widths, Bill-necked
+Scoop (<span class="tei tei-hi" style="text-align: center"><span style="font-style: italic">A</span></span>);
+Tile-layer (<span class="tei tei-hi" style="text-align: center"><span style="font-style: italic">B</span></span>);
+Pick-axe (<span class="tei tei-hi" style="text-align: center"><span style="font-style: italic">C</span></span>); and
+Scoop Spades, and
+Shovel.</p></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Writers on drainage, almost without exception, recommend
+the use of elaborate sets of tools which are intended<span class="tei tei-pb" id="page115">[pg 115]</span><a name="Pg115" id="Pg115" class="tei tei-anchor"></a>
+for cutting very narrow ditches,—only wide enough at the
+bottom to admit the tile, and not allowing the workmen
+to stand in the bottom of the ditch. A set of these tools
+is shown in Fig. 22.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Possibly there may be soils in which these implements,
+in the hands of men skilled in their use, could be employed
+with economy, but they are very rare, and it is not believed
+to be possible, under any circumstances, to regulate
+the bottom of the ditch so accurately as is advisable, unless
+the workman can stand directly upon it, cutting it
+more smoothly than he could if the point of his tool were
+a foot or more below the level on which he stands.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">On this subject, Mr. J. Bailey Denton, one of the first
+draining engineers of Great Britain, in a letter to Judge
+French, says:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"As to tools, it is the same with them as it is with the
+art of draining itself,—too much rule and too much drawing
+upon paper; all very right to begin with, but very
+prejudicial to progress. I employ, as engineer to the
+General Land Drainage Company, and on my private
+account, during the drainage season, as many as 2,000
+men, and it is an actual fact, that not one of them uses
+the set of tools figured in print. I have frequently purchased
+a number of sets of the Birmingham tools, and
+sent them down on extensive works. The laborers would
+purchase a few of the smaller tools, such as Nos. 290,
+291, and 301, figured in Morton's excellent Cyclopædia
+of Agriculture, and would try them, and then order
+others of the country blacksmith, differing in several
+respects; less weighty and much less costly, and moreover,
+much better as working tools. All I require of the
+cutters, is, that the bottom of the drain should be evenly
+cut, to fit the size of the pipe. The rest of the work
+takes care of itself; for a good workman will economize
+his labor for his own sake, by moving as little earth as
+practicable; thus, for instance, a first-class cutter, in<span class="tei tei-pb" id="page116">[pg 116]</span><a name="Pg116" id="Pg116" class="tei tei-anchor"></a>
+clays, will get down 4 feet with a 12-inch opening, <span class="tei tei-hi"><span style="font-style: italic">ordinarily</span></span>;
+if he wishes to <span class="tei tei-hi"><span style="font-style: italic">show off</span></span>, he will sacrifice his
+own comfort to appearance, and will do it with a 10-inch
+opening."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the Central Park work, sets of these tools were procured,
+at considerable expense, and every effort was made
+to compel the men to use them, but it was soon found that,
+even in the easiest digging, there was a real economy in
+using, for the first 3 feet of the ditch, the common spade,
+pick, and shovel,—finishing the bottoms with the narrow
+spade and scoop hereafter described, and it is probable
+that the experience of that work will be sustained by that
+of the country at large.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Marking the Lines.</span></span>—To lay a drain directly under the
+position of its stakes, would require that enough earth be
+left at each point to hold the stake, and that the ditch be
+tunneled under it. This is expensive and unnecessary. It
+is better to dig the ditches at one side of the lines of
+stakes, far enough away for the earth to hold them
+firmly in their places, but near enough to allow measurements
+to be taken from the grade pegs. If the ditch be
+placed always to the right, or always to the left, of the line,
+and at a uniform distance, the general plan will remain the
+same, and the lines will be near enough to those marked
+on the map to be easily found at any future time. In fact,
+if it be known that the line of tiles is two feet to the right
+of the position indicated, it will only be necessary, at any
+time, should it be desired to open an old drain, to
+measure two feet to the right of the surveyed position to
+strike the line at once.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In soils of ordinary tenacity, ditches 4 feet deep need
+not be more than twenty (20) inches wide at the surface,
+and four (4) inches wide at the bottom. This will allow,
+in each side, a slope of eight (8) inches, which is sufficient
+except in very loose soils, and even these may be braced
+up, if inclined to cave in. There are cases where the soil<span class="tei tei-pb" id="page117">[pg 117]</span><a name="Pg117" id="Pg117" class="tei tei-anchor"></a>
+contains so much running sand, and is so saturated with
+water, that no precautions will avail to keep up the banks.
+Ditches in such ground will sometimes fall in, until the excavation
+reaches a width of 8 or 10 feet. Such instances,
+however, are very rare, and must be treated as the occasion
+suggests.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">One of the garden lines should be set at a distance of
+about 6 inches from the row of stakes, and the other at a
+further distance of 20 inches. If the land is in grass, the
+position of these lines may be marked with a spade, and
+they may be removed at once; but, if it is arable land, it
+will be best to leave the lines in position until the ditch is
+excavated to a sufficient depth to mark it clearly. Indeed,
+it will be well to at once remove all of the sod and surface
+soil, say to a depth of 6 inches, (throwing this on the same
+side with the stakes, and back of them.) The whole force
+can be profitably employed in this work, until all of the
+ditches to be dug are scored to this depth over the entire
+tract to be drained, except in swamps which are still too
+wet for this work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Water Courses.</span></span>—The brooks which carry the water
+from the springs should be "jumped" in marking out
+the lines, as it is desirable that their water be kept in separate
+channels, so far as possible, until the tiles are ready
+to receive it, as, if allowed to run in the open ditches, it
+would undermine the banks and keep the bottom too soft
+for sound work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">With this object, commence at the southern boundary
+of our example tract, 10 or 15 feet east of the point of
+outlet, and drive a straight, temporary, shallow ditch to a
+point a little west of the intersection of the main line <span class="tei tei-hi"><span style="font-style: italic">D</span></span>
+with its first lateral; then carry it in a northwesterly
+direction, crossing <span class="tei tei-hi"><span style="font-style: italic">C</span></span> midway between the silt-basin and
+stake <span class="tei tei-hi"><span style="font-style: italic">C 1</span></span>, and thence into the present line of the brook,
+turning all of the water into the ditch. A branch of this<span class="tei tei-pb" id="page118">[pg 118]</span><a name="Pg118" id="Pg118" class="tei tei-anchor"></a>
+ditch may be run up between the lines <span class="tei tei-hi"><span style="font-style: italic">F</span></span> and <span class="tei tei-hi"><span style="font-style: italic">G</span></span> to receive
+the water from the spring which lies in that direction.
+This arrangement will keep the water out of the way
+until the drains are ready to take it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Outlet.</span></span>—The water being all discharged through
+the new temporary ditch, the old brook, beyond the
+boundary, should be cleared out to the final level (3.75,)
+and an excavation made, just within the boundary, sufficient
+to receive the masonry which is to protect the outlet.
+A good form of outlet is shown in Fig. 23. It may
+be cheaply made by any farmer, especially if he have good
+stone at hand;—if not, brick may be used, laid on a solid
+foundation of stout planks, which, (being protected from
+the air and always saturated with water,) will last a very
+long time.</p>
+
+<a name="fig29" id="fig29"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image23.png" width="640" height="333" alt="Illustration: Fig. 23 - OUTLET, SECURED WITH MASONRY AND GRATING." title="Fig. 23 - OUTLET, SECURED WITH MASONRY AND GRATING." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 23 - OUTLET, SECURED WITH MASONRY AND GRATING.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If made of stone, a solid floor, at least 2 feet square,
+should be placed at, or below, the level of the brook. If
+this consist of a single stone, it will be better than if of
+several smaller pieces. On this, place another layer extending
+the whole width of the first, but reaching only
+from its inner edge to its center line, so as to leave a foot<span class="tei tei-pb" id="page119">[pg 119]</span><a name="Pg119" id="Pg119" class="tei tei-anchor"></a>
+in width of the bottom stone to receive the fall of the
+water. This second layer should reach exactly the grade
+of the outlet (3.50) or a height of 3 inches from the brook
+level. On the floor thus made, there should be laid the
+tiles which are to constitute the outlets of the several
+drains; <span class="tei tei-hi"><span style="font-style: italic">i.e.</span></span>, one 3-1/2-inch tile for the line from the silt-basin,
+two 1-1/4-inch for the lines <span class="tei tei-hi"><span style="font-style: italic">F</span></span> and <span class="tei tei-hi"><span style="font-style: italic">G</span></span>, and one 2-1/4-inch
+for the main line <span class="tei tei-hi"><span style="font-style: italic">E</span></span>. These tiles should lie close to each
+other and be firmly cemented together, so that no water
+can pass outside of them, and a rubble-work of stone may
+with advantage be carried up a foot above them. Stone
+work, which may be rough and uncemented, but should
+always be solid, may then be built up at the sides, and
+covered with a secure coping of stone. A floor and sloping
+sides of stone work, jointed with the previously described
+work, and well cemented, or laid in strong clay or
+mortar, may, with benefit, be carried a few feet beyond the
+outlet. This will effectually prevent the undermining of
+the structure. After the entire drainage of the field is
+finished, the earth above these sloping sides, and that back
+of the coping, should be neatly sloped, and protected by
+sods. An iron grating, fine enough to prevent the entrance
+of vermin, placed in front of the tile, at a little distance
+from them,—and secured by a flat stone set on edge and
+hollowed out, so as merely to allow the water to flow freely
+from the drains,—the stone being cemented in its place so
+as to allow no water to pass under it,—will give a substantial
+and permanent finish to the structure.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">An outlet finished in this way, at an extra cost of a few
+dollars, will be most satisfactory, as a lasting means of
+securing the weakest and most important part of the system
+of drains. When no precaution of this sort is taken,
+the water frequently forces a passage under the tile for some
+distance up the drains, undermining and displacing them,
+and so softening the bottom that it will be difficult, in
+making repairs, to secure a solid foundation for the work.<span class="tei tei-pb" id="page120">[pg 120]</span><a name="Pg120" id="Pg120" class="tei tei-anchor"></a>
+Usually, repairs of this sort, aside from the annoyance attending
+them, will cost more than the amount required to
+make the permanent outlet described above. As well constructed
+outlets are necessarily rather expensive, as much
+of the land as possible should be drained to each one that
+it is necessary to make, by laying main lines which will
+collect all of the water which can be brought to it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Main Silt-Basin.</span></span>—The silt-basin, at which the
+drains are collected, may best be built before any drains
+are brought to it, and the work may proceed simultaneously
+with that at the outlet. It should be so placed that
+its center will lie exactly under the stake which marks its
+position, because it will constitute one of the leading landmarks
+for the survey of the drains.<a id="noteref_17" name="noteref_17" href="#note_17"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">17</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Before removing the stake and grade stake, mark their
+position by four stakes, set at a distance from it of 4 or 5
+feet, in such positions that two lines, drawn from those
+which are opposite to each other, will intersect at the point
+indicated; and place near one of them a grade stake,
+driven to the exact level of the one to be removed. This
+being done, dig a well, 4 feet in diameter, to a depth of
+2-1/2 feet below the grade of the outlet drain, (in the example
+under consideration this would be 5 feet below the
+grade stake.) If much water collects in the hole, widen
+it, in the direction of the outlet drain, sufficiently to give
+room for baling out the water. Now build, in this well,
+a structure 2 feet in interior diameter, such as is shown in
+Fig. 24, having its bottom 2 feet, in the clear, below the
+grade of the outlet, and carry its wall a little higher than
+the general surface of the ground. At the proper height
+insert, in the brick work, the necessary for tiles all incoming
+and outgoing drains; in this case, a 3-1/2-inch tile for<span class="tei tei-pb" id="page121">[pg 121]</span><a name="Pg121" id="Pg121" class="tei tei-anchor"></a>
+the outlet, 2-1/4-inch for the mains <span class="tei tei-hi"><span style="font-style: italic">A</span></span> and <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, and 1-1/4-inch for
+<span class="tei tei-hi"><span style="font-style: italic">B</span></span> and <span class="tei tei-hi"><span style="font-style: italic">D</span></span>.</p>
+
+<a name="fig30" id="fig30"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image24.png" width="640" height="961" alt="Illustration: Fig. 24 - SILT-BASIN, BUILT TO THE SURFACE." title="Fig. 24 - SILT-BASIN, BUILT TO THE SURFACE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 24 - SILT-BASIN, BUILT TO THE SURFACE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This basin being finished and covered with a flat stone
+or other suitable material, connect it with the outlet by an
+open ditch, unless the bottom
+of the ditch, when laid open to the proper depth, be
+found to be of muck or quicksand.
+In such case, it will be best to lay the tile at
+once, and cover it in for the
+whole distance, as, on a soft
+bottom, it would be difficult
+to lay it well when the full
+drainage of the field is flowing
+through the ditch. The
+tiles should be laid with all
+care, on a perfectly regulated
+fall,—using strips of board
+under them if the bottom
+is shaky or soft,—as on this line
+depends the success of all the
+drains above it, which might
+be rendered useless by a
+single badly laid tile at this point, or by any other cause
+of obstruction to the flow.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">While the work is progressing in the field above, there
+will be a great deal of muddy water and some sticks,
+grass, and other rubbish, running from the ditches above
+the basin, and care must be taken to prevent this drain
+from becoming choked. A piece of wire cloth, or basket
+work, placed over the outlet in the basin, will keep out the
+coarser matters, and the mud which would accumulate in
+the tile may be removed by occasional flushing. This is
+done by crowding a tuft of grass,—or a bit of sod,—into<span class="tei tei-pb" id="page122">[pg 122]</span><a name="Pg122" id="Pg122" class="tei tei-anchor"></a>
+the lower end of the tile (at the outlet,) securing it there
+until the water rises in the basin, and then removing it.
+The rush of water will be sufficient to wash the tile clean.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This plan is not without objections, and, as a rule, it is
+never well to lay any tiles at the lower end of a drain
+until all above it is finished; but when a considerable outlet
+must be secured through soft land, which is inclined to
+cave in, and to get soft at the bottom, it will save labor
+to secure the tile in place before much water reaches it,
+even though it require a daily flushing to keep it clean.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Opening the Ditches.</span></span>—Thus far it has been sought to
+secure a permanent outlet, and to connect it by a secure
+channel, with the silt-basin, which is to collect the
+water of the different series of drains. The next step
+is to lay open the ditches for these. It will be best to
+commence with the main line <span class="tei tei-hi"><span style="font-style: italic">A</span></span> and its laterals, as they
+will take most of the water which now flows through the
+open brook, and prevent its interference with the rest of
+the work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The first work is the opening of the ditches to a depth
+of about 3 feet, which may be best done with the common
+spade, pick, and shovel, except that in ground which is
+tolerably free from stones, a subsoil plow will often take
+the place of the pick, with much saving of labor. It <span class="tei tei-hi"><span style="font-style: italic">may</span></span>
+be drawn by oxen working in a long yoke, which will allow
+them to walk one on each side of the ditch, but this is dangerous,
+as they are liable to disturb the stakes, (especially
+the grade stakes,) and to break down the edges of the
+ditches. The best plan is to use a small subsoil plow,
+drawn by a single horse, or strong mule, trained to walk
+in the ditch. The beast will soon learn to accommodate
+himself to his narrow quarters, and will work easily in a
+ditch 2-1/2 feet deep, having a width of less than afoot at the
+bottom; of course there must be a way provided for him
+to come out at each end. Deeper than this there is no<span class="tei tei-pb" id="page123">[pg 123]</span><a name="Pg123" id="Pg123" class="tei tei-anchor"></a>
+economy in using horse power, and even for this depth it
+will be necessary to use a plow having only one stilt.</p>
+
+<a name="fig31" id="fig31"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image25.png" width="76" height="480" alt="Illustration: Fig. 25 - FINISHING SPADE." title="Fig. 25 - FINISHING SPADE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 25 - FINISHING SPADE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Before the main line is cut into the open brook, this
+should be furnished with a wooden trough, which will
+carry the water across it, so that the ditch shall
+receive only the filtration from the ground.
+Those laterals west of the main line, which are
+crossed by the brook, had better not be opened
+at present,—not until the water
+of the spring is admitted to and
+removed by the drain.</p>
+
+<a name="fig32" id="fig32"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image26.png" width="103" height="480" alt="Illustration: Fig. 26 - FINISHING SCOOP." title="Fig. 26 - FINISHING SCOOP." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 26 - FINISHING SCOOP.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The other laterals and the
+whole of the main line, having
+been cut to a depth of 3 feet,
+take a finishing spade, (Fig. 25,)
+which is only 4 inches wide at
+its point, and dig to within 2 or
+3 inches of the depth marked
+on the stakes, making the bottom
+tolerably smooth, with the
+aid of the finishing scoop, (Fig. 26,) and
+giving it as regular an inclination as can be
+obtained by the eye alone.</p>
+
+<a name="fig33" id="fig33"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image27.png" width="640" height="862" alt="Illustration: Fig. 27 - BRACING THE SIDES IN SOFT LAND." title="Fig. 27 - BRACING THE SIDES IN SOFT LAND." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 27 - BRACING THE SIDES IN SOFT LAND.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the ground is "rotten," and the banks
+of the ditches incline to cave in, as is often
+the case in passing wet places, the earth which is thrown
+out in digging must be thrown back sufficiently far from<span class="tei tei-pb" id="page124">[pg 124]</span><a name="Pg124" id="Pg124" class="tei tei-anchor"></a>
+the edge to prevent its weight from increasing the
+tendency; and the sides of the ditch
+may be supported by bits of board
+braced apart as is shown in Fig. 27.</p>
+
+<a name="fig34" id="fig34"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image28.png" width="121" height="480" alt="Illustration: Fig. 28 - MEASURING STAFF." title="Fig. 28 - MEASURING STAFF." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 28 - MEASURING STAFF.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The manner of opening
+the ditches, which
+is described above,
+for the main <span class="tei tei-hi"><span style="font-style: italic">A</span></span> and
+its laterals, will apply
+to the drains of the
+whole field and to all
+similar work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Grading the Bottoms.</span></span>—The next step
+in the work is to grade the bottoms of the
+ditches, so as to afford a bed for the tiles
+on the exact lines which are indicated by
+the figures marked on the different stakes.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The manner in which this is to be
+done may be illustrated by describing the
+work required for the line from <span class="tei tei-hi"><span style="font-weight: 700">C10</span></span> to
+<span class="tei tei-hi"><span style="font-weight: 700">C17</span></span>, (Fig. 20,) after it has been opened,
+as described above, to within 2 or 3 inches
+of the final depth.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A measuring rod, or square, such as is
+shown in Fig. 28,<a id="noteref_18" name="noteref_18" href="#note_18"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">18</span></span></a> is set at <span class="tei tei-hi"><span style="font-weight: 700">C10</span></span>, so that
+the lower side of its arm is at the mark
+4.59 on the staff, (or at a little less than 4.6
+if it is divided only into feet and tenths,)
+and is held upright in the ditch, with its
+arm directly over the grade stake. The
+earth below it is removed, little by little, until it will touch
+the top of the stake and the bottom of the ditch at the<span class="tei tei-pb" id="page125">[pg 125]</span><a name="Pg125" id="Pg125" class="tei tei-anchor"></a>
+same time. If the ground is soft, it should be cut out
+until a flat stone, a block of wood, or a piece of tile, or of
+brick, sunk in the bottom, will have its surface at the exact
+point of measurement. This point is the bottom of the
+ditch on which the collar of the tile is to lie at that stake.
+In the same manner the depth is fixed at <span class="tei tei-hi"><span style="font-style: italic">C11</span></span> (4.19,) and
+<span class="tei tei-hi"><span style="font-style: italic">C12</span></span> (4.41,) as the rate of fall changes at each
+of these points, and at <span class="tei tei-hi"><span style="font-style: italic">C15</span></span> (3.89,) and <span class="tei tei-hi"><span style="font-style: italic">C17</span></span>
+(4.17,) because (although the fall is uniform
+from <span class="tei tei-hi"><span style="font-style: italic">C12</span></span> to <span class="tei tei-hi"><span style="font-style: italic">C17</span></span>,) the distance is too great
+for accurate sighting.</p>
+
+<a name="fig35" id="fig35"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image29.png" width="97" height="480" alt="Illustration: Fig. 29 - BONING ROD." title="Fig. 29 - BONING ROD." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 29 - BONING ROD.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Having provided <span class="tei tei-hi"><span style="font-style: italic">boning-rods</span></span>, which are
+strips of board 7 feet long, having horizontal
+cross pieces at their upper ends, (see Fig.
+29,) set these perpendicularly on the spots
+which have been found by measurement to
+be at the correct depth opposite stakes 10,
+11, 12, 15, and 17, and fasten each in its
+place by wedging it between two strips of
+board laid across the ditch, so as to clasp it,
+securing these in their places by laying stones
+or earth upon their ends.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As these boning-rods are all exactly 7 feet
+long, of course, a line sighted across their
+tops will be exactly 7 feet higher, at all
+points, than the required grade of the ditch
+directly beneath it, and if a plumb rod, (similar to
+the boning-rod, but provided with a line and plummet,)
+be set perpendicularly on any point of the bottom of
+the drain, the relation of its cross piece to the line of sight
+across the tops of the boning-rods will show whether the
+bottom of the ditch at that point is too high, or too low,
+or just right. The manner of sighting over two boning-rods
+and an intermediate plumb-rod, is shown in Fig. 31.</p>
+
+<a name="fig36" id="fig36"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image30.png" width="640" height="385" alt="Illustration: Fig. 30 - POSITION OF WORKMAN AND USE OF FINISHING SCOOP." title="Fig. 30 - POSITION OF WORKMAN AND USE OF FINISHING SCOOP." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 30 - POSITION OF WORKMAN AND USE OF FINISHING SCOOP.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Three persons are required to finish the bottom of the<span class="tei tei-pb" id="page126">[pg 126]</span><a name="Pg126" id="Pg126" class="tei tei-anchor"></a>
+ditch; one to sight across the tops of the boning-rods, one
+to hold the plumb-rod at different points as the finishing
+progresses, and one in the ditch, (see Fig. 30,) provided
+with the finishing spade and scoop,—and, in hard ground,
+with a pick,—to cut down or fill up as the first man calls
+"too high," or, "too low." An inch or two of filling maybe
+beaten sufficiently hard with the back of the scoop,
+but if several inches should be required, it should be well
+rammed with the top of a pick, or other suitable instrument,
+as any subsequent settling would disarrange the fall.</p>
+
+<a name="fig37" id="fig37"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image31.png" width="640" height="81" alt="Illustration: Fig. 31 - SIGHTING BY THE BONING-RODS." title="Fig. 31 - SIGHTING BY THE BONING-RODS." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 31 - SIGHTING BY THE BONING-RODS.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As the lateral drains are to be laid first, they should be
+the first graded, and as they are arranged to discharge into
+the tops of the mains, their water will still flow off,
+although the main ditches are not yet reduced to their final<span class="tei tei-pb" id="page127">[pg 127]</span><a name="Pg127" id="Pg127" class="tei tei-anchor"></a>
+depth. After the laterals are laid and filled in, the main
+should be graded, commencing at the upper end; the tiles
+being laid and covered as fast as the bottom is made ready,
+so that it may not be disturbed by the water of which the
+main carries so much more than the laterals.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Tile-Laying.</span></span>—Gisborne says: "It would be scarcely
+more absurd to set a common blacksmith to eye needles
+than to employ a common laborer to lay pipes and collars."
+The work comes under the head of <span class="tei tei-hi"><span style="font-style: italic">skilled labor,</span></span>
+and, while no very great exercise of judgment is required
+in its performance, the little that is required is imperatively
+necessary, and the details of the work should be
+deftly done. The whole previous outlay,—the survey and
+staking of the field, the purchase of the tiles, the digging
+and grading of the ditches—has been undertaken that we
+may make the conduit of earthenware pipes which is now
+to be laid, and the whole may be rendered useless by a
+want of care and completeness in the performance of this
+chief operation. This subject, (in connection with that of
+finishing the bottoms of the ditches,) is very clearly treated
+in Mr. Hoskyns' charming essay,<a id="noteref_19" name="noteref_19" href="#note_19"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">19</span></span></a> as follows:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It was urged by Mr. Brunel, as a justification for more
+attention and expense in the laying of the rails of the
+Great Western, than had been ever thought of upon
+previously constructed lines, that all the embankments
+and cuttings, and earthworks and stations, and law and
+parliamentary expenses—in fact, the whole of the outlay
+encountered in the formation of a railway, had for its
+main and ultimate object <span class="tei tei-hi"><span style="font-style: italic">a perfectly smooth and level
+line of rail</span></span>; that to turn stingy at this point, just when
+you had arrived at the great ultimatum of the whole
+proceedings, viz: the iron wheel-track, was a sort of
+saving which evinced a want of true preception of the
+great object of all the labor that had preceded it. It<span class="tei tei-pb" id="page128">[pg 128]</span><a name="Pg128" id="Pg128" class="tei tei-anchor"></a>
+may seem curious to our experiences, in these days, that
+such a doctrine could ever have needed to be enforced
+by argument; yet no one will deem it wonderful who
+has personally witnessed the unaccountable and ever new
+difficulty of getting proper attention paid to the leveling
+of the bottom of a drain, and the laying of the tiles in
+that continuous line, where one single depression or irregularity,
+by collecting the water at that spot, year
+after year, tends toward the eventual stoppage of the
+whole drain, through two distinct causes, the softening
+of the foundation underneath the sole, or tile flange, and
+the deposit of soil inside the tile from the water collected
+at the spot, and standing there after the rest had run off.
+Every depression, however slight, is constantly doing
+this mischief in every drain where the fall is but trifling;
+and if to the two consequences above mentioned, we
+may add the decomposition of the tile itself by the
+action of water long stagnant within it, we may deduce
+that every tile-drain laid with these imperfections in
+the finishing of the bottom, has a tendency toward
+obliteration, out of all reasonable proportion with
+that of a well-burnt tile laid on a perfectly even inclination,
+which, humanly speaking, may be called a permanent
+thing. An open ditch cut by the most skillful
+workman, in the summer, affords the best illustration of
+this underground mischief. Nothing can look smoother
+and more even than the bottom, until that uncompromising
+test of accurate levels, the water, makes its appearance:
+all on a sudden the whole scene is changed, the
+eye-accredited level vanishes as if some earthquake had
+taken place: here, there is a gravelly <span class="tei tei-hi"><span style="font-style: italic">scour</span></span>, along which
+the stream rushes in a thousand little angry-looking ripples;
+there, it hangs and looks as dull and heavy as if it
+had given up running at all, as a useless waste of energy;
+in another place, a few dead leaves or sticks, or a morsel
+of soil broken from the side, dams back the water for a<span class="tei tei-pb" id="page129">[pg 129]</span><a name="Pg129" id="Pg129" class="tei tei-anchor"></a>
+considerable distance, occasioning a deposit of soil along
+the whole reach, greater in proportion to the quantity
+and the muddiness of the water detained. All this shows
+the paramount importance of perfect evenness in the
+bed on which the tiles are laid. <span class="tei tei-hi"><span style="font-style: italic">The worst laid tile is
+the measure of the goodness and permanence of the
+whole drain</span></span>, just as the weakest link of a chain is the
+measure of its strength."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The simple laying of the smaller sizes of pipes and collars
+in the lateral drains, is an easy matter. It requires
+care and precision in placing the collar equally under the
+end of each pipe, (having the joint at the middle of
+the collar,) in having the ends of the pipes actually touch
+each other within the collars, and in brushing away any
+loose dirt which may have fallen on the spot on which the
+collar is to rest. The connection of the laterals with
+the mains, the laying of the larger sizes of tiles so as to
+form a close joint, the wedging of these larger tiles firmly
+into their places, and the trimming which is necessary in
+going around sharp curves, and in putting in the shorter
+pieces which are needed to fill out the exact length of the
+drain, demand more skill and judgment than are often
+found in the common ditcher. Still, any clever workman,
+who has a careful habit, may easily be taught all that is
+necessary; and until he is thoroughly taught,—and not
+only knows how to do the work well, but, also, understands
+the importance of doing it well,—the proprietor
+should carefully watch the laying of every piece.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Never have tiles laid by the rod, but always by the
+day.</span></span> "The more haste, the less speed," is a maxim which
+applies especially to tile-laying.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the proprietor or the engineer does not overlook the
+laying of each tile as it is done, and probably he will not,
+he should carefully inspect every piece before it is covered.
+It is well to walk along the ditches and touch each tile
+with the end of a light rod, in such a way as to see<span class="tei tei-pb" id="page130">[pg 130]</span><a name="Pg130" id="Pg130" class="tei tei-anchor"></a>
+whether it is firm enough in its position not to be displaced
+by the earth which will fall upon it in filling the
+ditches.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Preparatory to laying, the tiles should be placed along
+one side of the ditch, near enough to be easily reached by
+a man standing in it. When collars are to be used, one of
+these should be slipped over one end of each tile. The
+workman stands in the ditch, with his face toward its
+upper end. The first tile is laid with a collar on its lower
+end, and the collar is drawn one-half of its length forward,
+so as to receive the end of the next tile. The upper end
+of the first tile is closed with a stone, or a bit of broken
+tile placed firmly against it. The next tile has its nose
+placed into the projecting half of the collar of the first
+one, and its own collar is drawn forward to receive the
+end of the third, and thus to the end of the drain, the
+workman walking backward as the work progresses. By
+and by, when he comes to connect the lateral with the
+main, he may find that a short piece of tile is needed to
+complete the length; this should not be placed next to the
+tile of the main, where it is raised above the bottom of
+the ditch, but two or three lengths back, leaving the connection
+with the main to be made with a tile of full
+length. If the piece to be inserted is only two or three
+inches long, it may be omitted, and the space covered by
+using a whole 2½-inch tile in place of the collar. In turning
+corners or sharp curves, the end of the tile may be
+chipped off, so as to be a little thinner on one side, which
+will allow it to be turned at a greater angle in the collar.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the drain turns a right angle, it will be better to dig
+out the bottom of the ditch to a depth of about eight
+inches, and to set a 6-inch tile on end in the hole, perforating
+its sides, so as to admit the ends of the pipes at
+the proper level. This 6-inch tile, (which acts as a small
+silt-basin,) should stand on a board or on a flat stone, and
+its top should be covered with a stone or with a couple of<span class="tei tei-pb" id="page131">[pg 131]</span><a name="Pg131" id="Pg131" class="tei tei-anchor"></a>
+bricks. Wood will last almost forever below the level of
+the drain, where it will always be saturated with water,
+but in the drier earth above the tile, it is much more liable
+to decay.</p>
+
+<a name="fig38" id="fig38"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image32.png" width="355" height="480" alt="Illustration: Fig. 32 - PICK FOR DRESSING AND PREFORATING TILE." title="Fig. 32 - PICK FOR DRESSING AND PREFORATING TILE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 32 - PICK FOR DRESSING AND PREFORATING TILE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The trimming and perforating of the tile is done with a
+"tile-pick," (Fig. 32,) the hatchet end,
+tolerably sharp, being used for the
+trimming, and the point, for making
+the holes. This is done by striking
+lightly around the circumference of
+the hole until the center piece falls in,
+or can be easily knocked in. If the
+hole is irregular, and does not fit the
+tile nicely, the open space should be
+covered with bits of broken tile, to
+keep the earth out.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As fast as the laterals are laid and inspected, they should
+be filled in to the depth of at least a foot, to protect the
+tiles from being broken by the falling of stones or lumps
+of earth from the top, and from being displaced by water
+flowing in the ditch. Two or three feet of the lower
+end may be left uncovered until the connection with the
+main is finished.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the main drains, when the tiles are of the size with
+which collars are used, the laying is done in the same manner.
+If it is necessary to use 3-1/2-inch tiles, or any larger
+size, much more care must be given to the closing of the
+joints. All tiles, in manufacture, dry more rapidly at the
+top, which is more exposed to the air, than at the bottom,
+and they are, therefore, contracted and made shorter at
+the top. This difference is most apparent in the larger
+sizes. The large <span class="tei tei-hi"><span style="font-style: italic">round</span></span> tiles, which can be laid on any side,
+can easily be made to form a close joint, and they
+should be secured in their proper position by stones or
+lumps of earth, wedged in between them and the sides of
+the ditch. The sole tiles must lie with the shortest sides<span class="tei tei-pb" id="page132">[pg 132]</span><a name="Pg132" id="Pg132" class="tei tei-anchor"></a>
+up, and, usually, the space between two tiles, at the top,
+will be from one-quarter to one-half of an inch. To
+remedy this defect, and form a joint which may he protected
+against the entrance of earth, the bottom should he
+trimmed off, so as to allow the tops to come closer together.
