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
[76] Ad. Mayer (Agriculturchemie 2, p. 141) designates this minimum
content of liquid water as the “absolute” water capacity of the same;
but it is not obvious wherein this factor is better entitled to this
name than would be the maximum (see Wollny’s Forsch., 1892, p. 1.). M.
Whitney (Rep. Proceedings Ass’n Agr. Coll. & Exp’t St’ns, Nov. 1904)
gives as a new observation the fact that in soils approaching the
drought condition water “does not obey the ordinary physical laws as
we recognize them in capillarity.” This evidently refers simply to the
well-known phenomenon mentioned above.
_Capillary Water held at Different Heights in a Soil Column._—To
determine the amounts of water held in the different portions in
columns of soils in which water ascends by capillary rise, the
following plan was adopted by the writer in collaboration with
Loughridge (Rep. Calif. Sta. 1892-4, p. 99).
Instead of glass tubes the soils to be tested were placed in copper
tubes one inch in diameter, divided into segments six inches long,
and flattened on one side. In the flattened side a slot half an inch
wide was left, and glass plates, held in position by rubber elastics,
were cemented on the slotted side by means of paraffin, to prevent a
sifting-out of the soil. The short sections can be connected at the
ends like joints of stove-pipe, and the earths can be easily introduced
in proper, even condition. It was thus possible to gain access to any
portion of the column at any time, for the taking of samples.
WATER CONTENTS OF SOIL COLUMNS AT VARIOUS HEIGHTS
ABOVE WATER LEVEL.
==================+===========+===============+================
No. | 233 | 1197 | 1679
------------------+-----------+---------------+----------------
Height above Water|Sandy Soil,|Sandy Alluvium,|Adobe, Berkeley.
Level. | Morano. | Gila. |
------------------+-----------+---------------+----------------
47 inches | | 4.33 |
42 inches | | 10.26 |
36 inches | | 11.99 |
30 inches | | 15.26 |
24 inches | | 21.39 | 10.26[77]
18 inches | | 27.63 | 29.48
12 inches | 3.93 | 32.48 | 33.04
6 inches | 14.15 | 35.04 | 38.47
3 inches | | | 38.49
1 inch | 24.34 | 36.64 | 44.41
------------------+-----------+---------------+----------------
[77] This figure represents only a temporary condition; the full height
of 46 inches was not reached until the 195th day.
Public-domain text, read in full here on John Shaqi.
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