IIR I CXT I 0I\ FARM, GARDEN, AND ORCHARD. HENRY STEWART, AITD G ENGUM, MEMBER OF THlE CIVIL ZNG~I"isl CILUB OF Th WORTH-W3CST, ASSOCIATE EDITOR OF THlE A31ERICAN AGRICULTURIST. WITH[ NUMEROUS ILLUSTRATIONS. NEW YORK: ORANGE JUDD COMPANY, 245 BRO&DWAY. FOR THE -BY Entered, according to Act of Congress, in the year 1877, by the ORANGE JUDD COMPANY, In the Office of the Librarian of Congress, at Washington. TABLE OF CONTENTS. PAGE. CHAPTER I. The Necessity for Irrigation............................................ 7-10 CHAPTER IH. Importance of an Adequate Supply of Water.............................11 —20 CHAPTER I. Amount of Water Needed for Irrigation...................................21-30 CHAPTER IV. Irrigation of Gardens......................................................31-39 CHAPTER V. Preparation of the Surface..............................................40 50 CHAPTER VI. Irrigation by Pipes and Tiles..............................................51-57 CHAPTER VII. Irrigation with Liquid Manure...........................................57 —7 CHAPTER VIII. Culture of Irrigated Garden Crops.........................................78-87 CHAPTER IX. Irrigation of Orchards and Vineyards...................................... 87-95 CHAPTER X. Irrigation of Meadows....................................................9-105 CHAPTER XI. Use of Springs in Irrigation.......................................105-117 CHAPTER XII. Formation of Water Meadows.........................................118-133 CHAPTER XIII. Irrigation of Meadows and Pastures..................................... 133-145 CHAPTER XIV. Drainage of Irrigated Fields....................................14152 CHAPTER XV. Management of Irrigated Fields.........................................152-162 CHAPTER XVI. Irrigation of Arable Lands............................................. 16.188 CHAPTER XVIL. Preparing the Surface for Irrigation...................................1206 CHAPTER XVIIL Supply of Water-Dams-Ptmps-Reservoirs-Artesian Wells..........207-237 CHAPTER XIX, Canals and their Construction......................................237-252 CHAPTER XX. Reclamation of River Flats, Salt Marshes and Submerged Lands.......3-262 3 384373 LIST OF WORKS AND PERIODICALS, WHICH HAVE BEEN CONSULTED OR QUOTED IN THE PREPA RATION OF THIS WORK. ,tudes sur les irrigations de Pyrenees Orientales. M. Vigan. Economie Rurale. Boussingault. }4rnces sur l'emploi des eaux dans les irrigations. Herve Mangon. ltalian Irrigation. M. Baird Smith. Iigation in &ohet Europe C. C. Scott Moncrieff. Des Irryations du iemont, etc. A. Vignotti. Manual of Hydrology. N. Beardmore. tude sur le service Hydraulique. De Passy. Irrigations du midi de l'Espagne. M. Aymard. panish Irrigation. C. R. Markham. La cience des Fontaines. Dumas. Hydrologie Agricole. De Buffon. Traitd d'hydrauligues Agricoles. Duponchel. Outlines of Modern Farming. R. Scott Burns. Hydrauic Engineering. C. R. Burnell. Hydraulic'ab>es. John Neville. Drainae, Irrigations, etc. M. Barrol. Manud de l'Irriateur. M. Villeroy. Irrigations et assainiment des terres. Pareto. TheoeH et rtiqet sur les igations. De Cossigny. Fratique des Irriqations en France et en Algereid. F. Vidalin. Culture des plantes Industrielles. G. Heuze. Reclion and rovement of Agriultural Land. D. Stevenson. Jourmd d'Agriture pratique. Paris. rt of the Department of Agriwture. Washington. Ifc Rural Press. San Francisco. American Agriculturit. New York. 4 PREFACE. This work is respectfully offered to those American Farmers, and other cultivators of the soil, who from painful experience can readily appreciate the losses which result from the scarcity of water at critical periods, as well as to those enterprising pioneers whose efforts are showing it to be possible to reclaim from sterility the socalled "Great American Desert." Being the first effort in American literature in this direction, it is presented with diffidence as a necessarily imperfect attempt to supply the information anxiously sought for by the classes of persons above indicated. The information here given has been acquired during some years of observation and study, and to some extent from rude, but effective practice. Hitherto there has been no work in the English language in which the practical details of irrigation were comprehensively described. The literature of the subject consists chiefly of the writings of French and Italian authors. Systems of irrigation are neither few nor modern, but all the existing methods have been the slow growth of hundreds or thousands of years. No one would be so rash as to assert that no advance upon the ancient, or even the modern methods, can be made by Americans. A nation that has done so much in originating and developing steam navigation, railroads, and the electric telegraph, can not fail to learn the best methods of utilizing streams of water, or of storing the excessive rainfall of one part of the year for use in a season of drouth. The fact that land, which without 5 PREFACE. water has no salable value, immediately finds purchasers at $50 to $200 per acre, when a supply of water has been brought to it, can not fail to call attention to irrigation and quicken enterprise in its practice. The endeavor to popularize information upon this subject and hasten the benefits that may result from its practice, is a work not without value or honor, even if it may have no other effect than to point out the way which some more competent laborer may follow with greater success. The present is a favorable time for such an attempt. At the time these lines are written the expected seasonable rains are withheld in California, and the harvest of 1877 is endangered. Prices of wheat are rising; numerous flocks are in danger for want of water, and distress is threatened in many quarters. Farmers and gardeners in the East, who for some years past, for want of rain, have seen the profit of their labors lost, are seeking some cheap and effective methods of irrigation, by which such calamity may be avoided in future. In the great West millions of fertile acres are waiting to be reclaimed from aridity, that they may furnish homes for enterprising young men, and help to supply Europe with bread. Irrigation is the only resource which can provide for all these contingencies. To show what has already been done; how it has been done; how our circumstances match with or differ from those in which the older systems have been applied; to offer plans and suggest cautions which occur to one who is both a farmer and an engineer, are the aims of the following pages. That the work may be at least of some help to his fellow laborers -the agriculturists of America-is the earnest wish of TE, Author. Hackensack,. J., January, 1877. 6 IRRIGATION FOR THE FARM, GARDEN AND ORCHARD. CHAPTER I. THE NECESSITY FOR IRRIGATION. The American climate is especially subject to destructive drouths, and scarcely a year passes in which the crops do not partially or wholly fail over extensive districts. That famines do not occur is not that there are no failures of crops sufficiently serious to cause them, but that our social system is so instantly helpful in case of need, that the want and misery that would otherwise certainly occur are averted by immediate and generous relief. The farmer, when rain fails, is helpless, yet there may be abundant water flowing uselessly past his suffering crops. We possess vast districts, the soil of which is of the highest fertility, but which remain barren and desert because the climate is rainless, yet large rivers flow through these arid tracts, and exhaustless subterranean streams pass through the subsoil. Water only is needed to make these tracts highly productive. The proof of this exists in the fact that already several successful efforts have been made to reclaim portions of these dry wastes by the application of a system of irrigation. But it is not only a question whether or not crops can be produced where they are now impossible, or whether or not the effects of (7) - 6 6 IRRIGATION. drouths may be averted by irrigation, but whether or not the general average of the crops may be largely increased by the systematic use of partial irrigation, and the use of such supplies of water as a majority of farmers can readily avail themselves of in every part of the country. What farmer is there who has not, in the majority of seasons, felt that some at least of his crops could have been largely benefited and increased by a copious supply of water at critical times? Market gardeners, whose crops on the average reach a value of several hundred dollars per acre, and to whom a loss of crop is partial or complete ruin, every year experience a vast amount of loss which might have been avoided were a supply of water available. A portion of this loss, in the shape of higher prices, necessarily falls upon the consumers, whose resources are insufficient to meet the increased demand; and the poorer of them are compelled in consequence to deny themselves those articles of food which are necessary to their complete health. The failure is then a public calamity. The season of 1874 was especially disastrous to strawberry growers, whose crops failed for want of rain at the season when the fruit is formed. Here were losses approaching in many cases the large sum of a thousand dollars per acre to the growers, which might have been avoided by the timely application of water. Every year there are more or less of such cases in connection with such special crops. The present year (1876) has been equally disastrous to gardeners and market farmers over a large extent in the East. The great difficulty experienced by the orange growers of Florida is precisely this want of water at critical periods. It is unnecessary to multiply instances. No one doubts the absolute necessity of water to the growth of plants. The value of water as a nutriment or as a means of conveying nutriment to plants, however, 8 WATER A FOOD FOR PLANTS. depends upon some facts in vegetable physiology that are not generally known or considered. These may be condensed into the following statement: Growing plants contain from 70 to 95 per cent of water. To the extent that water supplies this necessary constituent of a growing plant, it is an actual nutriment. The solid portion of the plant consists of matters which enter into it only while in solution in water. Water is the vehicle by which the solid part of a plant is carried into its circulation for assimilation. If water is not adequately supplied, an insufficient quantity of nutriment only will be carried into the circulation of the plant, and its growth will be stunted or arrested altogether. No water, whether it be in the state of liquid or vapor, can enter into any other part of a plant than its roots. The common idea that water or watery vapor is ever absorbed through the leaves of a plant is unfounded. The quantity of water that must pass through the roots of a plant of our ordinary farm crops, and to be transpired through the leaves, to carry it from germination to maturity, is equal to a depth of 12 inches over the whole soil covered by the crop. This is the requirement of an average crop upon a moderately well-cultivated soil. If the crop is stimulated to extraordinary growth by large applications of manure or other fertilizers, a still greater supply of water is needed to meet the demands of the crop. Thus the yield of a crop depends in certain cases entirely upon the amount of water supplied, and to a certain extent bears an exact ratio with it. The summer rainfall in our climate is rarely, if ever, adequate to the requirements of what would be a maximum crop, consistent with the possibilities of the soil. Our intense heats cause a large proportion of the rain-fall to be evaporated directlyfrom the soil. Our copious summer rains are seldom wholly retained by the soil, but frequently in large part escape into streams and water 9 IRRIGATION. courses, and are lost to vegetation. Our fall, winter, and early spring rains come at times when the crops derive the least benefit, or none at all, from them. The amount of rain-fall that thus escapes paying tribute to our crops is by far the largest portion of it. To estimate it at three-fourths of the whole would not be unreasonable. There would then be left less than 12 inches of water to meet the necessities of the growing crops. That this sufficiently accounts for the low average of our yearly production of grass and grain is not at all improbable. The supply of water then becomes the measure of the fertility of our soil, and our climate, subject to torrid drouths in the midst of the growing season, is the obstacle to success which meets the farmer rather than the impoverished soil -a condition, indeed mainly due to a poverty of water. To remove this obstacle to successful cultivation, it is only necessary that a system of irrigation, be adopted. An adequate supply of water, ready for use in case of emergency, will render the farmer, the gardener, or the fruit grower, to a very large extent, independent of the vicissitudes of the season, and secure, beyond accident, a full reward for his labor. If with a system of irrigation a proper system of drainage be also adopted, the cultivator of the soil will have removed two adverse influences, against which he is now called upon so frequently, and so ineffectually, to strive. To irrigate economically, and successfully, however, is a business which requires a large amount of technical knowledge and skill, and the expenditure of a considerable amount of capital either in money or labor. Irrigation belongs, in fact, to a highly advanced condition of agriculture, and can only be applied to lands of high value or capacity in the hands of intelligent owners. But it is clearly manifest at the present time, if it never was before, that the farmer, or other cultivator of the soil, who would succeed in keeping abreast of our progressive 10 AMOUNT OF WATER USED BY PLANTS. age must labor more intelligently, must greatly increase the productive capacity and value of his land, and must employ a larger amount of capital in money, or its equivalent in labor and skill, than he has hitherto done. One of the means placed in his hands, by those circumstances which ever favor the enterprising and industrious man, to employ all these, is to make use of the supply of water, from springs, wells, and streams, which may be available to nourish and increase his crops when rain is withheld, and their growth is consequently arrested. CHAPTER II. IMPORTANCE OF AN ADEQUATE SUPPLY OF WATER. Water is not only necessary for vegetable growth, but it is well established that to a great extent the amount of growth depends upon the quantity of water supplied to a crop. Years ago, when a large portion of the country was covered with forests, and when the cleared soil was well filled with the decaying remains of the removed woods, the produce of the newly cleared fields was more than double that of to day. Then the soil was absorbent of water, it was not subjected to the influence of sweeping winds; the rain-fall was held in the soil for a longer time, and did not pass off in immediate freshets and floods. Consequently the crops had a constant supply of water, and their yield was a maximum one. As a coincidence might be cited the comparatively large average yield of the soil, in the so-called moist climate of England and Ireland. "So-called moist," because, as it happens, the annual rain-fall in our so-called dry climate, is nearly, if not quite, double that of Great Britain. Here the rain-fall is over 40 inches in the year, there it is not much over 20 inches. But the English climate is insular, and 11 IRRIGATION. is influenced by the moist winds of the ocean, and the fogs from the Gulf Stream. The evaporation from the soil is therefore reduced to a minimum, and the light rain-fall, more constant than with us, and consisting of frequent light showers, is ample for the needs of vegetation. On the contrary our climate is continental and subject to the influence of dry winds, and a higher temperature, and our heavier but more inconstant rainfall is found inadequate. Hence our low average of those crops which need a large quantity of water for their maximum growth, and hence the ineffective efforts of American farmers to reach the high averages of the crops grown in England. Some very interesting experiments showing this relation between the weight of grain produced and the quantity of water consumed by the plants, whether evaporated through their leaves, or appropriated by their tissues, were made in 1874, at the Agricultural Observatory of Montsouris, France. The grain grown was wheat. Several kinds of soils and fertilizers were used, which gave very varying results, but the variety in the amounts of the product was remarkably illustrative of the facts proved. The means adopted for determining the results were the most complete, and there is no reason to doubt the entire accuracy of the conclusions reached. The results are given in the following table: I.-Table showing the total qtuatity of water evaporated and the grain pro duced; also the quantity of water consumed for one pound of grain in nine eperiments with various fertilizers. Pounds of water Pounds of.rain Pounds of water evaporated. produced. for one of grain. No. 1........... 1,616 0.6 2,693 " 2........... 1,512 0.8 1,890 " 3............... 4,703 2.4 1,960 " 4.............. 2,202 2.7 816 " 5............... 3,262 2.9 1,125 6............... 4,327 3.1 1,395 " 7.............. 4,751 5.5 861 " 8............... 7,417 9.2 806 " 9.............. 7,702 10.6 727 12 ILNSUFFICIENCY OF RAINFALL. The production of straw was very nearly double that of grain in every case, and the increase constant and regular. In the very exhaustive experiments which have been made by Mr. J. B. Lawes, of Rothamstead, England, to ascertain the amount of water consumed by a growing crop of wheat, it was very clearly shown, that for every pound of dry matter produced, 200 pounds of water was evaporated, and that for every pound of mineral matter assimilated by the crop, 2,000 pounds of water passed through the plant. Mr. Lawes therefore declared, that for a maximum crop of wheat, in England, the supply of rain water was totally inadequate. Leguminous plants, (beans, clover, etc.,) required a still more abundant supply of water than wheat, and of course the more luxuriant the growth, the greater the expenditure of water. Comparing the results of Mr. Lawes investigations with those at Montsouris, a striking equality is found. In the maximum crop there grown, 727 lbs. of water were evaporated for one pound of grain and two of straw, giving 242 pounds of water for one pound of total produce. If, as is probably the case, the weight of the roots was included in Mr. Lawes estimate, as it was not in the other, the approach to equality between the two results would be very close indeed. One therefore corroborates the other. These results show, in a very remarkable manner, the absolute necessity for an adequate supply of water for the successful prosecution of an advanced agriculture. The plants grown in these experiments were supplied with water at libitum. Those which grew luxuriantly under the effect of the most active and valuable manure, viz. a mixture of phosphate of ammonia, nitrate of potash, and chloride of sodium-a very complete fertilizer-are seen to have consumed a very large quantity of water, and nearly five times as much as those which grew most feebly. 13 IRRIGATION. The measure of the water consumed may thus be considered as the measure of the capacity of the soil to furnish itsproduct, for it is clear that if this large quantity of water was not supplied, the excessive product of grain could not have been grown. If this conclusion be correct, we have at once a satisfactory explanation of the hitherto strange fact that our best farmers, in no way less skillful or less enterprising, and with no less fertile soil, than the English farmers, can very rarely reach, and still more rarely surpass a crop of 40 bushels of wheat per acre, while in England 64 and 66 bushels are common with the best farmers. Taking the minimum quantity of water, (viz. 727 lbs.) evaporated for a pound of grain, a harvest of 40 bushels of wheat per acre, would consume, or pass through its leaves, an amount equal to 6 inches in depth, over the whole surface of the ground. But this is not a complete statement, for the average result of a large number of experiments made in the previous year, and these results as well, prove that a crop of wheat of 40 bushels per acre, may consume, or evaporate, through its leaves, a quantity of water equal to a rainfall of over 17 inches; for the less vigorous the growth, the greater is the proportionate consumption of water, and the yield which consumed 727 lbs. of water for one of grain, was greatly in excess of 40 bushels per acre. If to this consumption of water is added the excessive evaporation from the soil, consequent upon the hot suns and dry winds of our growing season, as well as the loss through the passage of water over the frozen surface of the soil, during our long winters, the totally inadequate supply of water, for a maximum crop, under our now usual conditions, is very evident. It is also evident, that where crops can be grown by irrigation, and an ample supply of water provided, there the success of the farmer will be assured, and there the risks from untimely drouths may be wholly avoided. It is also evident that every 14 RAINFALL IN CALIFORNIA. where that the conditions permit of it, our grass crops may, by means of irrigation, be made equal to those of the most favored climates, and that the productiveness of our meadows may be increased greatly beyond that which is now possible by the most skillful culture. But a large portion of our territory is practically rainless and arid. The configuration of the surface is such, that the passage of rain clouds is arrested by high mountains, and the precipitation is confined to very small and elevated areas. This is the case with nearly the whole of our territory west of the 100th meridian of longitude, or a line drawn through the western part of Kansas and Nebraska, from north to south. In this extensive district are found some of the richest soils in the world, which will yield, with irrigation, a yearly average of 30 to 40 bushels of wheat per acre. During the growing season the rain-fall is the least; the greatest amount taking place in the winter months in the form of snow. The amount of the rain-fall decreases from the 100th meridian, where it is less than 20 inches in the year, to 7 to 15 inches further west, and increases as the Pacific Coast is reached, where it measures 9' 14 inches in Southern California up to about 23 inches at San Francisco. But the fall is very irregular, depending greatly upon local causes. This is shown by the following facts, derived from scientific observations at various points in California, where the contiguity of the coast range of mountains with that of the Sierra Nevada causes many very surprising differences in the amount of the rain-fall. Thus while at San Francisco the fall averaged 23 inches yearly during 19 years, 14 miles distant at Pillarcito's Dam it averaged during nine years, 58 inches yearly. This irregularity is intensified by the dry winds which absorb moisture to an extraordinary degree; a north wind, hot and dry, which occasionally blows in the San Joaquin and other rallies, has evaporated one inch of water in a day. 15 IRRIGATION. The following table gives the range at the various localities for the period mentioned, viz.: Locality. Pmod. Rain-fallU. Fort Reading............... 3 years 15.9 to 37.4 inches. Sacramento................17 " 11.2 to 27.5 " Millerton.................. 6 " 9.7 to 49.3 " Stockton................... 3 " 11.6 to 20.3 Fort Tejou................ 5 " 9.8 to 34.2 Monterey................... 