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
In the case of native annuals, either the duration of their vegetation
is extremely short, ending with or shortly after the cessation of
rains; or else their tap roots descend so low, and the nutritive
rootlets are developed at such depth, as to be beyond reach of the
summer’s heat and drought. For while it is true that rootlets immersed
in air-dry soil may absorb plant-food, this absorption is very slow
and can only be auxiliary to the main root system which, instead of
terminating in the surface soil as in the humid region, will be found
to begin to branch off at depths of 15 and 18 inches, and may then in
sandy lands descend to from 4 to 7 feet even in the case of annual
fibrous-rooted plants like wheat and barley.[64] In the case of maize
the roots of a late-planted crop may sometimes be found descending
along the walls of the sun-cracks in heavy clay land poorly cultivated;
and it frequently matures a crop without the aid of a single shower
after planting. See figures 33, 34.
[64] Shaler (Origin and Nature of Soils; 12th Rept. U. S. Geol.
Survey, p. 311) says: “Annual plants cannot in their brief period of
growth push their roots more than six to twelve inches below their
root-crowns”—a generalization measurably true for the humid region
only. According to F. J. Alway, the roots of cereals penetrate to 5-7
feet in Saskatchewan, also.
[Illustration: FIG. 31.—Hop Root from Sacramento Bench-land.]
The annexed plate (No. 32) shows the main roots of two native perennial
weeds of California, the goosefoot (_Chenopodium californicum_) and the
figwort (_Scrophularia californica_), common on the lower slopes of the
coast ranges. The soil was a heavy clay loam or “black adobe” resulting
from the weathering of the clay shale bedrock, fragments of which are
so abundantly intermixed with the substrata that excavation of the
roots became very difficult. Yet the main root of the goosefoot went
down below the depth of eleven feet.
The main root of the figwort, also, was followed below the depth of ten
feet without reaching the extreme end. This proves clearly that the
great penetration of the goosefoot was not, as might be supposed, due
to its bulbous root. Yet such thickening of the root just below the
crown is a rather common feature in arid-region plants, and can here be
noted even in the figwort, within whose botanical relationship bulbous
roots are almost unknown.
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