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
_Moisture supplied by tap roots._—In most cases, sandy lands do not
require underdraining; and in them, root-penetration may reach to
extraordinary depths in the case of certain plants, especially when
taprooted. Thus the roots of alfalfa (lucern) are very commonly found
to reach depths of twenty to twenty-five feet, and even sixty feet has
been credibly reported for the same plant in the arid region. It is
obvious that for such plants, a high level of bottom water is wholly
undesirable, since they are enabled to obtain their moisture supply
from great depths, and can thus utilize for their nutrition much larger
soil-masses than can shallow-rooted plants.
_Reserve of Capillary Water._—It must be remembered that it is not
only, nor usually, the bottom water that supplies moisture to plant
growth; for all soils of proper texture for cultivation retain within
them a certain amount of capillary moisture after the ground water has
reached its permanent level (see this chap. p. 226), and when the tap
or main roots are plentifully supplied with water, the upper and chief
feeding roots draw but lightly upon the moisture within their immediate
reach for the purpose of leaf evaporation. This fact can be plainly
observed in the arid region, when on the advent of the summer drought,
young plantlets whose tap roots have reached a certain depth continue
to flourish and develop, while others practically of the same age, but
slightly behind, quickly succumb, though the _feeding_ roots of both
may draw upon the same soil layer. It is especially in sandy soils that
moisture is naturally thus conserved in the upper layers, because of
the failure of the water to rise by capillary ascent so as to evaporate
from the surface layer. It is often surprising to find a good amount
of moisture in the sandy soils of desert regions at the depth of eight
or ten inches, when the surface is so hot as to scorch the fingers;
and this moisture continues very uniformly to great depths, probably
to bottom water lying twenty or more feet below the surface, which in
such materials may readily be reached by taprooted plants such as the
“sagebrush” (Artemisia tridentata), the saltbushes (Atriplex) and
others.
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