+Any opening, of less than a quarter of an inch,
+can he satisfactorily covered,—more than that should not
+be allowed. In turning corners, or in passing around
+curves, with large tiles, their ends must he beveled off
+with the pick, so as to fit nicely in this position.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The best covering for the joints of tiles which are
+laid without collars, is a scrap of tin, bent so as to fit their
+shape,—scraps of leather, or bits of strong wood shavings,
+answer a very good purpose, though both of these latter require
+to be held in place by putting a little earth over their
+ends as soon as laid on the tile. <span class="tei tei-hi"><span style="font-style: italic">Very small</span></span> grass ropes
+drawn over the joints, (the ends being held down with
+stones or earth,) form a satisfactory covering, but care
+should be taken that they be not too thick. A small handful
+of wood shavings, thrown over the joints, also answers
+a good purpose. Care, however, should always be taken,
+in using any material which will decay readily, to have no
+more than is necessary to keep the earth out, lest, in its
+decay, it furnish material to be carried into the tile and obstruct
+the flow. This precaution becomes less necessary
+in the case of drains which always carry considerable
+streams of water, but if they are at times sluggish in their
+flow, too much care cannot be given to keep them free
+of all possible causes of obstruction. As nothing is gained
+by increasing the quantity of loose covering beyond what
+is needed to close the joints, and as such covering is only
+procured with some trouble, there is no reason for its extravagant
+use.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There seems to remain in the minds of many writers on
+drainage a glimmering of the old fallacy that underdrains,
+like open drains, receive their water from above, and it is<span class="tei tei-pb" id="page133">[pg 133]</span><a name="Pg133" id="Pg133" class="tei tei-anchor"></a>
+too commonly recommended that porous substances be
+placed above the tile. If, as is universally conceded, the
+water rises into the tile from below, this is unnecessary.
+The practice of covering the joints, and even covering the
+whole tile, (often to the depth of a foot,) with tan-bark,
+turf, coarse gravel, etc., is in no wise to be commended;
+and, while the objections to it are not necessarily very
+grave in all cases, it always introduces an element of insecurity,
+and it is a waste of money, if nothing worse.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The tile layer need not concern himself with the question,
+of affording entrance room for the water. Let him, so far
+as the rude materials at hand will allow, make the joints
+perfectly tight, and when the water comes, it will find
+ample flaws in his work, and he will have been a good
+workman if it do not find room to flow in a current, carrying
+particles of dirt with it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In ditches in which water is running at the time of laying
+the tiles, the process should follow closely after the
+grading, and the stream may even be dammed back, section
+after section, (a plugged tile being placed under the
+dam, to be afterwards replaced by a free one,) and graded,
+laid and covered before the water breaks in. There is one
+satisfaction in this kind of work,—that, while it is difficult
+to lay the drain so thoroughly well as in a dry ditch, the
+amount of water is sufficient to overcome any slight tendency
+to obstruction.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Connections.</span></span>—As has been before stated, lateral drains
+should always enter at the top of the main. Even in the
+most shallow work, the slightly decreased depth of the
+lateral, which this arrangement requires, is well compensated
+for by the free outlet which it secures.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">After the tile of the main, which is to receive a side
+drain, has been fitted to its place, and the point of junction
+marked, it should be taken up and perforated; then
+the end of the tile of the lateral should be so trimmed as<span class="tei tei-pb" id="page134">[pg 134]</span><a name="Pg134" id="Pg134" class="tei tei-anchor"></a>
+to fit the hole as accurately as may be, the large tile replaced
+in its position, and the small one laid on it,—reaching
+over to the floor of the lateral ditch. Then connect
+it with the lateral as previously laid, fill up solidly
+the space under the tile which reaches over to the top
+of the main, (so that it cannot become disturbed in filling,)
+and lay bits of tile, or other suitable covering,
+around the connecting joint.<a id="noteref_20" name="noteref_20" href="#note_20"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">20</span></span></a></p>
+
+<a name="fig39" id="fig39"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image33.png" width="640" height="194" alt="Illustration: Fig. 33 - LATERAL DRAIN ENTERING AT TOP." title="Fig. 33 - LATERAL DRAIN ENTERING AT TOP." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 33 - LATERAL DRAIN ENTERING AT TOP.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When the main drain is laid with collars, it should be
+so arranged that, by
+substituting a full
+tile in the place of
+the collar,—leaving,
+within it, a
+space between the
+smaller pipes,—a
+connection can be made with this larger tile, as is represented
+in Figures 33 and 34.</p>
+
+<a name="fig40" id="fig40"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image34.png" width="640" height="240" alt="Illustration: Fig. 34 - SECTIONAL VIEW OF JOINT." title="Fig. 34 - SECTIONAL VIEW OF JOINT." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 34 - SECTIONAL VIEW OF JOINT.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Silt-Basins</span></span> should be used at all points where a drain,
+after running for any considerable distance at a certain
+rate of fall, changes to a less rapid fall,—unless, indeed,
+the diminished fall be still
+sufficiently great for the
+removal of silty matters,
+(say two feet or more in a
+hundred). They may be
+made in any manner which
+will secure a stoppage of
+the direct current, and afford room below the floor of the
+tile for the deposit of the silt which the water has carried
+in suspension; and they may be of any suitable material;—even
+a sound flour barrel will serve a pretty good<span class="tei tei-pb" id="page135">[pg 135]</span><a name="Pg135" id="Pg135" class="tei tei-anchor"></a>
+purpose for many years.
+The most complete form
+of basin is that represented
+in Figure 24.</p>
+
+<a name="fig41" id="fig41"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image35.png" width="640" height="943" alt="Illustration: Fig. 35 - SQUARE BRICK SILT-BASIN." title="Fig. 35 - SQUARE BRICK SILT-BASIN." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 35 - SQUARE BRICK SILT-BASIN.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When the object is
+only to afford room for
+the collection of the silt
+of a considerable length
+of drain, and it is not
+thought worth while to
+keep open a communication
+with the surface, for
+purposes of inspection, a
+square box of brick
+work, (Fig. 35,) having
+a depth of one and a
+half or two feet below
+the floor of the drain,—tiles
+for the drains being
+built in the walls, and
+the top covered with a
+broad stone,—will answer
+very well.</p>
+
+<a name="fig42" id="fig42"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image36.png" width="640" height="879" alt="Illustration: Fig. 36 - SILT-BASIN OF VITRIFIED PIPE." title="Fig. 36 - SILT-BASIN OF VITRIFIED PIPE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 36 - SILT-BASIN OF VITRIFIED PIPE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A good sort of basin, to reach
+to the surface of the ground, may
+be made of large, vitrified drain
+pipes,—such as are used for town
+sewerage,—having a diameter of
+from six to twelve inches, according
+to the requirements of the work.
+This basin is shown in Figure 36.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Figure 37 represents a basin made
+of a 6-inch tile,—similar to that
+described on page 130, for turning a
+short corner. A larger basin of
+the same size, cheaper than if built<span class="tei tei-pb" id="page136">[pg 136]</span><a name="Pg136" id="Pg136" class="tei tei-anchor"></a>
+of brick, may be made by using a large vitrified drain
+pipe in the place of the one shown in the cut. These
+vitrified pipes may be perforated in the
+manner described for the common tile.</p>
+
+<a name="fig43" id="fig43"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image37.png" width="603" height="726" alt="Illustration: Fig. 37 - TILE SILT-BASIN." title="Fig. 37 - TILE SILT-BASIN." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 37 - TILE SILT-BASIN.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In laying the main line <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, (Fig. 21,)
+an underground basin of brick work,
+(Fig. 35,) or its equivalent, should be
+placed at stake 7, because at that point
+the water, which has been flowing on an
+inclination of 1.09, 2.00 and 2.83 per 100,
+continues its course over the much less
+fall of only 0.56 per 100.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If, among the tiles which have passed the inspection,
+there are some which, from over burning, are smaller than
+the average, they should be laid at the upper ends of the
+laterals. The cardinal rule of the tile layer should be
+<span class="tei tei-hi"><span style="font-style: italic">never to have a single tile in the finished drain of smaller
+size, of more irregular shape, or less perfectly laid, than
+any tile above it</span></span>. If there is to be any difference in the
+quality of the drain, at different points, let it grow better
+as it approaches the outlet and has a greater length
+above depending upon its action.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Covering the Tiles, and Filling-in the Ditches.</span></span>—The
+best material for covering the tiles is that which will the
+most completely surround them, so as to hold them in
+their places; will be the least likely to have passages for
+the flow of <span class="tei tei-hi"><span style="font-style: italic">streams</span></span> of water into the joints, and will afford
+the least silt to obstruct the drain. Clay is the best
+of all available materials, because it is of the most uniform
+character throughout its mass, and may be most perfectly
+compacted around the tiles. As has been before stated,
+all matters which are subject to decay are objectionable,
+because they will furnish fine matters to enter the joints,
+and by their decrease of bulk, may leave openings in the
+earth through which streams of muddy water may find<span class="tei tei-pb" id="page137">[pg 137]</span><a name="Pg137" id="Pg137" class="tei tei-anchor"></a>
+their way into the tiles. Gravel is bad, and will remain
+bad until its spaces are filled with fine dirt deposited by
+water, which, leaving only a part of its impurities here,
+carries the rest into the drain. A gravelly loam, free
+from roots or other organic matter, if it is strong enough
+to be worked into a ball when wet, will answer a very
+good purpose.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Ordinarily, the earth which was thrown out from the
+bottom of the ditch, and which now lies at the top of the
+dirt heap, is the best to be returned about the tiles, being
+first freed from any stones it may contain which are large
+enough to break or disturb the tiles in falling on to them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the bottom of the ditch consists of quicksand or
+other silty matters, clay or some other suitable earth
+should be sought in that which was excavated from a less
+depth, or should be brought from another place. A thin
+layer of this having been placed in the bottom of the
+ditch when grading, a slight covering of the same about
+the tiles will so encase them as to prevent the entrance of
+the more "slippy" soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The first covering of fine earth, free from stones and
+clods, should be sprinkled gently over the tiles, no full
+shovelfuls being thrown on to them until they are covered
+at least six inches deep. When the filling has reached a
+height of from fifteen to twenty inches, the men may jump
+into the ditch and tramp it down evenly and regularly,
+not treading too hard in any one place at first. When
+thus lightly compacted about the tile, so that any further
+pressure cannot displace them, the filling should be repeatedly
+rammed, (the more the better,) by two men
+standing astride the ditch, facing each other, and working
+a maul, such as is shown in Figure 38, and which may
+weigh from 80 to 100 pounds.</p>
+
+<a name="fig44" id="fig44"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image38.png" width="640" height="1700" alt="Illustration: Fig. 38 - MAUL FOR RAMMING." title="Fig. 38 - MAUL FOR RAMMING." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 38 - MAUL FOR RAMMING.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Those to whom this recommendation is new, will, doubtless,
+think it unwise. The only reply to their objection
+must be that others who shared their opinion, have, by<span class="tei tei-pb" id="page138">[pg 138]</span><a name="Pg138" id="Pg138" class="tei tei-anchor"></a>
+long observation and experience, been convinced of its
+correctness. They may practically convince themselves
+of the value of this sort of covering by a simple and inexpensive
+experiment: Take two large, water-tight hogsheads,
+bore through the side of each, a few inches from
+the bottom, a hole just large enough
+to admit a 1-1/4-inch tile; cover the bottom
+to the hight of the lower edge of
+the hole with strong, wet clay, beaten
+to a hard paste; on this, lay a line of
+pipes and collars,—the inner end sealed
+with putty, and the tile which passes
+through the hole so wedged about with
+putty, that no water could pass out
+between it and the outside of the hole.
+Cover the tile in one hogshead with
+loose gravel, and then fill it to the top
+with loose earth. Cover the tile in the
+other, twenty inches deep, with ordinary
+stiff clay, (not wet enough to
+<span class="tei tei-hi"><span style="font-style: italic">puddle</span></span>, but sufficiently moist to pack
+well,) and ram it thoroughly, so as
+to make sure that the tiles are completely
+clasped, and that there is no
+crack nor crevice through which water
+can trickle, and then fill this hogshead
+to the top with earth, of the
+same character with that used in
+the other case. These hogsheads should stand where
+the water of a small roof, (as that of a hog-pen,) may
+be led into them, by an arrangement which shall give
+an equal quantity to each;—this will give them rather
+more than the simple rain-fall, but will leave them
+exposed to the usual climatic changes of the season. A
+vessel, of a capacity of a quart or more, should be connected
+with each outlet, and covered from the dust,—<span class="tei tei-pb" id="page139">[pg 139]</span><a name="Pg139" id="Pg139" class="tei tei-anchor"></a>
+these will act as silt-basins. During the first few storms
+the water will flow off much more freely from the first
+barrel; but, little by little, the second one, as the water
+finds its way through the clay, and as the occasional drying,
+and repeated filtration make it more porous, will increase
+in its flow until it will, by the end of the season,
+or, at latest, by the end of the second season, drain as
+well as the first, if, indeed, that be not by this time somewhat
+obstructed with silt. The amount of accumulation
+in the vessels at the outlet will show which process has
+best kept back the silt, and the character of the deposit
+will show which would most probably be carried off by
+the gentle flow of water in a nearly level drain.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is no argument against this experiment that its results
+cannot be determined even in a year, for it is not pretended
+that drains laid in compact clay will dry land so completely
+during the first month as those which give more
+free access to the water; only that they will do so in a
+comparatively short time; and that, as drainage is a work
+for all time, (practically as lasting as the farm itself,) the
+importance of permanence and good working for long
+years to come, is out of all proportion to that of the temporary
+good results of one or two seasons, accompanied
+with doubtful durability.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It has been argued that <span class="tei tei-hi"><span style="font-style: italic">surface water</span></span> will be more
+readily removed by drains having porous filling. Even if
+this were true to any important degree,—which it is not,—it
+would be an argument against the plan, for the remedy
+would be worse than the disease. If the water flow from
+the surface down into the drain, it will not fail to carry
+dirt with it, and instead of the clear water, which alone
+should rise into the tiles from below, we should have a
+trickling flow from above, muddy with wasted manure
+and silty earth.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">The remaining filling of the ditch</span></span> is a matter of simple
+labor, and may be done in whatever way may be most<span class="tei tei-pb" id="page140">[pg 140]</span><a name="Pg140" id="Pg140" class="tei tei-anchor"></a>
+economical under the circumstances of the work. If the
+amount to be filled is considerable, so that it is desirable
+to use horse-power, the best way will be to use a scraper,
+such as is represented in Figure 39, which is a strongly
+ironed plank, 6 feet long and 18 inches wide, sharp shod
+at one side, and supplied with handles at the other. It is
+propelled by means of the curved rods, which are attached
+to its under side by flexible joints. These rods
+are connected by a chain which has links large enough to
+receive the hook of an ox-chain. This scraper may be
+used for any straight-forward work by attaching the power
+to the middle of the chain. By moving the hook a few
+links to the right or left, it will act somewhat after the
+manner of the mould-board of a plow, and will, if skillfully
+handled, shoot the filling rapidly into the ditch.</p>
+
+<a name="fig45" id="fig45"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image39.png" width="640" height="241" alt="Illustration: Fig. 39 - BOARD SCRAPER FOR FILLING DITCHES." title="Fig. 39 - BOARD SCRAPER FOR FILLING DITCHES." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 39 - BOARD SCRAPER FOR FILLING DITCHES.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the work is done by hand, mix the surface soil and
+turf with the subsoil filling for the whole depth. If with
+a scraper, put the surface soil at the bottom of the loose
+filling, and the subsoil at the top, as this will be an imitation,
+for the limited area of the drains, of the process of
+"trenching," which is used in garden cultivation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When the ditches are filled, they will be higher than
+the adjoining land, and it will be well to make them still
+more so by digging or plowing out a small trench at each
+side of the drain, throwing the earth against the mound,
+which will prevent surface water, (during heavy rains,)
+from running into the loose filling before it is sufficiently<span class="tei tei-pb" id="page141">[pg 141]</span><a name="Pg141" id="Pg141" class="tei tei-anchor"></a>
+settled. A cross section of a filled drain provided with
+these ditches is shown in Figure 40.</p>
+
+<a name="fig46" id="fig46"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image40.png" width="640" height="638" alt="Illustration: Fig. 40 - CROSS-SECTION OF DITCH (FILLED), WITH FURROW AT EACH SIDE." title="Fig. 40 - CROSS-SECTION OF DITCH (FILLED), WITH FURROW AT EACH SIDE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 40 - CROSS-SECTION OF DITCH (FILLED), WITH FURROW AT EACH SIDE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In order that the silt-basins may be examined, and their
+accumulations of earth removed,
+during the early action
+of the drains, those parts
+of the ditches which are above
+them may be left open, care
+being taken, by cutting surface
+ditches around them, to
+prevent the entrance of water
+from above. During this time
+the covers of the basins
+should be kept on, and should
+be covered with inverted sods
+to keep loose dirt from getting
+into them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Collecting the Water ©f Springs.</span></span>—The lateral which
+connects with the main drain, <span class="tei tei-hi"><span style="font-style: italic">A</span></span>, (Fig. 21,) at the point
+<span class="tei tei-hi"><span style="font-style: italic">m</span></span>, and which is to take the water of the spring at the
+head of the brook, should not be opened until the main
+has been completed and filled into the silt-basin,—the
+brook having, meantime, been carried over the other
+ditches in wooden troughs. This lateral may now be
+made in the following way: Dig down to the tile of
+the main, and carry the lateral ditch back, a distance of
+ten feet. In the bottom of this, place a wooden trough,
+at least six feet long, laid at such depth that its channel
+shall be on the exact grade required for laying the tiles,
+and lay long straw, (held down by weights,) lengthwise
+within it. Make an opening in the tile of the main and
+connect the trough with it. The straw will prevent any
+coarse particles of earth from being carried into the tile,
+and the flow of the water will be sufficient to carry on to
+the silt-basin any finer matters. Now open the ditch to<span class="tei tei-pb" id="page142">[pg 142]</span><a name="Pg142" id="Pg142" class="tei tei-anchor"></a>
+and beyond the spring, digging at least a foot below the
+grade in its immediate vicinity, and filling to the exact
+grade with small stones, broken bricks, or other suitable
+material. Lay the tiles from the upper end of the ditch
+across the stone work, and down to the wooden trough.
+Now spread a sufficient layer of wood shavings over the
+stone work to keep the earth from entering it, cover
+the tiles and fill in the ditch, as before directed, and then
+remove the straw from the wooden trough and lay tiles
+in its place. In this way, the water of even a strong
+spring may be carried into a finished drain without danger.
+In laying the tile which crosses the stone work, it is well
+to use full 2-1/2-inch tiles in the place of collars, leaving the
+joints of these, and of the 1-1/4-inch tiles, (which should
+join near the middle of the collar tile,) about a quarter of
+an inch open, to give free entrance to the water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The stone and tile drain, <span class="tei tei-hi"><span style="font-style: italic">H, I</span></span>, is simply dug out to the
+surface of the rock, if this is not more than two feet below
+the grade of the upper ends of the laterals with which it
+connects, and then filled up with loose stones to the line of
+grade. If the stones are small, so as to form a good bottom
+for the tiles, they may be laid directly upon it; if not, a
+bottom for them may be made of narrow strips of cheap
+boards. Before filling, the tiles and stone work should be
+covered with shavings, and the filling above these should
+consist of a strong clay, which will remain in place after
+the shavings rot away.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Amending the Map.</span></span>—When the tiles are laid, and before
+they are covered, all deviations of the lines, as in passing
+around large stones and other obstructions, which
+may have prevented the exact execution of the original plan,
+and the location and kind of each underground silt-basin
+should also be carefully noted, so that they may be transferred
+to the map, for future reference, in the event of repairs
+becoming necessary. In a short time after the work<span class="tei tei-pb" id="page143">[pg 143]</span><a name="Pg143" id="Pg143" class="tei tei-anchor"></a>
+is finished, the surface of the field will show no trace of
+the lines of drain, and it should be possible, in case of
+need, to find any point of the drains with precision, so that
+no labor will be lost in digging for it. It is much cheaper
+to measure over the surface than to dig four feet trenches
+through the ground.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page144">[pg 144]</span><a name="Pg144" id="Pg144" class="tei tei-anchor"></a>
+<a name="toc47" id="toc47"></a>
+<a name="pdf48" id="pdf48"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER V. - HOW TO TAKE CARE OF DRAINS AND DRAINED LAND.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">So far as tile drains are concerned, if they are once well
+laid, and if the silt-basins have been emptied of silt until
+the water has ceased to deposit it, they need no care nor
+attention, beyond an occasional cleaning of the outlet
+brook. Now and then, from the proximity of willows, or
+thrifty, young, water-loving trees, a drain will be obstructed
+by roots; or, during the first few years after the work
+is finished, some weak point,—a badly laid tile, a loosely
+fitted connection between the lateral and a main, or an
+accumulation of silt coming from an undetected and persistent
+vein of quicksand,—will be developed, and repairs
+will have to be made. Except for the slight danger
+from roots, which must always be guarded against to the
+extent of allowing no young trees of the dangerous class
+to grow near a drain through which a <span class="tei tei-hi"><span style="font-style: italic">constant</span></span> stream of
+water flows, it may be fairly assumed that drains which
+have been kept in order for four or five years have passed
+the danger of interruption from any cause, and they may
+be considered entirely safe.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A drain will often, for some months after it is laid, run
+muddy water after rains. Sometimes the early deposit of
+silt will nearly fill the tile, and it will take the water of<span class="tei tei-pb" id="page145">[pg 145]</span><a name="Pg145" id="Pg145" class="tei tei-anchor"></a>
+several storms to wash it out. If the tiles have been laid
+in packed clay, they cannot long receive silt from without,
+and that which makes the flow turbid, may be assumed to
+come from the original deposit in the conduit. Examinations
+of newly laid drains have developed many instances
+where tiles were at first half filled with silt, and three
+months later were entirely clean. The muddiness of the
+flow indicates what the doctors call "an effort of nature
+to relieve herself," and nature may be trusted to succeed,
+at least, until she abandons the effort. If we are sure that
+a drain has been well laid, we need feel no anxiety because
+it fails to take the water from the ground so completely
+as it should do, until it settles into a flow of clear water
+after the heaviest storms.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the case of art actual stoppage, which will generally
+be indicated by the "bursting out" of the drain, i.e., the
+wetting of the land as though there were a spring under
+it, or as though its water had no underground outlet,
+(which is the fact,) it will be necessary to lay open the
+drain until the obstruction is found.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In this work, the real value of the map will be shown,
+by the facility which it offers for finding any point of any
+line of drains, and the exact locality of the junctions with
+the mains, and of the silt-basins. In laying out the plan
+on the ground, and in making his map, the surveyor will
+have had recourse to two or more fixed points; one of
+them, in our example, (fig. 21,) would probably be the
+center of the main silt-basin, and one, a drilled hole or
+other mark on the rock at the north side of the field. By
+staking out on the ground the straight line connecting
+these two points, and drawing a corresponding line on the
+map; we shall have a <span class="tei tei-hi"><span style="font-style: italic">base-line</span></span>, from which it will be easy,
+by perpendicular offsets, to determine on the ground any
+point upon the map. By laying a small square on the
+map, with one of its edges coinciding with the base-line,
+and moving it on this line until the other edge meets the<span class="tei tei-pb" id="page146">[pg 146]</span><a name="Pg146" id="Pg146" class="tei tei-anchor"></a>
+desired point, we fix, at the angle of the square, the point
+on the base-line from which we are to measure the length
+of the offset. The next step is to find, (by the scale,) the
+distance of this point from the nearest end of the base-line,
+and from the point sought. Then measure off, in the
+field, the corresponding distance on the base-line, and, from
+the point thus found, measure on a line perpendicular to
+the base line, the length of the offset; the point thus
+indicated will be the locality sought. In the same manner,
+find another point on the same drain, to give the range on
+which to stake it out. From this line, the drains which
+run parallel to it, can easily be found, or it may be used
+as a base-line, from which to find, by measuring offsets,
+other points near it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The object of this staking is, to find, in an inexpensive
+and easy way, the precise position of the drains, for which
+it would be otherwise necessary to grope in the dark,
+verifying our guesses by digging four-foot trenches, at
+random.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If there is a silt-basin, or a junction a short distance below
+the point where the water shows itself, this will be the
+best place to dig. If it is a silt-basin, we shall probably
+find that this has filled up with dirt, and has stopped the
+flow. In this case it should be cleaned out, and a point
+of the drain ten feet below it examined. If this is found
+to be clear, a long slender stick may be pushed up as far
+as the basin and worked back and forth until the passage
+is cleared. Then replace the tile below, and try with the
+stick to clean the tiles above the basin, so as to tap the
+water above the obstruction. If this cannot be done, or
+if the drain ten feet below is clogged, it will be necessary
+to uncover the tiles in both directions until an opening is
+found, and to take up and relay the whole. If the wetting
+of the ground is sufficient to indicate that there is
+much water in the drain, only five or six tiles should be
+taken up at a time, cleaned and relaid,—commencing at<span class="tei tei-pb" id="page147">[pg 147]</span><a name="Pg147" id="Pg147" class="tei tei-anchor"></a>
+the lower end,—in order that, when the water commences
+to flow, it may not disturb the bottom of the ditch for the
+whole distance.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the point opened is at a junction with the main, examine
+both the main and the lateral, to see which is
+stopped, and proceed with one or the other, as directed
+above. In doing this work, care should be taken to send
+as little muddy water as possible into the drain below, and
+to allow the least possible disturbance of the bottom.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If silt-basins have been placed at those points at which
+the fall diminishes, the obstruction will usually be found to
+occur at the outlets of these, from a piling up of the silt in
+front of them, and to extend only a short distance below and
+above. It is not necessary to take up the tiles until they
+are found to be entirely clean, for, if they are only one-half
+or one-third full, they will probably be washed clean
+by the rush of water, when that which is accumulated
+above is tapped. The work should be done in settled fair
+weather, and the ditches should remain open until the effect
+of the flow has been observed. If the tiles are made
+thoroughly clean by the time that the accumulated water
+has run off, say in 24 hours, they may be covered up; if
+not, it may be necessary to remove them again, and clean
+them by hand. When the work is undertaken it should
+be thoroughly done, so that the expense of a new opening
+need not be again incurred.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is worse than useless to substitute larger sizes of tiles
+for those which are taken up. The obstruction, if by silt,
+is the result of a too sluggish flow, and to enlarge the
+area of the conduit would only increase the difficulty. If
+the tiles are too small to carry the full flow which follows
+a heavy rain, they will be very unlikely to become choked,
+for the water will then have sufficient force to wash them
+clean, while if they are much larger than necessary, a deposit
+of silt to one half of their height will make a broad,<span class="tei tei-pb" id="page148">[pg 148]</span><a name="Pg148" id="Pg148" class="tei tei-anchor"></a>
+flat bed for the stream, which will run with much less
+force, and will be more likely to increase the deposit.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the drains are obstructed by the roots of willows, or
+other trees, the proprietor must decide whether he will
+sacrifice the trees or the drains; both he cannot keep, unless
+he chooses to go to the expense of laying in cement
+all of the drains which carry constant streams, for a distance
+of at least 50 feet from the dangerous trees. The
+trouble from trees is occasionally very great, but its occurrence
+is too rare for general consideration, and must be
+met in each case with such remedies as circumstances suggest
+as the best.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The gratings over the outlets of silt-basins which open
+at the surface of the ground, are sometimes, during the
+first year of the drainage, obstructed by a fungoid growth
+which collects on the cross bars. This should be occasionally
+rubbed off. Its character is not very well understood,
+and it is rarely observed in old drains. The decomposition
+of the grass bands which are used to cover the joints of
+the larger tiles may encourage its formation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the surface soil have a good proportion of sand,
+gravel, or organic matter, so as to give it the consistency
+which is known as "loamy," it will bear any treatment
+which it may chance to receive in cultivation, or as pasture
+land; but if it be a decided clay soil, no amount of draining
+will enable us to work it, or to turn cattle upon it
+when it is wet with recent rains. It will much sooner
+become dry, because of the drainage, and may much sooner
+be trodden upon without injury; but wet clay cannot be
+worked or walked over without being more or less <span class="tei tei-hi"><span style="font-style: italic">puddled</span></span>,
+and, thereby, injured for a long time.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">No matter how thoroughly heavy clay pasture lands
+may be under-drained, the cattle should be removed from
+them when it rains, and kept off until they are comparatively
+dry. Neglect of this precaution has probably led<span class="tei tei-pb" id="page149">[pg 149]</span><a name="Pg149" id="Pg149" class="tei tei-anchor"></a>
+to more disappointment as to the effects of drainage than
+any other circumstances connected with it. The injury
+from this cause does not extend to a great depth, and in
+the Northern States it would always be overcome by the
+frosts of a single winter; as has been before stated, it is
+confined to stiff clay soils, but as these are the soils which
+most need draining, the warning given is important.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page150">[pg 150]</span><a name="Pg150" id="Pg150" class="tei tei-anchor"></a>
+<a name="toc49" id="toc49"></a>
+<a name="pdf50" id="pdf50"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER VI. - WHAT DRAINING COSTS.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Draining is expensive work. This fact must be accepted
+as a very stubborn one, by every man who proposes to
+undertake the improvement. There is no royal road to
+tile-laying, and the beginner should count the cost at the
+outset. A good many acres of virgin land at the West
+might be bought for what must be paid to get an efficient
+system of drains laid under a single acre at home. Any
+man who stops at this point of the argument will probably
+move West,—or do nothing.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Yet, it is susceptible of demonstration that, even at the
+West, in those localities where Indian Corn is worth as
+much as fifty cents per bushel at the farm, it will pay to
+drain, in the best manner, all such land as is described in
+the first chapter of this book as in need of draining. Arguments
+to prove this need not be based at all on cheapness
+of the work; only on its effects and its permanence.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In fact, so far as draining with tiles is concerned, cheapness
+is a delusion and a snare, for the reason that it implies
+something less than the best work, a compromise between
+excellence and inferiority. The moment that we come
+down from the best standard, we introduce a new element
+into the calculation. The sort of tile draining which it is
+the purpose of this work to advocate is a system so complete<span class="tei tei-pb" id="page151">[pg 151]</span><a name="Pg151" id="Pg151" class="tei tei-anchor"></a>
+in every particular, that it may be considered as an
+absolutely permanent improvement. During the first
+years of the working of the drains, they will require more
+or less attention, and some expense for repairs; but, in
+well constructed work, these will be very slight, and will
+soon cease altogether. In proportion as we resort to cheap
+devices, which imply a neglect of important parts of the
+work, and a want of thoroughness in the whole, the expense
+for repairs will increase, and the duration of the usefulness
+of the drains will diminish.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Drains which are permanently well made, and which
+will, practically, last for all time, may be regarded as a
+good investment, the increased crop of each year, paying
+a good interest on the money that they cost, and the
+money being still represented by the undiminished value
+of the improvement. In such a case the draining of the
+land may be said to cost, not $50 per acre,—but the interest
+on $50 each year. The original amount is well invested,
+and brings its yearly dividend as surely as though
+it were represented by a five-twenty bond.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">With badly constructed drains, on the other hand, the
+case is quite different. In buying land which is subject
+to no loss in quantity or quality, the farmer considers, not
+so much the actual cost, as the relation between the yearly
+interest on the cost, and the yearly profit on the crop,—knowing
+that, a hundred years hence, the land will still be
+worth his money.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">But if the land were bounded on one side by a river which
+yearly encroached some feet on its bank, leaving the field
+a little smaller after each freshet; or if, every spring, some
+rods square of its surface were sure to be covered three feet
+deep with stones and sand, so that the actual value of the
+property became every year less, the purchaser would
+compare the yearly value of the crops, not only with the
+interest on the price, but, in addition to this, with so much<span class="tei tei-pb" id="page152">[pg 152]</span><a name="Pg152" id="Pg152" class="tei tei-anchor"></a>
+of the prime value as yearly disappears with the destruction
+of the land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is exactly so with the question of the cost of drainage.
+If the work is insecurely done, and is liable, in five
+years or in fifty, to become worthless; the increase of the
+crops resulting from it, must not only cover the yearly
+interest on the cost, but the yearly depreciation as well.
