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
It must not be forgotten that there are in the lowlands of the arid
region (river swamps or tules, sea-coast marshes, etc.,) soils in which
surface soil and subsoil are differentiated as fully as in the humid
countries; at least so long as they have not been fully drained for a
considerable length of time. In swamp areas that have been elevated
above the reach of overflow or shallow bottom-water by geological
agencies, even the heavy swamp clays are fully aerated down to great
depths, and roots penetrate accordingly.
_Examples of Plant-growth on Arid Subsoils._—The fact that in the arid
region the surface-soil conditions reach to so much greater depths
than in the East and in Europe, is so important for farming practice
in that region that experimental evidence of the same should not be
withheld. Of such, some cases well established as typical of California
experience are therefore cited.
It is well known that in the Sierra Nevada of California
the placer mines of the Foothills, worked in the early
times, have long disappeared from sight, having been quickly
covered by a growth of the bull pine (_P. ponderosa_).
Much of this timber growth has for a number of years past
been of sufficient size to be used for timbering in mines,
and a second young forest is springing up on what was
originally the red earth of the placer mines, which appears
to the eye as hopelessly barren as the sands of the desert.
In this same red sandy earth not unfrequently cellars and
house foundations are dug, and the material removed, even to
the depth of eight feet, is fearlessly put on the garden and
there serves as a new soil, on which vegetables and small
fruits grow, the first year, as well as ever. In preparing
such land for irrigation by leveling or terracing no heed is
taken of the surface soil as against the subsoil, even where
the latter must be removed to the depth of several feet, so
long as a sufficient depth of soil material remains above
the bedrock.
Public-domain text, read in full here on John Shaqi.
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