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
_Mode of using Saline Irrigation Waters._—The fact that abundant
growths of native as well as cultivated plants may sometimes be seen
on the margins of “alkali lakes” where water of over a hundred grains
of mineral salts per gallon continuously bathes the roots, while the
same plants perish at some distance from the water’s edge, points the
way to the utilization, in emergencies, of fairly strong saline waters;
viz., by the prevention of their concentration to the point of injury
_by evaporation_. It is clear that when such waters are used sparingly,
so as to penetrate but a few feet underground, whence the moisture
re-ascends for evaporation at the surface, a few repetitions of its
use will accumulate so much alkali near the surface as to bring about
serious injury. If, on the other hand, the water is used so abundantly
that the roots may be considered as being, like the marginal vegetation
of alkali lakes, bathed only by water of moderate strength, no such
injury need occur; and what does accumulate in consequence of the
inevitable measure of evaporation occurring in the course of a season,
may be washed out of the land by _copious winter irrigation_.
This, of course, presupposes that the land, as is mostly the case
in the arid region, is readily drained downwards when a sufficiency
of water is used. When this is not the case, _e. g._, in clay or
adobe soils, or in those underlaid by hardpan, waters which in sandy
lands could have been used with impunity, may become inapplicable to
irrigation use.
_Apparent Paradox._—The prescription to use saline waters _more
abundantly_ than purer ones, in order to avoid injury from alkali,
though paradoxical at first sight, is therefore plainly justified by
common sense as well as by experience, in pervious (sandy) soils;
while in difficultly permeable ones, their use may be either wholly
impracticable, or subject to very close limitation.
Sometimes the alternate use of pure and salt-charged water serves to
eke out a too scant supply of the former. But in all such cases, close
attention to the _measure_ of water that will wet the soil to a certain
depth, and “eternal vigilance” with respect to the accumulation of
alkali near the surface, must be the price of immunity from injury. In
all cases the farmer should know how much of alkali salts he introduces
into his land with the irrigation water, and watch that it does not
approach too closely, or exceed, the tolerance of his crops for alkali
salts, as given in chapter 26.
Public-domain text, read in full here on John Shaqi.
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