5 " 8.2 to 21.6 San Diego..................12 6.9 to 13.4 " Benicia.....................12 " 11.8 to 20.0 " During these years in which the rain-fall marked the lowest range, the distress amongst farmers was extreme. South of Monterey, in the three years from 1868 to 1871, neither grass nor grain grew. Hundred of farms were abandoned, and stock men drove their cattle, horses, and sheep up into the mountains for food and water. In the Spring of 1870 the great Santa Clara valley was entirely destitute of grass, and the plains of Los Angeles, comprising over a million acres of land, were barren to the borders of the streams. Elsewhere the same effects were visible, and over the entire State hundreds of thousands of horses, cattle, and sheep, starved to death. The estimate of the farmers, in the southern part, of the great valley of California is, that but two crops can be secured in five years, without irrigation, but in the extreme south this is to be still further reduced. In 1850 only 7 inches of rain fell at San Francisco. Further east, in Nevada, Utah and Colorado, where the soil is rich and arable, no dependence can be placed upon the rain-fall, which does not even serve to start the growth of the crops. A great depth of snow, however, falls upon the mountains, which in melting fills the rivers and can be made to furnish an adequate supply during the growing season. Through the whole of this western territory the total supply of water is sufficient to ensure good crops yearly, if it can only be secured and utilized. The first difficulty lies in arresting its escape, and the 16 VALUE OF THE GRASS CROP. secondin distributing it where it is needed, in an econom ical manner. The great valley of California includes an area of 57,200 square miles, which is equal to that of Illinois or Michi gan. The area of the lesser valleys is equal to 18,750 square miles, or 12,000,000 acres, susceptible of irrigation. For every one of these acres capable of irrigation, there are three which serve as a water shed, thus, as it were, quadrupling the rain-fall of the valleys, if the water shed of the hills can be utilized. The area of land that may be brought under irrigation in other parts of the comparatively rainless district, and the area of water shed, has about the same relative proportion, but are of far greater extent. Altogether, the increase of wealth that must accrue from the reclamation of these vast fertile tracts, which want only water to cover them with verdure, is beyond computation. But this increase of wealth, great as it would be, cannot fail to be exceeded by that which would result from the general application of irrigation in those parts of the country where only partial watering is needed; and the prevention of losses by drouth, and the ravages of destructive insects to which moisture is fatal, which every year, in one portion or another of the country, reduce farmers profits, or cause them to disappear entirely. As an example the single case of the grass crop may be considered. The value of the grass crop of the United States, including hay and the products of pasture, is greater than the combined value of all other crops. This statement will doubtles be a surprise to many, nevertheless it may be substantiated by the following figures. The total hay crop of 1870 was 27,316,048 tons, the average value of this at a moderate estimate would not be less than $10 per ton, or over 273,000,000 dollars. The total dairy products, which should be credited to pasture, were estimated, in 1870, as 1,000,000,000 lbs. of 17 IRRIGATION. butter, 100,000,000 lbs. of cheese, and 400,000,000 gallons of milk sold or used. The total value of these is not less than 400,000,000 dollars. Then there should be credited to the grass crop, in large part, the value of the wool and lambs produced, or at least 100,000,000 dollars; also one half at least of the value of the yearly increase of live stock, which is supported on grass the greater part of the year, and this would reach a sum of 200,000,000 dollars. To place these in tabular form would further impress the importance of the grass crop upon the mind of a reader; this may be done as follows: Yearly value of the hay crop........................... $273,000,000 " " of dairy products, produced from grass... 400,000,000 " " of lambs and wool, due to pasturage...... 100,000,000 " " of increase of other live stock............ 200,000,000 Total annual value of the grass crop................$973,000,000 This vast amount is in excess of the value of all the rest of our farm products, in which may be included cotton, corn, wheat, and other grains. When we consider that by a complete system of irrigating our grass lands alone, the crop could easilybe doubled in value, the immense importance of the subject to the agricultural interestof the country is at once seen. There are, comparatively, few cases in which some system of irrigation, more or less complete, could not be applied at least to grass lands, or to now useless lands that could be turned into luxuriant meadows. But there is still another view of this matter which ought to be considered. It is not only true that water is needed to supply the requirements of plants, but when used in irrigation, it brings withis reach of the plants a largely increased amount of nutriment. Water is the universal solvent. No water in its natural condition is pure. The water of springs and streams holds in solution or suspension a quantity of mineral and gaseous matters, that possess high fertilizing value. The 18 MINERAL MATTER CONTAINED IN WATER. rain water washes the soil, and whether it flows over its surface or percolates through it to the subsoil, it takes up in its course a portion of the soluble matters which it meets. Thus the water of the earth contains lime, magnesia, soda, potash, iron, sulphur, silica, ammonia, carbonic acid, nitric acid and oxygen, in solution. Besides this, many solid substances are held mechanically and in suspension, and are deposited whenever the flow is arrested and the water becomes still. In Professor Geo. H. Cook's valuable work on the Geology of New Jersey, the following examples are given: Analysi of water of the Delawoare river, de by Henry Wurtz, NV.. State Chemist. Grains. Whole solid matter contained in a gallon..............3.97 Consisting of carbonate of lime...................... 1.30 " Carbonate of magnesia..................0.89 " Carbonate of potash.....................0.17 " Chloride of sodium......................0.11 " "Chloride of potassium...................0.01 " " Sulphate of lime........................0.19 " " Phosphate of lime......................0.14 " Silica...........................0.50 " Sesqui-oxide of iron.....................0.03 " Organic matter containing ammonia......0.63 The water of the Delaware is considered as exceptionally free from impurities. It is interesting to notice the composition of its impurities in connection with the practically inexhaustible fertility of the flats of this river, which are annually overflowed and thereby enriched. A comparison of the solid matters contained in 100,000 parts of the waters of several of our rivers is here given, as follows, viz.: Rivers............... Passaic. A.chuylkill. CGroton. Hudson. Solid contents......... 12.75 9.41 18.71 18.48 Inorganic.............. 7.85 7.29 11.32 14.52 Organic................ 4.90 2.12 7.39 3.96 Numerous other examples might be given were they needed; it will be sufficient for the purpose to notice 19 IRRIGATION. that these examples are taken from streams, the waters of which were carefully examined, with a view to their value and use for domestic supply of various neighboring cities; and if these waters, selected for their purity, contain so much foreign matter, how much must be contained in those turbid streams, the waters of which are not only highly charged with soluble matter, but carry in suspension solid matter of which vast banks are sometimes deposited in the course of a few weeks or months. The value of all the water which now passes away uselessly, but which might be arrested and made to deposit on the soil, or convey to the roots of crops, its burden of fertilizing matter, if it were made useful in irrigation, is more than can be readily calculated. An estimate made by Herve6 Mangon in his work entitled Experiences sur l'emploi des eaux dans les irrigations, of the yearly value of the solid matter conveyed into the ocean by the river Seine, may be cited. He says: "each 200,000 cubic meters of water employed in irrigation, will produce a quantity of alimentary substances equal to one average butcher's beef. Then the waters of the Seine that are lost from the services of irrigation carry into the sea the equivalent of one fat ox every two minutes, or 720 every twenty four hours, or 262,800 in the year." As compared with American rivers the Seine is a small stream; what then might be the value of the Missouri, or the Mississippi, with its affluents, or any one or all of our other rivers and streams, great and small, that now pay no tribute to us in this direction in any way whatever. 20 LANDS THAT MAY BE IRRIGATED. CHAPTER III. THE AMOUNT OF WATER NEEDED FOR IRRIGATION. There are but few fields or gardens so situated that water may not be applied to them in one or more of the methods which have been at one time or another, or may be, adopted to irrigate the soil. The only prerequisites are, the supply of water and the power to bring it into such a position that it can be spread over the land. Where, however, the cost of procuring and applying water will be greater than the profit to be derived from its use, it may be concluded that there irrigation is impossible. There are some lands situated so far above the supply, that the cost of raising the water and of providing reservoirs to receive and hold it until it could be distributed, would be greater than the value of any benefits likely to accrue from its use. There are others so low that to irrigate them, without at the same time providing for a perfect system of sub-soil drainage, would be to turn them into marshes and ruin them for agricultural purposes. In these cases, if the cost of drainage should exceed the value of the benefits received from the land, it would manifestly be impossible to irrigate them. On the other hand, where these hindrances do not exist, there are very few physical features of the land that could stand in the way of irrigating it. Level lands, or lands level in one direction with a slope in another; lands sloping in every direction; hill sides either of moderate slope or such abrupt slope that terraces must be made to retain the soil; all these may be prepared by simple methods of engineering to receive any supply of water that can be economically brought to them. Equally those lands which happen to lie beneath the level of a stream or tidal river; a marsh, submerged wholly or par 21 IRRIGATION. tially at certain seasons, or land in similar situations, but not overflowed, may frequently be brought under reclamation and made subject to drainage and irrigation with great profit. There are also numerous tracts of lands along the borders of many rivers and streams that have been washed and injured by freshets so as to be in their present condition worthless for cultivation, which at a small outlay may be covered with new soil of a most fertile character, and again rendered useful and profitable by the use of appropriate methods of irrigation. Besides these, there are extensive tracts of land at the mouths of tidal streams or estuaries, or at the confluences of large rivers, which are always under water or exist as mud banks, which may be reclaimed by judicious engineering, and converted in a few years into agricultural land of the richest quality. All these processes belong to the art of irrigation, and the cases in which one or another of them are impossible of application are very rare indeed. The supply of water is a more serious consideration than the shape or configuration of the land. Where this is not naturally available no art of the engineer can provide it. The only safe dependence is upon streams or springs, and reservoirs in which the rain-fall of winter and spring may be gathered and stored. Wells can only be depended upon for such a small supply as would serve to irrigate a garden or small market farm, where the large value of the crops would admit of the cost of raising water for a lengthened season and storing it in reservoirs for use in emergencies. The idea that artesian wells may be made a source of supply for completely irrigating large tracts of land, if ever held by any over-sanguine persons, must be abandoned. For partial irrigation they may be made available, but the quantity of water needed for the irrigation of a few acres of land only, in localities where there is no summer rain-fall, as upon our Western plains, 22 CORRECT ESTIMATES OF WATER NEEDED. is far beyond the capacity of any artesian well to supply, unless it be one of extraordinary volume. It is very important that the quantity of water needed for irrigation should be accurately estimated. A mistake in an estimate may lead to the construction of inadequate works, and the useless expenditure of much money. Estimates generally err upon the side of insufficiency rather than otherwise, and much error has been spread abroad by persons and journals having considerable influence. Not long ago the "Scientific American" editorially announced that one artesian well would supply a farm of 640 acres upon the plains with water for irrigation, and would also form a nucleus for many large stock farms." The late Horace Greeley, who, although an enthusiast upon this subject, was more nearly correct, thought one artesian well would serve to irrigate a quarter section of land, or 160 acres. The wildly excessive estimates of the value of a certain amount of water might be easily disproved by the careful use of a few figures, and a little common sense. For instance, let any person who has ever watered a garden plot and who knows the effect of one inch in depth of water upon a dry soil, consider the following facts, and then apply them to the matter in question, and he will readily see the absurdity of the estimates above referred to. lst. There are 6,272,640 square inches in an acre. 2d. One inch of water, or a stream one inch wide and deep, flowing 4 miles an hour, will equal 6,082,560 inches in 24 hours. 3rd. Therefore 1 inch of water flowing 4 miles an hour, for 24 hours, will cover one acre nearly an inch deep. 4th. One inch of water per week equals 52 inches per year, or more than the yearly rain-fall. 5t. Therefore 1 inch of water should serve to irrigate only 7 acres once a week, at least as well as the average rain-falL 23 IPRRIGATION. 6th. One inch of water flowing 4 miles per hour, equal one and one-fifth quart per second. 7th. One quart per second, flowing for 24 hours, will cover an acre five-sixths of an inch deep. 8th. One inch of water flowing 4 miles an hour is equal to 18 gallons per minute, or 1,080 gallons per hour. 9th. An artesian well, 6 inches in diameter, would give a stream of 28 square inches, and would deliver 32 quarts per second, if the flow were at the rate of 4 miles an hour. o10th. Such a well would furnish an inch of water per day for 28 acres, or an inch a week for 196 acres, which would be a very insufficient quantity to irrigate dry open soils in places where the climate is arid. 11th. The cost of such a well would be at least $5,000 to $10,000, or more than the value of the land when irrigated. The estimates made by various authorities upon irrigation, as to the -quantity of water needed, vary considerably. As a rule, the quantity of water used by some irrigators, would seem to be extravagant. Thus we find standard authorities upon irrigation, and practical irrigators, recommending and using quantities of water varying from one to four quarts per second, continuously flowing for 24 hours for each acre, at intervals of from five to fourteen days. It is evident, however, that the quantity of water needed to moisten the soil thoroughly, depends on certain conditions, which are very variable. These conditions are: First-the nature of the soil. Second-the character of the climate. Third-the nature of the subsoil. As to the Soil.-Soils differ greatly in their power to absorb and retain water. Those which absorb most water retain it for the longest time. The power of absorption is due to the surface attraction of the particles of soil for water. The finer the particles of the soil, the 24 POROSITY OF SOILS. greater will be the amount of water absorbed, because the total surface of the particles is greater, and the longer will it be retained. Thus a soil consisting of coarse gravel will not retain water. A soil of pure quartz sand will absorb but a small quantity, and will soon part with it, while a fine alluvial soil will absorb a large amount, and retain it a long time. The following table gives the results of experiments made by Schu-bler, to determine the capacities of different soils for water and their comparative power of retaining it. In these experiments the different soils were thoroughly wetted with water up to the point of saturation, and the increase of weight noted; this is shown in the first column. In the second column are given the quantities of water which evaporated in four hours, the samples of soil being spread over equal surfaces. Per cent of water Per cent of water absorbed. evaporated in 4 hours. Quartz sand.............................25 88.4 Limestone sand.........................29 75.9 Clay soil (40 per cent sand).............. 40 52.0 Loam.................................51 45.7 Common arable land.....................52 32.0 Heavy clay (20 per cent sand)............61 34.6 Fine Carbonate of lime..................85 28.0 Garden soil..............................89 24.8 Humus (peat or decayed vegetable matter)181 25.5 Thus the greater capacity a soil possesses for the absorption of water, the longer it retains it. It is obvious that upon this depends to a very great extent the quantity of water that will be needed for the irrigation of any particular soil. Before any calculation, as to the needed supply, can be made, this point will have to be duly considered and determined by the irrigator or hydraulic engineer. The difference arising from the variations in the texture and composition of soils has been closely studied by the French irrigators and engineers. M. Gasparin, who stands at the head of the numerous writers upon this subject in that country, states that a soil which con 2 25 IRRIGATION. tains 20 per cent of sand needs to be irrigated but once in fifteen days, while under similar circumstances, another soil which contains 80 per cent of sand, should be irrigated once in five days. The difference would be still greater between soils varying still more in their character, and less with those which may be classed between these limits. As to the Climate.-As already stated, by far the largest portion of the water which falls upon the earth's surface is removed by evaporation. Observations made at Abbot's Hill, England, by Mr. Dickinson, during eight years, showed that 90 per cent of the water which fell in the summer, or between April 1st and October 1st, was removed by evaporation, and only 10 per cent found its way into the drains which were from 3 to 4 feet deep. The total quantity of waterwhich fel in those six months was equal to 2,900,000 lbs. per acre, and of this more than 2,600,000 evaporated. It should be remembered that this occurred in a moist, cool climate, the verdure of the meadows in which is hardly equalled in any other country, unless it be in the still more humid Ireland, " the emerald isle." In England showers occur almost daily, and the winds blowing in any direction from the sea, seldom more than a hundred miles distant, and generally much less than that, are charged with moisture; the maximum summer temperature rarely reaches 80 degrees, and also from the more northern latitude, the sun's rays fall at a comparatively low angle; if then, under these conditions, evaporation carries off nine-tenths of the moisture from the soil, what allowance must be made in our climate, where the atmosphere is drier, the summer temperature 20 degrees higher, and where the sun's rays fall upon the surface more directly, and more ardently. And further, if a large allowance must be made in those parts of the country where the rain-fall amounts to 40 inches and over, how much more liberal .26 FRENCH UNIT OF SUPPLY. must the allowance be for those districts where the rainfall is 10, 15, or 20 inches, and where the winds, almost completely deprived of moisture, thirst intensely for it? Here is a consideration of great importance, and one which cannot be disregarded. It will be evident to the thoughtful reader, that much will depend upon the condition of the surface of the soil maintained by the cultivator. The amount of evaporation can be largely controlled by keeping the soil in a finely divided and mellow condition, in hich it holds its moisture with the greatest tenacity. But there are crops, such as wheat, oats, etc., which do not admit of cultivation during their season of growth, and these must necessarily require a larger quantity of water than such crops as corn, or roots, which can be cultivated. In the dry and hot climate of Provence, a district in the south of France where irrigation is extensively practiced, it has been found necessary to use for each watering of the soil a volume of water equal to a depth of 31 12 to 4 inches over the whole surface every 10 to 12 days,the usual interval betweenthe waterings. This is equal to about 24 cubic inches, or nearly half a quart per second, continually flowing for each acre of surface. This allowance, which in French measures is equal to 1 litre per hectare, or 61 cubic inches (=1 litre) per 107,640 square feet (-1 hectare), is the basis for all contracts between the government which controls or supervises the water supply, and the owners of the canals (compagnies concessionaires de canaux), and between the latter and the farmers who buy the water from them. It is the official and legal unit of supply, as it were, and is a valuable general indication, applicable to any locality or country, where water may be used to irrigate soils of different characters and for different crops. This may be taken as the mean quantity, to be decreased or enlarged as circumstances may necessitate the change. 27 IRRIGATION. As examples of the nature of these varying circumstances, the following are cited: M. Herve6 Magnon (a frequently quoted authority in works upon irrigation, and already referred to here), determines the limits of supply as from one to four litres per second per hectare, which is equal to from one pint to two quarts per acre, per second, continuously flowing. Gardens and market gardens require the larger extreme. M. Pareto, another French author, in his work upon the irrigation and drainage of lands, (Irrigation et assainissement des terres), mentions some cases in which a quantity equal to one quart per second was sufficient to effectively irrigate eight acres. This may be taken as the extreme minimum limit of supply, very rarely occurring, and altogether exceptional. The Italian canals, which irrigate 1,600,000 acres, supply 24,000 cubic feet per second for this area. This is equal to one cubic foot (30 quarts) for 66 acres, or a flow of 26 cubic inches per second per acre; or very nearly one quart (which is 57'1 4 cubic inches) for each two acres. In that country the rain-fall equals 37 to 38 inches per annum, the most of which occurs in the irrigating season, when there are on the average 71 rainy days in the six months from March to October. There the summer temperature is from 70 to 90 degrees. It will be observed that the climatic conditions of Italy closely approach to those of the rainy portion of the lUnited States. The mean water-supply may therefore be taken as closely approximating the quantity required in this country-viz., one pint per second, constantly flowing, or 10,800 gallons, or 17221',0 cubic feet every 24 hours for every acre. In India, one cubic foot per second is made to serve for 200 acres of grain crops. In some parts of Spain the same quantity serves for 240 acres; in others the same quantity is spread over 1,000 acres, and the legal allowance in some recent Spanish grants, varies from 70 to 260 acres per cubic foot per 28 SUBSOIL ABSORPTION. second. Rice culture requires a supply equal to one cubic foot per second, for each 30 to 80 acres. These examples will serve as a basis for calculations, needed to meet the widely different circumstances which exist in the United States, where possibly the variations of soil and climate, over our extensive territory, are unparalleled in any other single country in the world. As to the Subsoil. -This point needs very little elucidation. From the preceding remarks, the effects of loose or compact subsoils will be seen to exert a considerable influence upon the requisite water supply. There are soils which rest upon open, coarse, gravelly subsoils, which may be compared to a sieve. Other soils, with retentive clay subsoils, furnish examples exactly the reverse. These are unusual cases, but as they may occur, they ought to be considered. It does not seem necessary to discuss this point further than to call attention to the importance of ascertaining the character of the subsoil of any tract which it is proposed to irrigate, as a serious element in calculating the needed supply of water. The minimum direct loss through absorption by the subsoil should not be estimated at less than 15 per cent of the supply, and a much larger allowance should be made when, upon examination, the subsoil is found to consist of coarse sand or gravel. When we consider the quantity of water needed for irrigation, it is clearly seen that springs are rarely of sufficient volume to be ef material value, excepting for meadows, and then only for small surfaces or partial watering. They may be made, however, to serve an important purpose in such cases as these where the area to be irrigated is small. Storage reservoirs, in which is collected the water of those temporary courses, which flow only when the rain-fall is largest and the amount of evaporation is least, may be made important sources of supply. It is by means of these that a large portion of 29 IRRIGATION. the irrigation needed to make the dry plains of India fruitful is accomplished. But by far the most important sources of water for irrigation are rivers and streams. In these there is an abundant supply, and there is generally ample provision for elevating the water, by means of dams with canals or by water wheels, to the highest portion of the adjacent land which is to be irrigated. The scope for the utilization of rivers and small streams in irrigation in the United States is of vast extent, and the statement which has been made that there are 500,000 homesteads in the country that could be brought under a partial or complete system of irrigation, does certainly not overestimate the reality, but on the contrary is doubtless greatly below it. It is for every cultivator of the soil to closely scan his own resources in this respect, wisely determining to turn them to accouut as soon as he shall have discovered their existence and perceived how to employ them. The cost of works for irrigation will be greatest where the area to be irrigated is the smallest, as for instance in gardens and market gardens; it will be least in the case of meadows, where the distributing canals are permanent in character, and between these extremes upon arable lands, where for each crop the surface must be disturbed, and furrows for spreading the water must be made anew at each plowing. The cost will also vary greatly, as the facilities for procuring and elevating the water may differ. But it may be accepted as beyond doubt that there are few gardens, market farms, orchards, or meadows that might not be brought under a more or less systematic irrigation, and few localities near the borders of rivers in the great Western plains, or other rainless localities, in which the present arid desert may not be redeemed and made to blossom and become fruitful beneath the beneficient influence of the fertilizing waters which now flow uselessly by them. a 30 IRRIGATION OF GARDENS. CHAPTER IV. IRRIGATION OF GARDENS.