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
_Shattering of Dense Substrata by Dynamite._—The permanent loosening
of dense substrata is best accomplished by moderate charges (½ to
¾ pounds) of “No. 2” dynamite at a sufficient depth (3 to 5 feet).
The shattering effect of the explosive will be sensible to the depth
of eight feet or more, and will fissure the clay or hardpan to a
corresponding extent sidewise. If properly proportioned the charge
will hardly disturb the surface; but if this be desired, from 1½ to
2½ pounds of black powder placed above the dynamite will throw out
sufficient earth to plant the tree without farther digging. Where labor
is high-priced this proves the cheapest as well as the best way to
prepare such ground for tree planting; and it has often been found that
in the course of time, the loosening begun by the powder has extended
through the mass of the land so as to permit the roots to utilize it
fully, and even to permit, in after years, of the planting of field
crops where formerly they would not succeed.
_Leachy Substrata._—While we may thus overcome the disadvantages of a
dense subsoil or hardpan, there is another difficulty not uncommonly
met with in alluvial lands, which cannot be so readily remedied. It
is the occurrence, at from two to six feet depth, of coarse sand or
gravel, through which capillary moisture will not ascend, but through
which irrigation water will waste rapidly, leaving the overlying soil
dry. Then unless very frequent irrigation can be given, the crop will
suffer from drought, unless indeed the gravel itself is filled with
bottom water upon which the root-ends can draw.
This case is a common one in the larger valleys of the arid region, and
in time of unusual drought the sloughs originally existing, but since
filled up, will be clearly outlined by the dying crops, while outside
of the old channels there may be no suffering.
_“Going-back” of Orchards._ On such land as this, and on such as has a
shallow soil underlaid by an impervious subsoil, trees will often grow
finely for three to five years; then suddenly languish, or turn yellow
and die, as the demand of their larger growth exceeds what moisture or
plant-food the shallow soil and subsoil can supply. Enormous losses
have arisen from this cause in many portions of the arid region, but
more especially in California, owing to the implicit confidence reposed
even by old settlers, and still more by newcomers, in the excellence
of the lands, as illustrated by farms perhaps a short distance away,
but differently situated with respect to the country drainage and the
geological formations. All such disappointments could have been avoided
by an intelligent observation of the substrata, either by probing or
digging. Important as is such preliminary examination in the region of
summer rains, it is a _vitally_ needful precaution in the arid region,
where the margin between adequate and inadequate depth of soil and
moisture-supply is much smaller.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account