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
The results produced by long-continued shallow plowing and irrigation
in shallow furrows is well illustrated in the last of the irrigation
profiles, which shows the observations made on the same land as the
others, but where rational cultivation and deep-furrow irrigation
had not yet been introduced. It will be seen that after applying,
and of course paying for, the water for three days, its average
penetration was only about eighteen inches; so that the trees of the
orchard received very little benefit, and were supposed to be needing
fertilization when in fact they were simply suffering from lack of
water at the lower roots.
One somewhat unexpected point is shown by these diagrams, viz., the
slight sidewise penetration of the water; the wetted areas having a
nearly vertical lateral outline. This means, of course, that unless the
furrows run very near the trees of an orchard, the soil immediately
beneath the trees will remain dry; thus inducing the roots to spread
sideways and losing depth of penetration and soil. It will be noted
especially in the lower figure that here again the deep furrow offers
a material advantage over the shallow, the sidewise spread being much
more pronounced than in the shallow furrow alongside.
_Distance Between Furrows and Ditches._—The distance between the
furrows must, of course, be proportioned to the readiness with which
the water penetrates, being less as the land is of closer texture.
The distance between head ditches must, on the contrary, vary in
the opposite sense, since if these are too far apart, the water near
the head ditch will in sandy lands be wasting into the subdrainage
before the end of the furrows is reached; so that the distribution
will be very uneven. The great differences observed between crops, and
especially trees, _below_ and _above_ the head ditches, are mainly due
to this unevenness in water distribution, caused by too great distance
between successive head ditches. Each farmer must himself, however,
determine by actual trial the proper distances between ditches as well
as furrows, for his particular case; since everything depends upon the
rapidity with which water will penetrate the soil and subsoil. Actual
tests to determine this point[91] should be the first step, before
laying off the system of ditches as well as furrows. It not uncommonly
happens that the failure to do this at first, compels a subsequent
total change of arrangements in this respect. (See page 253 below).
[91] Such tests can be readily made by any one, by digging a pit to
four or five feet depth, and supplying water to a shallow basin dug
into the surface 8 to 12 inches distant from the vertical wall of the
pit. The descent of the water is then readily observed on the vertical
side of the pit nearest to the water basin. Preliminary tests with soil
probe (see chap. 10, p. 177).
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