-THE SUPPLY OF WATER Gardens and market farms, by reason of the greater value of the crops raised upon them, in constant succession, will permit the application of more costly methods of irrigation than any other cultivated grounds, and from their smaller area there is less difficulty in procuring an ample supply of water. Few gardens are so situated that water can be procured from a stream without the employment of a water wheel or other motive power, a force pump, and pipes laid underground, and a reservoir in which water may be stored when not needed. But nearly every one may be supplied from a well by the use of a windmill. A windmill of the smallest size made, and of the best construction and self-regulating, costing about $100, is able to raise two quarts of water per second to a hight of 25 feet. A windmill may be constructed by any fair mechanic at a cost of from $10 to $25, which will answer every purpose of those manufactured and sold at higher prices, excepting that of regulating themselves to the varying forces of the winds. A mill of this character may be fixed in a frame over the well, and the arms, of which there may be six, eight, or more, with fans fixed so as to present their faces at an angle of 45 degrees to the wind. are kept in position by means of a vertical vane behind them. Another, which consists of six arms mounted upon a rotating frame, carries cloth sails. This mill requires to be changed as the wind changes, and a ladder is attached to the frame upon which it is mounted for this purpose. The frame on which to mount it may be of timber, as shown in the engraving (fig. 1), or it may be a stone or brick building if desired for a substantial machine for heavier work. The power is con 31, IRRIGATION. structed in the shape of arms-shorter or longer, accord ing to the power needed-fixed to a center-wheel or hub, which is mounted and keyed on to an axle. Sails are carried on these arms, of sail-cloth or heavy sheeting, of a triangular shape, as shown in the en graving, which are fastened closely to one arm and by a cord in the corner, shown at a, a foot 1 or less in length, to cJ1 I _ ~ another. This gives =, l 7 sufficient inclina tion backward to the sails to gain the mo tion required with a I5 2!front wind. On the :., Zart_ axle is a crank wheel, b, which moves the rod to be connected with the pump, or it may be connected by means of pulleys and bands to get an upright rotary motion, or a Fig. I.-WINDMILL WITH SAILS. pair of bevel-wheels pair of bevel-wheels will give a horizontal rotary movement. A frame, c, is carried on a circular table, on which it may be revolved so as to enable the sails to be presented fairly to the breeze; a box, d, at the rear end of the frame is weighted with stone, to balance the weight of the arms and sails. A pin passed through holes in the circular table retains the frame to the position needed, and keeps the sails faced to the wind. 32 CISTERNS AND TANKS. A mill with arms six feet long may be made to do work equal to one-fourth of a horse-power, if all the working parts are well fitted and kept well lubricated, as all machinery should be. When out of use, the sails are untied and removed, or they may be furled and dclewed to the arms until again required. A one-horse railroad-power would also serve a useful purpose in raising water from wells into an elevated reservoir, where it could be stored for use. For small F t. _~~~~~ Fig. 2.-SQUARE To gardens the water from the roofs of buildings may be collected in tanks or cisterns raised a few feet above the level of the ground. A round tank, hooped with iron bands, 12 feet deep and 15 feet in diameter, will hold over 15,000 gallons. A square tank (fig. 2) may be made of jointed and matched planks, which are forced closely together by wedges, acting upon a timber frame which encloses the planks. This t 33 IRRIGATION. is the cheapest kind of tank that can be made. One 16 feet square and 10 feet deep will contain nearly 20,000 gallons. Tanks of this character can only serve for small gardens, or to store water which is pumped at night for use during the day time. Either of these tanks, if filled during the night (to do which will require a stream from a pipe of an inch and a half in diameter constantly running), and replenished during the day, will furnish enough water to give more than one inch in depth over an acre of surface. This is the least quantity that could be depended upon in a dry season for any effective purpose, and would need repeating after an interval of four to seven days, so that the maximum effort of a tank of this size, with a well, windmill or horse-power attached, would suffice only in an emergency to water four to seven acres of land. Where the ground to be irrigated is of larger extent, the tank room and water supply must be enlarged, or the diameter of the pipe and power increased. The capacity of the pipe increases as the square of the diameter, by which is meant that if the diameter is doubled the capacity is quadrupled. Thus if a pipe one inch in diameter supplies one quart per second, a pipe of two inches diameter will furnish four quarts per second (or two multiplied by two), and a pipe three inches diameter will yield nine quarts (or three multiplied by three), per second. At the same time the power must be increased in proportion to the amount of water elevated; or disappointment will result. In estimating power a large allowance must be made for loss. A horse working in a railway-power can only raise an equivalent of three-fourths of his weight; the rest disappears in friction; and when a stream of water is forced through a pipe of small diameter for a considerable distance, the loss of power in friction is very large, and another fourth of the horse's effort must generally be allowed to compensate for it. One horse may be expected to raise 180 quarts one foot 34 MEASUREMENT OF STREAMS. high every second, or 6 quarts to a hight of 30 feet. The small size windmills are about one-sixth of one horsepower. Where streams are available, the supply of water will be found most ample and most economical. No storage tanks are needed in which the water must remain for a time, that its temperature may be raised nearly to that of the soil, as when wells are used. The water may be taken directly from the stream and flowed upon the ground. A low dam of two feet in hight may be constrtucted of planks across the stream, by which power to run a small undershot wheel may be secured. Where there is facility for backing the water to a greater extent, or of procuring a greater fall, a breast-wheel may be used. A dam four or five feet high will be sufficient for a wheel of this kind, if the stream is four feet wide and six inches deep, and runs with a velocity of two miles per hour. Such a stream with this fall of water would give sufficient power to elevate 11 quarts of water per second a hight of 30 feet, or a sufficient supply for about 12 acres of ground, or more in proportion to the less hight that the water would have to be raised. To calculate the nominal horse-power furnished by a fall of water, the velocity of the stream in feet per minute, the hight of fall, and the sectional area (the width and depth) of the stream in square feet, must be multiplied together, and by 62'1,, and divided by 33,000. For instance, it the stream is found to be 5 feet wide at the surface, and 3 feet at the bottom, with banks evenly sloping from the surface to the bottom, the mean diameter is found by adding the surface and bottom widths together and taking half the sum. In this case the mean width will be 4 feet. If the depth in the middle is 6 inches or half a foot, this mean width is multiplied by the depth and the product is the sectional area, which in this case is two square feet. To find the velocity of the 35 IRRIGATION. stream a thin shaving or other light floating substance is thrown upon the surface, and the exact time in which it moves over a definite distance, say 10 rods or 165 feet, is carefully noted by walking along the bank watch in hand. Let this time be supposed to be one minute. Then the sectional area of the stream being 2 feet, this is multiplied by 165 and the product 330 is the number of cubic feet of water passing down the stream in one minute. A cubic foot of water weighs 62' 12 pounds, therefore 330 cubic feet weighs 20,625 lbs. If the dam is 4 feet high we have 20,625 lbs. of water per minute falling 4 feet, which is equal to 82,500 lbs. per minute falling one foot. This would, as a matter of course, exactly balance the same weight rising the same hight. The whole power of a horse attached to suitable machinery is equal to that necessary to raise 33,000 pounds one foot high in a minute. The force exerted by the falling of 82,500 pounds in a minute is equal to 2'11 horse-power. But a considerable allowance must be made for friction, when waterwheels are used, and especially where the fall is so small as here supposed. It would not be safe to expect to gain more than one half of the whole effect in this case. The power gained would therefore, under ordinary circumstances, be about 1'14 horse-power, or sufficient to raise about 40,000 lbs. or 20,000 quarts a foot high per minute. This is equal to about 11 quarts, 30 feet high, per second. If it is found necessary to store the water thus elevated so as to extend the area that may be irrigated, cisterns of substantial construction will be required. These should be of brick or stone laid in cement, or hydraulic lime, and strengthened with buttresses upon the outside. A bank of earth should then be heaped up around it and sodded, and if the bank be terraced, it may be utilized by planting it. A remarkably elegant structure of this kind is to be seen in a market garden at Astoria, Long Island. It consists of a large cistern of stone work surrounded by 36 TANKS AND CISTERNS. earth sodded in part and in part planted, and surmounted by a rustic stage and summer-house built of cedar boughs and roots. Above the whole, towers a powerful windmill which serves to pump the water from a well near by into the tank and force it from thence into the extensive greenhouses and other buildings upon the farm. Although the cost of such a structure is large, yet it is in such a case as this no more than a necessary outlay of capital, without which the business could not be carried on, and is simply an expenditure made in a true spirit of economy. Such a tank of considerable size and great utility (see fig. 3), may be dug in the ground at the highest part of fig. 3.-BRICK CISTERN. the garden, to such a depth that the soil excavated will make a retaining bank to support the portion of the wall that is above the surface of the ground. This tank, which is circular, may be covered with an arch of brick work, and may be surmounted by a tool-house or other useful building. In this case a brick shaft 2' 1, feet thick each way should be build in the center from which the arch would spring to the circular wall of the cistern; the wall should be 9 inches thick and the bottom may be either of bricks laid flat or of cement laid upon the earth. 37 IRRIGATION-. This cistern, if 20 feet in diameter and 12 feet deep, would hold 30,000 gallons, or enough to water over three acres at one time. If the cistern is open the wall could slope outward, making an inverted frustrum of a cone (as seen in fig. 4), 32 feet wide at the surface and 8 feet wide at the bottom. The earth thrown out at the bottom will form a support for the upper portion of the wall. But before the wall is built the earth thrown out should be solidly rammed down in layers made hollow or of the form of a basin. The form is shown by the curved lines in that part of the engraving. There is a large variety of pumps adapted to the purpose of irrigation, but the severe uses to which they are put make it desirable to have only those which are constructed entirely of metal or wood. Leather valves are soon worn and become useless, causing delays, and serious loss of time in repairs. The double action force pumps, with metal valves, or the rotary pumps of the ordinary kinds with metal pinions which work into each other similarly to cogwheels, or those which work upon the oldfashioned principle of the Archimedean screw, but which nevertheless are protected by a modern patent are all suitable for this work on account of their durability. A double-acting force pump of the most simple character (fig. 5), made almost entirely of wood, is one of the best for this purpose on account of its cheapness and the ease with which it is kept in working order. It is formed of a block of wood, A, A4, in which two parallel holes are Fig. 4.-OPEN CISTERN. 38 PUMPS. bored lengthwise. In these holes the plungers, B, B, made of wood-maple being preferable-are worked by rods affixed to a rocking shaft in connection with the hole, shown by the dotted lines, is bored. - This bore 5~'1 ~ is made to communicate U l[I with the other two by a I lhole bored from the out ~~I I~ l side (seen at C, that por tion shaded and where l1/~, the letter C is seen being ~ ~ ~~~~~afterwards plugged up). A leather valve is placed o Fig. 36.-DRIVE-WAY. plan which, with such modifications as circumstances require, may be adopted for the irrigation of any land with sufficient slope. "Fig. 35 shows a corner of the manure-cellar with an escape pipe (valved) leading from the very bottom-allowing the cellar to be drained dry at pleasure. In front of the entrance to this pipe a screen of iron rods or wooden slats, reaching vertically from floor to ceiling, prevents solid matters and litter from choking the pipe. If this becomes clogged, it can be cleared with a rake through a trap-door in the floor above. This pipe should be used only when the water will not flow at the outlets above. "Fig. 36 shows the arrangement at the west end of the 74 ii I DISTRIBUTION FROM THE CELLAR. cellar, with an overflow pipe to the north and one to the south. The drive-way should be dammed up to raise the water to the level of these pipes. "Fig. 37 shows the arrangement for the distribution of the flow. A main furrow runs from a and x to d. This ,,,,,,,,,_ y ".,-;,,: ~ \,_S $ _,- no g _~~~~~~~~~~~~~~ -- \ _-of 4, 4 — \,,- Go I, \ 5 E n go~~~~ Fig. 37.-PLY OF FURIROWS FOR DISTRrBUTION. is the general direction of the slope of the land. The laterals 1 to 18 are furrows laid on a fall of 1 inch in 100 feet. They will not be straight, but must follow the conformation of the ground, so as to preserve a uniform fall. The main furrow at x may be supplied either from a or from c, and others from b, as in figs. 36 and 37. "The flow being let on, and kept up by a corresponding flow into the cellar from the brook, it should pass on to 75 IRRIGATION. the end of 18. (The main furrow is a little deeper than the entrance to the laterals.) Here it will overflow the land lying below so much of the lateral as is beyond y. Then a gate should be set at y, and kept there until the land below the lateral between that point and z has been sufficiently flooded. Then remove the gate to z. When all the land below lateral 18 has had its supply, set a gate in the main just below 17, and repeat the process with that. When the south side of the farm has been completed, the gate is taken from the main and the water allowed to flow to the end of No. 9. "Nos. 1, 2, 10, and 11 can be flushed only from outlets a and b. All the others are low enough for c. "Of course, any portion of the land may be flooded at pleasure, the directions above being given only as an illustration." The scope for the employment of such methods as these suggested in this chapter is far from narrow. The profitable employment of liquid manure upon gardens and small farms upon which the crops grown are of high comparative value, cannot be doubted. It remains only that the lead in introducing it be taken by some enterprising but cautious man, in each neighborhood, whose success would stimulate hundreds of others to follow his example. It is probably too soon to more than hint towards the use of liquid manure upon farms in this country, or the utilization of the sewage matter of towns and cities. This can only be done with profit when the high value of lands bears some proportion to the cost of the necessary machinery. But upon gardens, especially market gardens, and upon highly cultivated farms where heavy fodder crops are grown, and the soil is abundantly manured, and where the closest economy in the saving and use of manure is practiced, much may be done in this way. The author has had practical experience in the use of liquid manure-in gardens, and in growing fodder 76 SOILING CROPS. crops, to be used for soiling dairy cows-and is firmly convinced that, with ordinary care and ingenuity, the crops may be quadrupled, and the profit doubled. For instance a clover crop that would under ordinary circumstances be ready to cut for soiling only in June has, by weekly irrigating with liquid manure, been made ready early in May, and by more frequent watering has been cut four times before the first of July, or once every two weeks after the first cutting, at a cost, for each watering, of not more than 50 cents per acre. - Each cutting of the crop at least equalled an ordinary yield, or one ton and a half of hay per acre. As to the value of the system as applied to market gardens for the production of such crops as onions, cabbages, cauliflowers, and the smaller vegetables, in which flavor, tenderness, and succulence are only secured by rapid growth, there can be no better proof than the successful cultivation of the small farms of Belgium, a country which supports the densest population in Europe, or of the market gardens in the vicinity of many French, Italian and English cities and towns. In these localities the solid and liquid refuse is gathered with the greatest care, mixed so as to be readily used, and applied to the crops, which, under this treatment, possess a size and quality that is never equalled in this country, except by a few premium vegetables that are grown in this same manner. To have seen this demonstrated in the gardens and in the markets of European cities and in isolated cases in this country, is sufficient proof, at least, to induce American cultivators to attempt to utilize in this most effective manner this most effective fertilizer. 77 IRRIGATION. CHAPTER VIII. CULTURE OF IRRIGATED GARDEN CROPS. There are a few important leading principles involved in the practice of irrigating gardens that should be well considered. These will be referred to in the order of their importance. Drainage.-It is rarely that a well drained soil can be injured by a copious supply of water; but one that is not drained may easily be turned into a quagmire by an excess of it. Drainage, therefore, should be the first thing provided before this method of cultivation, let it be complete or partial only, is attempted. If the soil is not naturally drained by means of an open and porous subsoil of sand or gravel, tile drains should be laid in such a manner as to carry off the surplus water in the most effective manner. The method of drainage will depend upon the system of irrigation adopted. If the bedding plan is used, as illustrated in fig. 7, page 42, the drains should be laid between the beds, and beneath the drain furrows, as shown in fig. 37, in which the open spaces seen at a, a, represent the drain. These drains should be of inch tile, laid three feet below the surface. If laid at a less depth there is danger that the roots of some varieties of plants may penetrate between the crevices and choke the tiles. Where the arrangement of the water-furrows is such as to need change every year, or such as is shown in figures 15, 17, or 23, the method of drainage should be the ordinary one of inch tiles laid 24 feet apart, if the soil is heavy; or 30 feet if of a lighter character, and leading into main drains of two or three inch tile. Surface draining would be a very unsatisfactory resource, and should be adopted only where the crops would resist the effects of a very 78 DRAINS. cool, moist soil, or upon inclined ground where there would be no danger of saturation. Whatever the arrangement of water supply may be, the plan of the drain should be as nearly as possible exactly the reverse. In effect the drains should be so arranged as to take up the surplus or unused water and carry it off as rapidly as possible; at the same time care should be taken not to permit the water to flow into the drains until it has done its duty, nor to use so much water that the soil may be carried into the drains and these be soon filled with sediment. No drain should be carried beneath a canal or distributing furrow, unless it cannot be avoided, and then never at a less depth than three feet, else a channel of communication may be opened between them and the water escape, and, what is worse, wash the soil into the drains and render them useless. Further remarks upon drainage will be found in a succeeding chapter where field irrigation is treated, and which may be referred to. Cultivation or Disturbance of the Soil. -The soil should never be disturbed while it is wet. The operations of hoeing, cultivating, weeding, sowing, or gathering the mature crops, should be so timed with reference to the watering, or the watering should be so timed with reference to them, that these operations may be performed when the soil is dry and just before the watering. If after the watering, upon soils liable to "bake," or become encrusted, the surface under the effects of a hot sun becomes hard, the crust should be broken up by cultivation before it has time to completely harden. The Application of Water.