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
Thus while in some very pervious land furrows may be six
or even eight feet apart, in other cases, in certain
finely pulverulent or silty soils such as the “dust soils”
described in a former chapter; (see chapter 6, p. 104),
furrows drawn three feet apart may fail to allow the water
to penetrate so as to prevent grain on the middle foot
from suffering from drought after the water has run for
twenty-four hours.
_Irrigation by lateral Seepage._—Is in reality a mere modification
of furrow irrigation, practiced in the case of lands very readily
permeable, and where water is abundant. The fields are laid off in
“lands” twelve to twenty-five feet wide, with a deep furrow or narrow
ditch between, from which water percolates in a short time so as to
overlap from the two sides. In this case sometimes the water does not
reach the surface visibly at all; a very great advantage where alkali
exists, as surface evaporation, and the consequent accumulation of
alkali, is thus effectually prevented; while deep-rooting is favored to
the utmost.
_Basin Irrigation._—In this method of irrigation, practiced only in
the case of trees and sometimes vines, and when water is scarce, a
wide circular furrow or basin is excavated around each trunk and water
is run either from one to the other, or sideways from a furrow laid
along the rows. The water thus applied of course percolates immediately
around the trunk first, and in practice is found to follow also the
large roots; so that it goes precisely where it is most wanted, besides
forming a vertical body of moist soil reaching to considerable depth,
where it is most desirable that the root system should follow. By
this deep penetration to natural moisture in the depths of the soil,
comparatively small quantities of water produce very marked effects.
On the same principle, the grape vines which bear some of the choicest
raisins of Malaga on the arid coastward slopes, are made to supply
themselves with moisture, without irrigation, by opening around them
large, funnel-shaped pits, which remain open in winter so as to catch
the rain, causing it to penetrate downward along the taproot of the
vine, in clay shale quite similar to that of the California Coast
Ranges, and like the latter almost vertically on edge. Yet on these
same slopes scarcely any natural vegetation now finds a foothold.
Similarly the “ryats” of parts of India water their crops by applying
to each plant immediately around the stem such scanty measure of the
precious fluid as they have taken from wells, often of considerable
depth, which form their only source of water-supply. Perhaps in
imitation of these, an industrious farmer has practiced a similar
system on the high benches of Kern River, California, and has
successfully grown excellent fruit for years, on land that would
originally grow nothing but cactus. Sub-irrigation from pipes has been
applied in a similar manner.
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