+Therefore what may seem at the time of doing the work
+to be cheapness, is really the greatest extravagance. It is
+like building a brick wall with clay for mortar. The bricks
+and the workmanship cost full price, and the small saving on
+the mortar will topple the wall over in a few years, while,
+if well cemented, it would have lasted for centuries. The
+cutting and filling of the ditches, and the purchase and
+transportation of the tiles, will cost the same in every
+case, and these constitute the chief cost; if the proper
+care in grading, tile-laying and covering, and in making
+outlets be stingily withheld,—saving, perhaps, one-tenth
+of the expense,—what might have been a permanent improvement
+to the land, may disappear, and the whole outlay
+be lost in ten years. A saving of ten per cent. in
+the cost will have lost us the other ninety in a short time.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">But, while cheapness is to be shunned, economy is to be
+sought in every item of the work of draining, and should
+be studied, by proprietor and engineer, from the first examination
+of the land, to the throwing of the last shovelful
+of earth on to the filling of the ditch. There are few
+operations connected with the cultivation of the soil in
+which so much may be imperceptibly lost through neglect,
+and carelessness about little details, as in tile-draining. In
+the original levelling of the ground, the adjustment of the
+lines, the establishing of the most judicious depth and inclination
+at each point of the drains, the disposition of
+surface streams during the prosecution of the work, and in
+the width of the excavation, the line which divides
+economy and wastefulness is extremely narrow and the<span class="tei tei-pb" id="page153">[pg 153]</span><a name="Pg153" id="Pg153" class="tei tei-anchor"></a>
+most constant vigilance, together with the best judgment
+and foresight, are needed to avoid unnecessary cost. In
+the laying and covering of the tile, on the other hand, it
+is best to disregard a little slowness and unnecessary care
+on the part of the workmen, for the sake of the most perfect
+security of the work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Details of Cost.</span></span>—The items of the work of drainage
+may be classified as follows:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1. Engineering and Superintendence.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2. Digging the ditches.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">3. Grading the bottoms.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">4. Tile and tile-laying.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">5. Covering the tile and filling the ditches.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">6. Outlets and silt-basins.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">1. <span class="tei tei-hi"><span style="font-style: italic">Engineering and Superintendence.</span></span>—It is not easy to
+say what would be the proper charge for this item of the
+work. In England, the Commissioners under the Drainage
+Acts of Parliament, and the Boards of Public Works,
+fix the charge for engineering at $1.25 per acre. That is in a
+country when the extent of lands undergoing the process
+of draining is very great, enabling one person to superintend
+large tracts in the same neighborhood at the same
+time, and with little or no outlay for travelling expenses.
+In this country, where the improvement is, thus far, confined
+to small areas, widely separated; and where there
+are comparatively few engineers who make a specialty of
+the work, the charge for services is necessarily much
+higher, and the amount expended in travelling much
+greater. In most cases, the proprietor of the land must
+qualify himself to superintend his own operations, (with
+the aid of a country surveyor, or a railroad engineer in the
+necessary instrumental work.) As draining becomes more
+general, the demand for professional assistance will, without
+doubt, cause local engineers to turn their attention to
+the subject, and their services may be more cheaply obtained.
+At present, it would probably not be prudent to<span class="tei tei-pb" id="page154">[pg 154]</span><a name="Pg154" id="Pg154" class="tei tei-anchor"></a>
+estimate the cost of engineering and superintendence, including
+the time and skill of the proprietor, at less than
+$5 per acre, even where from 20 to 50 acres are to be
+drained at once.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">2. <span class="tei tei-hi"><span style="font-style: italic">Digging the Ditches.</span></span>—The labor required for the
+various operations constitutes the principal item of cost in
+draining, and the price of labor is now so different in different
+localities, and so unsettled in all, that it is difficult
+to determine a rate which would be generally fair. It will
+be assumed that the average wages of day laborers of the
+class employed in digging ditches, is $1.50 per day, and
+the calculation will have to be changed for different districts,
+in proportion to the deviation of the actual rate of
+wages from this amount. There is a considerable advantage
+in having the work done at some season, (as after the
+summer harvest, or late in the fall,) when wages are comparatively
+low.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The cutting of the ditches should always be let by the
+rod. When working at day's work, the men will invariably
+open them wider than is necessary, for the sake of the
+greater convenience of working, and the extra width
+causes a corresponding waste of labor.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A 4-foot ditch, in most soils, need be only 20 inches wide
+at the surface, and 4 inches at the bottom. This gives a
+mean width of 12 inches, and requires the removal of
+nearly 2-1/2 cubic yards of earth for each rod of ditch; but
+an increase to a mean width of 16 inches, (which day
+workmen will usually reach, while piece workmen almost
+never will,) requires the removal of 3-1/4 cubic yards to the
+rod. As the increased width is usually below the middle
+of the drain, the extra earth will all have to be raised from
+2 to 4 feet, and the extra 3/4 yards will cost as much as a
+full yard taken evenly from the whole side, from top to
+bottom.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In clay soils, free from stones or "hard pan," but so
+stiff as to require considerable picking, ordinary workmen,<span class="tei tei-pb" id="page155">[pg 155]</span><a name="Pg155" id="Pg155" class="tei tei-anchor"></a>
+after a little practice, will be able to dig 3-1/2 rods of ditch
+per day, to an average depth of 3.80,—leaving from 2 to
+3 inches of the bottom of 4-foot ditches to be finished by
+the graders. This makes the cost of digging about 43
+cents per rod. In loamy soil the cost will be a little less
+than this, and in very hard ground, a little more. In
+sandy and peaty soils, the cost will not be more than 30
+cents. Probably 43 cents would be a fair average for soils
+requiring drainage, throughout the country.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This is about 17 cents for each yard of earth removed.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In soft ground, the caving in of the banks will require a
+much greater mean width than 12 inches to be thrown out,
+and, if the accident could not have been prevented by
+ordinary care on the part of the workman, (using the bracing
+boards shown in Fig. 28,) he should receive extra pay
+for the extra work. In passing around large stones it may
+also be necessary to increase the width.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The following table will facilitate the calculations for
+such extra work:</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="6"></colgroup><thead><tr><th colspan="6" class="tei tei-head tei-head-table" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em"><span style="font-weight: 700">CUBIC YARDS OF EXCAVATION IN DITCHES OF VARIOUS WIDTH.</span></th></tr></thead><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span class="tei tei-hi"><span style="font-style: italic">Length of Ditch.</span></span></td><td class="tei tei-cell">12 <span class="tei tei-hi"><span style="font-style: italic">Inches Wide.</span></span></td><td class="tei tei-cell">18 <span class="tei tei-hi"><span style="font-style: italic">Inches Wide.</span></span></td><td class="tei tei-cell">24 <span class="tei tei-hi"><span style="font-style: italic">Inches Wide.</span></span></td><td class="tei tei-cell">30 <span class="tei tei-hi"><span style="font-style: italic">Inches Wide.</span></span></td><td class="tei tei-cell">36 <span class="tei tei-hi"><span style="font-style: italic">Inches Wide.</span></span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"></td><td class="tei tei-cell">Yds. Feet.</td><td class="tei tei-cell">Yds. Feet.</td><td class="tei tei-cell">Yds. Feet.</td><td class="tei tei-cell">Yds. Feet.</td><td class="tei tei-cell">Yds. Feet.</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">1 Yard.</td><td class="tei tei-cell">0 12</td><td class="tei tei-cell">0 18</td><td class="tei tei-cell">0 24</td><td class="tei tei-cell">1 3</td><td class="tei tei-cell">1 9</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">1 Rod.</td><td class="tei tei-cell">2 12</td><td class="tei tei-cell">3 18</td><td class="tei tei-cell">4 24</td><td class="tei tei-cell">6 3</td><td class="tei tei-cell">7 9</td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Men will, in most soils, work best in couples,—one
+shovelling out the earth, and working forward, and the
+other, (moving backward,) loosening the earth with a
+spade or foot-pick, (Fig. 41.) In stony land, the men should
+be required to keep their work well closed up,—excavating
+to the full depth as they go. Then, if they strike a
+stone too large to be taken out within the terms of their
+contract, they can skip a sufficient distance to pass it, and
+the digging of the omitted part may be done by a faithful
+day workman. This will usually be cheaper and more
+satisfactory than to pay the contractors for extra work.</p>
+
+<span class="tei tei-pb" id="page156">[pg 156]</span><a name="Pg156" id="Pg156" class="tei tei-anchor"></a>
+
+<a name="fig51" id="fig51"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image41.png" width="147" height="480" alt="Illustration: Fig. 41 - FOOT PICK." title="Fig. 41 - FOOT PICK." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 41 - FOOT PICK.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Concerning the amount of work that one man can do
+in a day, in different soils, digging ditches 4 feet deep,
+French says: "In the writer's own field,
+where the pick was used to loosen the lower
+two feet of earth, the labor of opening and
+<span class="tei tei-hi"><span style="font-style: italic">filling</span></span> drains 4 feet deep, and of the mean
+width of 14 inches, all by hand labor, has
+been, in a mile of drains, being our first experiments,
+about one day's labor to 3 rods
+in length. The excavated earth of such a
+drain measures not quite 3 cubic yards,
+(exactly, 2.85.)" In a subsequent work,
+in a sandy soil, two men opened, <span class="tei tei-hi"><span style="font-style: italic">laid</span></span>, and
+<span class="tei tei-hi"><span style="font-style: italic">refilled</span></span> 14 rods in one day;—the mean width
+being 12 inches.<a id="noteref_21" name="noteref_21" href="#note_21"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">21</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In the same season, the same men opened,
+<span class="tei tei-hi"><span style="font-style: italic">laid</span></span>, and <span class="tei tei-hi"><span style="font-style: italic">filled</span></span> 70 rods of 4-foot drain of
+the same mean width of 12 inches, in the
+worst kind of clay soil, where the pick
+was constantly used. It cost 35 days' labor to complete
+the job, being 50 cents <span class="tei tei-hi"><span style="font-style: italic">per</span></span> rod for the labor alone." Or,
+under the foregoing calculation of $1.50 per day, 75
+cents per rod. These estimates, in common with nearly
+all that are published, are for the entire work of digging,
+grading, tile-laying, and refilling. Deducting the time required
+for the other work, the result will be about as
+above estimated; for the rough excavation, 3 1/2-rods to the
+day's work, costing, at $1.50 per day, 43 cents to the rod.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Grading</span></span> is the removal of 2 or 3 inches in depth, and
+about 4 inches in width, of the soil at the bottom of the
+ditch. It is chiefly done with the finishing scoop, which,
+(being made of two thin plates, one of iron and one of
+steel, welded together, the iron wearing away and leaving<span class="tei tei-pb" id="page157">[pg 157]</span><a name="Pg157" id="Pg157" class="tei tei-anchor"></a>
+the sharp steel edge always prominent,) will work in a
+very hard clay without the aid of the pick. Three men,—the
+one in the ditch being a skillful workman, and the
+others helping him when not sighting the rods,—will grade
+about 100 rods per day, making the cost about 6 cents per
+rod. Until they acquire the skill to work thus rapidly, they
+should not be urged beyond what they can readily do in
+the best manner, as this operation, (which is the preparing
+of the foundation for the tiles,) is probably the most important
+of the whole work of draining.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Tiles and Tile-Laying.</span></span>—After allowing for breakage, it
+will take about 16 tiles and 16 collars to lay a rod in
+length of drain. The cost of these will, of course, be
+very much affected by the considerations of the nearness
+of the tile-kiln and the cost of transportation. They
+should, in no ordinary case, cost, delivered on the ground,
+more than $8 per thousand for 1-1/4-inch tiles, and $4 per
+thousand for the collars, making a total of $12 for both,
+equal to about 19 cents per rod. The laying of the tiles,
+may be set down at 2 cents per rod,—based on a skilled
+man laying 100 rods daily, and receiving $2 per day.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Covering and filling</span></span> will probably cost 10 cents per
+rod, (if the scraper, Fig. 39, can be successfully used for
+the rough filling, the cost will be reduced considerably
+below this.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The four items of the cost of making one rod of lateral
+drain are as follows:</p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 1.00em"><colgroup span="2"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell">Digging the ditches</td><td class="tei tei-cell">- - - .43</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Grading</td><td class="tei tei-cell">- - - .06</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Tiles and laying</td><td class="tei tei-cell">- - - .21</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">Covering and filling</td><td class="tei tei-cell">- - - .10</td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell">- - -.80 cts.</td>
+</tr></tbody></table>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the drains are placed at intervals of 40 feet, there are
+required 64 rods to the acre,—this at 80 cents per rod will
+make the cost per acre,—for the above items,—$51.20.</p>
+
+<span class="tei tei-pb" id="page158">[pg 158]</span><a name="Pg158" id="Pg158" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">How much should be allowed for main drains, outlets,
+and silt-basins, it is impossible to say, as, on irregular
+ground, no two fields will require the same amount of this
+sort of work. On very even land, where the whole surface,
+for hundreds of acres, slopes gradually in one or two
+directions, the outlay for mains need not be more than
+two per cent. of the cost of the laterals. This would allow
+laterals of a uniform length of 800 feet to discharge into
+the main line, at intervals of 40 feet, if we do not consider
+the trifling extra cost of the larger tiles. On less
+regular ground, the cost of mains will often be considerably
+more than two per cent. of the cost of the laterals;
+but in some instances the increase of main lines will be
+fully compensated for by the reduction in the length of
+the laterals, which, owing to rocks, hills too steep to need
+drains at regular intervals, and porous, (gravelly,) streaks
+in the land, cannot be profitably made to occupy the whole
+area so thoroughly.<a id="noteref_22" name="noteref_22" href="#note_22"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">22</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Probably 7-1/2 per cent. of the cost of the laterals for
+mains, outlets, and silt-basins will be a fair average allowance.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This will bring the total cost of the work to about $60
+per acre, made up as follows:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Cost of the finished drains per acre - - - $51.20</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">7-1/2 per cent. added for mains, etc. - - - 3.83</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">Engineering and Superintendence - - - 5.00</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of course this is an arbitrary calculation, an estimate
+without a single ascertained fact to go upon,—but it is as<span class="tei tei-pb" id="page159">[pg 159]</span><a name="Pg159" id="Pg159" class="tei tei-anchor"></a>
+close as it can be made to what would probably be the
+cost of the best work, on average ground, at the present
+high prices of labor and material. Five years ago the
+same work could have been done for from $40 to $45 per
+acre, and it will be again cheaper when wages fall, and
+when a greater demand for draining tiles shall have caused
+more competition in their manufacture. With a large
+general demand, such as has existed in England for the last
+20 years, they would now be sold for one-half of their present
+price here, and the manufacture would be more profitable.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There are many light lands on retentive subsoils, which
+could be drained, at present prices, for $50 or less per acre,
+and there are others, which are very hard to dig, on which
+thorough-draining could not now be done for $60.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The cost and the promise of the operation in each instance,
+must guide the land owner in deciding whether or
+not to undertake the improvement.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In doubtful cases, there is one compromise which may
+be safely made,—that is, to omit each alternate drain, and
+defer its construction until labor is cheaper.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This is doing half the work,—a very different thing
+from half-doing the work. In such cases, the lines should
+be laid out as though they were to be all done at once, and,
+finally, when the omitted drains are made, it should be in
+pursuance of the original plan. Probably the drains which
+are laid will produce more than one-half of the benefit
+that would result if they were all laid, but they will rarely
+be satisfactory, except as a temporary expedient, and the
+saving will be less than would at first seem likely, for when
+the second drains are laid; the cultivation of the land
+must be again interrupted; the draining force must be
+again brought together; the levels of the new lines must
+be taken, and connected with those of the old ones; and
+great care must be taken, selecting the dryest weather for<span class="tei tei-pb" id="page160">[pg 160]</span><a name="Pg160" id="Pg160" class="tei tei-anchor"></a>
+the work,—to admit very little, if any, muddy water into
+the old mains.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This practice of draining by installments is not recommended;
+it is only suggested as an allowable expedient,
+when the cost of the complete work could not be borne
+with out inconvenience.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If any staid and economical farmer is disposed to be
+alarmed at the cost of draining, he is respectfully reminded
+of the miles of expensive stone walls and other
+fences, in New England and many other parts of the
+country, which often are a real detriment to the farms, occupying,
+with their accompanying bramble bushes and
+head lands, acres of valuable land, and causing great
+waste of time in turning at the ends of short furrows in
+plowing;—while they produce no benefit at all adequate
+to their cost and annoyance.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It should also be considered that, just as the cost of
+fences is scarcely felt by the farmer, being made when his
+teams and hands could not be profitably employed in ordinary
+farming operations, so the cost of draining will be
+reduced in proportion to the amount of the work which
+he can "do within himself,"—without hiring men expressly
+for it. The estimate herein given is based on the
+supposition that men are hired for the work, at wages
+equal to $1.50 per day,—while draining would often
+furnish a great advantage to the farmer in giving employment
+to farm hands who are paid and subsisted by the year.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<a name="toc52" id="toc52"></a><a name="pdf53" id="pdf53"></a>
+<span class="tei tei-pb" id="page161">[pg 161]</span><a name="Pg161" id="Pg161" class="tei tei-anchor"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER VII. - "WILL IT PAY?"</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Starting with the basis of $60, as the cost of draining
+an acre of ordinary farm land;—what is the prospect that
+the work will prove remunerative?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In all of the older States, farmers are glad to lend their
+surplus funds, on bond and mortgage on their neighbors'
+farms, with interest at the rate of 7, and often 6 per cent.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In view of the fact that a little attention must be given
+each year to the outlets, and, to the silt-basins, as well,
+for the first few years, it will be just to charge for the use
+of the capital 8-1/3 per cent.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This will make a yearly charge on the land, for the benefits
+resulting from such a system of draining as has been
+described, <span class="tei tei-hi"><span style="font-variant: small-caps">of five dollars per acre</span></span>.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Will it Pay?</span></span>—Will the benefits accruing, year after
+year,—in wet seasons and in dry,—with root crops and
+with grain,—with hay and with fruit,—in rotations of crops
+and in pasture,—be worth $5 an acre?</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">On this question depends the value of tile-draining as a
+<span class="tei tei-hi"><span style="font-style: italic">practical</span></span> improvement, for if there is a self-evident proposition
+in agriculture, it is that what is not profitable,
+one year with another, is <span class="tei tei-hi"><span style="font-style: italic">not</span></span> practical.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">To counterbalance the charge of $5, as the yearly cost<span class="tei tei-pb" id="page162">[pg 162]</span><a name="Pg162" id="Pg162" class="tei tei-anchor"></a>
+of the draining, each acre must produce, in addition to
+what it would have yielded without the improvement:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">10 bushels of Corn at .50 per bushel.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">3 bushels of Wheat at $1.66 per bushel.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">5 bushels of Rye at 1.00 per bushel.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">12-1/2 bushels of Oats at .40 per bushel.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">10 bushels of Potatoes at .50 per bushel.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">6-2/3 bushels of Barley at .75 per bushel.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">1,000 pounds of Hay at 10.00 per ton.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">50 pounds of Cotton at .10 per pound.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">20 pounds of Tobacco at .25 per pound.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Surely this is not a large increase,—not in a single case,—and
+the prices are generally less than may be expected
+for years to come.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The United States Census Report places the average
+crop of Indian Corn, in Indiana and Illinois, at 33 bushels
+per acre. In New York it was but 27 bushels, and in Pennsylvania
+but 20 bushels. It would certainly be accounted
+extremely liberal to fix the average yield of such soils as
+need draining, at 30 bushels per acre. It is extremely unlikely
+that they would yield this, in the average of seasons,
+with the constantly recurring injury from backward
+springs, summer droughts, and early autumn frosts.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Heavy, retentive soils, which are cold and late in the
+spring, subject to hard baking in midsummer, and to become
+cold and wet in the early fall, are the very ones which are
+best suited, when drained, to the growth of Indian Corn.
+They are "strong" and fertile,—and should be able to
+absorb, and to prepare for the use of plants, the manure
+which is applied to them, and the fertilizing matters which
+are brought to them by each storm;—but they cannot properly
+exercise the functions of fertile soils, for the reason
+that they are strangled with water, chilled by evaporation,
+or baked to almost brick-like hardness, during nearly the
+whole period of the growth and ripening of the crop.<span class="tei tei-pb" id="page163">[pg 163]</span><a name="Pg163" id="Pg163" class="tei tei-anchor"></a>
+The manure which has been added to them, as well as their
+own chemical constituents, are prevented from undergoing
+those changes which are necessary to prepare them for the
+uses of vegetation. The water of rains, finding the spaces
+in the soil already occupied by the water of previous rains,
+cannot enter to deposit the gases which it contains,—or,
+if the soil has been dried by evaporation under the influence
+of sun and wind, the surface is almost hermetically
+sealed, and the water is only slowly soaked up, much of
+it running off over the surface, or lying to be removed
+by the slow and chilling process of evaporation. In wet
+times and in dry, the air, with its heat, its oxygen, and its
+carbonic acid, (its universal solvent,) is forbidden to enter
+and do its beneficent work. The benefit resulting from
+cultivating the surface of the ground is counteracted by
+the first unfavorable change of the weather; a single heavy
+rain, by saturating the soil, returning it to nearly its original
+condition of clammy compactness. In favorable
+seasons, these difficulties are lessened, but man has no control
+over the seasons, and to-morrow may be as foul as
+to-day has been fair. A crop of corn on undrained, retentive
+ground, is subject to injury from disastrous changes
+of the weather, from planting until harvest. Even supposing
+that, in the most favorable seasons, it would yield
+as largely as though the ground were drained, it would
+lose enough in unfavorable seasons to reduce the average
+more than ten (10) bushels per acre.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The average crop, on such land, has been assumed to be
+30 bushels per acre; it would be an estimate as moderate
+as this one is generous, to say that, with the same cultivation
+and the same manure, the average crop, after draining,
+would be 50 bushels, or an increase equal to twice as
+much as is needed to pay the draining charge. If the
+method of cultivation is improved, by deep plowing, ample
+manuring, and thorough working,—all of which may
+be more profitably applied to drained than to undrained<span class="tei tei-pb" id="page164">[pg 164]</span><a name="Pg164" id="Pg164" class="tei tei-anchor"></a>
+land,—the <span class="tei tei-hi"><span style="font-style: italic">average</span></span> crop,—of a series of years,—will not
+be less than 60 bushels.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The cost of extra harvesting will be more than repaid
+by the value of the extra fodder, and the increased cultivation
+and manuring are lasting benefits, which can be
+charged, only in small part, to the current crop. Therefore,
+if it will pay to plow, plant, hoe and harvest for 30
+bushels of corn, it will surely pay much better to double
+the crop at a yearly extra cost of $5, and, practically, it
+amounts to this;—the extra crop is nearly all clear gain.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The quantity of Wheat required to repay the annual
+charge for drainage is so small, that no argument is needed
+to show that any process which will simply prevent
+"throwing out" in winter, and the failure of the plant in
+the wetter parts of the field, will increase the product
+more than that amount,—to say nothing of the general
+importance to this crop of having the land in the most
+perfect condition, (in winter as well as in summer.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is stated that, since the general introduction of drainage
+in England, (within the past 25 years,) the wheat
+crop of that country has been more than doubled. Of
+course, it does not necessarily follow that the amount <span class="tei tei-hi"><span style="font-style: italic">per
+acre</span></span> has been doubled, large areas which were originally
+unfit for the growth of this crop, having been, by draining,
+excellently fitted for its cultivation;—but there can be no
+doubt that its yield has been greatly increased on all
+drained lands, nor that large areas, which, before being
+drained, were able to produce fair crops only in the best
+seasons, are now made very nearly independent of the
+weather.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is not susceptible of demonstration, but it is undoubtedly
+true, that those clay or other heavy soils, which are
+devoted to the growth of wheat in this country, would,
+if they were thoroughly under-drained, produce, on the
+average of years, at least double their present crop.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Mr. John Johnston, a venerable Scotch farmer, who has<span class="tei tei-pb" id="page165">[pg 165]</span><a name="Pg165" id="Pg165" class="tei tei-anchor"></a>
+long been a successful cultivator in the Wheat region of
+Western New York,—and who was almost the pioneer of
+tile-draining in America,—has laid over 50 miles of drains
+within the last 30 years. His practice is described in
+Klippart's Land Drainage, from which work we quote the
+following:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Mr. Johnston says he never saw 100 acres in any one
+farm, but a portion of it would pay for draining. Mr.
+Johnston is no rich man who has carried a favorite hobby
+without regard to cost or profit. He is a hardworking
+Scotch farmer, who commenced a poor man, borrowed
+money to drain his land, has gradually extended his
+operations, and is now reaping the benefits, in having
+crops of 40 bushels of wheat to the acre. He is a gray-haired
+Nestor, who, after accumulating the experience
+of a long life, is now, at 68 years of age, written to by
+strangers in every State of the Union for information,
+not only in drainage matters, but all cognate branches
+of farming. He sits in his homestead, a veritable Humboldt
+in his way, dispensing information cheerfully
+through our agricultural papers and to private correspondents,
+of whom he has recorded 164 who applied to
+him last year. His opinions are, therefore, worth more
+than those of a host of theoretical men, who write without
+practice." * * * * *</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Although his farm is mainly devoted to wheat, yet a
+considerable area of meadow and some pasture has been
+retained. He now owns about 300 acres of land. The
+yield of wheat has been 40 bushels this year, and in former
+seasons, when his neighbors were reaping 8, 10, or
+15 bushels, he has had 30 and 40." * * * * *</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Mr. Johnston says tile-draining pays for itself in two
+seasons, sometimes in one. Thus, in 1847, he bought a
+piece of 10 acres to get an outlet for his drains. It was
+a perfect quagmire, covered with coarse aquatic grasses,
+and so unfruitful that it would not give back the seed<span class="tei tei-pb" id="page166">[pg 166]</span><a name="Pg166" id="Pg166" class="tei tei-anchor"></a>
+sown upon it. In 1848 a crop of corn was taken from it,
+which was measured and found to be <span class="tei tei-hi"><span style="font-style: italic">eighty bushels</span></span> per
+acre, and as, because of the Irish famine, corn was worth
+$1 per bushel that year, this crop paid not only all the expense
+of drainage, but the first cost of the land as well.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Another piece of 20 acres, adjoining the farm of the
+late John Delafield, was wet, and would never bring
+more than 10 bushels of corn per acre. This was drained
+at a great cost, nearly $30 per acre. The first crop after
+this was 83 bushels and some odd pounds per acre. It
+was weighed and measured by Mr. Delafield, and the
+County Society awarded a premium to Mr. Johnston.
+Eight acres and some rods of this land, at one side, averaged
+94 bushels, or the trifling increase of 84 bushels
+per acre over what it would bear before those insignificant
+clay tiles were buried in the ground. But this increase
+of crop is not the only profit of drainage; for Mr.
+Johnston says that, on drained land, one half the usual
+quantity of manure suffices to give maximum crops. It
+is not difficult to find a reason for this. When the soil
+is sodden with water, air can not enter to any extent,
+and hence oxygen can not eat off the surfaces of soil-particles
+and prepare food for plants; thus the plant
+must in great measure depend on the manure for sustenance,
+and, of course, the more this is the case, the more
+manure must be applied to get good crops. This is one
+reason, but there are others which we might adduce if
+one good one were not sufficient.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Mr. Johnston says he never made money until he
+drained, and so convinced is he of the benefits accruing
+from the practice, that he would not hesitate,—as he did
+not when the result was much more uncertain than at
+present,—to borrow money to drain. Drains well laid,
+endure, but unless a farmer intends doing the job well,
+he had best leave it alone and grow poor, and move out
+West, and all that sort of thing. Occupiers of apparently<span class="tei tei-pb" id="page167">[pg 167]</span><a name="Pg167" id="Pg167" class="tei tei-anchor"></a>
+dry land are not safe in concluding that they need
+not go to the expense of draining, for if they will but
+dig a three-foot ditch in even the driest soil, water will
+be found in the bottom at the end of eight hours, and
+if it does come, then draining will pay for itself
+speedily."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Some years ago, the Rural New Yorker published a
+letter from one of its correspondents from which the following
+is extracted:—</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"I recollect calling upon a gentleman in the harvest field, when something
+like the following conversation occurred:</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Your wheat, sir, looks very fine; how many acres have you in this
+field?'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'In the neighborhood of eight, I judge.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Did you sow upon fallow?'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'No sir. We turned over green sward—sowed immediately upon the
+sod, and dragged it thoroughly—and you see the yield will probably be
+25 bushels to the acre, where it is not too wet.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Yes sir, it is mostly very fine. I observed a thin strip through it,
+but did not notice that it was wet.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Well, it is not </span><span class="tei tei-hi"><span style="font-size: 90%; font-style: italic">very</span></span><span style="font-size: 90%"> wet. Sometimes after a rain, the water runs
+across it, and in spring and fall it is just wet enough to heave the wheat
+and kill it.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">I inquired whether a couple of good drains across the lot would not
+render it dry.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Perhaps so—but there is not over an acre that is killed out.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Have you made an estimate of the loss you annually sustain from
+this wet place?'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'No, I had not thought much about it.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Would $30 be too high?'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'O yes, double.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Well, let's see; it cost you $3 to turn over the sward? Two bushels
+of seed, $2; harrowing in, 75 cents; interest, taxes, and fences,
+$5.25; 25 bushels of wheat lost, $25.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Deduct for harvesting—--'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'No; the straw would pay for that.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Very well, all footed $36.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'What will the wheat and straw on this acre be worth this year?'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Nothing, as I shall not cut the ground over.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Then it appears that you have lost, in what you have actually expended,
+and the wheat you would have harvested, had the ground been
+dry, $36, a pretty large sum for one acre.'</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">'Yes I see,' said the farmer."</span></p>
+</div>
+
+<span class="tei tei-pb" id="page168">[pg 168]</span><a name="Pg168" id="Pg168" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">While Rye may be grown, with tolerable advantage, on
+lands which are less perfectly drained than is necessary
+for Wheat, there can be no doubt that an increase of more
+than the six and two-thirds bushels needed to make up the
+drainage charge will be the result of the improvement.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">While Oats will thrive in soils which are too wet for
+many other crops, the ability to plant early, which is secured
+by an early removal from the soil of its surplus water,
+will ensure, one year with another, more than twelve
+and a half bushels of increased product.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the case of Potatoes, also, the early planting will be
+a great advantage; and, while the cause of the potato-rot
+is not yet clearly discovered, it is generally conceded
+that, even if it does not result directly from too great
+wetness of the soil, its development is favored by this
+condition, either from a direct action on the tubers, or
+from the effect in the air immediately about the plants,
+of the exhalations of a humid soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">An increase of from five to ten per cent. on a very ordinary
+crop of potatoes, will cover the drainage charge,
+and with facilities for marketing, the higher price of the
+earlier yield is of much greater consequence.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Barley will not thrive in wet soil, and there is no question
+that drainage would give it much more than the increased
+yield prescribed above.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As to hay, there are many wet, rich soils which produce
+very large crops of grass, and it is possible that drainage
+might not always cause them to yield a thousand pounds
+more of hay to the acre, but the <span class="tei tei-hi"><span style="font-style: italic">quality</span></span> of the hay from
+the drained soil, would, of itself, more than compensate
+for the drainage charge. The great benefit of the improvement,
+with reference to this crop, however, lies in
+the fact that, although wet, grass lands,—and by "wet" is
+meant the condition of undrained, retentive clays, and
+heavy loams, or other soils requiring drainage,—in a very
+few years "run out," or become occupied by semi-aquatic<span class="tei tei-pb" id="page169">[pg 169]</span><a name="Pg169" id="Pg169" class="tei tei-anchor"></a>
+and other objectionable plants, to the exclusion of the
+proper grasses; the same lands, thoroughly drained, may
+be kept in full yield of the finest hay plants, as long as the
+ground is properly managed. It must, of course, be manured,
+from time to time, and care should be taken to prevent
+the puddling of its surface, by men or animals,
+while it is too wet from recent rain. With proper attention
+to these points, it need not be broken up in a lifetime,
+and it may be relied on to produce uniformly good crops,
+always equal to the best obtained before drainage.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">So far as Cotton and Tobacco are concerned, there are
+not many instances recorded of the systematic drainage
+of lands appropriated to their cultivation, but there is
+every reason to suppose that they will both be benefitted
+by any operation which will have the effect of placing the
+soil in a better condition for the uses of all cultivated
+plants. The average crop of tobacco is about 700 lbs.,
+and that of cotton probably 250 lbs. An addition of one-fifth
+to the cotton crop, and of only one thirty-fifth to the
+tobacco crop, would make the required increase.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The failure of the cotton crop, during the past season,
+(1866,) might have been entirely prevented, in many districts,
+by the thorough draining of the land.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The advantages claimed for drainage with reference to
+the above-named staple crops, will apply with equal, if not
+greater force, to all garden and orchard culture. In fact,
+with the exception of osier willows, and cranberries, there
+is scarcely a cultivated plant which will not yield larger
+and better crops on drained than on undrained land,—enough
+better, and enough larger, to pay much more than
+the interest on the cost of the improvement.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Yet, this advantage of draining, is, by no means, the
+only one which is worthy of consideration. Since the
+object of cultivation is to produce remunerative crops, of
+course, the larger and better the crops, the more completely
+is the object attained;—and to this extent the greatest<span class="tei tei-pb" id="page170">[pg 170]</span><a name="Pg170" id="Pg170" class="tei tei-anchor"></a>
+benefit resulting from draining, lies in the increased yield.