-It is not well to put off the watering until the ground is very dry, but to apply the water while the soil is still somewhat moist and mellow; it is then more absorptive, and the after effects upon the worst of soils, as regards baking, will be less troublesome. The soil should be moderately watered 79 IRRIGATION. a day or two before seed is sown or plants are transplanted, that it may be in a finely pulverulent condition, and when the supply of water is always under the control of the operator there is no danger in sprouting the seed and thus hastening germination. After sowing or transplanting, the chief care should be to water only very moderately, and never allow the water to flow over the seed or plant rows, lest the surface should become hard and need stirring, and the young plants be endangered by one or the other of these alternatives. Moderate, frequent waterings are best for young, growing plants. There is far greater danger of giving too much rather than too little water at this time. During early growth the application of water at a lower temperature than that of the soil is injurious. For this reason, when well-water is used, it should be exposed to the air in open tanks or reservoirs for at least one day before it is used. For the same reason watering during a clear sunny, or a windy day is to be avoided, and it should only be done in the evenings, or when the sun is obscured with clouds. The effect of wind is to increase the evaporation, and thus reduce the temperature of the soil immediately after its saturation. The quantity of water to be applied will depend upon several circumstances that have already been referred to. For garden crops, frequent moderate waterings are preferable, and intervals of five days are usually allowed. The soil is then kept constantly moist, and the growth of the crops continuous. Of course when rain falls, a sufficient allowance must be made, but, judging from the quantities of water that may be safely applied to.crops in the market garden, unless the rain is unusually heavy and continuous, it may safely be ignored. The quantities used in garden culture in different countries, as mentioned in many works upon irrigation, are exceedingly irregular. It would seem as though the abundance of water, and the porosity of the soil, measured the sup 80 CROPS. ply, rather than the needs of the crop. Thus quantities varying from a total depth, during the growing season, of 50 up to over 300 inches upon the surface, have been used without any ill effect when the drainage has been perfect. Experience can be the only safe guide; the thorough soaking of the soil at intervals of five days, should be the limit of the irrigation, and the quantity of water needed to effect this will be the maximum supply required. When economy of water is a point to be considered, as it must needs be when every pint of it is elevated by power, it will be necessary to watch the flow in the distributing furrows and prevent any escapes into pools and surface drains, and such copious watering as would leave water standing in the furrows for more than an hour or two after the flow has been stopped. This must be regulated by the judgment of the irrigator acting through a knowledge of the principles involved. THE MANAGEMENT OF VARIOUS CROPS. Where the climate admits of it a succession of crops of garden vegetables may be grown throughout the year, and the variations of the seasons practically removed. In the climate of California this is easily done by means of irrigation there practiced, and in most of our Southern States the season of growth may be extended, and in some maybe continued throughout the year, if the supply of water is only secured. This is one of the -great advantages of a system of irrigation, by which every where a succession of crops, more or less extended, may be secured. The general management of the principal garden crops will be briefly indicated. Asparagus. -The most convenient method of cultivating this crop is by "floors," (see fig. 9, p. 43), over which a thin sheet of water may be flowed from a furrow at the head towards another at the foot, from which the water may be again flowed over another floor below the first. 81 IRRIGATION. This arrangement makes it necessary that the ground should slope slightly in one direction. The method of watering by pipes laid upon the surface, or by hydrants, which have been already described, may easily be applied to the culture of this vegetable. This crop is one that needs but very moderate irrigation. Beans.-This crop requires to be planted in beds, arranged as shown in figs. 7 and 8, and can be cultivated in long succession by means of irrigation. It willstand a good deal of moisture, especially when grown to use green as "snap beans" which should be fresh and succulent. The periods of irrigation should be at intervals of five to seven days. Lima beans need equally frequent waterings. Corn.-This is a plant which needs much moisture, and the watering may be both copious and frequent. It may be planted in hills or drills, in either case the system of beds or of alternate drills and furrows, which are fed from a distributing canal at the head of the bed or drills, may be used. Cabbage.-This crop is cultivated in beds to which the water is supplied by furrows, made with the hoe after each cultivation. It is a greedy feeder and responds quickly to the application of liquid manure. Heads of enormous size have been thus grown, and specimens of 60 pounds in weight have been frequently exhibited that were produced by irrigation with liquid manure. It will submit without complaint to much moisture if the soil is cool; how it would behave under our hot suns, when stimulated by excessive irrigation, is something that is yet to be learned. In Florida, however, it thrives well when supplied with sufficient moisture; in central Europe, where the market gardener irrigates all his crops, the cabbage is only moderately watered, doubtless lest it might be stimulated to run to seed; but where the character of the soil and climate are favorable, and abun 82 CROPS. dance of water is procurable, there the cabbage, as well as the cauliflower, is extensively cultivated not only for home consumption but for shipment abroad to distant countries. This is the case in Belgium, and in the neighborhood of Erfurt, (Germany,) where both of these crops are cultivated with success and profit, unequaled elsewhere. There the method of culture is to choose a low spot of ground and divide it into beds of convenient shape, which are separated by permanent furrows, in which the water flows. The water is sometimes dipped from these furrows by long-handled scoops and poured around the roots of the plants. Otherwise the water is flowed on to the crops by means of small furrows between slightly raised ridges upon which the plants are grown. Beets.-This crop is peculiarly suited to culture by irrigation. Few crops thrive so well under the combined influence of abundant moisture and a continued high temperature. The sugar beet, especially, enjoys these conditions when planted in deep, well-drained soil, and crops equal to from 60 to 75 tons of roots per acre are frequently grown in the sugar manufacturing districts of central and southern France. A specially noteworthy case was cited in the Journal d'Agriculture by MI. Barral, in which a manufacturer of beet sugar at Masny, directed the flow of water from the water wheels, which furnished the power for the factory, on to the field of beets. The water was charged with all the refuse of the works, the washings of the roots and of the impure bone-black, as well as that of the sacks in which the pulp had been pressed, the skimmings of evaporating pans, and also the washings of the outhouses used by the workmen; and carried all this matter in suspension through the channels and distributing furrows to the growing crops. No other fertilizer has been used during 8 years, and the value to the farm is estimated at a yearly sum of $2,000. This example, however, relates to field culture, but is yet 83 IRRIGATION. worthy of note as showing how refuse matter may be applied in a similar manner to garden crops. The irrigation of beets, although it may be profusely applied upon light, deep, and well drained soil, must be done with proper moderation upon soils that are retentive and not well drained. Only so much water must be used as to keep the soil fresh, moist, and mellow, and it will be safest to irrigate such soils as these more moderately and oftener than those of a loose, open, sandy character. Carrots. -This crop has been found to thrive exceedingly well under irrigation upon light soils. A succession of crops may be grown throughout the whole summer, and by the use of some active artificial fertilizer, the growth is rapid and remarkably clean and healthy. Upon clay soils this and other deep-rooted crops do not thrive very well, and more shallow-rooted crops should be chosen. When irrigated, the carrot is cultivated in rows upon the flat, the water being led to the plants in channels made by the hoe in the intervals between the rows. It is very common in garden culture to plant carrots for a late crop in rows between other and earlier ones, by which the tender young plants are shaded and protected from the heat. Sweet Potato. -This crop is planted in broad, fiat beds slightly raised above the level, and the water is flowed into the furrow between the beds. Upon the light soils, in which the crop succeeds best, the waterings are given copiously at intervals of from five to seven days. The abundant foliage requires a good supply of water. The system of rounded or doubly sloping beds, described on page 41, in which the water is carried along the crown of the bed, is well adapted to the culture of this root. Onions. —This crop is grown very successfully under irrigation, and water may be copiously applied. The excellent quality mild flavor, and extraordinary size of the 84 CROPS. Portugal and Italian onions are due to their manner of growth in which irrigation is extensively used. The crop should be planted in rows between which water is flowed, in broad, shallow channels made with a hoe. The water should not come in contact with the bulbs, nor should the earth be thrown upon them in making the furrow. Potatoes. -To grow common potatoes under irrigation, with success, needs caution and judgment. As the quality of the tubers depends greatly upon the supply of water, judiciously regulated with regard to the character of the soil, some care must be exercised as to the quantity. Upon light soils the water is given only at intervals of nine or ten days, and upon heavier soils, which are more retentive, fourteen days elapse between the waterings. As soon as the soil is sufficiently dry after watering, the surface should be cultivated, which will cause the moisture to be better retained. A system of drills, or of beds slightly raised, is used for this crop, the water being given in broad, shallow furrows, made with the hoe at the time of cultivation. When the plants nearly cover the ground, as they should do at the time of blossoming, the final watering is given. No further cultivation should be given after this period. Peas.-As this crop is generally sown in rows upon a flat surface, the mode of watering should be suited to this method of planting, and it may be either by a system of beds, fig. 6, or of shallow furrows made between the rows with the hoe at the time of cultivation. As this crop flowers and seeds during a lengthened period, it may be irrigated without regard to the flowering, care of course being taken to keep the soil only in a healthful state of moisture. ThTe Small Crops.-Small crops, such as lettuce, radishes, etc., are more conveniently cultivated in beds of the form shown in fig. 6, over the surface of which the 85 IRRIGATION. water flows or trickles from a furrow at the ridge. The quality of all these small vegetables is improved by copious Caterings, and a very profitable succession may be procured by continuous sowings, the growth of which for market or domestic use may be hastened and matured at pleasure. GARDEN FRUITS.-The various small fruits usually grown in gardens may be greatly increased in luxuriance of growth, and by cautious treatment, much improved in quality, by irrigation. Over-watering, however, will infallibly tend to deteriorate the quality, if it does not even weaken the growth. As soon as the blossom appears water should be withheld, unless under extraordinary circumstances, and under the supervision of an experienced gardener. For strawberries the bedding system is preferable, and for other fruits the water may be led by temporary furrows made with the hoe around the roots of the bushes or the vines. In concluding these remarks which are not intended as a guide to an already practiced and competent gardener, but as suggestions to those who desire to secure in a moderate way by the use of some plan of irrigation, that is feasible for them, the full advantages which they can derive from a family or market garden, and which they so often fail to gain, by reason of the frequently recurring drouths; it may be said as a matter of caution, that with a supply of water constantly at hand, the danger of using too much is greater than that of using too little; that moderately copious waterings at extended intervals is far preferable to light but frequent irrigation, which scarcely reaches the roots and packs the surface. To saturate the soil once a week, or every ten days, will have the effect of forcing out of it much of the air that is contained in it, which will be replaced by a fresh supply as the moisture evaporates or sinks in the subsoil. Thus the soil is kept loose and mellow, and the necessary cul 86 CROPS. tivation, which should always follow the watering, will retain this condition of the soil. The crops then are refreshed and invigorated, and can resist a comparatively long interval of dry weather. An excess of water may very easily be worse than a severe drouth, for permanent and irreparable injury may be done to a crop by flooding the soil to excess; and not only the season's crop itself be lost, but the plants themselves be seriously damaged and future crops be imperiled. With caution in this respect, an adequate sonsideration for the peculiar character and needs of the different plants, a sufficient regard for the nature of the soil and its facilities for proper drainage, whether natural or artificial, and some reference to the ordinary provisions of nature in regard to the supply of water, one can scarcely go wrong in applying the practice of irrigation to the culture of any of our usual crops of vegetables, fruits, flowers or shrubs. The general application of irrigation, with few exceptions in this country, will be to make up for the short-comings of dry seasons, in which the deficient supply of rain may be made up artificially. CHAPTER IX. IRRIGATING ORCHARDS AND VINEYARDS. It is doubtful if there is a single orchard or vineyard in the United States, except in California, Utah, or Colorado, subjected to a systematic irrigation. At the same time it is doubtful if there is any country in the world in which irrigation could be more profitably applied to fruit culture than here. The experience of orchardists proves that drouth is accompanied by destructive attacks of insects. How far these depredations might be prevented by irrigation cannot be predicated, but it is beyond doubt 87 IRRIGATION. that the vigor of growth that would result from a sufficient supply of moisture to the roots would greatly mitigate the effects of these attacks. The apple trees that never have an "off-year" are those grown near bodies of water. A California vineyardist who irrigated his vines immediately raised his product to eight tons of grapes per acre, and greatly improved the quality. The newly planted orange groves of Florida are frequently destroyed by drouth, and methods of irrigation are eagerly sought to render their culture more safe and certain. But if it were necessary to enforce the advantages of the irrigation of orchards, abundant evidence could be gathered in the south of France, Italy, and other countries of Southern Europe, where the olive, orange, lime, almond, fig, apple, and other orchard trees, as well as the vineyards, are systematically brought under irrigation. As to the vine, it is a question which so far has not been thoroughly investigated, whether or not irrigation might be made the means of vanquishing the destructive phylloxera. An experienced vineyardist of Avignon (France) submitted his vines during the Winter, which in that locality is mild and free from severe frosts, to a lengthened irrigation of 30 days, during which a depth of four inches of water was constantly maintained in the vineyard. This operation has been found to considerably diminish the injurious effects of the phylloxera, and to greatly improve the condition of the vines. This practice might be found somewhat dangerous where early Spring frosts occur, by which the vines brought prematurely into growth might suffer. But no cautious cultivator will make serious innovations upon his practice without previous careful experiment. In Southern California the vineyards are copiously irrigated four times only-at the starting of the first growth, at the blossoming, at the setting of the fruit, and at the period when the fruit commences to color. 88 ORCHARDS. But without entering into speculations as to what events might occur, it is sufficient to know that orchards are irrigated with profit; that in some cases they are destroyed, and in numberless instances they are injured by a want of water, and that there are probably few cases in which a supply of water brought into the orchard would not be found advantageous and profitable. The methods of irrigating orchards are very simple. It is only necessary to put the water where it will do the most good, and that is as near as possible to the extremities of the rootlets. The extent of the roots of a tree bears a ratio somewhat approaching that of the branches. Near. . -f/ ../. c a/ X\' g~lY f \r'./ / e/ *. e/ Fig. 38.-PLAN OF IRRIGATING AN ORCHARD. the stem there are few of the root-hairs or fine fibers by which nutriment is absorbed. These are found at the extremities of the very fine rootlets, and these exist in a ring around the tree, the inner edge of which is from 3 to 411,2 feet distant from the stem. In irrigating an orchard, then, the most perfect method of applying the water is to distribute it in a broad circular channel around the free, distant about six feet from the stem. Where irrigation of orchards is practiced two different plans are adopted. The first is a somewhat rude method, but is easy and effective. The water is led into a channel between two rows of trees, a, b, fig. 38, and from thence b b 89 IRRIGATION. into distributing canals, c, c, c, which carry the water within a few feet of each tree. (The position of the trees in the figure is indicated by the dots.) Here a sharp bar is trust into the ground in several places, penetrating in different directions toward the roots, and leaving holes by which the water soaks into the earth and reaches the roots. The second is a more elaborate but a more preferable method. The water is led from the canals into circular furrows which curve so as to embrace the tree. (This is shown at d, e, in fig. 38.) These furrows are broad and shallow, and the water overflows from them in a thin sheet or a multitude of little rills which lead to a a Fig. 39.-FORMATION OF FURTROWS. the lower side of the tree, where they are arrested by means of a slight embankmentraised with the hoe. In this case the water is brought exactly where it is needed, and every rootlet is supplied. This is also seen at fig. 39. In irrigating vines very similar methods are adopted. As the vines are planted in rows, the distributing furrows are carried down the center of each alternate row, fig. 40, the ground being sloped towards the center of each intermediate row, fig. 41. The water is thus made to pass across each row of vines. Beneath the center of the intermediate rows a tile drain should be placed to carry off surplus water, and this brings into notice the question of drainage as a part of this system of orchard and vineyard 9O IRRIGATION OF VINEYARDS. irrigation. As a rule irrigation and drainage should go together. Irrigation without drainage will in most cases convert a tract of land into a morass. Stagnant water is fatal to the life of useful vegetation, and it is here that the causes of the failure of many attempts to irrigate Fig. 40.-LA OF IRRIGATING A VINEYARD. originate. In arid territories without rainfall, skillful irrigation will supply such a quantity as will be needed to supply evaporation from the surface of the soil and the transpirations of the plants. If more is given, the surplus must pass off through the subsoil, or remaining in it will work mischief to the crop. But such an excess of F 1 RIa a Fig. 41.-FURROWS AND DRAINS IN A VINEYARD. water can rarely be procured in arid districts. On the contrary, the greatest economy must be exercised in using the limited supply, and waste is impossible. It is otherwise in those parts of the country where partial or periodical irrigation is used. There the water 91 -1 ~ ~ ~~~~~~~~.: r iY S df 9> IRRIGATION. supply may be copious, and the skill of the cultivator is to be exercised in conveying to his field only so much as may be serviceable and no more. But to hit the just mean is a matter of difficulty, if not impossibility, for several reasons. For safety, therefore, in these cases a system of drainage is imperatively needed. Especially is this the case in orchards and vineyards which are subject to so many varieties of blight and mildew, and other diseases which have their origin in atmospheric or meteorological conditions. Except in very rare cases, then, it will be imperative that a tile or other drain be laid in the subsoil at least four feet beneath the surface, between every two rows of distributing canals. This will remove the danger of injuring the plantation by excessive watering. The position of the drains is shown by the dark lines, f, f, f, in figs. 38 and 40, and by the small rings a, a, beneath the surface in figs. 39, 41. The roots of trees seek out and follow a supply of water with great avidity. Drain pipes in orchards and gardens have been frequently penetrated by the roots of the trees and completely choked by a dense mass of fibers, eagerly appropriating the water found therein. For this reason the drainage of orchards by tiles is a somewhat hazardous business. To irrigate the soil of an orchard would tend to keep the roots near the surface where they would receive a sufficiently copious supply of water. With an abundant supply of water it is not probable that the roots would enter the drains, as the only purpose of their entrance there is to seek moisture. This being supplied as far as necessary upon the surface, the seeming instinct of the roots to enter and choke the drains would have no reason to exist, and would not be likely to occur. The great depth to which the roots of fruit trees and vines penetrate is undoubtedly due in part, if not wholly, to the effort to seek and procure sufficient moisture. The roots of vines have been found spreading at a depth of 92 NECESSITY FOR DRAINAGE. eight feet below the surface in soils that were naturally drained and not retentive of water. Although it is a matter of conjecture if the roots would descend so far when ample moisture may be found near the surface, the reasonable probability is that they would not. If the habit of deep growth should be a fixed one, it would be a question as to how deep the drains should be made in soils that are well supplied with plant-food in the subsoil, but were too retentive of water to permit a healthy growth at considerable depth. It is evident that with irrigation, and sufficiently deep drainage combined, the vine and fruit grower can render himself largely independent of seasons and locality, and give his vines and trees an ample depth of soil in which to spread their roots, and at the same time furnish them with all the moisture they may need near the surface. The practice will necessarily be modified by the character of the soil and situation; fruit growers, however, are rarely deficient in intelligence, skill, or patience, and are abundantly able to make such modifications of the general principles given in this work as may be needed. The practice in those countries where orchards and vineyards are irrigated is as follows: The periods of irrigation depend upon the heatof the season and the dryness of the soil. In the north of France and parts of Germany, water is given without any regularity, and only when the exceptional circumstances of the season make it needful. - But further south, where the summers are hot and dry, and periodical drouths occur, fruit trees are irrigated constantly and vines periodically. The penalty for an excessive irrigation is a crop of fruit of inferior quality; watery, soft, and without flavor; the wood and leaf are pushed at the expense of the fruit; succulent fruits crack and burst, and shelled fruits have soft and imperfect husks. The effect of too copious irrigation upon nut-bearing trees is to develop the whole fruit simultaneously, the inner portions complete its growth 93 IRRIGATION. while the woody husk is still soft, and the latter is either burst open prematurely, or fails to open at all, from want of the growing pressure of the kernels within. It is therefore necessary to act with extreme caution. Early fruiting trees require little or no irrigation, and late bearing ones are watered only after the fruit is set, and need to grow vigorously. As the ripening season approaches, the water is withdrawn, unless the necessity is absolute. During flowering no water is given at all, unless exceptional drouths occur, and then with moderation and at intervals. The custom prevalent in the vineyards of the Crimea, a locality in Southern Europe, on the north shore of the Black Sea, and one subject to dry hot summers and cold bleak winters, is thus described by AI. Clement-Bertron in the Journal d'Agyriculture Pratique: " There are in the Crimea four valleys completely planted in vineyards to the extent of about 15,000 acres. The vines are irrigated each year as copiously as possible, not only during the winter, but from the termination of the vintages up to the season of the next flowering. Some growers even irrigate their vines after the flower is passed, but in general little water is given after the month of June up to October. As soon as the water has been applied, and the ground has dried, the vineyards are cultivated or dug over with the spade, and the vines are pruned. About 15 days before the vintage, the vines are clipped so as to give air to the fruit. After the grapes are ripe, there is no work done in the vineyard until the next season's labor begins. The cold of winter has not been found to injure the vines, although this is sometimes severe and long continued. The strength of the wines is not diminished by the process, the proportion of alcohol in them varying from 10 to 15 per cent. It is found that once the vines have been irrigated, the practice cannot be changed without loss of the product, and injury to the plants. Clear water is preferred to that which contains suspended matter." 