Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
[95] Bull. Arizona Exp’t Station Nos. 2, 38.
These variations in the character of the irrigation water must of
course be watched by the farmer who does not receive directly from
mountain streams, or from deep artesian wells water known to have a
constant content of saline matter.
THE DUTY OF IRRIGATION WATER.—The amount of water thought to be needed
for the production of satisfactory crops varies widely in different
regions, ranging all the way from about two feet to as much as eight
annually, within the United States; while in the sugar-cane fields
of the Hawaiian Islands as much as three inches per week, or over
twelve acre-feet in the course of the year, have been thought to be
beneficial, if not absolutely required for the best crop results.
As has been stated above (chap. 12, p. 215), the rainfall limit below
which irrigation becomes, if not absolutely essential, at least a
highly desirable condition for the safety of crops, is usually assumed
to lie at about 20 inches (500 milimeters). This general statement
is, however, subject to material modification according to the manner
in which the rainfall is distributed. Thus in central Montana with 24
inches of rainfall distributed throughout the year, irrigation is
indispensable; while in the Santa Clara valley of central California,
with an average rainfall of 15 inches falling through the winter and
spring, the growth of all ordinary field crops has for fifty years
not failed oftener than is commonly the case in the humid region of
the North Central states. This is because in California the winter
and spring are the growing seasons, while the rainless summers do not
stand in the way, for crops are already harvested; and the deep rooting
of trees and vines provides these with the needful moisture from the
depths of the substrata (see chap. 10, pp. 163 to 173).
It would thus seem that twenty inches of irrigation water properly
applied ought to be sufficient for all purposes, when added to the
natural rainfall, which is rarely entirely absent. Yet in actual
practice less than 24 acre-inches is rarely used, and much more is
the rule; 72 to 96 ins. being sometimes used in Arizona. Evidently
enormous losses occur in practice, and it is of the utmost importance
to discover the causes of these.
_Causes of Loss._—Since irrigation water is commonly measured at the
distributing weirs, loss from seepage and evaporation on the way to the
fields is an obvious source of an overestimate of the water actually
supplied to the farmer. In sandy districts the loss thus incurred is
reliably estimated at nearly 50% in many cases. The apparent duty of
the water is thus at once reduced to half its effect, and four instead
of two feet of water are supposed to have been used, and are charged
for.
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