+But there is another advantage,—a material and moral
+advantage,—which is equally to be considered.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Instances of the profit resulting from under-draining,
+(coupled, as it almost always is, with improved cultivation,)
+are frequently published, and it would be easy to
+fortify this chapter with hundreds of well authenticated
+cases. It is, however, deemed sufficient to quote the following,
+from an old number of one of the New York
+dailies:—</p>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"Some years ago, the son of an English farmer came to the United
+States, and let himself as a farm laborer, in New York State, on the following
+conditions: Commencing work at the first of September, he was
+to work ten hours a day for three years, and to receive in payment a
+deed of a field containing twelve acres—securing himself by an agreement,
+by which his employer was put under bonds of $2,000 to fulfill his
+part of the contract; also, during these three years, he was to have the
+control of the field; to work it at his own expense, and to give his employer
+one-half the proceeds. The field lay under the south side of a
+hill, was of dark, heavy clay resting on a bluish-colored, solid clay subsoil,
+and for many years previous, had not been known to yield anything
+but a yellowish, hard, stunted vegetation.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"The farmer thought the young man was a simpleton, and that he,
+himself, was most wise and fortunate; but the former, nothing daunted
+by this opinion, which he was not unconscious that the latter entertained
+of him, immediately hired a set of laborers, and set them to work in
+the field trenching, as earnestly as it was well possible for men to labor.
+In the morning and evening, before and after having worked his ten
+hours, as per agreement, he worked with them, and continued to work
+in this way until, about the middle of the following November, he had
+finished the laying of nearly 5,000 yards of good tile under-drains. He
+then had the field plowed deep and thoroughly, and the earth thrown up
+as much as possible into ridges, and thus let it remain during the winter.
+Next spring he had the field again plowed as before, then cross-plowed
+and thoroughly pulverized with a heavy harrow, then sowed it
+with oats and clover. The yield was excellent—nothing to be compared
+to it had ever before been seen upon that field. Next year it gave two
+crops of clover, of a rich dark green, and enormously heavy and luxuriant;
+and the year following, after being manured at an expense of some
+$7 an acre, nine acres of the field yielded 936 bushels of corn, and 25
+wagon loads of pumpkins; while from the remaining three acres were
+taken 100 bushels of potatoes—the return of this crop being upwards
+of $1,200. The time had now come for the field to fall into the young</span><span class="tei tei-pb" id="page171">[pg 171]</span><a name="Pg171" id="Pg171" class="tei tei-anchor"></a><span style="font-size: 90%">
+man's possession, and the farmer unhesitatingly offered him $1,500 to
+relinquish his title to it; and when this was unhesitatingly refused, he
+offered $2,000, which was accepted.</span></p>
+
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"The young man's account stood thus</span></p>
+
+<table summary="This is a table" cellspacing="0" class="tei tei-table" style="margin-bottom: 0.90em"><colgroup span="2"></colgroup><tbody><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Half proceeds of oats and straw, first year</span></td><td class="tei tei-cell"><span style="font-size: 90%">$165 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Half value of sheep pasturage, first year</span></td><td class="tei tei-cell"><span style="font-size: 90%">25 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Half of first crops of clover, first year</span></td><td class="tei tei-cell"><span style="font-size: 90%">112 50</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Half of second crops of clover, including seed, second year</span></td><td class="tei tei-cell"><span style="font-size: 90%">135 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Half of sheep pasturage, second year</span></td><td class="tei tei-cell"><span style="font-size: 90%">15 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Half of crops of corn, pumpkins and potatoes, third year</span></td><td class="tei tei-cell"><span style="font-size: 90%">690 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Received from farmer, for relinquishment of title</span></td><td class="tei tei-cell"><span style="font-size: 90%">2,000 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"></td><td class="tei tei-cell"><span style="font-size: 90%">———</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Account Dr.</span></td><td class="tei tei-cell"><span style="font-size: 90%">$3,142 50</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">To under-draining, labor and tiles</span></td><td class="tei tei-cell"><span style="font-size: 90%">$325 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">To labor and manure, three seasons</span></td><td class="tei tei-cell"><span style="font-size: 90%">475 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">To labor given to farmer, $16 per month, 36 months</span></td><td class="tei tei-cell"><span style="font-size: 90%">576 00—1,376 00</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"></td><td class="tei tei-cell"><span style="font-size: 90%">———</span></td>
+</tr><tr class="tei tei-row">
+<td class="tei tei-cell"><span style="font-size: 90%">Balance in his favor</span></td><td class="tei tei-cell"><span style="font-size: 90%">$1,766 50</span></td>
+</tr></tbody></table>
+</div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Draining makes the farmer, to a great extent, the
+master of his vocation. With a sloppy, drenched, cold,
+uncongenial soil, which is saturated with every rain, and
+takes days, and even weeks, to become sufficiently dry to
+work upon, his efforts are constantly baffled by unfavorable
+weather, at those times when it is most important that
+his work proceed without interruption. Weeks are lost,
+at a season when they are all too short for the work to be
+done. The ground must be hurriedly, and imperfectly
+prepared, and the seed is put in too late, often to rot in the
+over-soaked soil, requiring the field to be planted again at
+a time which makes it extremely doubtful whether the
+crop will ripen before the frost destroys it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The necessary summer cultivation, between the rows,
+has to be done as the weather permits; and much more
+of it is required because of the baking of the ground.
+The whole life of the farmer, in fact, becomes a constant
+struggle with nature, and he fights always at a disadvantage.
+What he does by the work of days, is mainly undone
+by a single night's storm. Weeds grow apace, and
+the land is too wet to admit of their being exterminated.
+By the time that it is dry enough, other pressing work<span class="tei tei-pb" id="page172">[pg 172]</span><a name="Pg172" id="Pg172" class="tei tei-anchor"></a>
+occupies the time; and if, finally, a day comes when they
+may be attacked, they offer ten times the resistance that
+they would have done a week earlier. The operations of
+the farm are carried on more expensively than if the
+ability to work constantly allowed a smaller force to be
+employed. The crops which give such doubtful promise,
+require the same cultivation as though they were certain
+to be remunerative, and the work can be done only with
+increased labor, because of the bad condition of the soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">From force of tradition and of habit, the farmer accepts
+his fate and plods through his hard life, piously ascribing
+to the especial interference of an inscrutable Providence,
+the trials which come of his own neglect to use the means
+of relief which Providence has placed within his reach.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Trouble enough he must have, at any rate, but not necessarily
+all that he now has. It is not within the scope
+of the best laid drains to control storm or sunshine,—but
+it is within their power to remove the water of the storm,
+rapidly and sufficiently, and to allow the heat of the sunshine
+to penetrate the soil and do its hidden work. No
+human improvement can change any of the so-called
+"phenomena" of nature, or prevent the action of the
+least of her laws; but their effects upon the soil and its
+crops may be greatly modified, and that which, under certain
+circumstances, would have caused inconvenience or
+loss, may, by a change of circumstances, be made positively
+beneficial.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the practice of agriculture, which is pre-eminently
+an economic art, draining will be prosecuted because of
+the pecuniary profit which it promises, and,—very properly,—it
+will not be pursued, to any considerable extent,
+where the money, which it costs, will not bring money in
+return. Yet, in a larger view of the case, its collateral
+advantages are of even greater moment than its mere
+profits. It is the foundation and the commencement of
+the most intelligent farming. It opens the way for other<span class="tei tei-pb" id="page173">[pg 173]</span><a name="Pg173" id="Pg173" class="tei tei-anchor"></a>
+improvements, which, without it, would produce only
+doubtful or temporary benefits; and it enables the farmer
+so to extend and enlarge his operations, with fair promise
+of success, as to raise his occupation from a mere waiting
+upon the uncertain favors of nature, to an intelligent
+handling of her forces, for the attainment of almost certain
+results.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The rude work of an unthinking farmer, who scratches
+the surface soil with his plow, plants his seed, and trusts
+to the chances of a greater or less return, is unmitigated
+drudgery,—unworthy of an intelligent man; but he
+who investigates all of the causes of success and failure in
+farming, and adapts every operation to the requirements
+of the circumstances under which he works; doing everything
+in his power that may tend to the production of the
+results which he desires, and, so far as possible, avoiding
+everything that may interfere with his success,—leaving
+nothing to chance that can be secured, and securing all
+that chance may offer,—is engaged in the most ennobling,
+the most intelligent and the most progressive of all industrial
+avocations.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the cultivation of retentive soils, drainage is the key
+to all improvement, and its advantage is to be measured
+not simply by the effect which it directly produces in increasing
+production, but, in still greater degree, by the
+extent to which it prepares the way for the successful application
+of improved processes, makes the farmer independent
+of weather and season, and offers freer scope to
+intelligence in the direction of his affairs.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page174">[pg 174]</span><a name="Pg174" id="Pg174" class="tei tei-anchor"></a>
+<a name="toc54" id="toc54"></a>
+<a name="pdf55" id="pdf55"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER VIII. - HOW TO MAKE DRAINING TILES.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Draining tiles are made of burnt clay, like bricks and
+earthen-ware.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In general terms, the process is as follows:—The clay is
+mixed with sand, or other substances which give it the proper
+consistency, and is so wetted as to form a plastic mass, to
+which may be given any desired form, and which is sufficiently
+stiff to retain its shape. Properly prepared clay is
+forced through the aperture of a die of the shape of the outside
+of the tile, while a plug,—held by a support in the rear
+of the die,—projects through the aperture, and gives the
+form to the bore of the tile. The shape of the material
+of the tile, as it comes from the die, corresponds to the
+open space, between the plug and the edge of the aperture.
+The clay is forced out in a continuous pipe, which
+is cut to the desired length by a wire, which is so thin as
+to pass through the mass without altering the shape of the
+pipe. The short lengths of pipe are dried in the air as
+thoroughly as they can be, and are then burned in a kiln,
+similar to that used for pottery.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Materials.</span></span>—The range of earths which may be used in
+the manufacture of tiles is considerable, though clay is
+the basis of all of them. The best is, probably, the clay<span class="tei tei-pb" id="page175">[pg 175]</span><a name="Pg175" id="Pg175" class="tei tei-anchor"></a>
+which is almost invariably found at the bottom of muck
+beds, as this is finer and more compact than that which is
+dug from dry land, and requires but little preparation.
+There is, also, a peculiar clay, found in some localities,
+which is almost like quick-sand in its nature, and which is
+excellent for tile-making,—requiring no freezing, or washing
+to prepare it for the machine. As a general rule, any
+clay which will make <span class="tei tei-hi"><span style="font-style: italic">good</span></span> bricks will make tiles. When
+first taken from the ground, these clays are not usually adhesive,
+but become so on being moistened and kneaded.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is especially important that no limestone <span class="tei tei-hi"><span style="font-style: italic">pebbles</span></span> be
+mixed with the clay, as the burning would change these
+to quicklime, which, in slaking, would destroy the tiles.
+The presence of a limey earth, however, mixed through
+the mass, is a positive advantage, as in this intimate
+admixture, the lime forms, under the heat of the
+kiln, a chemical combination with the other ingredients;
+and, as it melts more readily than some of them, it hastens
+the burning and makes it more complete. What is
+known as <span class="tei tei-hi"><span style="font-style: italic">plastic clay</span></span>, (one of the purest of the native
+clays,) is too strong for tile-making, and must be "tempered,"
+by having other substances mixed with it, to give
+it a stiffer quality.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The clay which is best for brick-making, contains
+Silica, and Alumina in about the following proportions:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Silica ... 55 to 75 per cent.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">Alumina ... 35 to 25 per cent.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Variable quantities of other materials are usually found
+in connection with the clay, in its native condition. The
+most common of these are the following:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Magnesia 1 to 5 per cent.—sometimes 20 to 30 per cent.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">Lime 0 to 19 per cent.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">Potash 0 to 5 per cent.</p>
+<p class="tei tei-p" style="margin-bottom: 1.00em">Oxyd of iron 0 to 19 per cent.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"These necessary elements give fusibility to earthenware,<span class="tei tei-pb" id="page176">[pg 176]</span><a name="Pg176" id="Pg176" class="tei tei-anchor"></a>
+and, therefore, allow its constituent substances to
+combine in such a manner as to form a resisting body;
+and thus is performed with a temperature lower in proportion
+as the necessary elements are more abundant."<a id="noteref_23" name="noteref_23" href="#note_23"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">23</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When the earth of the locality where tiles are to be
+made is not sufficiently strong for the purpose, and plastic
+clay can be cheaply obtained from a distance, a small
+quantity of this may be used to give strength and tenacity
+to the native material.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The compound must always contain a proper proportion
+of clay and sand. If too little <span class="tei tei-hi"><span style="font-style: italic">clay</span></span> is used, the mass will
+not be sufficiently tough to retain its compactness as it
+passes through the die of the tile machine; if too little
+<span class="tei tei-hi"><span style="font-style: italic">sand</span></span>, the moulded tiles will not be strong enough to bear
+handling, and they will crack and warp in drying and burning.
+Within the proper limits, the richer earths may be
+moulded much thinner, and tiles made from them may,
+consequently, be made lighter for transportation, without
+being too weak. The best materials for tempering stiff
+clays are sand, pounded brick or tile, or <span class="tei tei-hi"><span style="font-style: italic">scoria</span></span>, from
+smelting furnaces.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Preparation Of Earths.</span></span>—The clay from which tiles are
+to be made, should be thrown out in the fall, (the upper
+and lower parts of the beds being well mixed in the operation,)
+and made into heaps on the surface, not more than
+about 3 feet square and 3 feet high. In this form, it is left
+exposed to the freezing and thawing of winter, which will
+aid very much in modifying its character,—making it less
+lumpy and more easily workable. Any stones which may
+appear in the digging, should, of course, be removed, and
+most earths will be improved by being passed through a
+pair of heavy iron rollers, before they are piled up for the
+winter. The rollers should be made of cast iron, about
+15 inches in diameter, and 30 inches long, and set as close<span class="tei tei-pb" id="page177">[pg 177]</span><a name="Pg177" id="Pg177" class="tei tei-anchor"></a>
+together as they can be, and still be revolved by the power
+of two horses. The grinding, by means of these rollers,
+may add 50 cents per thousand to the cost of the tiles,
+but it will greatly improve their quality.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the spring, the clay should be prepared for tempering,
+by the removal of such pebbles as it may still contain.
+The best way to do this is by "washing," though, if there
+be only a few coarse pebbles, they may be removed by
+building the clay into a solid cone 2 or 3 feet high, and
+then paring it off into thin slices with a long knife having
+a handle at each end. This paring will discover any pebbles
+larger than a pea that may have remained in the clay.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Washing</span></span> is the process of mixing the clay with a considerable
+quantity of water, so as to form a thin paste, in
+which all stones and gravel will sink to the bottom; the
+liquid portion is then drawn off into shallow pits or vats,
+and allowed to settle, the clear water being finally removed
+by pumping or by evaporation, according to the
+need for haste. For washing small quantities of clay, a
+common mortar bed, such as is used by masons, will answer,
+if it be supplied with a gate for draining off the
+muddy water after the gravel has settled; but, if the work
+is at all extensive, a washing mill will be required. It
+may be made in the form of a circular trough, with scrapers
+for mixing the clay and water attached to a circular
+horse-sweep.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Another convenient mixing machine may be constructed
+in the following manner: Take a large hollow log, of suitable
+length, say five or six feet; hew out the inequalities
+with an adz, and close up the ends with pieces of strong
+plank, into which bearing have been cut to support a revolving
+shaft. This shaft should be sufficiently thick to
+permit being transfixed with wooden pins long enough to
+reach within an inch or two of the sides of the log or
+trough, and they should be so beveled as to form in their
+aggregate shape an interrupted screw, having a direction<span class="tei tei-pb" id="page178">[pg 178]</span><a name="Pg178" id="Pg178" class="tei tei-anchor"></a>
+toward that end of the box where the mixed clay is designed
+to pass out. In order to effect the mixing more
+thoroughly, these pins may be placed sufficiently far apart
+to permit the interior of the box to be armed with other
+pins extending toward the center, between which they
+can easily move. The whole is placed either horizontally
+or vertically, and supplied with clay and water in proper
+quantities, while the shaft is made to revolve by means of
+a sweep, with horse power, running water or steam, as
+the case may be. The clay is put into the end farthest
+from the outlet, and is carried forward to it and mixed
+by the motion, and mutual action and re-action of the pins
+in the shaft and in the sides of the box. Iron pins may,
+of course, be substituted for the wooden ones, and have
+the advantage of greater durability and of greater strength
+in proportion to their size, and the number may therefore
+be greater in a machine of any given length. The fluid
+mass of clay and water may be permitted to fall upon a
+sieve or riddle, of heavy wire, and afterward be received
+in a settling vat, of suitable size and construction, to drain
+off the water and let the clay dry out sufficiently by subsequent
+evaporation. A machine of this construction
+may be made of such a size that it may be put in motion
+by hand, by means of a crank, and yet be capable of
+mixing, if properly supplied, clay enough to mold 800
+or 1000 pieces of drain pipe per day."<a id="noteref_24" name="noteref_24" href="#note_24"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">24</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Mr. Parkes, in a report to the Royal Agricultural Society
+of England, in 1843, says:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It is requisite that the clay be well washed and sieved
+before pugging, for the manufacture of these tiles, or the
+operation of drawing them would be greatly impeded, by
+having to remove stones from the small space surrounding
+the die, which determines the thickness of the pipe.
+But it results from this necessary washing, that the substance<span class="tei tei-pb" id="page179">[pg 179]</span><a name="Pg179" id="Pg179" class="tei tei-anchor"></a>
+of the pipe is uniformly and extremely dense,
+which, consequently, gives it immense strength, and ensures
+a durability which cannot belong to a more porous,
+though thicker, tile.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The clay is brought from the pug-mill so dry that,
+when squeezed through the machine, not a drop of water
+exudes,—moisture is, indeed, scarcely apparent on the
+surface of the raw pipe. Hence, the tiles undergo little
+or no change of figure while drying, which takes place
+very rapidly, because of their firm and slight substance."</p>
+
+<a name="fig56" id="fig56"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image42.png" width="640" height="921" alt="Illustration: Fig. 42 - PUG-MILL." title="Fig. 42 - PUG-MILL." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 42 - PUG-MILL.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Tempering.</span></span>—After the fine clay is relieved of the water
+with which it was washed, and has become tolerably dry, it
+should be mixed with the sand, or other tempering material,
+and passed through the
+<span class="tei tei-hi"><span style="font-style: italic">Pug-Mill</span></span>, (Fig. 42,) which will
+thoroughly mix its various ingredients,
+and work the whole into a
+homogeneous mass, ready for the
+tile machine. The <span class="tei tei-hi"><span style="font-style: italic">pug-mill</span></span> is
+similar to that used in brick-yards,
+only, as the clay is worked much
+stiffer for tiles than for bricks,
+iron knives must be substituted
+for the wooden pins. These
+knives are so arranged as to cut
+the clay in every part, and, by
+being set at an angle, they force it
+downward toward the outlet gate
+at the bottom. The clay should
+be kept at the proper degree of moisture from the time of
+tempering, and after passing through the pug-mill it
+should be thoroughly beaten to drive out the air, and the
+beaten mass should be kept covered with wet cloths to
+prevent drying.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Moulding the Tiles.</span></span>—Machines for moulding tiles are<span class="tei tei-pb" id="page180">[pg 180]</span><a name="Pg180" id="Pg180" class="tei tei-anchor"></a>
+of various styles, with much variation in the details of
+their construction, but they all act on the same general
+principle;—that of forcing the clay through a ring-shaped
+aperture in an iron plate, forming a continuous pipe, which
+is carried off on an endless apron, or on rollers, and cut
+by wires into the desired lengths. The plates with the
+ring-shaped apertures are called <span class="tei tei-hi"><span style="font-style: italic">dies</span></span>; the openings are
+of any desired form, corresponding to the external shape
+of the tiles; and the size and shape
+of the bore, is determined by the
+core or plug, which is held in the
+centers of the apertures. The construction
+of the die plates, and the
+manner of fastening the plugs,
+which determine the bore of the tiles, is shown in Fig. 43.
+The view taken is of the inside of the plate.</p>
+
+<a name="fig57" id="fig57"></a><div class="floatright tei tei-figure" style="text-align: center; margin-left: 2.00em"><img src="images/image43.png" width="640" height="325" alt="Illustration: Fig. 43 - PLATE OF DIES." title="Fig. 43 - PLATE OF DIES." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 43 - PLATE OF DIES.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The machine consists usually of a strong iron chest,
+with a hinged cover, into which the clay is placed, having
+a piston moving in it, connected by a rod or bar, having
+cog-teeth, with a cog-wheel, which is moved by horse or
+hand power, and drives the piston forward with steadiness,
+forcing the clay through the openings in the die-plate.
+The clay issues in continuous lines of pipe. The machines
+most in use in this country are connected directly with
+the pug-mill, and as the clay is pugged, it at once passes
+into the box, and is pressed out as tiles. These machines
+are usually run by horse-power.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Mr. Barral, in his voluminous work on drainage,<a id="noteref_25" name="noteref_25" href="#note_25"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">25</span></span></a> describes,
+as follows, a cheap hand machine which can be
+made by any country wheelwright, and which has a capacity
+of 3,000 tiles per day (Fig. 44):</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Imagine a simple, wooden box, divided into two compartments.
+In the rear compartment there stands a
+vertical post, fastened with two iron bolts, having heads<span class="tei tei-pb" id="page181">[pg 181]</span><a name="Pg181" id="Pg181" class="tei tei-anchor"></a>
+at one end, and nuts and screws at the other. The box
+is thus fixed to its support. We simply place this support
+on the ground and bind its upper part with a rope
+to a tree, a stake, or a post. The front compartment is
+the reservoir for the clay, presenting at its front an
+orifice, in which we fix the desired die with a simple bolt.
+A wooden piston, of which the rod is jointed with a
+lever, which works in a bolt at the top of the supporting
+post, gives the necessary pressure. When the chest is
+full of clay, we bear down on the end of the lever,
+and the moulded tiles run out on a table supplied with
+rollers. Raising the piston, it comes out of the box,
+which is again packed with clay. The piston is replaced
+in the box; pressure is again applied to the lever, and
+so on. When the line of tiles reaches the end of the
+table, we lower a frame on which brass wires are
+stretched, and cut it into the usual lengths."</p>
+
+<a name="fig58" id="fig58"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image44.png" width="640" height="316" alt="Fig. 44 - CHEAP WOODEN MACHINE." title="Fig. 44 - CHEAP WOODEN MACHINE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 44 - CHEAP WOODEN MACHINE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The workmen must attend well to the degree of moisture
+of the clay which is put into the machine. It should
+be dry enough to show no undue moisture on its surface
+as it comes out of the die-plate, and sufficiently moist not<span class="tei tei-pb" id="page182">[pg 182]</span><a name="Pg182" id="Pg182" class="tei tei-anchor"></a>
+to be crumbled in passing the edge of the mould. The
+clay for small (thin) tiles must, necessarily, be more moist
+than that which is to pass through a wider aperture; and
+for the latter there may, with advantage, be more sand in
+the paste than would be practicable with the former.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">After the tiles are cut into lengths, they are removed
+by a set of mandrils, small enough to pass easily into
+them, such as are shown in Fig. 45, (the number of fingers
+corresponding with the
+number of rows of tiles
+made by the machine,) and
+are placed on shelves made
+of narrow strips sawn from
+one-inch boards, laid with spaces between them to allow
+a free circulation of air.</p>
+
+<a name="fig59" id="fig59"></a><div class="floatleft tei tei-figure" style="text-align: center; margin-right: 2.00em"><img src="images/image45.png" width="640" height="118" alt="Fig. 45 - MANDRIL FOR CARRYING TILES FROM MACHINE." title="Fig. 45 - MANDRIL FOR CARRYING TILES FROM MACHINE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 45 - MANDRIL FOR CARRYING TILES FROM MACHINE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Drying and Rolling.</span></span>—Care must be taken that freshly
+made tiles be not dried too rapidly. They should be
+sheltered from the sun and from strong winds. Too rapid
+drying has the effect of warping them out of shape, and,
+sometimes, of cracking the clay. To provide against this
+injury, the drying is done under sheds or other covering,
+and the side which is exposed to the prevailing winds is
+sometimes boarded up.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For the first drying, the tiles are placed in single layers
+on the shelves. When about half dried,—at which time
+they are usually warped more or less from their true
+shape,—it is well to <span class="tei tei-hi"><span style="font-style: italic">roll</span></span> them. This is done by passing
+through them a smooth, round stick, (sufficiently smaller
+than the bore to enter it easily, and long enough to project
+five or six inches beyond each end of the tile,) and,—holding
+one end of the stick in each hand,—rolling them
+carefully on a table. This operation should be performed
+when the tiles are still moist enough not to be broken by
+the slight bending required to make them straight. After
+rolling, the tiles may be piled up in close layers, some<span class="tei tei-pb" id="page183">[pg 183]</span><a name="Pg183" id="Pg183" class="tei tei-anchor"></a>
+four or five feet high, (which will secure them against
+further warping,) and left until they are dry enough for
+burning,—that is, as dry as they can be made by exposure
+to the air.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Burning.</span></span>—Tiles are burned in kilns in which, by the
+effect of flame acting directly upon them, they are raised
+to a heat sufficient to melt some of their more easily fusible
+ingredients, and give to them a stone-like hardness.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Kilns are of various construction and of various sizes.
+As this book is not intended for the instruction of those
+who are engaged in the general manufacture of tiles, only
+for those who may find it necessary to establish local
+works, it will be sufficient to describe a temporary earthen
+kiln which may be cheaply built, and which will answer
+an excellent purpose, where only 100,000 or 200,000 tiles
+per season will be required.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Directions for its construction are set forth in a letter
+from Mr. T. Law Hodges, of England, to the late Earl
+Spencer, published in the Journal of the Royal Agricultural
+Society for the year 1843, as follows:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The form of the clay-kiln is circular, 11 feet in diameter,
+and 7 feet high. It is wholly built of damp, clayey
+earth, rammed firmly together, and plastered, inside and
+out, with loam (clay?). The earth to form the walls is dug
+out around the base, leaving a circular trench about four
+feet wide and as many deep, into which the fire-holes of
+the kiln open. If wood be the fuel used, three fire-holes
+will be sufficient; if coal, four will be needed. About
+1,200 common brick will be wanted to build these fire-holes
+and flues; if coal is used, rather fewer bricks will
+be wanted, but, then, some iron bars are necessary,—six
+bars to each fire-hole.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The earthen walls are four feet thick at the floor of
+the kiln, seven feet high, and tapering to a thickness of
+two feet at the top; this will determine the slope of the<span class="tei tei-pb" id="page184">[pg 184]</span><a name="Pg184" id="Pg184" class="tei tei-anchor"></a>
+exterior face of the kiln. The inside of the wall is carried
+up perpendicularly, and the loam plastering inside
+becomes, after the first burning, like a brick wall. The
+kiln may be safely erected in March, or whenever the
+danger of injury from frost is over. After the summer
+use of it, it must be protected, by faggots or litter,
+against the wet and frost of winter. A kiln of these
+dimensions will contain 32,500 1-1/4-inch tiles, * * *
+or 12,000 2-1/4-inch tiles. * * *</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In good weather, this kiln can be filled, burnt, and
+discharged once in every fortnight, and fifteen kilns
+may be obtained in a good season, producing 487,500
+1-1/4-inch tiles, and in proportion for the other sizes.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It requires 2 tons 5 cwt. of good coals to burn the
+above kiln, full of tiles."</p>
+
+<a name="fig60" id="fig60"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image46.png" width="640" height="239" alt="Fig. 46 - CLAY-KILN." title="Fig. 46 - CLAY-KILN." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 46 - CLAY-KILN.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A sectional view of this kiln is shown in Fig. 46, in
+which <span class="tei tei-hi"><span style="font-style: italic">C, C</span></span> represent sections of the outer trench; <span class="tei tei-hi"><span style="font-style: italic">A</span></span>, one
+of the three fire-holes; and <span class="tei tei-hi"><span style="font-style: italic">B, B</span></span>, sections of a circular
+passage inside of the wall, connected with the fire-holes,
+and serving as a flue for the flames, which, at suitable intervals,
+pass through openings into the floor of the kiln.
+The whole structure should be covered with a roof of
+rough boards, placed high enough to be out of the reach
+of the fire. A door in the side of the kiln serves for putting<span class="tei tei-pb" id="page185">[pg 185]</span><a name="Pg185" id="Pg185" class="tei tei-anchor"></a>
+in and removing the tiles, and is built up, temporarily,
+with bricks or clay, during the burning. Mr. Hodges
+estimates the cost of this kiln, all complete, at less than
+$25. Concerning its value, he wrote another letter in
+1848, from which the following is extracted:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The experience of four years that have elapsed since
+my letter to the late Earl Spencer, published in the 5th
+volume of the proceedings of the Royal Agricultural
+Society, page 57, has thoroughly tested the merits of
+the temporary clay-kilns for the burning of draining-pipes
+described in that letter.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"I am well aware that there were persons, even among
+those who came to see it, who pronounced at once upon
+the construction and duration of the kiln as unworthy
+of attention. How far their expectations have been realized,
+and what value belongs to their judgment, the following
+short statement will exhibit:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The kiln, in question, was constructed, in 1844, at a
+cost of £5.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It was used four times in that year, burning each
+time between 18,000 and 19,000 draining pipes, of 1-3/4
+inches in diameter.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In 1845, it was used nine times, or about once a fortnight,
+burning each time the same quantity of nearly
+19,000 pipes.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In 1846, the same result.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In 1847, it has been used twelve times, always burning
+the same quantity. In the course of the last year a
+trifling repair in the bottom of the kiln, costing rather
+less than 10 shillings, was necessary, and this is the only
+cost for repair since its erection. It is now as good as
+ever, and might be worked at least once a fortnight
+through the ensuing season.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The result of this experiment of four years shows not
+only the practical value of this cheap kiln, but Mr.
+Hatcher, who superintends the brick and tile-yard at Benenden,<span class="tei tei-pb" id="page186">[pg 186]</span><a name="Pg186" id="Pg186" class="tei tei-anchor"></a>
+where this kiln stands, expresses himself strongly
+in favor of this kiln, as always producing better and
+more evenly burned pipes than either of his larger and
+better built brick-kilns can do."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The floor of the kiln is first covered with bricks, placed
+on end, at a little distance from each other, so as to allow
+the fire to pass between them, and the tiles are placed <span class="tei tei-hi"><span style="font-style: italic">on
+end</span></span> on these. This position will afford the best draft for
+the flames. After the kiln is packed full, the door-way is
+built up, and a slow fire is started,—only enough at first
+to complete the drying of the tiles, and to do this so
+slowly as not to warp them out of shape. They will be
+thoroughly dry when the smoke from the top of the kiln
+loses its dark color and becomes transparent. When the
+fires are well started, the mouths of the fire-holes may be
+built up so as to leave only sufficient room to put in fresh
+fuel, and if the wind is high, the fire-holes, on the side
+against which it blows, should be sheltered by some sort
+of screen which will counteract its influence, and keep up
+an even heat on all sides.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The time required for burning will be from two days and
+a night to four days and four nights, according to the dryness
+of the tiles, the state of the weather, and the character
+of the fuel. The fires should be drawn when the tiles in the
+hottest part of the kiln are burned to a "ringing" hardness.
+By leaving two or three holes in the door-way,
+which can be stopped with loose brick, a rod may be run
+in, from time to time, to take out specimen tiles from the
+hottest part of the kiln, which shall have been so placed
+as to be easily removed. The best plan, however,—the
+only prudent plan, in fact,—will be to employ an intelligent
+man who is thoroughly experienced in the burning
+of brick and pottery, and whose judgment in the management
+of the fires, and in the cooling off of the kiln, will
+save much of the waste that would result from inexperienced
+management. After the burning is completed, from<span class="tei tei-pb" id="page187">[pg 187]</span><a name="Pg187" id="Pg187" class="tei tei-anchor"></a>
+40 to 60 hours must be allowed for the cooling of the kiln
+before it is opened. If the cold air is admitted while it is
+still very hot, the unequal contraction of the material will
+cause the tiles to crack, and a large portion of them may
+be destroyed.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If any of the tiles are too much burned, they will be
+melted, and may stick together, or, at least, have their
+shape destroyed. Those which are not sufficiently burned
+would not withstand the action of the water in the
+soil, and should not be used. For the first of these accidents
+there is no remedy; for the latter, reburning will
+be necessary, and under-done tiles may be left, (or replaced,)
+in the kiln in the position which they occupied at the
+first burning, and the second heat will probably prove sufficient.