94 IRRIGATION OF MEADOWS. The effect of irrigation is sometimes found to render both vines and trees subjected to it, very susceptible to the frosts and severe weather of winter. This disadvantage seems to be a necessary adjunct, or set-off, to the advantages gained by the practice. Thus, a severe winter has been known to destroy whole groves of olive trees that have been irrigated, while scattered trees, not so cultivated, have escaped. It is rare that we can altogether escape a combination of circumstances that seem to offer us only a choice of evils; an alternative, either side of which is about as disagreeable as the other; a Scylla and Charybdis, neither of which can easily be escaped; and this business of irrigation of fruit trees seems especially to be one in which the operator is obliged to exercise the greatest care and circumspection to avoid, on the one hand, the evils of excess, and on the other hand, the periodical and certain dangers which this practice enables him to obviate or mitigate when intelligently applied. CHAPTER X. THE IRRIGATION OF MEADOWS. The permanent meadow is a very unusual adjunct to an American farm. Our climate is not naturally well adapted to the continued growth of grass. Our hot, dry summers are unfavorable. Generally it may be stated as beyond question, that the yield of grass is proportionate to the supply of water. As has been previously stated, no solid nutriment reaches any plant except as supplied to it in solution in water. What are the ultimate possibilities of growth in any crop is unknown to us, but it would seem as though they depended greatly upon the supply of water that can be absorbed, sufficient nutriment 95 IRRIGATION. of course being provided. Rye grass, upon irrigated fields richly fertilized, has grown at the rate of one inch per day, and repeated cuttings have been made at intervals of 14 days, during a season of several months. Crops of grass upon irrigated fields of a total weight of more than SO tons per acre, have been reported by trustworthy English farmers in one season. Irrigated grass fields in Italy support easily two head of fattening cattle per acre, every year, and have long done so. In hundreds of localities in European countries are irrigated meadows, which have borne grass without any sign of deterioration within the memory of the inhabitants, or the knowledge of readers of local histories, although the crop has been cut and removed every year during this indefinite period. Whether or not these immense yields could be further increased by more skillful management is not necessary to inquire. These products are so far beyond the dreams of an American farmer, that they may well be considered fabulous. But there is no reason to doubt the facts. On the contrary, they should be used as a stimulus for us to adopt, wherever practicable, the methods by which these crops are produced. The average product of grass upon our rich bottom lands, will not exceed two tons per acre, and upon uplands one ton per acre is a fair average yield. After a few years the best seeded of our meadows begin to deteriorate and run out. A change of crop is made and the meadows are once more seeded down to run out again in a few years. The cause of the failure is the heats and drouths which follow the hay harvest, and which cause a cessation of growth until they are past. Beneath a temperature which would be genial and invigorating to plant growth with sufficient moisture, the grass dies for want of the sustenance that water would afford. The most valuable crop we grow is thus reduced in its possible yield one-half or more. The only instance of an approach to permanent 96 EFFECTS OF PARTIAL IRRIGATION. meadows in this country, is the few partially irrigated grass fields which are very sparsely located in hilly regions where springs and brooks are led upon the grass upon sloping hillsides. In these few cases, year after year, crops of two or three tons, and sometimes more, of hay are cut. Where a very imperfect irrigation has thus been employed for 30 or 40 years, the meadows exhibit no sign of deterioration. An occasional dressing of manure, and a little fresh seed now and then, keep them in a productive condition. But in the majority of these cases the water has been utilized for this purpose, from sheer necessity rather than from choice. A spring issuing from a Fig. 42.-IRRIGATING A HHLBSIDE. hillside, or upon a level field, with high ground above.it, and low ground below, either meanders wastefully through the level and escapes in an unsightly gulley at the edge of the hill, or it spreads over acres of ground, and makes a useless and unsightly bog. The careful farmer, to avoid this evil, and with an eye to thrift, leads the flow into a channel that departs slightly from the level, across the field and down the slope. A stone placed here and there in the channel, causes the water to overflow, and spread in a sheet upon the surface. One by one portions of the field are thus watered, and the effect is to induce a growth of grass that remains green beneath the snow, and grows luxuriantly as soon as it has disappeared, yield 5 97 IRRIGATION. ing two crops of hay in the year, besides some pasture when the springs cease to flow and the ground is capable of bearing cattle. Upon hundreds of farms in Pennsylvania, and in the valley of Virginia which has been settled by farmers from the former State, there are watered meadows of this character which yield a steady crop of hay, year after year, and possess a sod which promises to remain productive indefinitely, with its present treatment. This accidental use of the water has been in reality forced upon the farmer. Hiad it not been brought into a channel and confined to one or two canals, it would have flowed irregularly over the surface and have formed a morass. The process really has been onef drainage rather than of irrigation, and the reclamation of the surface rather than its studied improvement. The methods of watering meadows in common use are illustrated in fig. 42, in which a small stream is led down a slope, and at fig. 43, in which the stream is dammed and the water carried laterally as far as possible. If such elementary and imperfect methods have been successful and profitable, how much more shall skillful and scientific irrigation add to the yield of our most valuable crop, and render possible the creation of permanent meadows, upon which grass may be grown in the greatest luxuriance, at an almost nominal expense! Numberless opportunities to make irrigated meadows present themselves everywhere. Far from being a matter of nicely arranged quantities of water, equally distributed at certain definite periods, as with other field crops; on the contrary, the irrigation of a meadow simply consists in causing a supply of water to pass over the grass at such periods as may be convenient; the convenience being only loosely circumscribed by times and seasons. It does not matter if the soil becomes saturated with water, it is only by the grossest negligence or ignorance that injury can be done. There is no danger, flthough the slope of 98 I EFFECTS OF COPIOUS IRRIGATION. * the field may be considerable, of washing the soil, or cutting the surface into ruts or gullies. Water may be turned on to the sod without fear of excessive irrigation if it is only kept in motion. The more water that passes over the surface the more valuable nutriment is brought within the reach of the plant. Every blade of grass acts as a part of a filter which retains matter that may be either in solution or in suspension in the water which slowly finds its way over the surface. The mechanical resistance offered by the myriads of stems and leaves of the grass blgjlJ~;,lUilil?Illqil'l'l~ muf.- / Xtllaellwl~l~m~~fllilir~lllllqqllltllll;M ix!:'1 ll ll/lAI l~/l} l.lipfflJlllt~W~ll~llJ/fflgl~lg#lllilW~lww.. Fig. 43.-IRRIGATING A RIVER-BOTTOM. to a current of water are such that the combined effect is equal to a loss of head or level of 16 inches in 200 feet. This retardation of the flow helps to cause the deposit of any sold matter suspended in the water, from which but few springs or streams are free, and also to bring every particle of the water into contact with the surface of the soil, or the surface roots of the plants. Not only, therefore, is the plant supplied with nutriment while the water is in contact with it, but a supply of nutriment is deposited and stored for future use. This freedom of application does not exist when cultivated or plowed lands are irrigated, and in their case more care and greater caution must be exercised to avoid injury. It is therefore advisable, in localities where only partial irrigation is:.. k ~ 99 IRRIGATION. needed, to cause these lands that are brought under the system, to bear grass in preference to any other crops, and to make the irrigation permanent and as perfect as possible. That is to say, thai in all other than arid or rainless countries, meadows only, and no other field crops, should be irrigated, unless under exceptional circum stances; for the reason that the irrigation of a meadow is easy and requires but little practical skill, is more cheaply performed, because the works are permanent, and is more certain and profitable in its effects than that of other field crops. It would not be difficult to give excellent reasons for these statements. It may be sufficient, however, to re mark that, excepting in those districts where irrigation is needed for all crops, the water supply can rarely be made available for any other lands than river bottoms; for the reason that the cooperative effort of many proprietors would be necessary to bring a supply of water to a large tract, and this would be difficult or impossible to effect. Bottom lands are naturally suited to the growth of grass, and the means and the end of their irrigation match so accurately, naturally, and conveniently, that there seems to be a foregone necessity that the one should exist for the other. Further on;, in considering more particularly the possibilities and methods of irrigating these lands, the advantages of keeping them as permanent grass lands will be still more conclusively shown if that need be. Where the climate admits of it, irrigation of meadows is performed in Summer and in Winter. There are two objects in view. One is, to supply moisture to the soil at a season when there is an insufficient amount of rain, and the other is, to convey to the soil, and deposit upon it, whatever fertilizing solid matter the water may contain at a season when water is very plentiful. The first object is : Atained by Summer irrigation, and the second by irriga t.'on in Winter. It is only, however, in those localities i,.* 100 WINTER IRRIGATION. where frosts are neither severe nor long continued that Winter irrigation is admissible. Where light frosts alternate with sunny days, a covering of a few inches of water, gently flowing across the meadows, protects as well as fertilizes the grass. At this season the copious rains or melting snows carry into the streams an immense amount of fine, earthymatter, which may be arrested and caused to be deposited in a thin sheet upon the soil. In the course of several years this deposit has been known to raise the surface of the meadow many inches, every inch of this increase consisting of matter of the greatest fertilizing value. Where Winter irrigations can be made, they will be found of the greatest value, for they prepare the crop which is to be cut in the Summer by supplying in a great measure the necessary subsistence for its growth. Where the level of the field or the supply of water is such as to permit it, a constant current may be kept flowing over the surface during the period when growth is suspended, or from November or December untilFebruary or March. Where it is necessary to make a series of levels to be irrigated in succession, each mayin its turn be overflowed for a week; or by arrangement of ditches and banks, the water from the upper level may pass over each lower one, supplying the whole, if it is in sufficient quantity. But where the supply of water is only limited, it is preferable to irrigate each level successively, for the reason that by far the largest quantity of suspended matter will be deposited by the first of the waters made to flow from one level to another, and in this case, the lower ones will receive a diminished quantity of deposit, in proportion to their distance from the source of supply. When the temperature falls sufficiently for ice to form, the quantity of water should be increased so as to keep a current constantly flowing beneath the ice. If the cold is sufficient to congeal the whole supply of water, so that ice rests upon the 101 IRRIGATION. grass, the flow should be cut off. No injury will occur to the grass in this case, but if the water is still allowed to flow, the ice will be increased in thickness, and a longer time will be needed for it to thaw. If this imprisonment is continued too long, vegetation may be injured, but a week or two is insufficient to cause any injury. In the Spring, when the water has been withdrawn and growth has commenced, there frequently occur cloudless nights and low temperatures, when hoar frosts are produced. On such occasions it is common to spread the water over the surface during the night, as a protection from the frost. The benefit derived is sufficient to repay the necessary care and labor during the months when these sudden changes are to be expected. There are many localities in the Middle and Southern States where this sort of irrigation might be practiced with very great profit. It is extensively practiced in Lombardy, where these II Winter meadows" are known as marcite, (marcia in the singular), and where they have long been known as the most productive of any meadows. As early as February, when the surrounding country may be yet covered with snow, these meadows, protected during the Winter by a covering of flowing water, begin to furnish their first cutting of grass. Five other cuttings follow, before the season closes, so that the cattle receive fresh grass during 11 months of the year. Twenty-eight tons of grass, or seven tons of hay, per acre, is the usual yield of these meadows. The valleys of several of the French, English, and Irish rivers, although subjected to a less genial climate than that of Italy, furnish many examples of successful Winter irrigations. Certainly a vast extent of the ULTnited States, where grass is a scarce product, might be made amenable to this profitable treatment. At this point a typical case might be cited. When visiting England some years ago, the author's attention was attracted to some extensive water meadows upon the 102 AN ENGLISH WATER MEADOW. banks of a small river, the Mersey, which finds its exit into the sea at Liverpool. The upper part of this stream flows through broad, alluvial lands, which, before their reclamation, must have been marshy, and of little value. Extensive works have been in existence, however, for many years; precisely how long could not be ascertained by enquiry, all that could be learned was that "they were always there." The river banks were enclosed by dikes, or as they are termed on our Western rivers, "levees," sufficiently high to prevent overflow, even in freshets. Substantial water-gates were made in these banks, leading into lateral channels at right angles to the river. These lateral channels had banks of equal hight and solidity with the main banks. The lateral banks extended from the river until they reached the gradually rising ground at their level. From these, other banks, enclosing lesser canals, with water gates at their heads, and parallel with the river, extended until they met the next range of cross banks; thus dividing the broad bottom lands into a series of parallelograms enclosed in a system of canals at right angles to each other. From these canals, gates sliding in perpendicular grooves, and raised or depressed by racks and pinions, opened into the meadows. When the level of the river was raised by unusual rains, the gates were opened, and the meadows enclosed within the different canals were flooded with water, to a depth of about six inches. So long as the river remained high, the gates were opened sufficiently to permit a gentle flow of water from one section of meadow to another, until it escaped into the river again at a lower level, by drains through the banks; or the water remained upon the meadows, in a state of quiescence, to deposit upon them the fertilizing matter which it held in suspension. For centuries this practice had been followed, and the gra,s thus grown had been mowed and fed to cattle, or made into hay. The same practice was afterwards ob 103 IPRRIGATION. served in other parts of England, Ireland, and in Continental Europe, where scarcely a possibility of utilizing a stream in this manner has been neglected. What is there in our circumstances that prevents the practice of so great an economy? There is no reason why our thousands of rivers might not each have its scores of watered meadows, along its banks. The skill to execute the necessary work is abundant. Hundreds of civil engineers, relieved from duty upon the suspended or finished railroads, might profitably turn their attention to this branch of their profession, if only farmers were alive to the advantages of thus improving their farms. The system adopted in Europe may be applied here with the greatest facility, but upon a much larger scale, as our rivers are larger, and our river bottoms more extensive. The irregular and unrestricted, and therefore sometimes destructive overflows would thus be controlled and profitably utilized. The supply of grass, our most valuable fodder, would be greatly increased, and a needed improvement would be effected in our agriculture. In the Northern States and Canada, Winter irrigation is impracticable, and there Summer irrigation only would be beneficial. As soon as the ground is free from frost, the water of the streams, highly charged with sediment, might begin to be utilized. Afterwards, when growth has begun, no check would be permitted, but every night during a dry season, the meadow might be flooded. Then, when the crop, brought to an early maturity by the stimulus of abundant moisture should be cut and removed, a new growth would be forced, and under the influence of a genial sun, would advance quickly. Two crops could be made by August, and in many cases a third could be procured by October. The economy of the system is sufficient to permit a considerable outlay in preparing the surface, and in addition there might be estimated a vast saving by the substitution of growing grass to be cut 104 USE OF SPRINGS. and fed to cattle, for the present costly practice of pasturing. Nevertheless it is not necessary that pasturing be abandoned, for irrigation is as applicable, to a large extent, to pastures as to meadows. The details of the methods here alluded to will be treated of in a succeeding chapter. CHAPTER XI. THEE USE OF SPRINGS FOR IRRIGATION. Springs are one of the sources from which water for irrigating meadows is most frequently procured. They are often situated advantageously, so that the water may be circulated by gravity over the land on a lower level. It is possible in many cases to reach the actual source of the spring at a point several feet above that at which it naturally issues from the ground. A vast number of springs really furnish a much larger supply of water than is suspected. Usually they are allowed to saturate the surface and escape into the subsoil by numerous hidden channels, which in the aggregate would furnish a respectable stream. By proper economy in using the water, a very small stream may be made to irrigate a field of considerable extent. It is by using water in driblets that many springs are wasted. A stream yielding one quart per second may have its water wholly swallowed by the thirsty soil within 200 feet of its source, when by arresting the flow and accumulating it in a reservoir, which may be discharged at intervals by automatic arrangements, the water may be made to escape in a volume four times as large, and sufficient to cover eight times the surface. 105 so. IRRIGATION. By this contrivance a very small spring may be utilized. One yielding 2 quarts per second will serve to water four acres of meadow if stored for 24 hours, and discharged periodically at intervals of that length of time. During this period 43,200 gallons would be accumulated, which would supply nearly one quart of water to every square foot upon the four acres; a very ample allowance in addition to what is furnished by the rainfall, to secure a full crop of grass. It would be preferable to accumulate a larger quantity of water than this, if possible, and to give a more copious watering less frequently. A thorough saturation of the soil at intervals, as has been before explained, is better than more moderate waterings more frequently given. Air is as vital a necessity to vegetation as water, and if access of air is denied, the roots of the plants must perish. Where water goes, air follows, and as evaporation takes place, air fills the space previously occupied by the water. To moisten the soil to a depth of several inches gives that coolness which the grass roots find necessary for their healthful growth; but to moisten the soil to a depth of only an inch or two, gives no supply sufficient to resist the drying effects of the sun's heat, or a hot dry summer breeze. Two inches of water given every week would be a very good supply, and with a spring of the size of flow mentioned, economically stored, twelve acres of grass could be watered once a-week. The effect would be equivalent to that of the fall of a steady, moderate shower during a whole day and night, and occurring every week, and every farmer can readily understand the value of such a shower upon his meadows. To store 43,200 gallons of water will require a reservoir of 5,760 cubic feet. One 40 by 20 feet, and 7 feet deep, will have about this capacity. If the width is doubled, the depth may be decreased one half. The shallower it it can be made the better for many reasons. The temperature of spring water is generally too low in the Summer 106 RESERVOIRS. for immediate use, and its value is greatly enhanced by being raised to an equal or greater temperature than that of the air. This is most quickly done by exposure in a shallow pond. Every foot saved in depth is a foot added to the level of the outlet, and so much more added to the area that may be irrigated. This is evident, because if the reservoir is 7 feet deep, the surface of the water can be no higher than the level of the source, unless the water is pumped up into the reservoir, and it is clear that the water discharged cannot be made to irrigate any land that lies higher than the bottom of the reservoir. With a 7 foot reservoir, all the land that lies between the levels of the bottom of the reservoir and the surface of the water cannot be irrigated; unless there are a Fig. 44.