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
(S) = 10 Sacramento. Sacramento Co.
(T) = 506 Gila. San Diego Co.
(Z) = Hygroscopic Moisture (+7 = to +21°C)
===========+==================
| CALIFORNIA.
+------------------
Designation | River Deposit.
of +---------+--------
Materials. | |
| (S) | (T)
| |
-----------+---------+--------
Grit | |
| |
{ | |
{ | | .13
Sand { | | .15
{ | | .11
{ | .32 | .75
| |
{ | 3.16 | 2.51
{ | 10.27 | 8.32
Silt { | 13.67 | 12.64
{ | 13.11 | 11.28
{ | } 43.61 | } 31.79
{ | } | }
| |
Clay | 12.06 | 23.97
+---------+--------
| 96.20 | 91.71
| |
(Z) | 9.18 | 9.26
Ferric Oxid | |
-----------+---------+--------
_Number of soil grains per gram._—It is of some interest to consider
the number of grains of different sizes that may be contained in, _e.
g._, a gram of soil. If for this purpose we assume all the soil grains
to be spherical, we shall obtain the minimum figures, for most other
shapes will pack more closely. King (Physics of Agriculture, p. 117)
calculates such figures for different grain-sizes, assuming the density
to be that of quartz (2.65), with the result that while with a diameter
of one millimeter (1-25 inch) the number of grains would be 720, and
with one-tenth of a mm. 720,000; if made of the finest particles only,
viz., one thousandth of a mm., the number would be 720,000 billions.
Probably few of the clayey soils we ordinarily deal with are of this
order; it is doubtless approached in certain fine plastic clays.
_Surface afforded by various grain-sizes._—The amount of _surface_
afforded by a similar amount of soil must naturally be considered in
this connection, since upon it depends not only the amount of moisture
which the soil may hold in the form of superficial films, but also the
extent of surface upon which the weathering agencies as well as the
root hairs of plants may act. Quoting again from King’s work, we find
on the same premises given above for the _number_ of grains, that their
_surface_ would in the case of grains of one mm. diameter be eleven
square feet per pound (about half a pint) of material; while in the
case of the finest grade we should have 110,538 square feet, or more
than two and a half acres.
Public-domain text, read in full here on John Shaqi.
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