+There is less danger of unequal burning in circular
+than in square kilns. Soft wood is better than hard,
+as making a better flame. It should be split fine, and well
+seasoned.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Arrangement of the Tilery.</span></span>—Such a tilery as is described
+above should have a drying shed from 60 to 80
+feet long, and from 12 to 18 feet wide. This shed may be
+built in the cheapest and roughest manner, the roof being
+covered with felting, thatch, or hemlock boards, as economy
+may suggest. It should have a tier of drying shelves,
+(made of slats rather than of boards,) running the whole
+length of each side. A narrow, wooden tram-way, down
+the middle, to carry a car, by which the green tiles may
+be taken from the machine to the shelves, and the dry
+ones from the shelves to the kiln, will greatly lessen the
+cost of handling.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The pug-mill and tile-machine, as well as the clay pit
+and the washing-mill, should be at one end of the shed,
+and the kiln at the other, so that, even in rainy weather,
+the work may proceed without interruption. A shed of
+the size named will be sufficient to dry as many tiles of<span class="tei tei-pb" id="page188">[pg 188]</span><a name="Pg188" id="Pg188" class="tei tei-anchor"></a>
+assorted sizes as can be burned in the clay-kiln described
+above.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Cost of Tiles.</span></span>—It would be impossible, at any
+time, to say what should be the precise cost of tiles in a
+given locality, without knowing the prices of labor and
+fuel; and in the present unsettled condition of the currency,
+any estimate would necessarily be of little value.
+Mr. Parker's estimated the cost of inch pipes in England at
+6<span class="tei tei-hi"><span style="font-style: italic">s.</span></span>, (about $1.50,) per thousand, when made on the estate
+where they were to be used, by a process similar to that
+described herein. Probably they could at no time have
+been made for less than twice that cost in the United States,—and
+they would now cost much more; though if the clay
+is dug out in the fall, when the regularly employed farm
+hands are short of work, and if the same men can cut and
+haul the wood during the winter, the hands hired especially
+for the tile making, during the summer season, (two men
+and two or three boys,) cannot, even at present rates of
+wages, bring the cost of the tiles to nearly the market
+prices. If there be only temporary use for the machinery,
+it may be sold, when no longer needed, for a good percentage
+of its original cost, as, from the slow movement
+to which it is subjected, it is not much worn by its work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There is no reason why tiles should cost more to make
+than bricks. A common brick contains clay enough to
+make four or five 1-1/4-inch tiles, and it will require about
+the same amount of fuel to burn this clay in one form as
+in the other. This advantage in favor of tiles is in a
+measure offset by the greater cost of handling them, and
+the greater liability to breakage.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The foregoing description of the different processes of
+the manufacture of draining tiles has been given, in order
+that those who find it necessary, or desirable, to establish
+works to supply the needs of their immediate localities
+may commence their operations understandingly, and form<span class="tei tei-pb" id="page189">[pg 189]</span><a name="Pg189" id="Pg189" class="tei tei-anchor"></a>
+an approximate opinion of the promise of success in the
+undertaking.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Probably the most positive effect of the foregoing description,
+on the mind of any man who contemplates establishing
+a tilery, will be to cause him to visit some successful
+manufactory, during the busy season, and examine for
+himself the mode of operation. Certainly it would be unwise,
+when such a personal examination of the process is
+practicable, to rely entirely upon the aid of written descriptions;
+for, in any work like tile-making, where the selection,
+combination and preparation of the materials, the
+means of drying, and the economy and success of the
+burning must depend on a variety of conditions and circumstances,
+which change with every change of locality, it is
+impossible that written directions, however minute, should
+be a sufficient guide. Still, in the light of such directions,
+one can form a much better idea of the bearing of the
+different operations which he may witness, than he could
+possibly do if the whole process were new to him.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If a personal examination of a successful tilery is impracticable,
+it will be necessary to employ a practical
+brick-maker, or potter, to direct the construction and operation
+of the works, and in any case, this course is advisable.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In any neighborhood where two or three hundred acres
+of land are to be drained, if suitable earths can be readily
+obtained, it will be cheaper to establish a tile-yard, than
+to haul the necessary tiles, in wagons, a distance of ten or
+twenty miles. Then again, the prices demanded by the
+few manufacturers, who now have almost a monopoly of
+the business, are exorbitantly high,—at least twice what
+it will cost to make the tiles at home, with the cheap
+works described above, so that if the cost of transportation
+on the quantity desired would be equal to the cost of
+establishing the works, there will be a decided profit in
+the home manufacture. Probably, also, a tile-yard, in a
+neighborhood where the general character of the soil is<span class="tei tei-pb" id="page190">[pg 190]</span><a name="Pg190" id="Pg190" class="tei tei-anchor"></a>
+such as to require drainage, will be of value after the object
+for which it was made has been accomplished.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">While setting forth the advantage to the farmer of
+everything which may protect him against monopolies,
+whether in the matter of draining-tile, or of any other
+needful accessory of his business, or which will enable
+him to procure supplies without a ruinous outlay for transportation,
+it is by no means intended that every man shall
+become his own tile-maker.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In this branch of manufacture, as in every other, organized
+industry will accomplish results to which individual
+labor can never attain. A hundred years ago,
+when our mill-made cloths came from England, and cost
+more than farmers could afford to pay, they wore home-spun,
+which was neither so handsome nor so good as the
+imported article; but, since that time, the growing population
+and the greater demand have caused cloth mills to
+be built here, greater commercial facilities have placed
+foreign goods within easy reach, and the house loom has
+fallen into general disuse.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">At present, the manufacture of draining tiles is confined
+to a few, widely separated localities, and each manufacturer
+has, thus far, been able to fix his own scale of
+charges. These, and the cost of transportation to distant
+points, make it difficult, if not impossible, for many farmers
+to procure tiles at a cost low enough to justify their
+use. In such cases, small works, to supply local demand,
+may enable many persons to drain with tiles, who, otherwise,
+would find it impossible to procure them cheaply
+enough for economical use; and the extension of under-draining,
+causing a more general acquaintance with its
+advantages, would create a sufficient demand to induce
+an increase of the manufacture of tiles, and a consequent
+reduction of price.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page191">[pg 191]</span><a name="Pg191" id="Pg191" class="tei tei-anchor"></a>
+<a name="toc61" id="toc61"></a>
+<a name="pdf62" id="pdf62"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER IX. - THE RECLAIMING OF SALT MARSHES.</span></h1>
+
+<div class="block tei tei-quote" style="margin-bottom: 1.80em; margin-left: 3.60em; margin-top: 1.80em; margin-right: 3.60em">
+<p class="tei tei-p" style="margin-bottom: 0.90em"><span style="font-size: 90%">"Adjoining to it is Middle Moor, containing about 2,500 acres, spoken
+of by Arthur Young as 'a watery desert,' growing sedge and rushes,
+and inhabited by frogs and bitterns;—it is now fertile, well cultivated,
+and profitable land."</span></p>
+</div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The foregoing extract, from an account of the Drainage
+of the Fens on the eastern coast of England, is a text
+from which might be preached a sermon worthy of the
+attention of all who are interested in the vast areas of
+salt marsh which form so large a part of our Atlantic
+coast, from Maine to Florida.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Hundreds of thousands of acres that might be cheaply
+reclaimed, and made our most valuable and most salubrious
+lands, are abandoned to the inroads of the sea;—fruitful
+only in malaria and musquitoes,—always a dreary
+waste, and often a grave annoyance.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A single tract, over 20,000 acres in extent, the center
+of which is not seven miles from the heart of New York
+City, skirts the Hackensack River, in New Jersey, serving
+as a barrier to intercourse between the town and the
+country which lies beyond it, adding miles to the daily
+travel of the thousands whose business and pleasure require
+them to cross it, and constituting a nuisance and
+an eyesore to all who see it, or come near it. How long it<span class="tei tei-pb" id="page192">[pg 192]</span><a name="Pg192" id="Pg192" class="tei tei-anchor"></a>
+will continue in this condition it is impossible to say, but
+the experience of other countries has proved that, for an
+expense of not more than fifty dollars per acre, this tract
+might be made better, for all purposes of cultivation, than
+the lands adjoining it, (many of which are worth, for market
+gardening, over one thousand dollars per acre,) and
+that it might afford profitable employment, and give homes,
+to all of the industrious poor of the city. The work of
+reclaiming it would be child's play, compared with the
+draining of the Harlaem Lake in Holland, where over 40,000
+acres, submerged to an average depth of thirteen feet,
+have been pumped dry, and made to do their part toward
+the support of a dense population.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The Hackensack meadows are only a conspicuous example
+of what exists over a great extent of our whole seaboard;—virgin
+lands, replete with every element of fertility,
+capable of producing enough food for the support of
+millions of human beings, better located, for residence and
+for convenience to markets, than the prairies of the Western
+States,—all allowed to remain worse than useless;
+while the poorer uplands near them are, in many places,
+teeming with a population whose lives are endangered,
+and whose comfort is sadly interfered with by the insects
+and the miasma which the marsh produces.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The inherent wealth of the land is locked up, and all of
+its bad effects are produced, by the water with which it is
+constantly soaked or overflowed. Let the waters of the
+sea be excluded, and a proper outlet for the rain-fall and
+the upland wash be provided,—both of which objects
+may, in a great majority of cases, be economically accomplished,—and
+this land may become the garden of the
+continent. Its fertility will attract a population, (especially
+in the vicinity of large towns,) which could no
+where else live so well nor so easily.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The manner in which these salt marshes were formed
+may be understood from the following account of the<span class="tei tei-pb" id="page193">[pg 193]</span><a name="Pg193" id="Pg193" class="tei tei-anchor"></a>
+"Great Level of the Fens" of the eastern coast of England,
+which is copied, (as is the paragraph at the head of
+this chapter,) from the Prize Essay of Mr. John Algernon
+Clarke, written for the Royal Agricultural Society in 1846.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The process is not, of course, always the same, nor are
+the exact influences, which made the English Fens, generally,
+operating in precisely the same manner here, but the
+main principle is the same, and the lesson taught by the
+improvement of the Fens is perfectly applicable in our case.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"This great level extends itself into the six counties of
+Cambridge, Lincoln, Huntington, Northampton, Suffolk
+and Norfolk, being bounded by the highlands of each.
+It is about seventy miles in length, and varies from
+twenty to forty miles in breadth, having an area of more
+than 680,000 acres. Through this vast extent of flat
+country, there flow six large rivers, with their tributary
+streams; namely, the Ouse, the Cam, the Nene, the Welland,
+the Glen, and the Witham.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"These were, originally, natural channels for conveying
+the upland waters to the sea, and whenever a heavier
+downfall of rain than usual occurred, and the swollen
+springs and rivulets caused the rivers to overflow, they
+must necessarily have overflowed the land to a great extent.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"This, however, was not the principal cause of the inundation
+of the Fens: these rivers were not allowed a
+free passage to the ocean, being thus made incapable of
+carrying off even the ordinary amount of upland water
+which, consequently, flowed over the land. The obstruction
+was two-fold; first, the outfalls became blocked up
+by the deposits of silt from the sea waters, which accumulated
+to an amazing thickness. The well known
+instances of boats found in 1635 eight feet below the
+Wisbeck River, and the smith's forge and tools found at
+Skirbeck Shoals, near Boston, buried with silt sixteen feet
+deep, show what an astonishing quantity of sediment<span class="tei tei-pb" id="page194">[pg 194]</span><a name="Pg194" id="Pg194" class="tei tei-anchor"></a>
+formerly choked up the mouths of these great rivers.
+But the chief hindrance caused by the ocean, arose from
+the tide rushing twice every day for a very great distance
+up these channels, driving back the fresh waters,
+and overflowing with them, so that the whole level became
+deluged with deep water, and was, in fact, one
+great bay.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In considering the state of this region as it first attracted
+the enterprise of man to its improvement, we
+are to conceive a vast, wild morass, with only small, detached
+portions of cultivated soil, or islands, raised above
+the general inundation; a most desolate picture when
+contrasted with its present state of matchless fertility."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Salt marshes are formed of the silty deposits of rivers
+and of the sea. The former bring down vegetable mould
+and fine earth from the uplands, and the latter contribute
+sea weeds and grasses, sand and shells, and millions of
+animalculæ which, born for life in salt water only, die,
+and are deposited with the other matters, at those points
+where, from admixture with the fresh flow of the rivers, the
+water ceases to be suitable for their support. It is estimated
+that these animalculæ alone are the chief cause of
+the obstructions at the mouths of the rivers of Holland,
+which retard their flow, and cause them to spread over the
+flat country adjoining their banks. It is less important,
+however, for the purposes of this chapter, to consider the
+manner in which salt marshes are formed, than to discuss
+the means by which they may be reclaimed and made
+available for the uses of agriculture. The improvement
+may be conveniently considered under three heads:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">First—The exclusion of the sea water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Second—The removal of the causes of inundation from
+the upland.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Third—The removal of the rain-fall and water of filtration.</p>
+
+<span class="tei tei-pb" id="page195">[pg 195]</span><a name="Pg195" id="Pg195" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The Exclusion of the Sea</span></span> is of the first importance,
+because not only does it saturate the land with water,—but
+this water, being salt, renders it unfertile for the
+plants of ordinary cultivation, and causes it to produce
+others which are of little, or no value.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The only means by which the sea may be kept out is,
+by building such dykes or embankments as shut out the
+highest tides, and, on shores which are exposed to the action
+of the waves, will resist their force. Ordinarily, the
+best, because the cheapest, material of which these embankments
+can be made, is the soil of the marsh itself.
+This is rarely,—almost never,—a pure peat, such as is
+found in upland swamps; it contains a large proportion of
+sand, blue clay, muscle mud, or other earthy deposits, which
+give it great weight and tenacity, and render it excellent
+for forming the body of the dyke. On lands which are
+overflowed to a considerable extent at each high tide,
+(twice a day,) it will be necessary to adopt more expensive,
+and more effective measures, but on ordinary salt meadows,
+which are deeply covered only at the spring tides, (occurring
+every month,) the following plan will be found practical
+and economical.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">Locating the line of the embankment</span></span> far enough back
+from the edge of the meadow to leave an ample flat outside
+of it to break the force of the waves, if on the open
+coast, or to resist the inroads of the current if on the bank
+of an estuary or a river,—say from ten to one hundred
+yards, according to the danger of encroachment,—set a
+row of stakes parallel to the general direction of the shore,
+to mark the outside line of the base of the dyke. Stake
+out the inside line at such distance as will give a pitch or
+inclination to the slopes of one and a half to one on the
+outside, and of one to one on the inside, and will allow
+the necessary width at the top, which should be at least
+two feet higher than the level of the highest tide that is
+known ever to have occurred at that place. The width<span class="tei tei-pb" id="page196">[pg 196]</span><a name="Pg196" id="Pg196" class="tei tei-anchor"></a>
+of the top should never be less than four feet, and in exposed
+localities it should be more. If a road will be needed
+around the land, it is best, if a heavy dyke is required, to
+make it wide enough to answer this purpose, with still
+wider places, at intervals, to allow vehicles to turn or to pass
+each other. Ordinarily, however, especially if there be a
+good stretch of flat meadow in front, the top of the dyke
+need not be more than four feet wide. Supposing such a
+dyke to be contemplated where the water has been known
+to rise two feet above the level of the meadows, requiring
+an embankment four feet high, it will be necessary to allow
+for the base a width of fourteen feet;—four feet for
+the width of the top, six feet for the reach of the front
+slope, (1-1/2 to 1,) and four feet for the reach of the back
+slope, (1 to 1.)</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Having staked out two parallel lines, fourteen feet apart,
+and erected, at intervals of twenty or thirty feet, frames
+made of rough strips of board of the exact shape of the
+section of the proposed embankment, the workmen may
+remove the sod to a depth of six inches, laying it all on
+the outside of the position of the proposed embankment.
+The sod from the line of the ditch, from which the earth
+for the embankment is to be taken, should also be removed
+and placed with the other. This ditch should be always
+<span class="tei tei-hi"><span style="font-style: italic">inside</span></span> of the dyke, where it will never be exposed to the
+action of the sea. It should be, at the surface, broader
+than the base of the dyke, and five feet deep in the center,
+but its sides may slope from the surface of the ground directly
+to the center line of the bottom. This is the best
+form to give it, because, while it should be five feet deep,
+for future uses as a drain, its bottom need have no width.
+The great width at the surface will give such a pitch to
+the banks as to ensure their stability, and will yield a large
+amount of sod for the facing of the dyke. The edge of
+this ditch should be some feet away from the inner line of
+the embankment, leaving it a firm support or shoulder at<span class="tei tei-pb" id="page197">[pg 197]</span><a name="Pg197" id="Pg197" class="tei tei-anchor"></a>
+the original level of the ground, the sod not being removed
+from the interval. The next step in the work should
+be to throw, or wheel, the material from the ditch on to
+the place which has been stripped for the dyke, building
+it up so as to conform exactly to the profile frames,
+these remaining in their places, to indicate the filling necessary
+to make up for the settling of the material, as the
+water drains out of it.</p>
+
+<a name="fig63" id="fig63"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image47.png" width="640" height="175" alt="Fig. 47 - DYKE AND DITCH." title="Fig. 47 - DYKE AND DITCH." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 47 - DYKE AND DITCH.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As fast as a permanent shape can be given to the outer
+face of the dyke, it should be finished by having the sod
+placed against it, being laid flatwise, one on top of another,
+(like stone work,) in the most solid manner possible.
+This should be continued to the top of the slope, and the
+flat top of the dyke should also be sodded,—the sods on
+the top, and on the slope, being firmly beaten to their places
+with the back of the spade or other suitable implement.
+This will sufficiently protect the exposed parts of the work
+against the action of any waves that may be formed on
+the flat between the dyke and the deep water, while the
+inner slope and the banks of the ditch, not being exposed
+to masses of moving water, will retain their shape and
+will soon be covered with a new growth.<a id="noteref_26" name="noteref_26" href="#note_26"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">26</span></span></a> A sectional
+view of the above described dyke and ditch is shown in
+the accompanying diagram, (Fig. 47.)</p>
+
+<span class="tei tei-pb" id="page198">[pg 198]</span><a name="Pg198" id="Pg198" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In all work of this character, it is important to regulate
+the amount of work laid out to be done between the
+spring tides, to the laboring force employed, so that no unfinished
+work will remain to be submerged and injured.
+When the flood comes, it should find everything finished
+up and protected against its ravages, so that no part of it
+need be done over again.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the land is crossed by creeks, the dyke should be finished
+off and sodded, a little back from each bank, and
+when the time comes for closing the channel, sufficient
+force should be employed to complete the dam at a single
+tide, so that the returning flow shall not enter to wash
+away the material which has been thrown in.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If, as is often the case, these creeks are not merely tidal
+estuaries, but receive brooks or rivers from the upland,
+provision must be made, as will be hereafter directed, for
+either diverting the upland flow, or for allowing it to pass
+out at low water, through valve gates or sluices. When
+the dam has been made, the water behind it should never
+be allowed to rise to nearly the level of the full tide, and,
+as soon as possible, grass and willows should be grown on
+the bank, to add to its strength by the binding effect of
+their roots.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When the dyke is completed across the front of the
+whole flat,—from the high land on one side to the high
+land on the other, the creeks should be closed, one after
+the other, commencing with the smallest, so that the experience
+gained in their treatment may enable the force
+to work more advantageously on those which carry more
+water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the flow of water in the creek is considerable, a row
+of strong stakes, or piles, should be firmly driven into the
+bottom mud, across the whole width of the channel, at intervals
+of not more than one or two feet, and <span class="tei tei-hi"><span style="font-style: italic">fascines</span></span>,—bundles
+of brush bound together,—should be made ready
+on the banks, in sufficient quantity to close the spaces between<span class="tei tei-pb" id="page199">[pg 199]</span><a name="Pg199" id="Pg199" class="tei tei-anchor"></a>
+the piles. These will serve to prevent the washing
+away of the filling during construction. The pile driving,
+and the preparation of the fascines may be done before
+the closing of the channel with earth is commenced, and
+if upland clay or gravel, to be mixed with the local material,
+can be economically brought to the place by boats or
+wagons, it will be an advantage. Everything being in
+readiness, a sufficient force of laborers to finish the dam in
+six hours should commence the work a little before dead
+low-water, and, (with the aid of wheelbarrows, if necessary,)
+throw the earth in rapidly <span class="tei tei-hi"><span style="font-style: italic">behind</span></span> the row of stakes
+and fascines, giving the dam sufficient width to resist the
+pressure of the water from without, and keeping the work
+always in advance of the rising of the tide, so that, during
+the whole operation, none of the filling shall be washed
+away by water flowing over its top.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the creek has a sloping bottom, the work may be
+commenced earlier,—as soon as the tide commences to recede,—and
+pushed out to the center of the channel by the
+time the tide is out. When the dam is built, it will be
+best to heavily sod, or otherwise protect its surface against
+the action of heavy rains, which would tend to wash it
+away and weaken it; and the bed of the creek should be
+filled in back of the dam for a distance of at least fifty
+yards, to a height greater than that at which water will
+stand in the interior drains,—say to within three feet of
+the surface,—so that there shall never be a body of water
+standing within that distance of the dam.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This is a necessary precaution against the attacks of muskrats,
+which are the principal cause of the insecurity of all
+salt marsh embankments. It should be a cardinal rule
+with all who are engaged in the construction of such
+works, never to allow two bodies of water, one on each
+side of the bank to be nearer than twenty-five yards of each
+other, and fifty yards would be better. Muskrats do not
+bore through a bank, as is often supposed, to make a passage<span class="tei tei-pb" id="page200">[pg 200]</span><a name="Pg200" id="Pg200" class="tei tei-anchor"></a>
+from one body of water to another, (they would find
+an easier road over the top); but they delight in any elevated
+mound in which they can make their homes above
+the water level and have its entrance beneath the surface,
+so that their land enemies cannot invade them. When
+they enter for this purpose, only from one side of the dyke,
+they will do no harm, but if another colony is, at the same
+time, boring in from the other side, there is great danger
+that their burrows will connect, and thus form a channel for
+the admission of water, and destroy the work. A disregard
+of this requirement has caused thousands of acres of
+salt marsh that had been enclosed by dykes having a
+ditch on each side, (much the cheapest way to make them,)
+to be abandoned, and it has induced the invention of various
+costly devices for the protection of embankments
+against these attacks.<a id="noteref_27" name="noteref_27" href="#note_27"><span class="tei tei-noteref"><span style="font-size: 60%; vertical-align: super">27</span></span></a></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When the creek or estuary to be cut off is very wide,
+the embankment may be carried out, at leisure, from each
+side, until the channel is only wide enough to allow the
+passage of the tide without too great a rush of water
+against the unfinished ends of the work; but, even in these
+cases, there will be economy in the use of fascines and piles
+from the first, or of stones if these can be readily procured.
+In wide streams, partial obstructions of the water<span class="tei tei-pb" id="page201">[pg 201]</span><a name="Pg201" id="Pg201" class="tei tei-anchor"></a>
+course will sometimes induce the deposit of silt in such
+quantities as will greatly assist the work. No written description
+of a single process will suffice for the direction
+of those having charge of this most delicate of all drainage
+operations. Much must be left to the ingenuity of
+the director of the work, who will have to avail himself
+of the assistance of such favorable circumstances as may,
+in the case in hand, offer themselves.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If the barrier to be built will require a considerable outlay,
+it should be placed in the hands of a competent engineer,
+and it will generally demand the full measure of his
+skill and experience.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The work cannot be successful, unless the whole line of
+the water-front is protected by a continuous bank, sufficiently
+high and strong in all of its parts to resist the action
+of the highest tides and the strongest waves to which
+it will be subjected. As it is always open to inspection, at
+each ebb tide, and can always be approached for repair, it
+will be easy to keep it in good condition; and, if properly
+attended to, it will become more solid and effective with
+age.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The removal of the causes of inundation from the upland</span></span>
+is often of almost equal importance with the shutting
+out of the sea, since the amount of water brought down
+by rivers, brooks, and hill-side wash, is often more than
+can be removed by any practicable means, by sluice gates,
+or pumps.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It will be quite enough for the capacity of these means
+of drainage, to remove the rain-water which falls on the
+flat land, and that which reaches it by under-ground
+springs and by infiltration,—its proper drainage-water in
+short,—without adding that which, coming from a higher
+level, may be made to flow off by its own fall.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Catch-water drains, near the foot of the upland, may be
+so arranged as to receive the surface water of the hills and<span class="tei tei-pb" id="page202">[pg 202]</span><a name="Pg202" id="Pg202" class="tei tei-anchor"></a>
+carry it off, always on a level above that of the top of the
+embankment, and these drains may often be, with advantage,
+enlarged to a sufficient capacity to carry the streams
+as well. If the marsh is divided by an actual river, it
+may be best to embank it in two separate tracts; losing
+the margins, that have been recommended, outside of
+the dykes, and building the necessary additional length
+of these, rather than to contend with a large body of water.
+But, frequently, a very large marsh is traversed by a
+tortuous stream which occupies a large area, and which,
+although the tidal water which it contains gives it the appearance
+of a river, is only the outlet of an insignificant
+stream, which might be carried along the edge of the upland
+in an ordinary mill-race. In such case it is better to
+divert the stream and reclaim the whole area.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When a stream is enclosed between dykes, its winding
+course should be made straight in order that its water may
+be carried off as rapidly as possible, and the land which it
+occupies by its deviations, made available for cultivation.
+In the loose, silty soil of a salt marsh, the stream may be
+made to do most of the work of making its new bed, by
+constructing temporary "jetties," or other obstructions to
+its accustomed flow, which shall cause its current to deposit
+silt in its old channel, and to cut a new one out of the
+opposite bank. In some instances it may be well to make an
+elevated canal, straight across the tract, by constructing
+banks high enough to confine the stream and deliver it
+over the top of the dyke; in others it may be more expedient
+to carry the stream over, or through, the hill which
+bounds the marsh, and cause it to discharge through an
+adjoining valley. Improvements of this magnitude, which
+often affect the interest of many owners, or of persons interested
+in the navigation of the old channel, or in mill
+privileges below the point at which the water course is to
+be diverted, will generally require legislative interference.<span class="tei tei-pb" id="page203">[pg 203]</span><a name="Pg203" id="Pg203" class="tei tei-anchor"></a>
+But they not seldom promise immense advantages for a
+comparatively small outlay.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The instance cited of the Hackensack Meadows, in New
+Jersey, is a case in point. Its area is divided among many
+owners, and, while ninety-nine acres in every hundred are
+given up to muskrats, mosquitoes, coarse rushes and
+malaria, the other one acre may belong to the owner of an
+adjacent farm who values the salt hay which it yields him,
+and the title to the whole is vested in many individual
+proprietors, who could never be induced to unite in an improvement
+for the common benefit. Then again, thanks
+to the tide that sets back in the Hackensack River, it is
+able to float an occasional vessel to the unimportant villages
+at the northern end of the meadows, and the right
+of navigation can be interfered with only by governmental
+action. If the Hackensack River proper, that part of it
+which only serves as an outlet for the drainage of the high
+land north of the meadows, could be diverted and carried
+through the hills to the Passaic; or confined within straight
+elevated banks and made to discharge at high water mark
+at the line of the Philadelphia Rail-road;—the wash of
+the highlands, east and west of the meadows, being also
+carried off at this level,—the bridge of the railroad might
+be replaced by an earth embankment, less than a quarter
+of a mile in length, effecting a complete exclusion of the
+tidal flow from the whole tract.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This being done, a steam-pump, far less formidable than
+many which are in profitable use in Europe for the same
+purpose, would empty, and keep empty, the present bed
+of the river, which would form a capital outlet for the
+drainage of the whole area. Twenty thousand acres, of
+the most fertile land, would thus be added to the available
+area of the State, greatly increasing its wealth, and inducing
+the settlement of thousands of industrious inhabitants.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As the circumstances under which upland water reaches<span class="tei tei-pb" id="page204">[pg 204]</span><a name="Pg204" id="Pg204" class="tei tei-anchor"></a>
+lands of the class under consideration vary with every
+locality, no specific directions for the treatment of individual
+cases can be given within the limits of this chapter;
+but the problem will rarely be a difficult one.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">The removal of the rain-fall and water of filtration</span></span>
+is the next point to be considered.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">So far as the drainage of the land, in detail, is concerned,
+it is only necessary to say that it may be accomplished, as
+in the case of any other level land which, from the slight
+fall that can be allowed the drains, requires close attention
+and great care in the adjustment of the grades.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The main difficulty is in providing an outlet for the
+drains. This can only be done by artificial means, as the
+water must be removed from a level lower than high-water
+mark,—sometimes lower than low-water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If it is only required that the outlet be at a point somewhat
+above the level of ordinary low-water, it will be sufficient
+to provide a sufficient reservoir, (usually a large
+open ditch,) to contain the drainage water that is discharged
+while the tide stands above the floor of the outlet
+sluice-way, and to provide for its outflow while the
+level of the tide water is below the point of discharge.
+This is done by means of sluices having self-acting valves,
+(or tide-gates,) opening outward, which will be closed by
+the weight of the water when the tide rises against them,
+being opened again by the pressure of the water from
+within, as soon the tide falls below the level of the water
+inside of the bank.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The gates and sluices may be of wood or iron,—square
+or round. The best would be galvanized iron pipes and
+valves; but a square wooden trunk, closed with a heavy
+oak gate that fits closely against its outer end, and moves
+freely on its hinges, will answer capitally well, if carefully
+and strongly made. If the gate is of wood, it will be
+well to have it lie in a slightly slanting position, so that its
+own weight will tend to keep it closed when the tide first<span class="tei tei-pb" id="page205">[pg 205]</span><a name="Pg205" id="Pg205" class="tei tei-anchor"></a>
+commences to rise above the floor, and might trickle in,
+before it had acquired sufficient head to press the gate
+against the end of the trunk.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">As this outlet has to remove, in a short time, all of the
+water that is delivered by the drains and ditches during
+several hours, it should, of course, be considerably larger
+than would be required for a constantly flowing drain from
+the same area; but the immense gates,—large enough for
+a canal lock,—which are sometimes used for the drainage
+of a few acres of marsh, are absurd. Not only are they
+useless, they are really objectionable, inasmuch as the
+greater extent of their joints increases the risk of leakage
+at the time of high water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The channel for the outflow of the water may sometimes,
+with advantage, be open to the top of the dyke or
+dam,—a canal instead of a trunk; but this is rarely the
+better plan, and is only admissible where the discharge is
+into a river or small bay, too small for the formation of
+high waves, as these would be best received on the face
+of a well sodded, sloping bank.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The height, above absolute low water, at which the outlet
+should be placed, will depend on the depth of the outlet
+of the land drain, and the depth of storage room required
+to receive the drainage water during the higher stages of
+the tide. Of course, it must not be higher than the floor
+of the land drain outlet, and, except for the purpose of
+affording storage room, it need not be lower, although all
+the drainage will discharge, not only while the tide water
+is below the bottom of the gate, but as long as it remains
+lower than the level of the water inside. It is well to place
+the mouth of the trunk nearly as low as ordinary low-water
+mark. This will frequently render it necessary to carry
+a covered drain, of wood or brick, through the mud, out
+as far as the tide usually recedes,—connected with the
+valve gate at the outlet of the trunk, by a covered box<span class="tei tei-pb" id="page206">[pg 206]</span><a name="Pg206" id="Pg206" class="tei tei-anchor"></a>
+which will keep rubbish from obstructing it, or interfering
+with its action.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">When the outlet of the land-drains is below low-water
+mark</span></span>, it is of course necessary to pump out the drainage
+water. This is done by steam or by wind, the latter being
+economical only for small tracts which will not bear
+the cost of a steam pump. Formerly, this work was done
+entirely by windmills, but these afford only an uncertain
+power, and often cause the entire loss of crops which are
+ready for the harvest, by obstinately refusing to work for
+days after a heavy rain has deluged the land. In grass
+land they are tolerably reliable, and on <span class="tei tei-hi"><span style="font-style: italic">small</span></span> tracts in
+cultivation, it is easy, by having a good proportion of
+open ditches, to afford storage room sufficient for general
+security; but in the reclaiming of large areas, (and it is
+with these that the work is most economical,) the steam
+pump may be regarded as indispensable. It is fast superseding
+the windmills which, a few years ago, were the sole
+dependence in Holland and on the English Fens. The
+magnitude of the pumping machinery on which the agriculture
+of a large part of Holland depends, is astonishing.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">There are such immense areas of salt marsh in the
+United States which may be tolerably drained by the use
+of simple valve gates, discharging above low-water mark,
+that it is not very important to consider the question of
+pumping, except in cases where owners of small tracts,
+from which a sufficient tidal outlet could not be secured,
+(without the concurrence of adjoining proprietors who
+might refuse to unite in making the improvement,) may
+find it advisable to erect small pumps for their own use.