-SECTION OF RESERVOIR. several discharging pipes at different portions of the reservoir. With regard to cheapness of construction, if not to effectiveness in operation, it will be found far better to have the reservoir as large as possible, at least of sufficient capacity to contain water enough for use every two to seven days. Where the surface slopes but one way, an embankment may be made on three sides of a square, inclosing a sufficient space, and open on the upper side at which the spring will discharge itself. This is shown at fig. 44 in section, and in plan at fig. 45. To irrigate the strip of land parallel with the reservoir, a canal or furrow may be carried on a level with the spring, seen at a, a, in the figures, to the boundary of the meadow. The overflow from the reservoir may be made to pass into this canal. 107 a IRRIGATION. This will be found a very convenient arrangement. Figures 44 and 45 are intentded to represent a typical form of such a reservoir as this. The spring, escaping by a small stream, seen in the plan, fig. 45, occupies the a~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ----—....... A Fig. 45.-PLAN OF IRESERVOIR. point a, in fig. 44. The ground around and below the spring is excavated as shown by the dotted line, (fig. 45), and by the part lightly shaded, marked c, in fig. 44. The earth removed serves to make the dam which is construct ~M. Fig. 46.-TRA FOR DISCARGING RIESERVOIRM. ed in the manner hereafter described. (Page 111). A pipe is laid in the dam, for convenience not far from the surface, and a valve, operated by a key, d, closes and opens the pipe. The pipe is in fact a siphon, and if opened 108 DISCHARGING THE WATER. when the reservoir is full will discharge until the water is exhausted, into the distributing furrow, b, fig. 44, and b, b, fig. 45. The dotted line, in fig. 44, shows the level of the water in the resewrvoir when it is full and overflowing at the outlet, a. When the reservoir is filled, the surplus is discharged on each or either side, by the channels made for that purpose. This will obviate the difficulty previously pointed out. The flow may then be turned upon the upper portion of the meadow for twelve hours, in such a manner that the whole of the water shall be absorbed by the soil, and afterwards the contents of the reservoir may be flowed on to the lower portion during the next twelve hours, when the outlet will be closed. Many different arrangements for the use of the water may be devised to meet the necessities of any peculiar case, and as experience is gained, any difficulty that may arise at the first will be readily overcome. The reservoir may be discharged by an intermittent self-acting arrangement which is either a siphon, already described, or a more complicated but equally effective method of a balanced trap, fig. 46. The balanced trap consists of a board having a weight, X, attached to one end, and a cup or basin at the other, and being suspended upon pivots in a frame erected at the edge of the main distributing ditch at the outlet in front of the dam. The board is nicely balanced, so that when the basin is empty the weighted end rests upon a prop, F, purposely placed for it; but when the basin is filled with water it overbalances the weight and falls. As it falls it releases a gate, I, upon which is fixed a leather cushion which closes the outlet pipe of the reservoir, M. When the reservoir is empty the gate is raised and the pipe is closed. When the reservoir is filled the overflow enters a pipe through the upper part of the dam, C, and flows into the basin. The basin descends and releases the gate; the force of the water flowing from the discharge pipe keeps 109 IRRIGATION. it open as long as the stream is running into the canal. When the water is exhausted the pipe is again closed. To prevent the water flowing over the dam, through any accidental stoppage in the machinery, a branch of the overflow pipe is carried down the face of the dam into the canal. This apparatus is of very general use in the Swiss Cantons, and in irrigating works elsewhere, and works with regularity and precision. It is necessary that the balance-trap be properly adjusted and looked after occasionally. The worst that can happen in case of accident is the overflow of the reservoir by the pipe into the canal without harm. If the overflow is provided for at the inlet by a pipe or a channel placed there, as already suggested, this overflow pipe in the dam will not be needed. In practice, however, it will be found safest to have every guard against accident and consequent damage to the works, and two outlets will be twice as safe as one. If it is thought desirable, the waste-pipe in the dam may be placed two inches above the level of the other outlet, so that it will come into use only in case of a stoppage of the lower one. The outlet pipe should be large enough to discharge the water as least four times as rapidly as it enters the reservoir; so that the storage of two days flow may be discharged in a night or during one cloudy day. (Under no circumstance should the water be permitted to escape during the day when the sun is shining). A three-inch pipe will discharge nine quarts per second, which would be more than enough to furnish two inches of water to four acres in 12 hours. A pipe of this diameter would therefore be of ample size for a 12-acre meadow, giving a weekly watering to each 4 acres by three discharges of the reservoir. A siphon is not always to be depended upon to discharge a reservoir automatically. Sometimes the water, when rising slowly and not filling the pipe completely, trickles over and does not set the siphon in operation. 110 MAKING THE DAM. When an arrangement is made for the safe overflow of the surplus in some manner, a valve may be attached to the head of the siphon, (d, fig. 44,) by which the flow may be started, or a tap may be fixed to the lower end of the pipe for the same purpose. This would be preferable to the plain siphon, although it would involve the necessity of personal attendance at stated times to discharge there servoir. But no one should undertake the irrigation of land who is averse to giving the necessary attention to the de tails at proper times. An unexpected accident, the work of vermin, the presence of some floating body, or some other trifle, may stop the work, and unless some oversight is given to it, mischief and loss might occur. It is therefore advisable to depend upon personal effort rather than automatic contrivances, although it may be as well to have the latter in use if it is not made an excuse for neglecting careful supervision. Of all automatic arrangements for discharging the water, the balanced trap is the most trustworthy one. Where the surface is not regularly sloping, a hollow or ravine may be made into a pond or reservoir by building a dam across the hollow. In building any dam of this character, the foundation must first be excavated until the solid subsoil is reached, or the dam will leak and its stability be destroyed. A trench at least a fourth of the width of the dam should be dug and filled with puddled earth or clay. The front and rear of the dam may be made of sods cut from the bottom of the reservoir, and the center up to the top should be made of earth or clay puddled and rammed solidly between the walls of sods. The dam, if a high one, should be at least twice as wide at the bottom as it is high; and the width of the top should be one-fifth that of the bottom. The inner slope should be 18 inches horizontal to one foot of hight. The bottom of the pond should be made of puddled clay to prevent a waste of water. A section of ill IRRIGATION. the dam is seen at fig. 44; the hight of which is 8 feet, width 16 feet, and the puddled clay wall in the center is shown by the darkly shaded portion. Where the spring is of sufficient volume to supply all the water that may be needed, it would still be worth while to provide the reservoir for the sake of gaining the increased temperature; but in such cases the reservoir will not be needed for the purpose of distribution, but only to warm the Fig. 47.-MANNE OF COLLECTING THE WATER OF SPRINGS. water. The overflow, then, only will be used, which will escape on the same level as that of the inlet. The course of the current through the reservoir should be made as circuitous as possible by means of a division of boards in the center, that the exposure of the cold water to the warm air or sun's heat may be the longer. When water is retained solely for this purpose, the space in which it is confined should be large and shallow, so that the exposure of the water to the sun's heat, and the 112 USE OF SPRINGS. influence of the atmosphere, may be as thorough as possible. The temperature of the water has a considerable effect upon the growth of grass. Every one has noticed the effect of a warm shower, in early Spring, in starting vegetation; and also the ill effect of a cold rain, in the Fall, in arresting growth. In all cases the water should at least be of an equal temperature with the air. When spring water is used, the temperature can only be raised by exposing it in ponds or reservoirs fora time, and the shallower the pond the more quickly will the water be warmed. Exposure to the atmosphere also exerts a chemical effect, and some waters that contain sulphate of iron, or other deleterious substances, are rendered harmless by the oxidation of these impurities. Thus the temporary storage is of sufficient advantage both in enabling an intermittent irrigation, and in warming and purifying the spring water, to make the cost of the reservoir and distributing apparatus a profitable expenditure for any meadow of not less than four acres in extent. It is often the case that a number of springs exist upon the surface that may be brought together into one channel with great economy. A spring is often merely the overflow of under-'...... X. ground streams, and by digging ~//;__ downwards the whole of the water may be captured and brought into one channel, with the double ad- Fig. 48.-THE DRAIN AND vantage of draining a wet field DISCHRGE PrE. and of utilizing the water for the irrigation of a meadow below the level of it. The diagram, fig. 47, represents a case of this character. A number of springs break out at the surface, and spreading make a marsh, but form no stream there. To utilize the water of these springs, and to drain the wet surface, all that is needed is to 113 IRRIGATION. cut a drain (see fig. 48) from each of them, leading to a common channel, and deep enough to reach the subterranean sources from whence the overflow comes. The main channel is made to discharge at a point l ~ ~ ~ required either into a cistern or into an irrigating ditch. The method of mak ing the drains need not be costly. If stone is at hand, and fiat long pieces can be easily procured, the drains may be made by placing long narrow stones against the sides of the ditch, at the bot tom, and covering them with shorter pieces placed crosswise. Small fragments maybe thrown upon these and earth up Fig. 49. on them. This is shown at fig. 49. If FLAT STOE DRAIN. round stones only can be procured, the drain may be made as shown in figs. 50 and 51. The depth of the drain, should not be more than is necessary to reach the main stream, as for every foot deeper than that, so much head at the outlet is lost, and so much less land can be watered. In digging the drains, for the Fig. 50. ROUW STONE DRANS. Fig. 51. same reason, no greater fall should be given than is needed. Six inches in 100 feet is ample fall to keep the drains clear from sediment, and more would probably result in washing out portions of the drains at the sides or bottoms. A very useful level for laying out the drains may 114 LEVELING THE DRAINS. be made as shown at fig. 52. It consists of a paralleledged board, seven or eight feet long, with a L affixed near one end, which supports a pendulum. A scale is marked on the board at the foot of the pendulum, whereby its motions are noted. When the board is perfectly level the foot of the pendulum marks 0. When the board inclines either way it varies accordingly. A handle is fixed to the end of the level, which serves to hold it in position when in use. In case it is not wished to lay out Fig. 52.-LEVEL. the bottom of a ditch to a very accurate grade, the mere movement of the pendulum to the right, when looking at the scale or index, will show that the grade is downwards. But if accurate measurement is desired, it will be necessary to make the instrument in proportion, and mark the index carefully also with a proportionate scale. Thus, if the bottom of the level is six feet long, and the 1 two feet high, an elevation of the hinder end of the instrument of half an inch would be equal to a grade of one inch in 12 feet, or one in 144, or eight inches in 100 feet, and would cause a deviation from the perpendicular of the pendulum of one-sixth of an inch; a grade of 16 inches in 100 feet would cause a deviation of one-third of an inch. If such close measurement is desired, the instrument will have to be carefully made. For ordinary operations, it will only be necessary to take care that the j. is set on quite square, and then the least movement III 115 12 ..k Ili. . 11 IRRIGATION. forward of the pendulum will show the grade to be correct. When the waters of springs, such as are now under consideration, are to be used directly in irrigation, the method shown at fig. 53 may be applied. The springs s, s, s, may be opened or cleared of rubbish, and may be led directly into furrows following the lines of level shown by the dotted lines. Or they may be led into the larger springs and the collected water be discharged as shown at S, S. Or several springs near the center may be ,, — /,, --,, , - -- Fig. 53. -DIRECT USE OF SPRIGS. gathered into a pool or reservoir, and the others led into it, and the whole supply be discharged into a main furrow following the level as seen at fig. 54, in which the springs are seen at s, s, the reservoir at R, and the irrigating channels at c, c, c. By this management the drainage of wet, arable lands, also may be made to furnish a supply of water to irrigate meadows, and the instances where such a combination of advantages may be availed of are far from scarce or few. Indeed the swamps that now produce very inferiorherbage, I I 116 I _ _ DOUBLE PROFIT IN DRAINAGE, or that are totally useless, or worse, because productive of miasma, or dangerous to cattle that may trespass upon them, and that might be reclaimed by drainage, and at the same time furnish a copious supply of water for irrigation, are far more numerous than would be suspected by any but an engineer, whose practiced eye can see at a glance the possibilities in this respect that others would fail to perceive. It nine cases out of ten, at least, a swamp is in reality a spring, or a number of them, which spread .. - - - - - - -.. F Fig. 54.-T SPRINGS COLLECTED INTO A POOL. themselves over the surface and stagnate, losing their flow by evaporation or slow filtration through the surrounding soil, or their own subsoil. To utilize this waste water would be to turn a diseased and pestilential spot into a healthful and productive field, that would also contribute the means of enhancing the productive capacity of neighboring fields. Then "out of the eater cometh forth meat," and out of the waste place cometh forth fertility. 117 .,s~~~~~~~~~~~A. I. _, IRRIGATION. CHAPTER XII. FORMATION OF WATER MEADOWS. Every American farmer will acknowledge that grass is the most desirable, but at the same time the most difficult crop he can raise. It costs less to raise than any other crop when the adverse climate can be vanquished. But fortunately the American climate it not invincible, and there are means by which this crop, (as well as others), may be cultivated with success, in spite of heat and drouths. One of these is the system of irrigated, or water meadows, upon which the growth of grass can be made continuous during both Summer and Winter, for where the climate is not sufficiently cold to form ice more than two inches in thickness, grass may be kept in a growing state throughout the Winter, and be made ready for the first cutting in February or March. The United States is the only civilized country in which grass is not so grown, more or less. There is scarcely a river in Europe whose waters are not compelled to nourish and protect thousands of acres of its bottom lands wherever they can be brought upon them by means of embankments and ditches. On every hand the observant traveler sees irrigation works of extensive and substantial character, and of great antiquity; and verdant meadows within them, covered with the most luxuriant vegetation. These works are to be found where the climate is naturally as unfavorable to the growth of grass as in any of our Southern States, although it is true that in warm, humid climates, or those where the heats of Summer are not so ardent, water meadows find their greatest developement. The small county of Wiltshire, in England, alone has 20,000 acres of water meadows, most of which have been in cultivation for over 150 years. This county is a famed dairy 118 ADVANTAGE OF WINTER IRRIGATION. county, and the Wiltshire cheese is a staple product in the markets of the country. But it is drouth, and not heat alone, that is fatal to the growth of grass, and which sears it as the breath of a furnace. Heat and moisture develop vegetable growth most abundantly. Without declaring that irrigation is to revolutionize our husbandry, it is only necessary to refer to the abundant opportunities which exist here for enterprise in this direction, to be assured that a vast change for the better would occur if it were brought into general use. It is a mistake to suppose that an irrigated meadow depends solely upon the use of water during the Summer months. On the contrary, wherever it is possible to be done, it is by application of water during the Winter season, or from the Autumn to the Spring, that the crop gains an accumulation of strength which enables it to pass through the Summer in safety, giving several crops in that season. Not that Summer irrigations are not useful or necessary, but that they are of less volume and of less continuance. The chief advantage of this system is the accumulation of fertility made during a period when otherwise the ground is wasted by rains, and denuded of soil and soluble matter that it is not in a condition to spare. The meadow is made the place of deposit for a large portion of the matter of which other lands, not so improved, are deprived by rains and floods, and if the whole of the waters of the streams could be arrested and made to give up their burden, the whole of the value lost by them would be regained, and none escape to the seaor the estuaries of the rivers to form future lands of the richest character. The opportunities for producing grass upon water meadows in the Southern States, where Winter irrigation is possible, and where the river flats are extensive and numerous, are many and great, and the advantages in this direction are too important to be neglected., 119 IRRIGATION. The nature of the herbage upon an irrigated meadow depends greatly upon the skill with which the irrigation is managed. If water is used in excess, the more valuable grasses disappear and inferior ones take their place, such as quack grass (Triticum repefls), the spear grasses (Glyceria aquatics), and G. fltuitans and other coarse species. By careful management, re-seeding, and manuring, timothy and clover may be retained in a watered meadow, but there are several grasses which are but slightly inferior to timothy, and which grow abundantly and constantly, that are much better adapted to this culture. These are the fowl meadow grass (Poa serotina), rough-stalked meadow grass (Poa trivialis), the tall meadow oat-grass, called ray grass in France, (Arrenatherum avenaceum), and the well-known red-top (Agrostis vulgaris). These grasses furnish a heavy burden of sweet, nutritious, palatable hay, and immediately after mowing, when watered, spring into a vigorous new growth. Italian rye-grass (Loliurnm Italicum), is extensively grown upon irrigated meadows in England, and yields repeated heavy cuttings of forage for soiling. It has been tried here without success, but not on irrigated lands. It is probable that under irrigation it will be found of equal value to other grasses that have already been naturalized, and are known to be available, as it is the chief grass grown upon the Italian water meadows, upon which it yields several cuttings, equal in the aggregate to 90 or 40 tons of green fodder per acre yearly. A mixture of five to seven pounds each of the four varieties named, as best adapted to watered meadows, would give a thick growth, and as some of them increase from the roots, a thick permanent sod would be formed, which would be in active and successive growth up to October, or even later in the season. The undulating character of the surface of the soil offers the greatest facilities for using the waters from streams, both small and great, in irrigation. There are 120 MODES OF APPLYING WATER. millions of acres upon the banks of streams that could be made to bear crops of grass permanently, with the greatest profit, at a comparatively small outlay per acre. It is where the surface to be irrigated is large that the process of irrigation is the cheapest. Where a stream flows naturally above the surface of a portion of the neighboring land, the cost of irrigating the land will be very small, and the cost per acre will be the minimum when the supply of water is abundant and the area to be watered is large. In this case no dam will be needed, or at most such a one as can be made at a small expense and maintained with little trouble. A simple barrier of stones, or a few planks, or a log laid across the stream and held in its place by a few stakes driven in the ground, will suffice to divert the flow into a canal, which will lead the water with the least possible loss of level to the ground to be irrigated. A narrow valley having a stream meandering through its center, and with sides gently sloping toward the stream, is peculiarly well adapted for irrigation. The whole length of the valley, from its head to its outlet, may be made a succession of meadows. The small tributary streams of the valley will be made to aid in the work and contribute their share to the general supply of water. Should the streams be subject to early Spring and late Fall freshets, so much the more valuable they will be. Every flood will bring down a large amount of solid matter to be deposited as a fertilizer upon the soil. The water of floods is also highly charged with soluble matters which are rendered up to the soil through which it is made to percolate. The only disadvantage is, that should a flood occur when the grass is nearly ready for cutting, a considerable quantity of sand may be deposited upon it, and much of the crop may be lodged. But this difficulty is unavoidable, and would occur in any case, and must be submitted to as one of the drawbacks incident to the 6 121 It IRRIGATION. process of doubling or trebling the usual amount of the crop. The first business to be undertaken in forming such a meadow is to thoroughly drain the land either by underdrains or by open drains. The most important drain will be that which cuts off all the springs which issue from the foot of the uplands, and which generally render the low land a sodden marsh. Frequently this drain should be dug to the depth of six feet, that every spring that may issue below may be intercepted and tapped. This drain should be cut above the highest level to which the irrigating ditch can be carried, and may discharge into it or be carried beneath it and made to issue in the lateral drains. Next, the surface is to be leveled, the hillocks cut down and the hollows filled, so that no stagnant water can be retained in them, and the lateral slope of the meadow be made perfect up to the edge of the stream. The stream, or so much of it as can be used, is then diverted into side channels, which are carried as nearly upon a level as possible until they reach the foot of the upland, when they are carried still upon a level or with a slope of not more than one foot in a thousand, in a direction parallel with the general course of the valley, but yet following the winding made necessary by the configuration of the surface. The general arrangement of the dam, canals, and drains, is as follows: see fig. 55. The winding stream which occupies the center of the valley, shown by the dotted lines is straightened, and dammed at a; the lateral canals are carried each way from the dam to the borders of the valley, and from them a regular system of distributing canals is supplied. The main cross drains, b, b, are above the canals on either side, and the drains, shown by the dotted lines, are carried directly to the stream, or they may be made to discharge into the water furrows if so desired. The level of the stream may be raised by' embanking its sides for a sufficient distance, in 122 A VALLEY MEADOW. stead of building a dam across it and forming a pond. But the value of a pond upon a farm, if for no other purpose than procuring a supply of ice, would amply repay the value of the land and labor in one year. The Il I I I/" II - IF4w?!