+In such cases, it would generally be most economical to
+use wind-power, especially if an accessory steam pump be
+provided for occasional use, in emergency. Certainly, the
+tidal drainage should first be resorted to, for when the
+land has once been brought into cultivation, the propriety
+of introducing steam pumps will become more apparent,<span class="tei tei-pb" id="page207">[pg 207]</span><a name="Pg207" id="Pg207" class="tei tei-anchor"></a>
+and the outlay will be made with more confidence of profitable
+return, and, in all cases, the tidal outlet should be
+depended on for the outflow of all water above its level.
+It would be folly to raise water by expensive means, which
+can be removed, even periodically, by natural drainage.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">When pumps are used, their discharge pipes should pass
+through the embankment, and deliver the water at low-water
+mark, so that the engine may have to operate only
+against the actual height of the tide water. If it delivered
+above high-water mark, it would work, even at low tide,
+against a constant head, equal to that of the highest tides.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page208">[pg 208]</span><a name="Pg208" id="Pg208" class="tei tei-anchor"></a>
+<a name="toc64" id="toc64"></a><a name="pdf65" id="pdf65"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER X. - MALARIAL DISEASES.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">So far as remote agricultural districts are concerned, it
+is not probable that the mere question of health would induce
+the undertaking of costly drainage operations, although
+this consideration may operate, in connection with
+the need for an improved condition of soil, as a strong
+argument in its favor. As a rule, "the chills" are accepted
+by farmers, especially at the West, as one of the slight
+inconveniences attending their residence on rich lands;
+and it is not proposed, in this work, to urge the evils of
+this terrible disease, and of "sun pain," or "day neuralgia,"
+as a reason for draining the immense prairies over which
+they prevail. The diseases exist,—to the incalculable detriment
+of the people,—and thorough draining would remove
+them, and would doubtless bring a large average return
+on the investment;—but the question is, after all,
+one of capital; and the cost of such draining as would
+remove fever-and-ague from the bottom lands and prairies
+of the West, and from the infected agricultural districts
+at the East, would be more than the agricultural capital
+of those districts could spare for the purpose.</p>
+
+<span class="tei tei-pb" id="page209">[pg 209]</span><a name="Pg209" id="Pg209" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the vicinity of cities and towns, however, where
+more wealth has accumulated, and where the number of
+persons subjected to the malarial influence is greater, there
+can be no question as to the propriety of draining, even
+if nothing but improved health be the object.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Then again, there are immense tracts near the large
+cities of this country which would be most desirable for
+residence, were it not that their occupancy, except with
+certain constant precautions, implies almost inevitable suffering
+from fever-and-ague, or neuralgia.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Very few neighborhoods within thirty miles of the city
+of New York are entirely free from these scourges, whose
+influence has greatly retarded their occupation by those
+who are seeking country homes; while many, who have
+braved the dangers of disease in these localities, have had
+sad cause to regret their temerity.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Probably the most striking instance of the effect of
+malaria on the growth and settlement of suburban districts,
+is to be found on Staten Island. Within five miles
+of the Battery; accessible by the most agreeable and best
+managed ferry from the city; practically, nearer to Wall
+street than Murray Hill is; with most charming views of
+land and water; with a beautifully diversified surface, and
+an excellent soil; and affording capital opportunities for sea
+bathing, it should be, (were it not for its sanitary reputation,
+it inevitably would be,) one vast residence-park. Except
+on its extreme northern end, and along its higher
+ridges, it has,—and, unfortunately, it deserves,—a most unenviable
+reputation for insalubrity. Here and there, on the
+southern slope also, there are favored places which are unaccountably
+free from the pest, but, as a rule, it is, during the
+summer and autumn, unsafe to live there without having
+constant recourse to preventive medication, or exercising
+unusual and inconvenient precautions with regard to exposure
+to mid-day sun and evening dew. There are always
+to be found attractive residences, which are deserted by<span class="tei tei-pb" id="page210">[pg 210]</span><a name="Pg210" id="Pg210" class="tei tei-anchor"></a>
+their owners, and are offered for sale at absurdly low prices.
+There are isolated instances of very thorough and very
+costly draining, which has failed of effect, because so extensive
+a malarial region cannot be reclaimed by anything
+short of a systematic improvement of the whole.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It has been estimated that the thorough drainage of the
+low lands, valleys and ponds of the eastern end of the
+island, including two miles of the south shore, would at
+once add $5,000,000 to the market value of the real estate
+of that section. There can be no question that any radical
+improvement in this respect would remove the only obstacle
+to the rapid settlement of the island by those who
+wish to live in the country, yet need to be near to the
+business portion of the city. The hope of such improvement
+being made, however, seems as remote as ever,—although
+any one at all acquainted with the sources of miasm,
+in country neighborhoods, can readily see the cause
+of the difficulty, and the means for its removal are as
+plainly suggested.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Staten Island is, by no means, alone in this respect. All
+who know the history of the settlement of the other suburbs
+of New York are very well aware that those places
+which are free from fever-and-ague and malarial neuralgia,
+are extremely rare.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The exact cause of fever-and-ague and other malarial
+diseases is unknown, but it is demonstrated that, whatever
+the cause is, it is originated under a combination of circumstances,
+one of which is undue moisture in the soil.
+It is not necessary that land should be absolutely marshy
+to produce the miasm, for this often arises on cold, springy
+uplands which are quite free from deposits of muck.
+Thus far, the attention of scientific investigators, given
+to the consideration of the origin of malarial diseases, has
+failed to discover any well established facts concerning it;
+but there have been developed certain theories, which<span class="tei tei-pb" id="page211">[pg 211]</span><a name="Pg211" id="Pg211" class="tei tei-anchor"></a>
+seem to be sustained by such knowledge as exists on the
+subject.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Dr. Bartlett, in his work on the Fevers of the United
+States, says:—"The essential, efficient, producing cause
+of periodical fever,—the poison whose action on
+the system gives rise to the disease,—is a substance or
+agent which has received the names of <span class="tei tei-hi"><span style="font-style: italic">malaria</span></span>, or <span class="tei tei-hi"><span style="font-style: italic">marsh
+miasm</span></span>. The nature and composition of this poison are
+wholly unknown to us. Like most other analogous
+agents, like the contagious principle of small-pox and of
+typhus, and like the epidemic poison of scarletina and
+cholera, they are too subtle to be recognized by any
+of our senses, they are too fugitive to be caught by any
+of our contrivances.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"As always happens in such cases and under similar
+circumstances, in the absence of positive knowledge, we
+have been abundantly supplied with conjecture and speculation;
+what observation has failed to discover, hypothesis
+has endeavored and professed to supply. It is
+quite unnecessary even to enumerate the different substances
+to which malaria has been referred. Amongst
+them are all of the chemical products and compounds
+possible in wet and marshy localities; moisture alone;
+the products of animal and vegetable decomposition;
+and invisible living organisms. * * * * Inscrutable,
+however, as the intimate nature of the substances
+or agents may be, there are some few of its laws and
+relations which are very well ascertained. One of these
+consists in its connection with low, or wet, or marshy
+localities. This connection is not invariable and exclusive,
+that is, there are marshy localities which are not
+malarious, and there are malarious localities which are
+not marshy; but there is no doubt whatever that it generally
+exists."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In a report to the United States Sanitary Commission,
+Dr. Metcalfe states, that all hypotheses, even the most<span class="tei tei-pb" id="page212">[pg 212]</span><a name="Pg212" id="Pg212" class="tei tei-anchor"></a>
+plausible, are entirely unsupported by positive knowledge,
+and he says:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"This confession of ignorance still leaves us in possession
+of certain knowledge concerning malaria, from which
+much practical good may be derived.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"1st. It affects, by preference, low and moist localities.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"2d. It is almost never developed at a lower temperature
+than 60° Fahrenheit.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"3d. Its evolution or active agency is checked by a
+temperature of 32°.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"4th. It is most abundant and most virulent as we approach
+the equator and the sea-coast.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"5th. It has an affinity for dense foliage, which has the
+power of accumulating it, when lying in the course of
+winds blowing from malarious localities.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"6th. Forests, or even woods, have the power of obstructing
+and preventing its transmission, under these
+circumstances.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"7th. By atmospheric currents it is capable of being
+transported to considerable distances—probably as far as
+five miles.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"8th. It may be developed, in previously healthy places,
+by turning up the soil; as in making excavations for
+foundations of houses, tracks for railroads, and beds for
+canals.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"9th. In certain cases it seems to be attracted and absorbed
+by bodies of water lying in the course of such
+winds as waft it from the miasmatic source.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"10th. Experience alone can enable us to decide as to
+the presence or absence of malaria, in any given locality.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"11th. In proportion as countries, previously malarious,
+are cleared up and thickly settled, periodical fevers disappear—in
+many instances to be replaced by the typhoid
+or typhus."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">La Roche, in a carefully prepared treatise on "Pneumonia;
+its Supposed Connection with Autumnal Fevers," recites<span class="tei tei-pb" id="page213">[pg 213]</span><a name="Pg213" id="Pg213" class="tei tei-anchor"></a>
+various theories concerning the mode of action of
+marsh miasm, and finds them insufficient to account for
+the phenomena which they produce. He continues as
+follows:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"All the above hypotheses failing to account for the effects
+in question, we are naturally led to the admission
+that they are produced by the morbific influence of some
+special agent; and when we take into consideration all
+the circumstances attending the appearance of febrile
+diseases, the circumscribed sphere of their prevalence,
+the suddenness of their attack, the character of their
+phenomena, etc., we may safely say that there is nothing
+left but to attribute them to the action of some
+poison dissolved or suspended in the air of the infected
+locality; which poison, while doubtless requiring for its
+development and dissemination a certain degree of heat,
+and terrestrial and atmospheric moisture, a certain
+amount of nightly condensation after evaporation, and
+the presence of fermenting or decomposing materials,
+cannot be produced by either of these agencies alone,
+and though indicated by the chemist, betrays its presence
+by producing on those exposed to its influence the
+peculiar morbid changes characterizing fever."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">He quotes the following from the Researches of Dr.
+Chadwick:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In considering the circumstances external to the residence,
+which affect the sanitary condition of the population,
+the importance of a general land-drainage is developed
+by the inquiries as to the cause of the prevalent
+diseases, to be of a magnitude of which no conception had
+been formed at the commencement of the investigation.
+Its importance is manifested by the severe consequences
+of its neglect in every part of the country, as well as by
+its advantages in the increasing salubrity and productiveness
+wherever the drainage has been skillful and effectual."</p>
+
+<span class="tei tei-pb" id="page214">[pg 214]</span><a name="Pg214" id="Pg214" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">La Roche calls attention to these facts:—That the acclimated
+residents of a malarious locality, while they are
+less subject than strangers to active fever, show, in their
+physical and even in their mental organization, evident
+indications of the ill effects of living in a poisonous atmosphere,—an
+evil which increases with successive generations,
+often resulting in a positive deterioration of the
+race; that the lower animals are affected, though in a less
+degree than man; that deposits of organic matter which
+are entirely covered with water, (as at the bottom of a
+pond,) are not productive of malaria; that this condition
+of saturation is infinitely preferable to imperfect drainage;
+that swamps which are shaded from the sun's heat by
+trees, are not supposed to produce disease; and that
+marshes which are exposed to constant winds are not
+especially deleterious to persons living in their immediate
+vicinity,—while winds frequently carry the emanations of
+miasmatic districts to points some miles distant, where
+they produce their worst effects. This latter statement is
+substantiated by the fact that houses situated some miles
+to the leeward of low, wet lands, have been especially insalubrious
+until the windows and doors on the side toward
+the source of the miasm were closed up, and openings
+made on the other side,—and thenceforth remained free
+from the disease, although other houses with openings on
+the exposed sides continued unhealthy.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The literature relating to periodical fevers contains nothing
+else so interesting as the very ingenious article of Dr. J.
+H. Salisbury, on the "Cause of Malarious Fevers," contributed
+to the "American Journal of Medical Science," for
+January, 1866. Unfortunately, while there is no evidence
+to controvert the statements of this article, they do not
+seem to be honored with the confidence of the profession,—not
+being regarded as sufficiently authenticated to form a
+basis for scientific deductions. Dr. Salisbury claims to have
+discovered the cause of malarial fever in the spores of a very<span class="tei tei-pb" id="page215">[pg 215]</span><a name="Pg215" id="Pg215" class="tei tei-anchor"></a>
+low order of plant, which spores he claims to have invariably
+detected in the saliva, and in the urine, of fever patients,
+and in those of no other persons, and which he collected
+on plates of glass suspended over all marshes and
+other lands of a malarious character, which he examined,
+and which he was never able to obtain from lands which
+were not malarious. Starting from this point, he proceeds,
+(with circumstantial statements that seem to the unprofessional
+mind to be sufficient,) to show that the plant producing
+these spores is always found, in the form of a whitish,
+green, or brick-colored incrustation, on the surface of
+fever producing lands; that the spores, when detached
+from the parent plant, are carried in suspension <span class="tei tei-hi"><span style="font-style: italic">only in
+the moist exhalations of wet lands</span></span>, never rising higher,
+(usually from 35 to 60 feet,) nor being carried farther, than
+the humid air itself; that they most accumulate in the upper
+strata of the fogs, producing more disease on lands
+slightly elevated above the level of the marsh than at its
+very edge; that fever-and-ague are never to be found
+where this plant does not grow; that it may be at once
+introduced into the healthiest locality by transporting
+moist earth on which the incrustation is forming; that the
+plant, being introduced into the human system through
+the lungs, continues to grow there and causes disease;
+and that <span class="tei tei-hi"><span style="font-style: italic">quinia</span></span> arrests its growth, (as it checks the multiplication
+of yeast plants in fermentation,) and thus suspends
+the action of the disease.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Probably it would be impossible to prove that the foregoing
+theory is correct, though it is not improbable that it
+contains the germ from which a fuller knowledge of the disease
+and its causes will be obtained. It is sufficient for
+the purposes of this work to say that, so far as Dr. Salisbury's
+opinion is valuable, it is,—like the opinion of all
+other writers on the subject,—fully in favor of perfect
+drainage as the one great preventive of all malarial diseases.</p>
+
+<span class="tei tei-pb" id="page216">[pg 216]</span><a name="Pg216" id="Pg216" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">The evidence of the effect of drainage</span></span> in removing the
+cause of malarial diseases is complete and conclusive. Instances
+of such improvement in this country are not rare,
+but they are much less numerous and less conspicuous
+here than in England, where draining has been much more
+extensively carried out, and where greater pains have been
+taken to collect testimony as to its effects.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">If there is any fact well established by satisfactory experience,
+it is that thorough and judicious draining will
+entirely remove the local source of the miasm which produces
+these diseases.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The voluminous reports of various Committees of the
+English Parliament, appointed to investigate sanitary
+questions, are replete with information concerning experience
+throughout the whole country, bearing directly on
+this question.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Dr. Whitley, in his report to the Board of Health, (in
+1864,) of an extended tour of observation, says of one
+town that he examined:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Mr. Nicholls, who has been forty years in practice
+here, and whom I was unable to see at the time of my
+visit, writes: Intermittent and remittent are greatly on
+the decline since the improved state of drainage of
+the town and surrounding district, and more particularly
+marked is this alteration, since the introduction of the
+water-works in the place. Although we have occasional
+outbreaks of intermittent and remittent, with neuralgic
+attacks, they yield more speedily to remedies, and are
+not attended by so much enlargement of the liver or
+spleen as formerly, and dysentery is of rare occurrence."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Dr. Whitley sums up his case as follows:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It would appear from the foregoing inquiry, that intermittent
+and remittent fevers, and their consequences,
+can no longer be regarded as seriously affecting the
+health of the population, in many of the districts, in which
+those diseases were formerly of a formidable character.<span class="tei tei-pb" id="page217">[pg 217]</span><a name="Pg217" id="Pg217" class="tei tei-anchor"></a>
+Thus, in Norfolk, Lincolnshire, and Cambridgeshire,
+counties in which these diseases were both frequent and
+severe, all the evidence, except that furnished by the
+Peterborough Infirmary, and, in a somewhat less degree,
+in Spaulding, tends to show that they are at the present
+time, comparatively rare and mild in form."</p>
+
+<div class="tei tei-tb"> </div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">He mentions similar results from his investigations in
+other parts of the kingdom, and says:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It may, therefore, be safely asserted as regards England
+generally, that:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The diseases which have been made the subject of the
+present inquiry, have been steadily decreasing, both in
+frequency and severity, for several years, <span class="tei tei-hi"><span style="font-style: italic">and this decrease
+is attributed, in nearly every case, mainly to one
+cause,—improved land drainage;</span></span>" again:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The change of local circumstances, unanimously declared
+to be the most immediate in influencing the prevalence
+of malarious diseases, is land drainage;" and
+again:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Except in a few cases in which medical men believed
+that these affections began to decline previously to the
+improved drainage of the places mentioned, the decrease
+in all of the districts where extensive drainage has been
+carried out, was stated to have commenced about the
+same time, and was unhesitatingly attributed to that
+cause."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A select Committee of the House of Commons, appointed
+to investigate the condition and sanitary influence
+of the Thames marshes, reported their minutes of evidence,
+and their deductions therefrom, in 1854, The following
+is extracted from their report:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"It appears from the evidence of highly intelligent and
+eminent gentlemen of the medical profession, residing in
+the neighborhood of the marshes on both sides of the<span class="tei tei-pb" id="page218">[pg 218]</span><a name="Pg218" id="Pg218" class="tei tei-anchor"></a>
+Thames below London Bridge, that the diseases prevalent
+in these districts are highly indicative of malarious
+influences, fever-and-ague being very prevalent; and
+that the sickness and mortality are greatest in those localities
+which adjoin imperfectly drained lands, and far
+exceed the usual average; and that ague and allied disorders
+frequently extend to the high grounds in the vicinity.
+In those districts where a partial drainage has
+been effected, a corresponding improvement in the health
+of the inhabitants is perceptible."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the evidence given before the committee, Dr. P.
+Bossey testified that the malaria from salt marshes varied
+in intensity, being most active in the morning and in the
+Summer season. The marshes are sometimes covered by
+a little fog, usually not more than three feet thick,
+which is of a very offensive odor, and detrimental to
+health. Away from the marshes, there is a greater tendency
+to disease on the side toward which the prevailing
+winds blow.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Dr. James Stewart testified that the effect of malaria
+was greatest when very hot weather succeeds heavy rain
+or floods. He thought that malaria could be carried <span class="tei tei-hi"><span style="font-style: italic">up</span></span>
+a slope, but has never been known to descend, and that,
+consequently, an intervening hill affords sufficient protection
+against marsh malaria. He had known cases where
+the edges of a river were healthy and the uplands malarious.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In Santa Maura and Zante, where he had been stationed
+with the army, he had observed that the edge of a marsh
+would be comparatively healthy, while the higher places
+in the vicinity were exceedingly unhealthy. He thought
+that there were a great many mixed diseases which began
+like ague and terminated very differently; those diseases
+would, no doubt, assume a very different form if they
+were not produced by the marsh air; many diseases are
+very difficult to treat, from being of a mixed character<span class="tei tei-pb" id="page219">[pg 219]</span><a name="Pg219" id="Pg219" class="tei tei-anchor"></a>
+beginning like marsh fevers and terminating like inflammatory
+fevers, or diseases of the chest.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Dr. George Farr testified that rheumatism and tic-doloreux
+were very common among the ladies who live at the
+Woolwich Arsenal, near the Thames marshes. Some of
+these cases were quite incurable, until the patients removed
+to a purer atmosphere.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">W. H. Gall, M. D., thought that the extent to which
+malaria affected the health of London, must of course be
+very much a theoretical question; "but it is very remarkable
+that diseases which are not distinctly miasmatic, do
+become much more severe in a miasmatic district. Influenzas,
+which prevailed in England in 1847, were very
+much more fatal in London and the surrounding parts
+than they were in the country generally, and influenza
+and ague poisons are very nearly allied in their effects.
+Marsh miasms are conveyed, no doubt, a considerable
+distance. Sufficiently authentic cases are recorded to
+show that the influence of marsh miasm extends several
+miles." Other physicians testify to the fact, that near
+the Thames marshes, the prevalent diseases are all of them
+of an aguish type, intermittent and remittent, and that
+they are accompanied with much dysentery. Dr. John
+Manly said that, when he first went to Barking, he found a
+great deal of ague, but since the draining, in a population
+of ten thousand, there are not half-a-dozen cases annually
+and but very little remittent.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The following Extract is taken from the testimony
+of Sir Culling Eardly, Bart.:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Chairman:—I believe you reside at Belvidere, in the
+parish of Erith?—Yes.—Ch.: Close to these marshes?—Yes.—Ch.:
+Can you speak from your own knowledge,
+of the state of these marshes, with regard to public
+health?—Sir C.: I can speak of some of the results
+which have been produced in the neighborhood, from the
+condition of the marshes; the neighborhood is in one<span class="tei tei-pb" id="page220">[pg 220]</span><a name="Pg220" id="Pg220" class="tei tei-anchor"></a>
+continual state of ague. My own house is protected, from
+the height of its position, and a gentleman's house is less
+liable to the influence of malaria than the houses of the
+lower classes. But even in my house we are liable to
+ague; and to show the extraordinary manner in which
+the ague operates, in the basement story of this house
+where my men-servants sleep, we have more than once
+had bad ague. In the attics of my house, where my
+maid-servants sleep, we have never had it. Persons are
+deterred from settling in the neighborhood by the aguish
+character of the country. Many persons, attracted
+by the beauty of the locality, wish to come down and
+settle; but when they find the liability to ague, they
+are compelled to give up their intention. I may mention
+that the village of Erith itself, bears marks of the influence
+of malaria. It is more like one of the desolate
+towns of Italy, Ferrara, for instance, than a healthy,
+happy, English village. I do not know whether it is
+known to the committee, that Erith is the village described
+in Dickens' <span class="tei tei-hi"><span style="font-style: italic">Household Words</span></span>, as Dumble-down-deary,
+and that it is a most graphic and correct description
+of the state of the place, attributable to the unhealthy
+character of the locality."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">He also stated that the ague is not confined to the
+marshes, but extends to the high lands near them.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The General Board of Health, of England, at the close
+of a voluminous report, publish the following "Conclusions
+as to the Drainage of Suburban Lands:—</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"1. Excess of moisture, even on lands not evidently wet,
+is a cause of fogs and damps.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"2. Dampness serves as a medium for the conveyance of
+any decomposing matter that may be evolved, and adds
+to the injurious effects of such matters in the air:—in
+other words the excess of moisture may be said to increase
+or aggravate atmospheric impurities.</p>
+
+<span class="tei tei-pb" id="page221">[pg 221]</span><a name="Pg221" id="Pg221" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"3. The evaporation of the surplus moisture lowers the
+temperature, produces chills, and creates or aggravates
+the sudden and injurious changes or fluctuations by
+which health is injured."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In view of the foregoing opinions as to the cause of malaria,
+and of the evidence as to the effect of draining in removing
+the unhealthy condition in which those causes
+originate, it is not too much to say that,—in addition to
+the capital effect of draining on the productive capacity of
+the land,—the most beneficial sanitary results may be confidently
+expected from the extension of the practice, especially
+in such localities as are now unsafe, or at least
+undesirable for residence.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In proportion to the completeness and efficiency of the
+means for the removal of surplus water from the soil:—in
+proportion, that is, to the degree in which the improved
+tile drainage described in these pages is adopted,—will be
+the completeness of the removal of the causes of disease.
+So far as the drying of malarious lands is concerned, it is
+only necessary to construct drains in precisely the same
+manner as for agricultural improvement.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The removal of the waste of houses, and of other filth,
+will be considered in the next chapter.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page222">[pg 222]</span><a name="Pg222" id="Pg222" class="tei tei-anchor"></a>
+<a name="toc66" id="toc66"></a>
+<a name="pdf67" id="pdf67"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">CHAPTER XI. - HOUSE DRAINAGE AND TOWN SEWERAGE IN
+THEIR RELATIONS TO THE PUBLIC HEALTH.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The following is extracted from a report made by the
+General Board of Health to the British Parliament, concerning
+the administration of the Public Health Act and
+the Nuisances Removal and Diseases Prevention Acts
+from 1848 to 1854.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Where instances have been favorable for definite observation,
+as in broad blocks of buildings, the effects of
+sanitary improvement have been already manifested to an
+extent greater than could have been anticipated, and than
+can be readily credited by those who have not paid attention
+to the subject.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In one favorable instance, that of between 600 and 700
+persons of the working class in the metropolis, during a
+period of three years, the average rate of mortality has
+been reduced to between 13 and 14 in 1000. In another
+instance, for a shorter period, among 500 persons, the
+mortality has been reduced as low as even 7 in 1000.
+The average rate of mortality for the whole metropolis
+being 23 in 1000.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"In another instance, the abolishing of cess-pools and
+their replacement by water-closets, together with the
+abolishing of brick drains and their replacement by impermeable<span class="tei tei-pb" id="page223">[pg 223]</span><a name="Pg223" id="Pg223" class="tei tei-anchor"></a>
+and self-cleansing stone-ware pipes, has been
+attended with an immediate and extraordinary reduction
+of mortality. Thus, in Lambeth Square, occupied by a
+superior class of operatives, in the receipt of high wages,
+the deaths, which in ordinary times were above the general
+average, or more than 30 in 1000, had risen to a rate
+of 55 in 1000. By the abolishing of cess-pools, which
+were within the houses, and the substitution of water-closets,
+and with the introduction of tubular, self-cleansing
+house-drains, the mortality has been reduced to 13 in 1000.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The reduction of the mortality was effected precisely
+among the same occupants, without any change in their
+habits whatever."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Sewers are less important than the House-Drains and
+Water-Closets, and if not carrying much water, may become
+cess-pools. In the case of the Square just referred
+to, when cess-pools and drains of deposit were removed
+without any alteration whatever in the adjacent sewers,
+fevers disappeared from house to house, as these receptacles
+were filled up, and the water-closet apparatus substituted,
+merely in consequence of the removal of the decomposing
+matter from beneath the houses to a distant
+sewer of deposit or open water course.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"If the mortality were at the same rate as in the model
+dwellings, or in the improved dwellings in Lambeth
+Square, the annual deaths for the whole of the metropolis
+would be 25,000 less, and for the whole of England and
+Wales 170,000 less than the actual deaths.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"If the reduced rate of mortality in these dwellings
+should continue, and there appears to be no reason to
+suppose that it will not, the extension to all towns which
+have been affected, of the improvements which have been
+applied in these buildings, would raise the average age
+at death to about forty-eight instead of twenty-nine, the
+present average age at death of the inhabitants of towns
+in all England and Wales."</p>
+
+<span class="tei tei-pb" id="page224">[pg 224]</span><a name="Pg224" id="Pg224" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The branch of the Art of Drainage which relates to the
+removal of the fecal and other refuse wastes of the population
+of towns, is quite different from that which has been
+described in the preceding pages, as applicable to the agricultural
+and sanitary improvement of lands under cultivation,
+and of suburban districts. Still, the fact that town
+and house drainage affords a means for the preservation
+of valuable manures, justifies its discussion in an agricultural
+work, and "draining for health" would stop far short
+of completeness were no attention paid to the removal of
+the cause of diseases, which are far more fatal than those
+that originate in an undrained condition of the soil.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The extent to which these diseases, (of which typhoid
+fever is a type,) are prevented by sanitary drainage, is
+strikingly shown in the extract which commences this
+chapter. Since the experience to which this report refers,
+it has been found that the most fatal epidemics of the
+lower portions of London originated in the choked condition
+of the street sewers, whose general character, as well
+as the plan of improvement adopted are described in the
+following "Extracts from the Report of the Metropolitan
+Board of Works," made in 1866.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The main sewers discharged their whole contents direct
+into the Thames, the majority of them capable of
+being emptied only at the time of low water; consequently,
+as the tide rose, the outlets of the sewers were
+closed, and the sewage was dammed back, and became
+stagnant; the sewage and impure waters were also
+constantly flowing from the higher grounds, in some instances
+during 18 out of the 24 hours, and thus the thick
+and heavy substances were deposited, which had to be
+afterwards removed by the costly process of hand labor.
+During long continued or copious falls of rain, more particularly
+when these occurred at the time of high water
+in the river, the closed outlets not having sufficient storage
+capacity to receive the increased volume of sewage,<span class="tei tei-pb" id="page225">[pg 225]</span><a name="Pg225" id="Pg225" class="tei tei-anchor"></a>
+the houses and premises in the low lying districts, especially
+on the south side of the river, became flooded by
+the sewage rising through the house drains, and so continued
+until the tide had receded sufficiently to afford a
+vent for the pent-up waters, when the sewage flowed
+and deposited itself along the banks of the river, evolving
+gases of a foul and offensive character.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"This state of things had a most injurious effect upon
+the condition of the Thames; for not only was the sewage
+carried up the river by the rising tide, at a time
+when the volume of pure water was at its minimum, and
+quite insufficient to dilute and disinfect it, but it was
+brought back again into the heart of the metropolis, there
+to mix with each day's fresh supply, until the gradual
+progress towards the sea of many day's accumulation
+could be plainly discerned; the result being that the portion
+of the river within the metropolitan district became
+scarcely less impure and offensive than the foulest of the
+sewers themselves. * * * * * *</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The Board, by the system they have adopted, have
+sought to abolish the evils which hitherto existed, by
+constructing new lines of sewers, laid in a direction at
+right angles to that of the existing sewers, and a little
+below their levels, so as to intercept their contents and
+convey them to an outfall, on the north side of the Thames
+about 11-1/4 miles, and on the south side about 14 miles,
+below London Bridge. By this arrangement as large a
+proportion of the sewage as practicable is carried away
+by gravitation, and a constant discharge for the remainder
+is provided by means of pumping. At the outlets,
+the sewage is delivered into reservoirs situate on the
+banks of the Thames, and placed at such levels as enable
+them to discharge into the river at or about the time of
+high water. The sewage thus becomes not only at
+once diluted by the large volume of water in the river at
+the time of high water, but is also carried by the ebb<span class="tei tei-pb" id="page226">[pg 226]</span><a name="Pg226" id="Pg226" class="tei tei-anchor"></a>
+26 miles below London Bridge, and its return by the following
+flood-tide within the metropolitan area, is effectually
+prevented."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The details of this stupendous enterprise are of sufficient
+interest to justify the introduction here of the "General
+Statistics of the Works" as reported by the Board.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"A few statistics relative to the works may not prove
+uninteresting. The first portion of the works was commenced
+in January 1859, being about five months after
+the passing of the Act authorising their execution.
+There are 82 miles of main intercepting sewers in London.
+In the construction of the works 318,000,000 of bricks,
+and 880,000 cubic yards of concrete have been used,
+and 3,500,000 cubic yards of earth excavated. The cost,
+when completed, will have been about £4,200,000. The
+total pumping power employed is 2,300 nominal
+horse power: and if the engines were at full work, night
+and day, 44,000 tons of coals per annum would be used;
+but the average consumption is estimated at 20,000 tons.
+The sewage to be intercepted by the works on the north
+side of the river, at present amounts to 10,000,000 cubic
+feet, and on the south side 4,000,000 cubic feet per day;
+but provision is made for an anticipated increase in these
+quantities, in addition to the rainfall, amounting to a total
+of 63,000,000 cubic feet per day, which is equal to a
+lake of 482 acres, three feet deep, or 15 times as large as
+the Serpentine in Hyde Park."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A very large portion of the sewage has to be lifted
+thirty-six feet to the outfall sewer. The works on the
+north side of the Thames were formally opened, by the
+Prince of Wales, in April 1865.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the hope that the immense amount of sewage, for
+which an escape has been thus provided, might be profitably
+employed in agriculture, advertisements were inserted in
+the public journals asking for proposals for carrying out
+such a scheme; and arrangements were subsequently made<span class="tei tei-pb" id="page227">[pg 227]</span><a name="Pg227" id="Pg227" class="tei tei-anchor"></a>
+for an extension of the works, by private enterprise, by the
+construction of a culvert nine and a half feet in diameter,
+and forty miles in length, capable of carrying 12,000,000
+cubic feet of sewage per day to the barren sands on the
+coast of Essex; the intention being to dispose of the liquid
+to farmers along the line, and to use the surplus for the
+fertilization of 7000 acres, (to be subsequently increased,)
+which are to be reclaimed from the sea by embankments
+and valve sluice-gates.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The estimated cost of this enterprise is about $10,000,000.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The work which has been done, and which is now in
+contemplation, in England, is suggestive of what might,
+with advantage, be adopted in the larger cities in America.
+Especially in New York an improved means of outlet
+is desirable, and it is doubtful whether the high rate
+of mortality of that city will be materially reduced before
+effective measures are devised for removing the vast
+accumulations of filth, which ebb and flow in many of the
+larger sewers, with each change of the tide; and which
+are deposited between the piers along the river-sides.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It would be practicable to construct a main receiving
+sewer under the river streets, skirting the city, from the
+vicinity of Bellevue Hospital on the east side, passing near
+the outer edge of the Battery, and continuing to the high
+land near 60th street on the west side; having its water
+level at least twenty feet below the level of the street, and
+receiving all of the sewage which now flows into the river.
+At the Battery, this receiving sewer might be connected,
+by a tunnel, with the Brooklyn shore, its contents being
+carried to a convenient point south of Fort Hamilton,—where
+their discharge, (by lifting steam pumps), into the
+waters of the Lower Bay, would be attended with no inconvenience.
+The improvement being carried out to this point,
+it would probably not be long before the advantages to
+result from the application of the sewage to the sandy
+soil on the south side of Long Island would be manifest.</p>
+
+<span class="tei tei-pb" id="page228">[pg 228]</span><a name="Pg228" id="Pg228" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The effect of such an improvement on the health of the
+city,—which is now in constant danger from the putrefying
+filth of the sewers, (these being little better than covered
+cess-pools under the streets,)—would, no doubt, equal the
+improvement that has resulted from similar work in
+London.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The foregoing relates only to the main outlets for town
+sewage. The arterial drainage, (the lateral drains of the
+system,) which receives the waste of the houses and the
+wash of the streets, is entirely dependent on the outlet
+sewers, and can be effective only when these are so constructed
+as to afford a free outfall for the matters that it delivers
+to them. In many towns, owing to high situation,
+or to a rapid inclination of surface, the outfall is naturally
+so good as to require but little attention. In all cases, the
+manner of constructing the collecting drains is a matter of
+great importance, and in this work a radical change has
+been introduced within a few years past.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Formerly, immense conduits of porous brick work, in all
+cases large enough to be entered to be cleansed, by hand
+labor, of their accumulated deposits, were considered necessary
+for the accommodation of the smallest discharge. The
+consequence of this was, that, especially in sewers carrying
+but little water, the solid matters contained in the sewage
+were deposited by the sluggish flow, frequently causing
+the entire obstruction of the passages. Such drains always
+required frequent and expensive cleansing by hand, and the
+decomposition of the filth which they contained produced
+a most injurious effect on the health of persons living near
+their connections with the street. The foul liquids with
+which they were filled, passing through their porous
+walls, impregnated the earth near them, and sometimes
+reached to the cellars of adjacent houses, which were in
+consequence rendered extremely unhealthy. Many such
+sewers are now in existence, and some such are still being
+constructed. Not only are they unsatisfactory, they are<span class="tei tei-pb" id="page229">[pg 229]</span><a name="Pg229" id="Pg229" class="tei tei-anchor"></a>
+much more expensive in construction, and require much
+attention and labor for repairs, and cleansing, than do the
+stone-ware pipe sewers which are now universally adopted
+wherever measures are taken to investigate their comparative
+merits. An example of the difference between the old
+and modern styles of sewers is found in the drainage of the
+Westminster School buildings, etc., in London.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The new drainage conveys the house and surface drainage
+of about two acres on which are fifteen large houses.
+The whole length of the drain is about three thousand feet,
+and the entire outlet is through two nine inch pipes. The
+drainage is perfectly removed, and the pipes are always
+clean, no foul matters being deposited at any point. This
+drainage has been adopted as a substitute for an old system
+of sewerage of which the main was from 4 feet high, by
+3 feet 6 inches wide, to 17 feet high and 6 or 7 feet wide.
+The houses had cess-pools beneath them, which were filled
+with the accumulations of many years, while the sewers
+themselves were scarcely less offensive. This condition
+resulted in a severe epidemic fever of a very fatal character.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">An examination instituted to discover the cause of the
+epidemic resulted in the discovery of the facts set forth
+above, and there were removed from the drains and cess-pools
+more than 550 loads of ordure. The evaporating
+surface of this filth was more than 2000 square yards.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Since the new drainage, not only has there been no recurrence
+of epidemic fever, but "a greater improvement in
+the general health of the population has succeeded than
+might be reasonably expected in a small block of houses,
+amidst an ill-conditioned district, from which it cannot be
+completely isolated."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The principle which justifies the use of pipe sewers is precisely
+that which has been described in recommending small
+tiles for agricultural drainage,—<span class="tei tei-hi"><span style="font-style: italic">to wit</span></span>: that the rapidity of
+a flow of water, and its power to remove obstacles, is in proportion
+to its depth as compared with its width. It has been<span class="tei tei-pb" id="page230">[pg 230]</span><a name="Pg230" id="Pg230" class="tei tei-anchor"></a>
+found in practice, that a stream which wends its sluggish
+way along the bottom of a large brick culvert, when concentrated
+within the area of a small pipe of regular form,
+flows much more rapidly, and will carry away even whole
+bricks, and other substances which were an obstacle to its
+flow in the larger channel. As an experiment as to the
+efficacy of small pipes Mr. Hale, the surveyor, who was
+directed by the General Board of Health of London to
+make the trial, laid a 12-inch pipe in the bottom of a sewer
+5 feet and 6 inches high, and 3 feet and 6 inches wide.
+The area drained was about 44 acres. He found the velocity
+of the stream in the pipe to be four and a half times
+greater than that of the same amount of water in the
+sewer. The pipe at no time accumulated silt, and the
+force of the water issuing from the end of the pipe kept
+the bottom of the sewer perfectly clear for the distance of
+12 feet, beyond which point some bricks and stones were
+deposited, their quantity increasing with the distance from
+the pipe. He caused sand, pieces of bricks, stones, mud,
+etc., to be put into the head of the pipe. These were all
+carried clear through the pipe, but were deposited in the
+sewer below it.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It has been found by experiment that in a flat bottomed
+sewer, four feet wide, having a fall of eight inches in one
+hundred feet, a stream of water one inch depth, runs very
+sluggishly, while the same water running through a 12-inch
+pipe, laid on the same inclination, forms a rapid
+stream, carrying away the heavy silt which was deposited
+in the broad sewer. As a consequence of this, it has been
+found, where pipe sewers are used, even on almost imperceptible
+inclinations, that silt is very rarely deposited, and
+the waste matters of house and street drainage are carried
+immediately to the outlet, instead of remaining to ferment
+and poison the atmosphere of the streets through which
+they pass. In the rare cases of obstruction which occur,
+the pipes are very readily cleansed by flushing, at a tithe<span class="tei tei-pb" id="page231">[pg 231]</span><a name="Pg231" id="Pg231" class="tei tei-anchor"></a>
+of the cost of the constant hand-work required in brick
+sewers.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For the first six or seven hundred feet at the head of a
+sewer, a six inch pipe will remove all of the house and
+street drainage, even during a heavy rain fall; and if the
+inclination is rapid, (say 6 inches to 100 feet,) the acceleration
+of the flow, caused partly by the constant additions
+to the water, pipes of this size may be used for considerably
+greater distances. It has been found by actual trial
+that it is not necessary to increase the size of the pipe
+sewer in exact proportion to the amount of drainage that
+it has to convey, as each addition to the flow, where
+drainage is admitted from street openings or from houses,
+accelerates the velocity of the current, pipes discharging
+even eight times as much when received at intervals along
+the line as they would take from a full head at the upper
+end of the sewer.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For a district inhabited by 10,000 persons, a 12-inch pipe
+would afford a sufficient outlet, unless the amount of road
+drainage were unusually large, and for the largest sewers,
+pipes of more than 18 inches diameter are rarely used,
+these doing the work which, under the old system, was alloted
+to a sewer 6 feet high and 3 feet broad.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Of course, the connections by which the drainage of
+roads is admitted to these sewers, must be provided with
+ample silt-basins, which require frequent cleaning out. In
+the construction of the sewers, man-holes, built to the surface,
+are placed at sufficient intervals, and at all points
+where the course of the sewer changes, so that a light placed
+at one of these may be seen from the next one;—the contractor
+being required to lay the sewer so that the light
+may be thus seen, a straight line both of inclination and
+direction is secured.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The rules which regulate the laying of land-drains apply
+with equal force in the making of sewers, that is no
+part of the pipe should be less perfect, either in material<span class="tei tei-pb" id="page232">[pg 232]</span><a name="Pg232" id="Pg232" class="tei tei-anchor"></a>
+or construction, than that which lies above it; and where
+the inclination becomes less, in approaching the outlet, silt-basins
+should be employed, unless the decreased fall is still
+rapid. The essential point of difference is, that while land
+drains may be of porous material, and should have open
+joints for the admission of water, sewer pipes should be
+of impervious glazed earthen-ware, and their joints should
+be securely cemented, to prevent the escape of the sewage,
+which it is their province to remove, not to distribute.
+Drains from houses, which need not be more than 3 or 4
+inches in diameter, should be of the same material, and
+should discharge with considerable inclination into the
+pipes, being connected with a curving branch, directing
+the fluid towards the outlet.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In laying a sewer, it is customary to insert a pipe with
+a branch opposite each house, or probable site of a house.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is important that, in towns not supplied with waterworks,
+measures be taken to prevent the admission of too
+much solid matter in the drainage of houses. Water being
+the motive power for the removal of the solid parts of the
+sewage, unless there be a public supply which can be
+turned on at pleasure, no house should deliver more solid
+matter than can be carried away by its refuse waters.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The drainage of houses is one of the chief objects of
+sewerage.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In addition to the cases cited above of the model lodging
+houses in Lambeth Square, and of the buildings at Westminster,
+it may be well to refer to a remarkable epidemic
+which broke out in the Maplewood Young Ladies' Institute
+in Pittsfield, Mass., in 1864, which was of so violent and
+fatal a character as to elicit a special examination by a
+committee of physicians. The family consisted, (pupils,
+servants, and all,) of one hundred and twelve persons. Of
+these, fifty-one were attacked with well-defined typhoid
+fever during a period of less than three weeks. Of this<span class="tei tei-pb" id="page233">[pg 233]</span><a name="Pg233" id="Pg233" class="tei tei-anchor"></a>
+number thirteen died. The following is extracted from
+the report of the committee:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Of the 74 resident pupils heard from, 66 are reported
+as having had illness of some kind at the close of the
+school or soon after. This is a proportion of 33/37 or nearly
+90 per cent. Of the same 74, fifty-one had typhoid fever,
+or a proportion of nearly 69 per cent. If all the people
+in the town, say 8000, had been affected in an equal proportion,
+more than 7000 would have been ill during these
+few weeks, and about 5500 of them would have had
+typhoid fever, and of these over 1375 would have died.
+If it would be a more just comparison to take the whole
+family at Maplewood into the account, estimating the
+number at 112, fifty-six had typhoid fever, or 50 per
+cent., and of these fifty-six, sixteen died, or over 28.5 per
+cent. These proportions applied to the whole population
+of 8000, would give 4000 of typhoid fever in the same
+time; and of these 1140 would have died. According
+to the testimony of the practising physicians of Pittsfield,
+the number of cases of typhoid fever, during this period,
+aside from those affected by the influences at Maplewood,
+was small, some physicians not having had any, others
+had two or three." These cases amounted to but eight,
+none of which terminated fatally.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The whole secret of this case was proven to have been
+the retention of the ordure and waste matter from the
+kitchens and dormitories in privies and vaults, underneath
+or immediately adjoining the buildings, the odor from
+these having been offensively perceptible, and under certain
+atmospheric conditions, having pervaded the whole
+house.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The committee say "it would be impossible to bring
+this report within reasonable limits, were we to discuss the
+various questions connected with the origin and propagation
+of typhoid fever, although various theoretical views
+are held as to whether the poison producing the disease<span class="tei tei-pb" id="page234">[pg 234]</span><a name="Pg234" id="Pg234" class="tei tei-anchor"></a>
+is generated in the bodies of the sick, and communicated
+from them to the well, or whether it is generated in
+sources exterior to the bodies of fever patients, yet all
+authorities maintain that a peculiar poison is concerned
+in its production.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Those who hold to the doctrine of contagion admit
+that, to give such contagion efficacy in the production of
+wide spread results, filth or decaying organic matter is
+essential; while those who sustain the theory of non-contagion—the
+production of the poison from sources
+without the bodies of the sick—contend that it has its
+entire origin in such filth—in decomposing matter, especially
+in fermenting sewage, and decaying human excreta.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"The injurious influence of decomposing azotised matter,
+in either predisposing to or exciting severe disease, and
+particularly typhoid fever, is universally admitted among
+high medical authorities."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The committee were of the opinion "that the disease
+at Maplewood essentially originated in the state of the
+privies and drainage of the place; the high temperature,
+and other peculiar atmospheric conditions developing, in
+the organic material thus exposed, a peculiar poison,
+which accumulated in sufficient quantity to pervade
+the whole premises, and operated a sufficient length of
+time to produce disease in young and susceptible persons.
+ * * * * * * To prevent the poison of
+typhoid fever when taken into the system, from producing
+its legitimate effects, except by natural agencies,
+would require as positive a miracle as to restore a severed
+head, or arrest the course of the heavenly bodies in their
+spheres. * * * The lesson for all, for the future, is
+too obvious to need further pointing out; and the committee
+cannot doubt that they would hazard little in
+predicting that the wisdom obtained by this sad experience,
+will be of value in the future management of this<span class="tei tei-pb" id="page235">[pg 235]</span><a name="Pg235" id="Pg235" class="tei tei-anchor"></a>
+institution, and secure precautions which will forever
+prevent the recurrence of such a calamity."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The results of all sanitary investigation indicate clearly
+the vital necessity for the complete and speedy removal
+from human habitations of all matters which, by their decomposition,
+may tend to the production of disease,
+and early measures should be taken by the authorities of
+all towns, especially those which are at all compactly built,
+to secure this removal. The means by which this is to be
+effected are to be found in such a combination of water-supply
+and sewerage, as will furnish a constant and copious
+supply of water to dissolve or hold in suspension the whole
+of the waste matters, and will provide a channel through
+which they may be carried away from the vicinity of residences.
+If means for the application of the sewage water
+to agricultural lands can be provided, a part if not the
+whole of the cost of the works will be thus returned.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Concerning the details of house drainage, it would be
+impossible to say much within the limits of this book. The
+construction of water-closets, soil-pipes, sinks, etc., are too
+will be understood to need a special description here.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The principal point, (aside from the use of pipes instead
+of brick-sewers and brick house-drains,) is what is called
+in London the system of Back Drainage, where only
+principal main lines of sewers are laid under the streets,
+all collecting sewers passing through the centres of the
+blocks in the rear of the houses. Pipes for water supply
+are disposed in the same manner, as it is chiefly at
+the rears of houses that water is required, and that drainage
+is most necessary; and this adjustment saves the cost,
+the annoyance and the loss of fall, which accompany the
+use of pipes running under the entire length of each house.
+Much tearing up of pavements, expensive ditching in hard
+road-ways, and interference with traffic is avoided, while
+very much less ditching and piping is necessary, and repairs
+are made with very little annoyance to the occupants of<span class="tei tei-pb" id="page236">[pg 236]</span><a name="Pg236" id="Pg236" class="tei tei-anchor"></a>
+houses. The accompanying diagrams, (Figs. 48-49,) illustrate
+the difference between the old system of drainage
+with brick sewers under the streets, and brick drains under
+the houses, and pipe sewers under main streets and through
+the back yards of premises. A measurement of these two
+methods will show that the lengths of the drains in the
+new system, are to those of the old, as 1 to 2-1/4;—the fall of
+the house drains, (these having much less length,) would
+be 10 times more in the one case than in the other;—the
+main sewers would have twice the fall, their area would be
+only 1/30], and their cubic contents only 1/73.</p>
+
+<a name="fig68" id="fig68"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image48.png" width="640" height="776" alt="Fig. 48 - OLD STYLE HOUSE DRAINAGE AND SEWERAGE." title="Fig. 48 - OLD STYLE HOUSE DRAINAGE AND SEWERAGE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 48 - OLD STYLE HOUSE DRAINAGE AND SEWERAGE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Experience in England has shown that if the whole cost
+of water supply and pipe sewers is, with its interest, divided
+over a period of thirty years,—so that at the end of that
+time it should all be repaid,—the annual charge would not
+be greater than the cost of keeping house-drains and cess-pools<span class="tei tei-pb" id="page237">[pg 237]</span><a name="Pg237" id="Pg237" class="tei tei-anchor"></a>
+pools clean. The General Board of Health state that "the
+expense of cleansing the brick house-drains and cess-pools
+for four or five years, would pay the expense of properly
+constructed water-closets and pipe-drains, for the greater
+number of old premises."</p>
+
+<a name="fig69" id="fig69"></a><div class="tei tei-figure" style="text-align: center"><img src="images/image49.png" width="640" height="668" alt="Fig. 49 - MODERN HOUSE DRAINAGE AND SEWERAGE." title="Fig. 49 - MODERN HOUSE DRAINAGE AND SEWERAGE." /><div class="tei tei-head" style="text-align: center; margin-bottom: 1.00em; margin-top: 1.00em">Fig. 49 - MODERN HOUSE DRAINAGE AND SEWERAGE.</div></div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">One of the reports of this body, which has added more
+than any other organization to the world's knowledge on
+these subjects, closes with the following:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"Conclusions obtained as to house drainage, and the
+sewerage and cleansing of the sites of towns."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That no population living amidst impurities, arising
+from the putrid emanations from cess-pools, drains and
+sewers of deposit, can be healthy or free from the attacks
+of devastating epidemics.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That as a primary condition of salubrity, no ordure<span class="tei tei-pb" id="page238">[pg 238]</span><a name="Pg238" id="Pg238" class="tei tei-anchor"></a>
+and town refuse can be permitted to remain beneath or
+near habitations.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That by no means can remedial operations be so conveniently,
+economically, inoffensively, and quickly effected
+as by the removal of all such refuse dissolved or suspended
+in water.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That it has been subsequently proved by the operation
+of draining houses with tubular drains, in upwards of
+19,000 cases, and by the trial of more than 200 miles of
+pipe sewers, that the practice of constructing large brick
+or stone sewers for general town drainage, which detain
+matters passing into them in suspension in water, which
+accumulate deposit, and which are made large enough
+for men to enter them, and remove the deposit by hand
+labor, without reference to the area to be drained, has
+been in ignorance, neglect or perversion of the above
+recited principles.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That while sewers so constructed are productive of
+great injury to the public health, by the diffusion into
+houses and streets of the noxious products of the decomposing
+matters contained in them, they are wasteful from
+the increased expense of their construction and repair,
+and from the cost of ineffectual efforts to keep them free
+from deposit.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That the house-drains, made as they have heretofore
+been, of absorbent brick or stone, besides detaining substances
+in suspension, accumulating foul deposit, and
+being so permeable as to permit the escape of the liquid
+and gaseous matters, are also false in principle and wasteful
+in the expense of construction, cleansing and repair.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That it results from the experience developed in these
+inquiries, that improved tubular house-drains and sewers
+of the proper sizes, inclinations, and material, detain and
+accumulate no deposit, emit no offensive smells, and require
+no additional supplies of water to keep them clear.</p>
+
+<span class="tei tei-pb" id="page239">[pg 239]</span><a name="Pg239" id="Pg239" class="tei tei-anchor"></a>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That the offensive smells proceeding from any works
+intended for house or town drainage, indicate the fact
+of the detention and decomposition of ordure, and afford
+decisive evidence of mal-construction or of ignorant or
+defective arrangement.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That the method of removing refuse in suspension in
+water by properly combined works, is much better than
+that of collecting it in pits or cess-pools near or underneath
+houses, emptying it by hand labor, and removing
+it by carts.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"That it is important for the sake of economy, as well
+as for the health of the population, that the practice of
+the removal of refuse in suspension in water, and by combined
+works, should be applied to all houses, especially
+those occupied by the poorer classes."</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Later investigations of the subject have established two
+general conclusions applicable to the subject, namely, that:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"<span class="tei tei-hi"><span style="font-style: italic">In towns all offensive smells from the decomposition
+of animal and vegetable matter, indicate the generation
+and presence of the causes of insalubrity and of preventable
+disease, at the same time that they prove defective
+local administration;</span></span>
+and correlatively, that:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">"<span class="tei tei-hi"><span style="font-style: italic">In rural districts all continuous offensive smells from
+animal and vegetable decomposition, indicate preventable
+loss of fertilizing matter, loss of money, and bad
+husbandry.</span></span>"</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The principles herein set forth, whether relating to sanitary
+improvement, to convenience and decency of living,
+or to the use of waste matters of houses in agricultural
+improvement, are no less applicable in America than elsewhere;
+and the more general adoption of improved house
+drainage and sewerage, and of the use of sewage matters
+in agriculture, would add to the health and prosperity of
+its people, and would indicate a great advance in civilization.</p>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<span class="tei tei-pb" id="page240">[pg 240]</span><a name="Pg240" id="Pg240" class="tei tei-anchor"></a>
+<a name="toc70" id="toc70"></a>
+<a name="pdf71" id="pdf71"></a>
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">INDEX</span></h1>
+
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Absorption and Filtration, <a href="#Pg026" class="tei tei-ref">26</a>-39</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Angles to be, as far as possible, avoided, <a href="#Pg099" class="tei tei-ref">99</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Baking of clay soils by evaporation, <a href="#Pg030" class="tei tei-ref">30</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Barley, <a href="#Pg168" class="tei tei-ref">168</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Bartlett, Dr., quotation from, <a href="#Pg211" class="tei tei-ref">211</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Base-line, <a href="#Pg145" class="tei tei-ref">145</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Boning-rods, (with illustrations), <a href="#Pg125" class="tei tei-ref">125</a>-126</td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Central Park, <a href="#Pg074" class="tei tei-ref">74</a>-86</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Cess-pools, cause of epidemics, <a href="#Pg237" class="tei tei-ref">237</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Chadwick, Dr., quotation from, <a href="#Pg213" class="tei tei-ref">213</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Clay Soils, <a href="#Pg075" class="tei tei-ref">75</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Clay Soils, Baking of by Evaporation, <a href="#Pg030" class="tei tei-ref">30</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Clay Soils, Made mellow by draining, <a href="#Pg029" class="tei tei-ref">29</a>-30</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Clay Soils, Shrinkage of, <a href="#Pg028" class="tei tei-ref">28</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Clinometer, (illustration), <a href="#Pg056" class="tei tei-ref">56</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Collars, <a href="#Pg084" class="tei tei-ref">84</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Connections, <a href="#Pg132" class="tei tei-ref">132</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Connections (illustrations), <a href="#Pg134" class="tei tei-ref">134</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Corn, Indian, <a href="#Pg162" class="tei tei-ref">162</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Cost of draining, <a href="#Pg150" class="tei tei-ref">150</a>-153-158</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Cotton, <a href="#Pg169" class="tei tei-ref">169</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Covering and filling, cost of, <a href="#Pg157" class="tei tei-ref">157</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Covering for the joints of tiles, <a href="#Pg132" class="tei tei-ref">132</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Covering tiles, <a href="#Pg136" class="tei tei-ref">136</a></td></tr></tbody></table>
+
+<a name="Pg241" id="Pg241" class="tei tei-anchor"></a><table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Datum-line, <a href="#Pg052" class="tei tei-ref">52</a>-104</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Denton, J. Bailey, quotation from, <a href="#Pg115" class="tei tei-ref">115</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Distance between drains, <a href="#Pg073" class="tei tei-ref">73</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Diseases, malarial, <a href="#Pg208" class="tei tei-ref">208</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Ditches, cost of digging, <a href="#Pg154" class="tei tei-ref">154</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, amateur, <a href="#Pg047" class="tei tei-ref">47</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, indications of the need of, <a href="#Pg009" class="tei tei-ref">9</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, its effect on farming, <a href="#Pg171" class="tei tei-ref">171</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, tiles, how made, <a href="#Pg174" class="tei tei-ref">174</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, tiles, materials for, <a href="#Pg174" class="tei tei-ref">174</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, tools, (illustration), <a href="#Pg113" class="tei tei-ref">114</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, what it costs, <a href="#Pg150" class="tei tei-ref">150</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, will it pay? <a href="#Pg161" class="tei tei-ref">161</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Draining, when necessary, <a href="#Pg007" class="tei tei-ref">7</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, Cubic yards of excavation in, <a href="#Pg155" class="tei tei-ref">155</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, and drained land, care of, <a href="#Pg144" class="tei tei-ref">144</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, lateral, should be parallel, <a href="#Pg099" class="tei tei-ref">99</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, how they act, <a href="#Pg021" class="tei tei-ref">21</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, obstructed, how cleared, <a href="#Pg146" class="tei tei-ref">146</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, old, how formed, <a href="#Pg146" class="tei tei-ref">146</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, rate of fall, <a href="#Pg090" class="tei tei-ref">90</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drains, their action in the Central Park, <a href="#Pg086" class="tei tei-ref">86</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drained Soil, capacity for receiving water of rains, <a href="#Pg023" class="tei tei-ref">23</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drainage of dwelling houses, <a href="#Pg232" class="tei tei-ref">232</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Drought, <a href="#Pg037" class="tei tei-ref">37</a>-40</td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Economy versus cheapness, <a href="#Pg152" class="tei tei-ref">152</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Engineering and Superintendence, cost of, <a href="#Pg153" class="tei tei-ref">153</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Engineers, draining, <a href="#Pg047" class="tei tei-ref">47</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Epidemic at Maplewood Young Ladies' Institute, <a href="#Pg232" class="tei tei-ref">232</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Epidemics caused by cess-pools, <a href="#Pg237" class="tei tei-ref">237</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Epidemics caused by ordure beneath houses, <a href="#Pg238" class="tei tei-ref">238</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Evaporation, <a href="#Pg033" class="tei tei-ref">33</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Evaporation, amount of, <a href="#Pg034" class="tei tei-ref">34</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Evaporation, effect on temperature, <a href="#Pg033" class="tei tei-ref">33</a>-35</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Evaporation, heat lost during, <a href="#Pg034" class="tei tei-ref">34</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Fall, rate of in drains, <a href="#Pg077" class="tei tei-ref">77</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Fallacies in draining, <a href="#Pg062" class="tei tei-ref">62</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Fen-lands of England, <a href="#Pg193" class="tei tei-ref">193</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Fever and Ague, <a href="#Pg208" class="tei tei-ref">208</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Fever and Ague, exact cause unknown, <a href="#Pg210" class="tei tei-ref">210</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Filtration and absorption, <a href="#Pg026" class="tei tei-ref">26</a>-39</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Filling, illustration of—ditch with, furrows, <a href="#Pg141" class="tei tei-ref">141</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Filling, maul for ramming, (illustration), <a href="#Pg138" class="tei tei-ref">138</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Filling, scraper for, (illustration), <a href="#Pg140" class="tei tei-ref">140</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Filling, the ditches, <a href="#Pg136" class="tei tei-ref">136</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Finishing tools, (illustration), <a href="#Pg123" class="tei tei-ref">123</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Finishing scoop, <a href="#Pg123" class="tei tei-ref">123</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Finishing scoop, how used, <a href="#Pg126" class="tei tei-ref">126</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Foot-pick, (illustration), <a href="#Pg156" class="tei tei-ref">156</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Four-foot drains, <a href="#Pg070" class="tei tei-ref">70</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Germination of seeds, <a href="#Pg013" class="tei tei-ref">13</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Gisborne, Thos., quotations from, <a href="#Pg028" class="tei tei-ref">28</a>-31-35-47-66-78-84-93-127</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Grading, <a href="#Pg124" class="tei tei-ref">124</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Grading, cost of, <a href="#Pg156" class="tei tei-ref">156</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Grade stakes, <a href="#Pg103" class="tei tei-ref">103</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Grades, computation for, <a href="#Pg109" class="tei tei-ref">109</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Grades, how to establish, <a href="#Pg107" class="tei tei-ref">107</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Gratings in Silt-basins, <a href="#Pg148" class="tei tei-ref">148</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Hackensack meadows, <a href="#Pg203" class="tei tei-ref">203</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Hay, <a href="#Pg168" class="tei tei-ref">168</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Heat, amount of lost during evaporation, <a href="#Pg034" class="tei tei-ref">34</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">House drainage, <a href="#Pg220" class="tei tei-ref">220</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">House drainage, back drain system, <a href="#Pg235" class="tei tei-ref">235</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">House drainage bad, indicated by offensive smells, <a href="#Pg239" class="tei tei-ref">239</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Indications of the need of draining, <a href="#Pg009" class="tei tei-ref">9</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Injury from standing water in the subsoil, <a href="#Pg015" class="tei tei-ref">15</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Impervious soil, <a href="#Pg031" class="tei tei-ref">31</a></td></tr></tbody></table>
+
+<span class="tei tei-pb" id="page242">[pg 242]</span><a name="Pg242" id="Pg242" class="tei tei-anchor"></a>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">John Johnson, <a href="#Pg164" class="tei tei-ref">164</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Land requiring draining, <a href="#Pg007" class="tei tei-ref">7</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Lateral drains, <a href="#Pg061" class="tei tei-ref">61</a>-97</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Lateral drains, direction of, <a href="#Pg075" class="tei tei-ref">75</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Lateral drains, shallow, how connected with deep main, <a href="#Pg111" class="tei tei-ref">111</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">La Roche, quotations from, <a href="#Pg213" class="tei tei-ref">213</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Levels, how to take for drains, <a href="#Pg104" class="tei tei-ref">104</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Levelling instrument, (illustration), <a href="#Pg052" class="tei tei-ref">52</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Levelling rod, (illustration), <a href="#Pg053" class="tei tei-ref">53</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Location of main drains, <a href="#Pg058" class="tei tei-ref">58</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Madden, Dr., quotation from, <a href="#Pg012" class="tei tei-ref">12</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Main drain, <a href="#Pg096" class="tei tei-ref">96</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Main drain, location of, <a href="#Pg058" class="tei tei-ref">58</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malaria <a href="#Pg211" class="tei tei-ref">211</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malaria borne by winds, <a href="#Pg212" class="tei tei-ref">212</a>-214-219</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malaria conclusions of the General Board of Health of England, <a href="#Pg220" class="tei tei-ref">220</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malaria facts concerning, <a href="#Pg212" class="tei tei-ref">212</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malaria spread of, prevented by hills, <a href="#Pg218" class="tei tei-ref">218</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malarial diseases, evidence of the effect of drainage in removing, <a href="#Pg216" class="tei tei-ref">216</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malarial diseases, reports to the British Parliament concerning, <a href="#Pg216" class="tei tei-ref">216</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malarial diseases, rheumatism and tic-douloureux, <a href="#Pg219" class="tei tei-ref">219</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Malarious localities, effects of residence in, <a href="#Pg214" class="tei tei-ref">214</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Maps, amending the, <a href="#Pg142" class="tei tei-ref">142</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Maps, description of, (illustrations), <a href="#Pg049" class="tei tei-ref">49</a>-50-51-54-98</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Maps, importance of, <a href="#Pg048" class="tei tei-ref">48</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Marking the lines, <a href="#Pg116" class="tei tei-ref">116</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Mechi, Alderman, quotations from, <a href="#Pg029" class="tei tei-ref">29</a>-71</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Mellowness or Porosity, <a href="#Pg041" class="tei tei-ref">41</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Measuring staff (illustration), <a href="#Pg124" class="tei tei-ref">124</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Metcalf, Dr., quotation from, <a href="#Pg211" class="tei tei-ref">211</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Movement of water in the ground, <a href="#Pg032" class="tei tei-ref">32</a>-64-65</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Mortality, rate of reduced by improved house drainage, <a href="#Pg222" class="tei tei-ref">222</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Neuralgia, <a href="#Pg208" class="tei tei-ref">208</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">New York, suggestions for sewer outlets, <a href="#Pg227" class="tei tei-ref">227</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Oats, <a href="#Pg168" class="tei tei-ref">168</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Obstructions, <a href="#Pg090" class="tei tei-ref">90</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Opening ditches, <a href="#Pg122" class="tei tei-ref">122</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Outlet, <a href="#Pg095" class="tei tei-ref">95</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Outlet, how made (with illustrations), <a href="#Pg118" class="tei tei-ref">118</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Outlet, location of, <a href="#Pg058" class="tei tei-ref">58</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Parkes, Josiah, quotations from, <a href="#Pg036" class="tei tei-ref">36</a>-71-88-178</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Porosity, <a href="#Pg041" class="tei tei-ref">41</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Profile of a drain, (illustration), <a href="#Pg105" class="tei tei-ref">106</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Profit, instances of, <a href="#Pg167" class="tei tei-ref">167</a>-170</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Production, amount of increase of, necessary to make draining profitable, <a href="#Pg162" class="tei tei-ref">162</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Puddling, <a href="#Pg008" class="tei tei-ref">8</a>-31-148</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Pumping, <a href="#Pg206" class="tei tei-ref">206</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Pumping, London sewage, <a href="#Pg226" class="tei tei-ref">226</a></td></tr></tbody></table>
+
+<a name="Pg243" id="Pg243" class="tei tei-anchor"></a><table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Rock, sounding for, <a href="#Pg055" class="tei tei-ref">55</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Rock, how to collect water from, <a href="#Pg060" class="tei tei-ref">60</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Roots, depth to which they reach, <a href="#Pg040" class="tei tei-ref">40</a>-67</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Roots, as a cause of obstruction, <a href="#Pg093" class="tei tei-ref">93</a>-148</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Rye, <a href="#Pg168" class="tei tei-ref">168</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salisbury's, Dr., theory concerning malarious fever, <a href="#Pg214" class="tei tei-ref">214</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, catch water drains, <a href="#Pg201" class="tei tei-ref">201</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, construction of embankment, <a href="#Pg196" class="tei tei-ref">196</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, dyke and ditch, (illustration), <a href="#Pg197" class="tei tei-ref">197</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, exclusion of the sea, <a href="#Pg195" class="tei tei-ref">195</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, how formed, <a href="#Pg194" class="tei tei-ref">194</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, inundations from upland , <a href="#Pg201" class="tei tei-ref">201</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, location and size of embankment, <a href="#Pg195" class="tei tei-ref">195</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, management of creeks, <a href="#Pg198" class="tei tei-ref">198</a>-200</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, management of rivers, <a href="#Pg201" class="tei tei-ref">201</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, muskrats, <a href="#Pg199" class="tei tei-ref">199</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, outlet for under drainage, <a href="#Pg204" class="tei tei-ref">204</a>-205</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, pumping, <a href="#Pg206" class="tei tei-ref">206</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, rain-fall and filtration, <a href="#Pg204" class="tei tei-ref">204</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Salt marshes, valve-gates and sluices, <a href="#Pg204" class="tei tei-ref">204</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Scraper for filling ditches, (illustration), <a href="#Pg140" class="tei tei-ref">140</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Seeds, germination of, <a href="#Pg013" class="tei tei-ref">13</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewage, use of in agriculture, <a href="#Pg226" class="tei tei-ref">226</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewers, defects of large, <a href="#Pg228" class="tei tei-ref">228</a>-238</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewers, description of the London outfall, <a href="#Pg225" class="tei tei-ref">225</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewers, efficacy of glazed earthern pipes, <a href="#Pg229" class="tei tei-ref">229</a>-230-238</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewers, experiments of Hale on pipe sewers, <a href="#Pg230" class="tei tei-ref">230</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewers, imperfect, <a href="#Pg224" class="tei tei-ref">224</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewers, of brick, defective, <a href="#Pg228" class="tei tei-ref">228</a>-235-238</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewerage, conclusions of General Board of Health, <a href="#Pg237" class="tei tei-ref">237</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sewerage, of New York, <a href="#Pg227" class="tei tei-ref">227</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Shrinkage of clay soils, <a href="#Pg028" class="tei tei-ref">28</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sides of ditches in soft land, how braced, (illustration), <a href="#Pg124" class="tei tei-ref">124</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Silt, <a href="#Pg090" class="tei tei-ref">90</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Silt, basins, (illustrations), <a href="#Pg121" class="tei tei-ref">121</a>-135-136</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Silt, basins, how made, <a href="#Pg120" class="tei tei-ref">120</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Silt, basins, <a href="#Pg091" class="tei tei-ref">91</a>-96-134</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Silt, in tiles, <a href="#Pg144" class="tei tei-ref">144</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sources of the water in the soil, <a href="#Pg010" class="tei tei-ref">10</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Springs, how to collect the water of, <a href="#Pg059" class="tei tei-ref">59</a>-60-141</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Staking out the lines, <a href="#Pg102" class="tei tei-ref">102</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Staten Island, <a href="#Pg209" class="tei tei-ref">209</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Steam pumps, <a href="#Pg206" class="tei tei-ref">206</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Stone and tile drains, <a href="#Pg142" class="tei tei-ref">142</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Sub-mains, <a href="#Pg059" class="tei tei-ref">59</a></td></tr></tbody></table>
+
+<a name="Pg244" id="Pg244" class="tei tei-anchor"></a><table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Teams used in opening ditches, <a href="#Pg122" class="tei tei-ref">122</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Temperature, <a href="#Pg035" class="tei tei-ref">35</a>-66</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Temperature, affected by draining, <a href="#Pg036" class="tei tei-ref">36</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tile laying, <a href="#Pg127" class="tei tei-ref">127</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tile-pick, (illustration), <a href="#Pg131" class="tei tei-ref">131</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, and tile laying, cost of, <a href="#Pg157" class="tei tei-ref">157</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, capacity for discharging water, <a href="#Pg084" class="tei tei-ref">84</a>-86</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, double-style, <a href="#Pg080" class="tei tei-ref">80</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, drain—essential characteristics, <a href="#Pg022" class="tei tei-ref">22</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, how made, <a href="#Pg174" class="tei tei-ref">174</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, horse-shoe, <a href="#Pg078" class="tei tei-ref">78</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, kinds and sizes, <a href="#Pg077" class="tei tei-ref">77</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, ordering, <a href="#Pg082" class="tei tei-ref">82</a>-101</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, objections to large sizes, <a href="#Pg147" class="tei tei-ref">147</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, pipes and collars, <a href="#Pg081" class="tei tei-ref">81</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, rapidity with which they receive water, <a href="#Pg078" class="tei tei-ref">78</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, sizes of, <a href="#Pg081" class="tei tei-ref">81</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, sizes required for different areas, <a href="#Pg088" class="tei tei-ref">88</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, should be well formed, <a href="#Pg083" class="tei tei-ref">83</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, sole, <a href="#Pg080" class="tei tei-ref">80</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tiles, trimming and perforating, <a href="#Pg131" class="tei tei-ref">131</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tile making, material for, <a href="#Pg174" class="tei tei-ref">174</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tile preparation of earths, <a href="#Pg176" class="tei tei-ref">176</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tile rolling and drying, <a href="#Pg182" class="tei tei-ref">182</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tile washing the clay, <a href="#Pg177" class="tei tei-ref">177</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tobacco, <a href="#Pg169" class="tei tei-ref">169</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Tools required, <a href="#Pg113" class="tei tei-ref">113</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Town drainage, conclusions of General Board of Health, <a href="#Pg237" class="tei tei-ref">237</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Undrained land not reliable for cultivation, <a href="#Pg018" class="tei tei-ref">18</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Vermin as a cause of obstruction, <a href="#Pg093" class="tei tei-ref">93</a></td></tr></tbody></table>
+
+<table summary="This is a list." class="tei tei-list" style="margin-bottom: 1.00em; margin-top: 1.00em"><tbody><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water, depth of, <a href="#Pg066" class="tei tei-ref">66</a>-70</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water, in the sub-soil, injurious effects of, <a href="#Pg015" class="tei tei-ref">15</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water, movement of in the ground, <a href="#Pg032" class="tei tei-ref">32</a>-64-65</td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water, objections to excess of, <a href="#Pg011" class="tei tei-ref">11</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water, the best vehicle for removing ordure, <a href="#Pg238" class="tei tei-ref">238</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water, when beneficial and when injurious, <a href="#Pg024" class="tei tei-ref">24</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water-courses and brooks, how treated during draining operations, <a href="#Pg117" class="tei tei-ref">117</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Water-table, <a href="#Pg022" class="tei tei-ref">22</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Wind-mills, <a href="#Pg206" class="tei tei-ref">206</a></td></tr><tr class="tei tei-labelitem"><th class="tei tei-label"></th><td class="tei tei-item">Wheat, <a href="#Pg164" class="tei tei-ref">164</a>-167</td></tr></tbody></table>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">DRAINING ENGINEERING.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The undersigned is prepared to assume the personal
+direction of works of Agricultural and Town Drainage,
+and Water Supply, in any part of the country; or to send
+advice and information, by letter, for the guidance of
+others.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Persons sending maps of their land, with contour lines,
+(see Fig. 8, page 54,) accompanied by such information as
+can be given in writing, will be furnished with explicit instructions
+concerning the arrangement and depth of the
+drains required; kinds and sizes of tiles to be used; management
+of the work, etc., etc.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The lines of drains will be laid down, on the maps, for
+the direction of local engineers,—and, when required, the
+grades will be calculated and noted at the positions of the
+stakes.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">For particulars, address</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">GEO. E. WARING, JR.,<br />
+P. O. Box 290,<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Newport</span></span>, R. I.</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">THE SMALL FRUIT CULTURIST.</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">BY</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ANDREW S. FULLER.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span class="tei tei-hi"><span style="font-style: italic; font-weight: 700">Beautifully Illustrated.</span></span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">We have heretofore had no work especially devoted to small
+fruits, and certainly no treatises anywhere that give the information
+contained in this. It is to the advantage of special works that the
+author can say all that he has to say on any subject, and not be
+restricted as to space, as he must be in those works that cover the
+culture of all fruits—great and small.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This book covers the whole ground of Propagating Small Fruits,
+their Culture, Varieties, Packing for Market, etc. While very full on
+the other fruits, the Currants and Raspberries have been more carefully
+elaborated than ever before, and in this important part of his
+book, the author has had the invaluable counsel of Charles Downing.