-I I. ~$~L((~.<{)\ JI\ Fig. 55.-mIRRIGATION OF A VALLEY. arrangement of canals here described is a typical one for this kind of meadows; it is capable, however, of abundant modifications, to suit varying circumstances. It is given to illustrate the principle upon which these meadows may be formed. There are various other methods of raising the water than this which has been described, some of which may be mentioned as being applicable to various circumstances. The old-fashioned noria, which has been in use in Southern and Central Europe since the eleventh century, is not yet out of date. It is still used in Savoy, Lombardy, Spain, and parts of France, and being easily constructed, and cheaply effective, where the supply of water is sufficient, might be used in some cases here. A wheel, haviigbroad floats, is hung upon an axle, so that the lower floa." if 123 dl- - - -NC. -A-f~~~~~~ I -. 3(l l l to 1 And~~~~~~~~~~~~~~~ b IRRIGATION. are submerged in the stream, fig. 56. By offering a little obstruction to the stream, to increase the rapidity of the current where the natural velocity is not sufficient, the wheel is set in motion and revolved. Water buckets are fixed to the circumference of the wheel, in such a position that the direction of their longitudinal axle is 45 degrees from that of the axle of the wheel. The buckets are _... _ - nT-....... Fig. 56.', oB, OoR WART WREU partly filled as they pass through the water, and are discharged as the wheel brings them round to an inverted position, into a wooden trough placed alongside of the wheel. From this trough the water is conveyed to the distributing channels. Water may be raised by this rough and ready process, in the cheapest manner, to a hight of ten or twelve feet, requiring no attention and working by day and night so long as the stream flows. Another ]method by which a small portion of the water may be aised is applicable to brooks of moderately small volume, 124 I I A WATER MEADOW. as well as larger streams, viz., the use of a water-wheel. Where the stream cannot be raised conveniently, an undershot wheel may be set in motion by turning the current into a wooden trough or shute, and impelling it against the floats of the wheel. Where a dam can be made, an overshot wheel may be used. Either of these wheels may be made to operate a chain pump, and raise a considerable amount of water. This pump is preferable to any other, as there are no valves to be choked by small floating substances, or to be worn by sand, which may be brought down by the stream. Wooden pins may be inserted around the rim of the wheel, from which a wooden pinion or gear may convey the motion by a short shaft to the pump. The most economical form of meadow is the " water meadow," which is one so arranged that it can be flooded completely to a depth of several inches, and the water can either be retained upon the surface when desired, or made to pass over it with a slow, steady current. These are the meadows which in parts of Europe are so productive of grass, being protected during the winter from the slight frosts or snow which would stop the growth of the herbage, by a covering of water. Where the land cannot thus be completely covered, meadows cannot be irrigated in the winter season, in climates subjected to frosts sufficiently severe to freeze the ground an inch in depth. The too well known destructive effects of a frost upon a sod saturated with water, entirely forbid Winter irrigation in the Northern States. But in the Southern States, where frosts do not continue more than a few days at a time, the "water meadow" may be made a valuable addition to the farm, and supply such an increased amount of fodder for stock as may easily change the system of farming to a very considerable extent. In forming water meadows no dams are used, nor is any water raised above its level. The streams are embanked 125 IRRIGATION. so as to confine the water which is diverted from them and is carried in a level channel which gradually diverges more and more from the stream, until the whole of the land to be brought under treatment is inclosed. As the level of the surface slowly descends, that of the canal Fig. 57.-SECTIONAL PLAN OF WATER MEADOW. rises gradually above it until there is a difference of at least a foot between the levels of the water and the ground, at the upper portion of the meadow. The more regular the slope of the meadow the better in every way. If a perfectly smooth surface can be made, the meadow is then a perfect one. A perfectly formed meadow is the one that lies in a succession of smooth, gently sloping _a a-. Fig. 58.-RouD) RLAN OF MEADOW. tables, each one one or two feet, or more, below the level of the other. A meadow so prepared will show a section similar to that in fig. 57, in which the irrigating canals are seen at e, e, and the collecting drains at f, f. Spouts in the banks, at a, a, may pass the water from one level to another. (See also page 113.) 126 :r L. $ f& .1t t e _IA c te t WATER-GATES. Each portion of the meadow will be confined between banks upon the sides, one of which will be upon the edge of the river, and the other upon the opposite boundary, which is the main supply canal, and between a canal of distribution at the head and an open drain at the foot. __ ~ Fig. 59. —SELF-ACTING WATER GATE. This is shown in fig. 58, in which a, a, is the river; b, b, the river bank; c, c, the opposite bank; d, d, the supply canal; e, e, the distributing canal; and f, f, the drain. The drain discharges into the river through the bank by a self-acting gate, (fig. 59,) which yields to the outflow, but is closed by an inflow from the river. Or the surplus water from the upper level may be discharged into the distributing canal of the next lower level. The water is passed from the supply canals to those of distribution, either by a gate raised by a winch and pinion and rack, fig. 60, or a spout through the bank of the canal, which is closed by a slide, seen in fig. 61, and at a, a, infig. 58. Fig. 60.-WATER GATE. The water from the canal is first turned upon the upper level; when this is covered to a proper depth the gate is closed, and the water turned through the next gate upon 127 I II I IRRIGATION. the next level, and so on until all are covered. A sufficient quantity of water is allowed to pass on to each level to maintain the proper depth, and allow a gentle current to flow from the drains. This is important when the temperature falls below the freezing point. Observations have been made, which have shown that when this has occurred, and the temperature of the air has been as low Fig. 61.-SPOUT IN THE BANK. as 26~, that of the grass beneath the ice has been no lower than 42~, and that vegetation was still active, as shown by the color of the verdure. As regards the amount of water used, and the manner of using it, the following experiences may be cited. A comparison of fields that have been less abundantly watered, with those that have received a copious supply, has shown that the crops upon the latter have been infallibly increased. Where during one Winter the irrigation has been suspended, the succeeding crop has been little or nothing. Where the water that has passed over a field has been flowed upon another, the crop of the latter has been very inferior to that of the former, showing conclusively that the earth had completely abstracted the fertilizing property of the water in its first contact with it. In proportion to the abundance of water supplied during the Winter, so is the yield of grass in the Summer. In short, facts are conclusive to show that the quantity of water that can be used, is the gauge of the harvest to be expected. The Winterirrigation supplies the fertility, that of the Summer simply supplies the necessary moisture. In this respect the action of water constantly passing in a A- I, 128 i-1 I, SOME SETTLED PRINCIPLES. thin sheet over a grassy sod has a different effect from that of water passing over uncultivated soil. It does not wash the soil nor carry off soluble matter from it, but it is itself filtered of whatever matter it contains that can be appropriated by the roots of the grass. The width of the levels that may be irrigated is very irregular, and depending greatly upon the character of the surface. The larger the breadth the cheaper the process of preparing the surface, because the expense of forming the embankments, canals, sluices, and drains, is divided over a larger number of acres, and the cost per acre is diminished. It is cheaper to enclose a large area-100 acres for instance-although the works may be heavier and more costly, than a smaller one of 10 acres with much lighter works. In laying out water meadows, this consideration should not be neglected, and the largest area possible should be enclosed. Some of the dikes enclosing the English and Italian water meadows are not less than 20 feet in hight, but hundreds of acres are brought under irrigation by them. In such cases the works are massive, costly, and built to last for ages. Smaller meadows may not require embankments of more than one to three feet in hight, and the earth for these may be procured from the drains which carry off the surplus water, and which are necessarily of ample size. In making the banks it will be found the cheapest plan to dig the drains large enough to supply all the earth needed for the banks; the extra ground used will be of very little importance compared with the expense of bringing earth from a distance for the construction of the banks. A water meadow, or at least each section of a meadow in one enclosure, must necessarily be carefully leveled. The most perfect meadow is one that has a perfectly level surface between the banks, so that it can be covered evenly with six inches of water. The water may be flowed over the surface of a meadow of this character, and kept 129 I IRRIGATION. upon it, if desired, by closing the outlet at the foot; or the outlet may be opened only so much as to allow a gentle current to pass over the meadow and maintaining the water at its stated depth. Upon level meadows less water may be used than upon meadows having considerable slope. The more water that can be made to pass over the grass, the better, up to the point of the saturation of the soil. The quantity of water that may be used depends upon the inclination of the surface and the quality of the soil. Where the surface is perfectly level, and of a clayey character, the minimum quantity of water can be used. When the surface slopes so as to reach the extreme inclination practicable for these meadows, and the soil is gravelly, sandy, and porous, with a porous subsoil, then the maximum quantity of water can be used. An instance is stated by M. Herv6 Mangon, in his work already referred to, of the irrigation of meadows in the valleys of the Vosges, Eastern France, in which water is employed to such an extraordinary extent that the total quantity used in a year would cover the soil to a depth of thirteen hundred feet. In another case the quantity of water used between the end of November and the middle of August following, was equal to a total depth of 27 feet. The whole of this time was divided into eight periods of watering. But the locality in which these extreme cases occurred, is one where the meadows are rarely level, and have generally an extreme inclination; the soil is gravelly, being derived from the schistose rocks of the surrounding hills, and is very porous and loose in texture, and the water of the streams is highly charged with sediment and soluble matter, from the decomposed rocks. At least such is the case in the valley of Waldersbach, a locality much visited by travelers on account of its connection with the history of the renowned Father Oberlin, and where the author has seen the grassy hill sides flowed iso 1 5 I I SLOPING SURFACES, with sheets of water almost approaching the character of cascades, and the level meadows appearing as lakes. It is by the use of the most liberal supply of water, when the conditions; are favorable, that we can cause to pass over a given surface, the greater quantity of nitrogen, phosphates, and other valuable matters, contained in the water and needed by the soil. Irrigation of meadows is thus seen to be by no means a simple drenching of the soil by stagnant water; but, on the contrary, the bringing into active contact with the soil of the largest possible quantity of water surcharged with fertilizing gases, salts, and organic matter. When the surface slopes, the arrangements of ditches and drains should be made to suit the slope. If the slope is in only one direction, the water can readily be made to flow down the slope from the head to the foot by a system of gates from the canal which passes along the upper part of the meadow. At the foot the water passes into a drain and escapes into the stream, or it is carried from the drain beneath the dividing bank into the next section, and made to flow over the surface of that, as it has already done over that of the previous section. Where the slope is not more than one foot in 100, a considerable depth of water may be maintained upon the surface, as the flow is greatly retarded by the grass. Where the slope is greater than this, the construction of a water meadow must be abandoned, but a modification of it may be used, and a meadow upon which a current of water may be flowed from head to foot without any series of water furrows, may be made and laid out upon the general plan of the true water meadow. But to flood the surface in case of frost would be impossible or injurious, because of the great depth of water that would be required, and Winter irrigation would be either injurious or full of risk. So long as the slope does not much exceed 1 in 100, the meadow may be laid out as a water meadow, if other cir 131 IRRIGATION. cumstances favor it; (such as a location upon a stream where there is sufficient fall, to avoid heavy embanking, which however is a rare occurrence); but when the slope exceeds that ratio another system must be adopted. Be sides the systems of water meadows, previously described, there are other methods of irrigating grass lands which will be explained hereafter. The time of continuance and intervals of irrigation of these meadows is of importance. There is always danger that, by reason of a rise of temperature, vegetation may be unduly stimulated. In such a case the water, only in sufficiently charged with oxygen, cannot supply the de mands of the plants, and they are destroyed unless the water is withdrawn and air supplied, or the temperature lowered by exposure until the stimulus is removed. An interval of a few days is then to be given before the water is again turned on. An irrigation of 10 or 15 days and an interval of five is the general practice. Whenever practicable, a meadow may be divided into three or four portions in the manner before described. Then, in the first case, by flooding two of the divisions, and at the end of five days drawing off the water from the first and turning it upon the third, and after five days more drying the second and floodin the first, and so on continuing, each division would n da~ s under water and five days dry. In the second' ase, if are under water in succession and one dry, eac 5 days irrrigated and dry for five days. It is impio6ile to give directions in each case; the experience of the operator must be his guide, and the beginner must exercise caution, learn to know when he is right, and then go ahead. A reference to the principles upon which irrigation depends for its good effects, and the circumstances which would make it injurious, must be carefully made whenever there is doubt in the mind of the operator. The general rule already stated, that it is much more common, and easy, to err upon the side of 132 I MEADOWS AND PASTURES. excess, than on the contrary, may be remembered as a caution and safeguard. Still there is less danger from excess in irrigating grass than any other crop. It might be well to explain at this point that the arrangement here described fQr making water meadows is exactly applicable to cranberry plantations which require to be flooded. In many cases the slope of such plantations is too great, and consequently there is either an injurious depth of water flowed upon the vines, or the water is not in sufficient supply to permit the covering of the upper portion of the field, and the expense of making the necessary high banks is too onerous. By laying out the meadow as is shown in profile at fig. 57, and in plan at fig. 58, each plot can be flooded to a moderate and sufficient depth with the expenditure of a minimum quantity of water. The cost of making several low banks and smaller drains is not more than that of making one high bank and wide deep drain, and the crop is not injured by an excessive depth of water. CHAPTER XIII. IRRIGATION OF MEADOWS AND PASTURES. While the irrigation of grass land, situated in a river bottom, and having either a level surface or one with but very little slope, as has been described in the previous chapter, is an easy matter, and when the supply of water is ample is the most effective method of making a water meadow, yet the proportion of farms possessing the requisite facilities for a water meadow is comparatively small. Where therefore, there is but a small supply of water and no broad level space of ground, the meadow 133 I IRRIGATION. must be made in some other manner than that previously described. But in all cases, whatever may be the character of the surface, when there is a supply of water flowing above the level of the ground to be watered, an irrigated meadow may be made. It may be a level piece of land, or a piece sloping in one or two directions, or an irregular surface having meandering slopes, or a hill side so steep that wagons cannot be used upon it, any of these may be brought under irrigation, if there is the requisite supply of water. In preparing meadows for irrigation, the first consideration is the selection of the ground. In this is'included the supply of water. It may be that the area that can be covered by the water is too small to return a fair profit on the venture, or the supply of water may be too small for the area upon which it is to be spread. Close calculations should therefore be made, the supply closely measured and the needs accurately estimated. The first cost of preparing the surface being almost the whole expense to be incurred and this being less in proportion as the area increases, it is a measure of economy to spread the water over as much space as possible. If the water is sufficient to flow one acre in one day, by dividing the land into twelve plots and irrigating one each day in succession, the whole may be brought under the improvement. UIpon level lands or those which have but little slope, and that in only one direction, the preparation of the surface is very easy and simple. In this case the irrigation will be by narrow channels, or ditches sodded or sown over with grass which will offer no obstacle to the mower when the crop is cut. The form of the distributing ditches will be of a very obtuse angle, or a light depression of the surface sufficient to confine the current of water which will flow over its edge or edges, and spread in a thin sheet over the surface; slowly sinking in 134 f I I I I i I PLAN OF MEADOW. to the ground or finding its way into the drain, either by percolation through the soil or by surface flow at the foot of the field or plot. The form of the furrow is seen at fig. 62. It may be two feet wide and four inches deep. As there is no loss of crop in this case, the space occupied by these furrows is of no consideration; the wider and Fig. 62.-FORM OF WATER FURROW. shallower they are, however, the more permanent they will be, and the less subject to injury by trampling, should the meadow ever be pastured. The arrangement of the meadow would then be a main supply-canal, so located that the water may be diverted from it to supply any of the subordinate feeders in turn by means of the distribut a. - n t l ~~~~~~~ L I _~~~~~~~ 6 Fig. 63.-PLAN OF IRRIGATED MEADOW. ing canals. See fig. 63; a, a, being the main canal; b, b, distributing canals; c, c, drains. The flow may be diverted by means of the hand-gates already described, or by placing obstructions in the main canal, such as bricks or sods, as shown in fig. 64. Where there is an inclination of the surface insufficient to amount to what would be called a slope, a somewhat I 6 0 I 135 IRRIGATION. different arrangement would be required. See fig. 65. The water would be taken from the supply canals and diverted into a feeder to be carried in a diagonal direction across the plot, from which the distributing furrows ~\ I Fig. 64.-DIVERTING THE FLOW. would be carried. The overflow from the distributing furrows would even spread over the ground down the inclination. The triangular spaces below the junction of the distributing furrows with the feeders, are watered by means of small reflex furrows, which gather some of the overflow from the distributing furrows and carry it back toward the feeder. This system of irrigated meadows is applicable to numerous and varied circumstances. It may be adopted in cases where the surface is level, or where the inclina I1 IlIlllI1/l11 Ig. I O 1.FROO A INNI g O Fig. 65.-FoRe OF FURROW FORLA INCLINED FIELD. A: tion is slight but regular, and where the supply of water is not sufficient to permit of flooding or may be in minimum quantity. It may also be adopted in those cases where the surface is a plane of which the slope is moderate in one direction, so that the distributing furrows may be carried on a level, and in a nearly straight direction; or upon nearly all surfaces which will admit the use of a mowing machine. It is particularly adapted to many 136 INCLINED SURFACES. cases where the land in river bottoms has been injured by the washing of freshets, and a bare surface of sand or gravel has been left, upon which grass cannot now be grown because of the absence of soil. This last case, however, would more properly come under another head, and will be treated in the proper place hereafter. In preparing the surface of an irrigated meadow, the ground should be plowed without open or back furrows. There may be exceptions to this rule, where the ground is to be laid out in plots for successive irrigation, or where the surface is a dead level. In the former case, the ground may be plowed in broad flat lands, each land forming one plot, of which the open furrow will be the center, and the feeder for the distributing furrows. In the latter case the ground will be plowed in narrower lands, with a rise from side to center of not less than 6 inches to 100 feet; the back furrow or the ridge will be the place for the distributing canal, and the open furrow will be the drain. This will in fact be an extended application of the system of beds heretofore described as applied to gardens. The best implement for this work is the swivel plow, with which the furrows may be all laid the same way over the whole field. The plowing is to be carefully and evenly done, and as deeply as possible. No "balks" must be made, the furrows must be straight, and no trash, weeds, or coarse manure, are to be plowed under, that in rotting would leave depressions of the surface. Two or three plowed crops, or a Summer fallow, might be first taken, so that the surface may be made smooth and level. If there are hollows and knolls, the latter must be leveled and the former filled up. This can be done, in part, with the harrow, and in part with the scraper. The scraper for this purpose may be a plank, at the lower end of which a strip of wide band-iron or sawplate is fastened. A pair of plow handles are fixed behind, with which it is guided, and a pole or a chain fastened to 137 IRRIGATION. rings in front, by which it is drawn by a team of oxen or horses. See fig. 66. The common horse-shovel may be used where it is available, and where considerable earth is to be moved, but the plank scraper will make an effective leveler of the ground. The surface is to be rolled and harrowed alternately and repeatedly. Upon the care Fig. 66.