+The chapter on gathering and packing the fruit is a valuable one,
+and in it are figured all the baskets and boxes now in common use.
+The book is very finely and thoroughly illustrated, and makes an
+admirable companion to the Grape Culturist, by the same author.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">CONTENTS:</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-variant: small-caps">Chap. I. Barberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. II. Strawberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. III. Raspberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. IV. Blackberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. V. Dwarf Cherry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. VI. Currant</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. VII. Gooseberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. VIII. Cornelian Cherry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. IX. Cranberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. X. Huckleberry</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. XI. Sheperdia</span></span>.<br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Chap. XII. Preparation for gathering Fruit</span></span>.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Sent post-paid. Price $1.50.</p>
+
+<div class="tei tei-tb"> </div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ORANGE JUDD &amp; CO., 245 Broadway, New-York.</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">THE GRAPE CULTURIST</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">BY</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ANDREW S. FULLER.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">NEW AND ENLARGED EDITION.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">THE STANDARD WORK</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ON THE CULTIVATION OF THE HARDY GRAPE,
+AS IT NOT ONLY DISCUSSES PRINCIPLES,
+BUT</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">ILLUSTRATES PRACTICE</span></span>.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Every thing is made perfectly plain, and its teachings
+may be followed upon.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ONE VINE OR A VINEYARD</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-style: italic">The following are some of the topics that are treated:</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-variant: small-caps">Growing New Varieties From Seed.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Propagation by Single Buds or Eyes.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Propagating Houses and their Management fully described.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">How to Grow.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Cuttings in Open Air, and how to Make Layers.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Grafting the Grape—A Simple and Successful Method.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Hybridizing and Crossing—Mode of Operation.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Soil and Situation—Planting and Cultivation.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Pruning, Training, and Trellises—all the Systems Explained.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Garden Culture—How to Grow Vines in a Door-Yard.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Insects, Mildew, Sun-Scald, and other Troubles.</span></span><br />
+<span class="tei tei-hi"><span style="font-variant: small-caps">Description of the Valuable and the Discarded Varieties.</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Sent post-paid. Price $1.50.</p>
+
+<div class="tei tei-tb"> </div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Orange Judd &amp; Co., 245 Broadway.</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">AMERICAN POMOLOGY</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">APPLES.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">By Doct. JOHN A. WARDER,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">PRESIDENT OHIO POMOLOGICAL SOCIETY; VICE-PRESIDENT AMERICAN POMOLOGICAL
+SOCIETY.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">293 ILLUSTRATIONS.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This volume has about 750 pages, the first 375 of which are devoted
+to the discussion of the general subjects of propagation, nursery
+culture, selection and planting, cultivation of orchards, care of
+fruit, insects, and the like; the remainder is occupied with descriptions
+of apples. With the richness of material at hand, the trouble
+was to decide what to leave out. It will be found that while the
+old and standard varieties are not neglected, the new and promising
+sorts, especially those of the South and West, have prominence.
+A list of selections for different localities by eminent orchardists is
+a valuable portion of the volume, while the Analytical Index or
+<span class="tei tei-hi"><span style="font-style: italic">Catalogue Raisonné</span></span>, as the French would say, is the most extended
+American fruit list ever published, and gives evidence of a fearful
+amount of labor.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">CONTENTS.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Chapter I.—INTRODUCTORY.<br />
+Chapter II.—HISTORY OF THE APPLE.<br />
+Chapter III.—PROPAGATION. - Buds and Cuttings—Grafting—Budding—The Nursery.<br />
+Chapter IV.—DWARFING.<br />
+Chapter V.—DISEASES.<br />
+Chapter VI.—THE SITE FOR AN ORCHARD.<br />
+Chapter VII.—PREPARATION OF SOIL FOR AN ORCHARD.<br />
+Chapter VIII.—SELECTION AND PLANTING.<br />
+Chapter IX.—CULTURE, Etc.<br />
+Chapter X.—PHILOSOPHY OF PRUNING.<br />
+Chapter XI.—THINNING.<br />
+Chapter XII.—RIPENING AND PRESERVING FRUITS.<br />
+Chapter XIII and XIV.—INSECTS.<br />
+Chapter XV.—CHARACTERS OF FRUITS AND THEIR VALUE—TERMS USED.<br />
+Chapter XVI.—CLASSIFICATION. - Necessity for—Basis of—Characters—Shape—Its Regularity—Flavor—Color—Their several Values, etc. Description of Apples.<br />
+Chapter XVII.—FRUIT LISTS—CATALOGUE AND INDEX OF FRUITS.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Sent Post-Paid. Price $3.00.</p>
+
+<div class="tei tei-tb"> </div>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ORANGE JUDD &amp; CO., 245 Broadway, New-York</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">GARDENING FOR PROFIT</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the Market and Family Garden.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-variant: small-caps">By Peter Henderson.</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FINELY ILLUSTRATED.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This is the first work on Market Gardening ever published in this
+country. Its author is well known as a market gardener of eighteen
+years' successful experience. In this work he has recorded this
+experience, and given, without reservation, the methods necessary
+to the profitable culture of the commercial or</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">MARKET GARDEN.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It is a work for which there has long been a demand, and one
+which will commend itself, not only to those who grow vegetables
+for sale, but to the cultivator of the</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FAMILY GARDEN,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">to whom it presents methods quite different from the old ones generally
+practiced. It is an <span class="tei tei-hi"><span style="font-variant: small-caps">ORIGINAL AND PURELY AMERICAN</span></span> work, and
+not made up, as books on gardening too often are, by quotations
+from foreign authors.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Every thing is made perfectly plain, and the subject treated in all
+its details, from the selection of the soil to preparing the products
+for market.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">CONTENTS.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Men fitted for the Business of Gardening.<br />
+The Amount of Capital Required, and<br />
+Working Force per Acre.<br />
+Profits of Market Gardening.<br />
+Location, Situation, and Laying Out.<br />
+Soils, Drainage, and Preparation.<br />
+Manures, Implements.<br />
+Uses and Management of Cold Frames.<br />
+Formation and Management of Hot-beds.<br />
+Forcing Pits or Green-houses.<br />
+Seeds and Seed Raising.<br />
+How, When, and Where to Sow Seeds.<br />
+Transplanting, Insects.<br />
+Packing of Vegetables for Shipping.<br />
+Preservation of Vegetables in Winter.<br />
+Vegetables, their Varieties and Cultivation.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">In the last chapter, the most valuable kinds are described, and
+the culture proper to each is given in detail.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Sent post-paid, price $1.50.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ORANGE JUDD &amp; CO., 245 Broadway, New-York.</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">The American Agricultural Annual</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FOR 1870.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A YEAR BOOK</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">WANTED BY EVERY BODY.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">This valuable Year Book has now reached its fourth number.
+In its general features it follows the plan of the three numbers
+that have preceded it, and, like them, is beautifully illustrated.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">CONTENTS.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Almanac and Calendar for 1870. Agricultural and Kindred Journals. Agricultural
+and Kindred Books. Prospect and Retrospect. Immigration. Home
+Markets. Coöperation among Farmers. Commercial Fertilizers. The Crops
+and the Weather. Thorough Drainage. Agricultural Exhibitions. Poultry
+Societies and Shows. Importation of Live Stock. Death of Distinguished
+Agriculturists. Inventions affecting Agriculture. Novelties in Agricultural
+Seeds, etc. Oats. Sanford Corn. Potato Fever. Adobe or Earth-wall Building—by
+E. G. Potter. Potatoes Worth Raising—by Dr. F. M. Hexamer.
+Yield of Potatoes in 1869. Wheat Hoe. How to Train a Heifer. Care of Hen
+and Chickens. Cultivation of Root Crops. Kohl Rabi. Dry Earth—the Earth-Closet
+Principle in the Barn. General Agricultural Matters. Characteristics
+of Different Breeds of Thoroughbred Stock. Earth-Closets—Success of the
+System. Progress in Fish Culture. Cold Spring Trout Ponds. Bellows Falls
+Trout Pond. Montdale Ponds. S. H. Ainsworth's Ponds and Race. Mumford
+Ponds. Poheganut Trout Ponds. Breeds of Fish. Fish as Farm Stock—by
+W. Clift. The Stocking of Ponds and Brooks. English Agricultural Implements.
+Inventions affecting Milk, and Cheese-making—by Gardner B. Weeks.
+Notes on Veterinary Subjects. Coöperation in Swine-breeding. Letter from
+Dr. Calvin Cutter. Steaming Fodder for Milch Cows—by S. M. and D. Wells.
+The Harvester, Reaper, and Mower—by Isaac W. White. Improvement in
+Drain Tiles. Farmer's Directory.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Sent post-paid. Price, fancy paper covers, 50 cents;</span></span>
+<span class="tei tei-hi"><span style="font-weight: 700">Cloth, 75 cents.</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Either of these Annuals for the three preceding years may be
+had at the same prices.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">ORANGE JUDD &amp; CO.,</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">245 Broadway, New-York.</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">The American Horticultural Annual</span></h1>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FOR 1870.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A YEAR BOOK</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FOR EVERY HOME.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The fourth number of this beautiful serial is now ready. It
+contains a popular record of horticultural progress during the
+past year, with other valuable articles, many of which are
+illustrated with elegant engravings.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">CONTENTS.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Calendars for each Month in the Year. Astronomical Memoranda. Number
+of Trees, Plants, etc., required to Set an Acre. Hardy and Tender Vegetables.
+Postage on Horticultural Matter. Tables of Quantities of Seed. The
+Retinisporas—By <span class="tei tei-hi"><span style="font-variant: small-caps">Josiah Hoopes</span></span>. Selecting and Saving Seeds—By <span class="tei tei-hi"><span style="font-variant: small-caps">Wm G.
+Comstock</span></span>. Inarching the Grapevine—By "Al Fresco." Apples in 1869—with
+Descriptions of New Varieties—By <span class="tei tei-hi"><span style="font-variant: small-caps">J. A. Warder</span></span>. Pears in 1869—with
+Notes on some of the Newer Varieties—By <span class="tei tei-hi"><span style="font-variant: small-caps">P. Barry</span></span>. Quinces in 1869.
+Plums in 1869. Peaches in 1869—New Varieties—By <span class="tei tei-hi"><span style="font-variant: small-caps">F. R. Elliott</span></span>. Cherries
+in 1869—with Notes of New Varieties and Comments on the Nomenclature
+of Older Sorts. Native Grapes in 1869. Notes on the Small Fruits in 1869—By
+<span class="tei tei-hi"><span style="font-variant: small-caps">A. S. Fuller</span></span>. Hardy Trees and Shrubs in 1869. New Roses Tested in
+1869—By <span class="tei tei-hi"><span style="font-variant: small-caps">John Saul</span></span>. The American Pomological Society. New and Interesting
+Bedding and other Plants Tested in 1869—By <span class="tei tei-hi"><span style="font-variant: small-caps">Peter Henderson</span></span>. New
+or Noteworthy Vegetables in 1869—By <span class="tei tei-hi"><span style="font-variant: small-caps">Jas. J. H. Gregory</span></span>, and others. Horticultural
+implements, etc., in 1869. Horticultural and Kindred Journals.
+Books upon Horticulture and Allied Subjects, published in 1869. List of
+Nurserymen, Seedsmen, etc.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Sent post-paid. Price, fancy paper covers, 50 cents;</span></span>
+<span class="tei tei-hi"><span style="font-weight: 700">Cloth, 75 cents.</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">Either of these Annuals for the three preceding years may be
+had at the same prices.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">ORANGE JUDD &amp; CO.</span></span>,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">245 Broadway New-York.</p>
+</div>
+
+<hr class="page" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">[Established in 1842.]</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A Good, Cheap, and very Valuable Paper for
+Every Man, Woman and Child,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">IN CITY, VILLAGE and COUNTRY,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">THE</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">AMERICAN AGRICULTURIST,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FOR THE</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">FARM, GARDEN AND HOUSEHOLD,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Including a Special Department of Interesting and
+Instructive Reading for CHILDREN and YOUTH</span></span>.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-style: italic">Agriculturist</span></span> is a large periodical of <span class="tei tei-hi"><span style="font-style: italic">Forty-four pages</span></span>, quarto, not octavo,
+beautifully printed, and filled with <span class="tei tei-hi"><span style="font-style: italic">plain, practical, reliable, original</span></span> matter, including
+hundreds of <span class="tei tei-hi"><span style="font-style: italic">beautiful</span></span> and <span class="tei tei-hi"><span style="font-style: italic">instructive</span></span> <span class="tei tei-hi"><span style="font-weight: 700">Engravings</span></span> in every annual volume.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">It contains each month a Calendar of Operations to be performed on the <span class="tei tei-hi"><span style="font-weight: 700">Farm,</span></span>
+in the <span class="tei tei-hi"><span style="font-weight: 700">Orchard</span></span> and <span class="tei tei-hi"><span style="font-weight: 700">Garden,</span></span> in and around the <span class="tei tei-hi"><span style="font-weight: 700">Dwelling,</span></span> etc.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The thousands of hints and suggestions given in every volume are prepared by practical,
+intelligent <span class="tei tei-hi"><span style="font-weight: 700">working men,</span></span> who know what they talk and write about. The
+articles are thoroughly edited, and every way reliable.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-weight: 700">Household Department</span></span> is valuable to every Housekeeper, affording
+very many useful hints and directions calculated to lighten and facilitate in-door work.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The <span class="tei tei-hi"><span style="font-weight: 700">Department for Children and Youth,</span></span> is prepared with special care
+not only to amuse, but also to inculcate knowledge and sound moral principles.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Terms.</span></span>—The circulation of the <span class="tei tei-hi"><span style="font-style: italic">American Agriculturist</span></span>, (<span class="tei tei-hi"><span style="font-weight: 700">about 150,000</span></span>) is so
+large that it can be furnished at the low price of $1.50 a year; four copies, one year, for
+$5; ten copies, one year, for $12; twenty or more copies, one year, $1 each; single
+copies, 15 cents each. An extra copy to the one furnishing a club of ten or twenty.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">TRY IT A YEAR.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">ORANGE JUDD &amp; CO.,</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">Publishers &amp; Proprietors,</span></span></p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em"><span class="tei tei-hi"><span style="font-weight: 700">No. 245 Broadway, New-York City.</span></span></p>
+</div>
+</div>
+
+<hr class="doublepage" /><div class="tei tei-back" style="margin-bottom: 2.00em; margin-top: 6.00em">
+<div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+
+
+
+ <div class="tei tei-div" style="margin-bottom: 4.00em; margin-top: 4.00em">
+ <h1 class="tei tei-head" style="text-align: left; margin-bottom: 3.46em; margin-top: 3.46em"><span style="font-size: 173%">Footnotes</span></h1>
+ <dl class="tei tei-list-footnotes"><dt class="tei tei-notelabel"><a id="note_1" name="note_1" href="#noteref_1">1.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">—<span class="tei tei-hi"><span style="font-style: italic">Puddling</span></span> is the kneading or rubbing of clay with water, a process by
+which it becomes almost impervious, retaining this property until thoroughly
+dried, when its close union is broken by the shrinking of its
+parts. Puddled clay remains impervious as long as it is saturated with
+water, and it does not entirely lose this quality until it has been pulverized
+in a dry state.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">A small proportion of clay is sufficient to injure the porousness of
+the soil by puddling.—A clay subsoil is puddled by being plowed
+over when too wet, and the injury is of considerable duration. Rain
+water collected in hollows of stiff land, by the simple movement given
+it by the wind, so puddles the surface that it holds the water while the
+adjacent soil is dry and porous.</p>
+
+<p class="tei tei-p" style="margin-bottom: 1.00em">The term <span class="tei tei-hi"><span style="font-style: italic">puddling</span></span> will often be used in this work, and the reader will
+understand, from this explanation, the meaning with which it is employed.</p></dd><dt class="tei tei-notelabel"><a id="note_2" name="note_2" href="#noteref_2">2.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">By leaving a space between the wall and the plastering, this moisture
+is prevented from being an annoyance, and if the inclosed space is not
+open from top to bottom, so as to allow a circulation of air, but little
+vapor will come in contact with the wall, and but an inconsiderable
+amount will be deposited.</p></dd><dt class="tei tei-notelabel"><a id="note_3" name="note_3" href="#noteref_3">3.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The maps in this book are, for convenience, drawn to a scale of 160
+feet to the inch.</p></dd><dt class="tei tei-notelabel"><a id="note_4" name="note_4" href="#noteref_4">4.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The instrument from which this cut was taken, (as also Fig. 7) was
+made by Messrs. Blunt &amp; Nichols, Water st., N. Y.</p></dd><dt class="tei tei-notelabel"><a id="note_5" name="note_5" href="#noteref_5">5.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The slight deviations caused by carrying the drains around large
+stones, which are found in cutting the ditches, do not affect the general
+arrangement of the lines.</p></dd><dt class="tei tei-notelabel"><a id="note_6" name="note_6" href="#noteref_6">6.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The low price at which this instrument is sold, $1.50, places it within
+the reach of all.</p></dd><dt class="tei tei-notelabel"><a id="note_7" name="note_7" href="#noteref_7">7.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Except from quite near to the drain, it is not probable that the
+water in the soil runs laterally towards it.</p></dd><dt class="tei tei-notelabel"><a id="note_8" name="note_8" href="#noteref_8">8.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Some of the drains in the Central Park have a fall of only 1 in
+1,000, and they work perfectly; but they are large mains, laid with an
+amount of care, and with certain costly precautions, (including precisely
+graded wooden floors,) which could hardly be expected in private work.</p></dd><dt class="tei tei-notelabel"><a id="note_9" name="note_9" href="#noteref_9">9.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The tile has been said, by great authorities, to be broken by contraction,
+under some idea that the clay envelops the tile and presses it when it contracts.
+That is nonsense. The contraction would liberate the tile. Drive a stake into
+wet clay; and when the clay is dry, observe whether it clasps the stake tighter or
+has released it, and you will no longer have any doubt whether expansion or contraction
+breaks the tile. Shrink is a better word than contract.</p></dd><dt class="tei tei-notelabel"><a id="note_10" name="note_10" href="#noteref_10">10.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Taking the difference of friction into consideration, 1-1/4 inch pipes
+have fully twice the discharging capacity of 1-inch pipes.</p></dd><dt class="tei tei-notelabel"><a id="note_11" name="note_11" href="#noteref_11">11.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">No. 5 was one inch in diameter; No. 4, about 1-1/3 inches.</p></dd><dt class="tei tei-notelabel"><a id="note_12" name="note_12" href="#noteref_12">12.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">If the springs, when running at their greatest volume, be found to
+require more than 1-1/4-inch tiles, due allowance must be made for the
+increase.</p></dd><dt class="tei tei-notelabel"><a id="note_13" name="note_13" href="#noteref_13">13.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Owing to the irregularity of the ground, and the necessity for placing
+some of the drains at narrower intervals, the total length of tile exceeds
+by nearly 50 per cent. what would be required if it had a uniform slope,
+and required no collecting drains. It is much greater than will be required
+in any ordinary case, as a very irregular surface has been adopted
+here for purposes of illustration.</p></dd><dt class="tei tei-notelabel"><a id="note_14" name="note_14" href="#noteref_14">14.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The stakes used may be 18 inches long, and driven one-half of their
+length into the ground. They should have one side sufficiently smooth
+to be distinctly marked with red chalk.</p></dd><dt class="tei tei-notelabel"><a id="note_15" name="note_15" href="#noteref_15">15.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The depth of 4.13, in Fig. 21, as well as the other depths at the points
+at which the grade changes, happen to be those found by the computation,
+as hereafter described, and they are used here for illustration.</p></dd><dt class="tei tei-notelabel"><a id="note_16" name="note_16" href="#noteref_16">16.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The figures in this table, as well as in the next preceding one, are
+adopted for the published profile of drain <span class="tei tei-hi"><span style="font-style: italic">C</span></span>, Fig. 21, to avoid confusion.
+In ordinary cases, the points which are fixed as the basis of the computation
+are given in round numbers;—for instance, the depth at <span class="tei tei-hi"><span style="font-style: italic">C3</span></span> would
+be assumed to be 4.10 or 4.20, instead of 4.13. The fractions given in the
+table, and in Fig. 21, arise from the fact that the decimals are not absolutely
+correct, being carried out only for two figures.</p></dd><dt class="tei tei-notelabel"><a id="note_17" name="note_17" href="#noteref_17">17.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The drains, which are removed a little to one side of the lines of
+stakes, may be turned toward the basin from a distance of 3 or 4 feet.</p></dd><dt class="tei tei-notelabel"><a id="note_18" name="note_18" href="#noteref_18">18.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The foot of the measuring rod should be shod with iron to prevent
+its being worn to less than the proper length.</p></dd><dt class="tei tei-notelabel"><a id="note_19" name="note_19" href="#noteref_19">19.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">"Talpa, or the Chronicles of a Clay Farm."</p></dd><dt class="tei tei-notelabel"><a id="note_20" name="note_20" href="#noteref_20">20.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">When chips of tile, or similar matters, are used to cover openings in
+the tile-work, it is well to cover them at once with a mortar made of
+wet clay, which will keep them in place until the ditches are filled.</p></dd><dt class="tei tei-notelabel"><a id="note_21" name="note_21" href="#noteref_21">21.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Surely such soil ought not to require thorough draining; where men
+can go so easily, water ought to find its way alone.</p></dd><dt class="tei tei-notelabel"><a id="note_22" name="note_22" href="#noteref_22">22.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The land shown in Fig. 21, is especially irregular, and, for the purpose
+of illustrating the principles upon which the work should be done,
+an effort has been made to make the work as complete as possible in all
+particulars. In actual work on a field similar to that, it would not
+probably be good economy to make all the drains laid in the plan, but
+as deviations from the plan would depend on conditions which cannot
+well be shown on such a small scale, they are disregarded, and the system
+of drains is made as it would be if it were all plain sailing.</p></dd><dt class="tei tei-notelabel"><a id="note_23" name="note_23" href="#noteref_23">23.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Klippart's Land Drainage.</p></dd><dt class="tei tei-notelabel"><a id="note_24" name="note_24" href="#noteref_24">24.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Klippart's Land Drainage.</p></dd><dt class="tei tei-notelabel"><a id="note_25" name="note_25" href="#noteref_25">25.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">Drainage des Terres Arables, Paris, 1856.</p></dd><dt class="tei tei-notelabel"><a id="note_26" name="note_26" href="#noteref_26">26.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The ends of the work, while the operations are suspended during
+spring tides, will need an extra protection of sods, but that lying out of
+reach of the eddies that will be formed by the receding water will not be
+materially affected.</p></dd><dt class="tei tei-notelabel"><a id="note_27" name="note_27" href="#noteref_27">27.</a></dt><dd class="tei tei-notetext"><p class="tei tei-p" style="margin-bottom: 1.00em">The latest invention of this sort, is that of a series of cast iron plates,
+set on edge, riveted together, and driven in to such a depth as to reach
+from the top of the dyke to a point below low-water mark. The best
+that can be said of this plan is, that its adoption would do no harm. Unless
+the plates are driven deeply into the clay underlying the permeable
+soil, (and this is sometimes very deep,) they would not prevent the
+slight infiltration of water which could pass under them as well as
+through any other part of the soil, and unless the iron were very thick,
+the corrosive action of salt water would soon so honeycomb it that the
+borers would easily penetrate it; but the great objection to the use of
+these plates is, that they would be very costly and ineffectual. A dyke,
+made as described above, of the material of the locality, having a ditch
+only on the inside, and being well sodded on its outer face, would be far
+cheaper and better.</p></dd></dl>
+ </div>
+
+
+</div>
+
+<hr class="doublepage" /><div class="tei tei-div" style="margin-bottom: 5.00em; margin-top: 5.00em">
+<div id="pgfooter" class="tei tei-div" style="margin-bottom: 4.00em; margin-top: 4.00em"><pre class="pre tei tei-div" style="margin-bottom: 3.00em; margin-top: 3.00em">***END OF THE PROJECT GUTENBERG EBOOK DRAINING FOR PROFIT, AND DRAINING FOR HEALTH***
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