-THE SCRAPER. and completeness with which this work is done the after value of the meadow will depend. When the surface is prepared, the seed may be sown before the canals and ditches are dug, lest the water should disturb the earth before it is covered with grass and bound together by the roots. When a surface already level, but without soil sufficient to bear a crop of grass without help, is to be improved by irrigation, the grass seed is sown after flooding, and while the ground is moist, and is left until what will sprout and grow has done so. The water is then turned on to the surface, very gradually, and allowed to flow for 24 hours, when the supply is shut off, and what is upon the surface is permitted to sink into the ground, or flow gradually away. This is repeated, more seed being sown each year, and water being let on whenever it is more than usually charged with solid matter. At every watering some deposit is left, and as the grass increases in 1I8 i MAKING THE CANALS. growth, more of this solid matter will be arrested, until in a few seasons a sod will be formed, and the meadow begin to yield crops. This method consumes a great quantity of water, but is very usefully applied where there is a stream that is charged with mud or silt after every heavy rain. When the surface of the plowed meadow is ready for the water, the canals are laid out, with a fall of not more than one foot in 1,000. Whateveris lostin the fall reduces the area that may be watered. The sods are removed carefully from the surface where the canal is dug, and used, after it is completed, to cover the sides. Being cut into pieces, and the pieces placed here and there upon the sides, the intermediate spaces are sown with seed, and the gaps are soon filled. The distributing furrows are made in a similar manner. These may be made with a plow by turning a furrow-slice, in exactly the line laid out, on the opposite side of the furrow from which the water is to overflow. Fig. 67. Great care is to be exercised in laying out the Fig. 67.-METHOD OF PLOWING THE FURROW. canals and furrows. A builder's level, fixed to the edge of a plank 12 feet in length, of equal width from end to end, having a cross-bar or foot, a foot long, fastened to each end, will make a useful implement for this purpose. One foot being set on the ground in the line of the ditch, the other is moved from one side to the other in the same direction, until the level is found. A peg is driven there to mark the spot, and the level moved further on. It does not require much ingenuity to do this, and any farmer of ordinary intelligence need not fear that he will go wrong if he will only be careful and cautious as he goes along, and takes the precaution to 139 I IRRIGATION. verify his levels by turning the implement, and going back over the line. Many rough, stony, or swampy pieces of ground already in grass, may be improved without disturbing the surface, by thoroughly draining the subsoil and laying out canals without reference to any particular line, but merely causing them to follow the level in a direction meandering to suit the surface. Hollows should be filled up with earth taken from adjoining elevations, the sod being first removed and then replaced. Waste pieces of land, at present a refuge and nursery for weeds of many kinds, and a detraction to the farms to which they belong, may thus be changed at small cost into land of the most productive kind. The irrigation of an irregular surface, such as hill sides, although it may need more careful preparation and adjustment of the levels, is no more difficult than that of a perfect level. In fact, there are advantages in favor of the irregular surface which offset the apparently easier irrigation of a dead level. Drainage is an indispensable adjunct of irrigation, and no land is so frequently drained by iiature as a hill side, or what is known as rolling land. Generally the simplest methods of surface drainage will be sufficient for lands of considerable slope. The cost of thorough underdraining is therefore saved in the case of a meadow of this character. The water supply, and the character of the canals suitable for irregular surfaces, differ in no respect from those already described. It is in the method of distributing the water, and laying out the furrows, that especial direc tions are needed. There are several methods of irrigating lands of this character, which are applicable to our circumstances. Level furrows may be used by which the water is carried in winding directions around the elevations and depressions of the surface, from feeders which are taken from the main supply canal whenever it may be most con 140 LAYING OUT FURROWS. venient. To trace the course of these distributing furrows is very easy, if the common level, already described, is used. The course, as thus laid out, will form a succession of angles, the apex of each of which will be marked by a small peg driven in the ground. To pre Fig. 68.-LAYING OUT FURROWS. vent abrasion of the furrows at these angles, gentle curves are to be made from point to point. These curves will conform exactly to the level of the furrow. Fig. 68 illustrates the method of laying out these curves. If the slope is not so great as to permit washing out of the soil, the feeding canals may be carried straight down it. If the slope is too great for this to be done safely, the feeders will meander in the same manner as the furrows, or Fig. 69.-PFURROWS ON A REGULAR SLOPE. they may be made to follow a diagonal direction across the slope, so as to bring the fall within proper bounds. The meadow will then appear as in fig. 69, in which a, b, are the canals or feeders, and the lateral lines the furrows. But the least troublesome and cheapest'method is by inclined furrows carried in the straight lines across the planes of level, and supplied by feeeders carried either di 141 at -/ -~~~~~~~1 -11 II IRRIGATION. rectly or diagonally down the slope. The furrows branch both to the right and left from the feeders, and have but very little inclination from the level. They are made to diminish in size from the feeder until each disappears in a point at the extremity. Each feeder with its two lateral ranges of furrows thus appears upon the surface in shape like the backbone of a fish, or what is especially known as "herringbone shape." Fig. 70 exhibits a plan of a meadow thus laid out. The slope of the field is from top to bottom. The water is received by a main canal, 6~~~~~~~~~ Fig. 70.-FRows AND DRAINS FOR IRREGRULA SLOPES. ard is diverted into subsidiary canals, A, B, and from them into the feeders, a, a, a, and the furrows which branch from them upon each side. The drains are seen at b, b, b. The course of the water is shown by the arrows. The distance between the feeders should be from 100 to 150 feet, which will make the furrows from 50 to 75 feet long, and the latter should be from 15 to 20 feet apart. These distances will be regulated by the character of the soil as to its porosity or retentiveness. The lower 142 f. I t I STEEP HILLSIDES. extremity of each feeder is closed by a sod or a small gate, and the flow may be regulated or diverted when de sirable by the same means at any part of the channel. The drains are placed midway between each feeder, and receive the surplus water, carrying it off at the foot of the meadow. When the water is in flow, notice is to be taken of any portion of the meadow which does not receive a supply, and a special furrow is to be made to remedy the defect. Drains are not always necessary upon these meadows. If the soil is clay and retentive of moisture, and the slope is slight, they will be indispensable. Where the soil is open and porous, and naturally drained by the subsoil, they may be dispensed with. But attention must be given to so feed the water that it is all used, and not allowed to drown the lower portions of the field. One drain at the foot of the meadow is to be provided in all cases. Another method of irrigation is adapted to very steep hillsides. This is known as the catch-water system. Hillsides so steep that wagons cannot be taken upon them, may be watered by this system. A stream or canal flowing upon the crest of the hill is dammed, or closed temporarily, by means of a gate. The water then flows over the bank, in a sheet more or less perfect, as the bank has been leveled accurately or otherwise. At some distance down the slope, the water that is not absorbed by the soil is caught in a second canal or ditch, which, when full, overflows and spreads the water upon the section below it. The surplus is caught by a lower canal, and spread as before. This is repeated, until either the water is exhausted or the bottom is reached. If the supply is such that economy is to be exercised, the water may be carried into one of the lower canals by an underground spout of wood, and the meadow be watered in successive portions. The section of a field thus watered is shown in fig. 71. a, is the stream, and b, b, the canals, from 143 I IRRIGATION. which the water flows over the intermediate slopes. The canals in this system follow a perfectly level course, and much care is to be exercised to follow the sinuous course of this level across the meadow. A very safe method is to make the lower side of the canal of plank or slips of board, over the edge of which the water will flow without injury to the canal. The cost of this system of irriga Fig.71.-CATCI-WATER FURROWS. tion is frequently not more than $10 per acre. The canals need to be but very small; a furrow that will arrest the flow of water is all that is required, its main office being to restrain the velocity of the water, and to collect it from the numerous streamlets into which it soon gathers, and again spread it in a thin sheet over the whole surface. Where the surface admits of it, a series of slopes and terraces may be made, which can be irrigated upon this system. See fig. 72. In this case, the slopes may be covered with grass, and the intervals cultivated if desired. I Fig. 72.-SLOPES AND TERRACES. The water which flows down the slope is caught in the furrow at the foot, and then passes over the terrace on to the next slope. The furrow at the edge of the terrace is needed to retain the water sufficiently to thoroughly irrigate the soil of the terrace, which would possibly otherwise receive less than its share. In this system of irrigation, when the soil is open and porous and the supply of water limited, it will be necessary to puddle the bottom 144 (L~ 6. I DRAINAGE. of the canals to prevent loss of water. It may be that the cheapest plan would be to make the bottom and lower side of the canal of boards. In this case, a board of 14 inches in with would form the bottom of the canal, and one of 8 inches the lower side. A canal of this capacity would convey water enough for several acres, and would not be more costly than to puddle or cement the bottom, when clay is not readily at hand. CHAP T ER XIV. DRAINAGE OF IRRIGATED FIELDS. The absolute necessity of water to vegetable growth must not be accepted in an unqualified sense. Water is a good and necessary thing, but there may be too much of it, and too much is as fatal to the profitable culture of land as too little. As the circulation of air brings life and vigor to the lungs of an animal, so the circulation of water brings vitality to the roots of a plant. Stagnant water is as fatal to plant growth as stagnant air is to the health and well-being of animals. Therefore irrigation cannot be successfully used without adequate drainage. Sometimes this is naturally provided. Light soils, with gravelly subsoils, may permit the passage of water through them with facility, acting as filters to retain all its fertilizing qualities. Such lands are the most readily adapted to irrigation, and any artificial provision for carrying off the water from them is unnecessary. But there are many lands with retentive surface or subsoil, and others with subsoil practically impermeable to water, that if brought under irrigation must be thoroughly drained, or they will be injured instead of improved, and the charac 7 145 IRRIGATIOn. ter of the vegetation they bear be totally changed. An undrained meadow may be thus, by irrigation, changed into a marsh, and good, though scanty grass be replaced by useless marsh sedges and rushes. Sloping lands may need drainage as much as level lands. Hillsides that have been brought under irrigation, have sometimes discharged their surplus waters at a lower level, where they have gathered and changed a portion of the surface into a quagmire, until drains have been constructed to remedy the evil. Again, there are cases in which, by a judicious system of drains, a swamp may be reclaimed, and the water, which had been previously a hindrance to cultivation, may be gathered into ditches and used to irrigate a meadow, and yield bounteous crops. Such a case, which actually occurred, may be profitably described. It was a :ill-side of fertile clay soil, resting upon a clay slate, from which the soil of a level flat at its foot had been originally derived. Abundant springs broke out upon the hill-side, and after forming marshy spots around them,they disappeared until they again broke out at the foot of the hill, where they gathered and formed a dangerous and impassable swamp. Here were 30 acres of land rendered worthless, and a dangerous trap for any stock that might be tempted to trespass upon its treacherous surface. Hundreds of similar tracts exist where there are -hills and valleys. The reclamation of this tract was a very simple matter. Its outlines are shown at figure 73. A drain was cut near the foot of the hill. See a. It was necessary to take this drain to a depth of seven feet before the heaviest springs were cut. At this depth, a flow of water was reached which nearly filled the ditch, and furnished a large stream. The drain was placed, with a view to irrigation of the meadow, a few feet above the level of the flat. It then formed a supply canal from which the flat 146 II I. I.1 I IUSE OF DRAINAGE WATER. could be irrigated by means of shallow ditches which led to lateral furrows diverging on each side of the ditches. The surplus water escaped from the foot of the meadow over the bank into a stream, b. The plan of the meadow Fig. 73.-SECTION OF A D)RAINED HILL AND IRRIOATED FLAT. is shown at fig. 74. A being the hill; a, a, the drain, from which the ditches and furrows are led down to the stream, b, b, at the foot. By closing the shallow ditches the water could be backed up over the meadow or thrown into lateral ditches. None of these ditches were deep enough to obstruct a mowing machine. It only required ) z('U cc 1I; a1. i vI e - 0 ---,, 7lg. 74.-PLAN OF THE DRAIN AF!rQWS, the labor of two men fQr three months, and the lapse of two yesrs' time to ponvert this 30 Pcres into a dry, arable helm l 1. ha iUnd a. meadow of 18 acres, which was covered with grass and clover where, in former yea -- mired and smothered in mu,. 1 I .!I 147 ti~ b 11'X \I,0l'l cc I ? IRRIGATION. It is not the purpose here to treat of drainage with reference to itself alone, but only so far as it maybe used in connection with, or as an adjunct to, irrigation. Drainage may be superficial or subterranean. Superficial, or surface drainage, is the simplest. Nothing is needed for its practice but to provide open channels into which the surplus surface water may find its way. As a matter of necessity, these to be perfect must be placed at the lowest levels of the ground to be drained. Besides, they need to be placed in such relation to the distributing furrows of the irrigating system, as to catch the water as soon as it has completely accomplished its purpose, and remove it in the most effective manner. Sufficient description of needed methods has already been given, to make clear the means of doing this. For subterranean, or subsoil drainage, much more elaborate and costly methods are necessary. Not only must expensive ditches be made, and earthen tiles be used, but the arrangement of the drains, with reference to the irrigating ditches or furrows, must be carefully made. No drain should exist immediately beneath an irrigating ditch, canal or furrow, for the reason that excavated earth cannot be so returned as to be as compact as it laid before. If then a water channel passes across, or along a line of earth, that has been disturbed, a rapid infiltration occurs, the water makes itself a channel, which is rapidly enlarged; sand or earth is carried into the drains, and the water not only escapes without doing its work, but chokes the drains in a short time. Thus no drain should be made nearer to an irrigating furrow, or canal, than six feet, and no irrigating furrow should terminate at a less distance from the line of a drain, than six feet. The usual arrangement of drains and furrows is shown at figure 75. Here A, A, is the main canal; A, B, A, C, the feeders, with the lateral distributing canals or furrows; a, the main drain, which discharges into the 148 I II 4 I .i FLUISHIIG DRAINS. outlet, and c, c, are the small collecting drains. The small drains follow the direction of the greatest slope of the ground. The system of drains to be adopted will, in all cases, conform to that of the system of canals and furrows. When in perfection the drainage system will be an exact counterpart of that of the irrigation, and so devised as to carry off the water after its service has been performed, and to A l c c Fig. 75.-MA ER OF SUB-DRAINING AN IRRIGATED MEADOW. cause it to circulate completely through every portion of the soil occupied by the roots of the grass, after it has been spread completely over the surface. The construction of the drains is in no wise different from that of ordinary tile drains, and therefore needs no description here. It is sometimes found of great service, consequent upon the frequency with which sand or earthy sediment is carried into the drains, to provide a method of flooding and flushing them. This is called intermittent drainage. It is applied also very advantageously to fields that are subjected to intermittent irrigation, or irrigation by suc I .I i 149 0 d 0 1 CL a IRRIGATION. cessive portions. It consists in supplying an earthen or wooden pipe, which is set perpendicularly in the ground in the line of the main drain, so that the main drain pipe enters it upon one side, and leaves it upon the other. This pipe thus cuts the main drain at such intervals as may be desirable. It is covered by a cap, and is reached through a covered trap or box, placed on a level with the surface of the ground. This is seen at fig. 76. The proper situations for these pipes are just below the junc tion of a series of lateral drains, "~a as at d, d, in fig. 75. These pipes offer facilities for closing the drain by means of simple Ei~ g acontrivances. The most ef fective of these is a plug or cushion of wood, which fits ... in the drain leading from ...... the pipe or well. This plug is fastened horizontally to Fig. 76.-PLUG ]!OR CLOSING the lower portion of the T DRAIN. shaped arm. One of the upper cross parts of the T is fixed into a hole or groove in the pipe or well, and a wire is fastened to the other cross part. When the wire is pulled, it moves the lower portion of the T laterally, and draws the plug from the opening of the drain pipe. When the wire is released, the weight of the arm of the T carries the plug to its place again, or the force of the water flowing through the drain carries it and holds it there. This is shown in fig. 76, in which A, B, is the drain pipe; a, the box or trap by which the wire is reached; b, the plug with its movable arm, from which a copper wire is carried to the upper box, where it is secured by a ring upon a hook. The operation of the contrivance is as follows: When the drain is closed and the flow is stopped, all the drains 150 i i i ~ Ii METHODS OF FLUSHING. above the obstacle are charged with water. Water also accumulates in the subsoil and soil, and in fact the whole portion of the field under the influence of the drains, becomes filled with water as completely as may be desired. At any time when the drain may be opened, there is a rush of water through the drains, by which any sediment is effectively carried away, and the drains left free and clear. The operation may be repeated upon each division of the field consecutively from the foot upwards. Instead of the plug above described, an iron rod, having a curved sheet of zinc, or tinned or galvanized iron, attached to the end, see fig. 77, may be used. The curved sheet reaches quite round the well, and when drawn up opens the drain, but when pushed to the bottom, Fig 77-A CURVED DRAIN-STOPPER. closes it. If the well is square, a slide DR-TOPPE made to move in grooves may be used to close the drain. The simpler the method, the less risk there is in its use; but the need of permanence of structure is obvious, for if it gets out of order, nothing remains but to take up the well and replace it. Whatever system of drainage is adopted, is immaterial, if the main points here touched upon are provided for. It must not be forgotten, however, that drainage is indispensable, and that except under rare circumstances, thorough subsoil drainage only will be sufficient to meet all the requirements of the case; and that surface drainage may be an unsatisfactory makeshift for the more perfect method. The size of tile used, is one inch for the small drain, two inches for the laterals, and three or four inches, or even larger than that, for the main drains. The size of the main drains should bear a proper propor 151 i i IRRIGATION. tion to the quantity of water admitted to the field, and it may be that the discharge drain, into which the main drains enter, may need to be six or eight inches in diameter. This question, as to the size of tile, will need careful consideration, because if the size is insufficient, the flow will be retarded, with the inevitable result of sediment and choked drains. As a general rule, the main pipes for irrigated meadows should be twice as large as those used for ordinary drains, as the excess of surplus water at times may be very large. Any system of pipes, that is not equal to the most exacting emergency, will be insufficient, and calculations must be made to meet such an emergency. Before any large expenditure of money or labor is made in laying down drains, which once laid, admit of no remedy except total undoing of the work and relaying the pipes, it would be judicious to consult a capable civil engineer, who could readily make safe calculations as to the size of pipe, the position of the drains, and the number required. CaHAPTER XV MANAGEMENT OF IRRIGATED FIELDS. When a field has been successfully irrigated and drained at great expense, it may be seriously injured for want of proper management. To care properly for an irrigated meadow calls for the exercise of tact and skill of no mean character. A few general rules may be laid down for the proper management of irrigated meadows, which will serve to meet the majority of cases, and by modifications of which exceptional cases may be met. The point of chief importance is to avoid pasturing. No hoof should be permitted upon a completely irrigated meadow, unless it be, under certain restrictions, those of sheep. Sheep 152 i t II PASTURING. may be allowed to pasture such a meadow after the last crop of hay has been made, and a sufficient interval has elapsed to thoroughly dry the ground and give the grass a start again. There is no better or cheaper way to fertilize a meadow than this. But if heavy rains occur, the flock should be removed at once, and not admitted until the ground is dry again. Where a tough, thick sod covers the ground, greater latitude may be permitted. There are irrigated meadows in parts of England which possess a sod so dense, and such a heavy growth of grass, that one acre inclosed with hurdles is the regular daily r... _ X ~/ ~'J // \\ C. // Cow *;