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
================================+============+=========+========
| “ROTTEN | SUBSOIL | SOIL
|LIMESTONE.” |(YELLOW).|(BLACK).
--------------------------------+------------+---------+--------
FINE EARTH. |Depth 12 ft.| 2-3 ft. |15 ins.
Chemical analysis of fine earth.| | |
--------------------------------+------------+---------+--------
Insoluble matter | 10.90 | 71.54 | 78.29
Soluble silica | | |
Potash (K₂O) | .25 | .54 | .33
Soda (Na₂O) | .32 | .23 | .08
Lime (CaO) | 45.79 | 1.08 | 1.37
Magnesia (MgO) | .88 | .77 | .36
Br. Ox., of Manganese (Mn₃O₄) | | .05 | .14
Peroxide of Iron (FeO) | 1.42 | 5.42 | }
Alumina (Al₂O₃) | 1.96 | 13.15 | } 14.22
Phosphoric Acid (P₂O₅) | | .05 | .10
Sulfuric Acid (SO₃) | | .04 | .03
Carbonic Acid (CO₂) | 35.73 | |
Water and Organic matter | 2.84 | 6.99 | 5.75
| ------ | ----- | ------
Total | 100.09 | 99.86 | 100.67
| | |
Humus | | | 1.93
“ Ash | | | 4.38
Hygroscopic moisture | | 10.35 | 12.82
absorbed at °C | | 19° | 19°
--------------------------------+------------+---------+--------
It appears from the above table that in the change from the original
limestone to the soil mass as found at three feet depth, 81.5% of the
lime carbonate has been eliminated by leaching, leaving behind somewhat
less than one fifth of the original mass. Taking the average depth of
the soil mass at 8 feet, this thickness of material has required about
45 feet of the rotten limestone. Considering that notwithstanding the
tenacity of the clay soil, some of it must in the course of time have
been washed away, we may safely assume that the original rock surface
was from 50 to 60 feet higher than at present.
Public-domain text, read in full here on John Shaqi.
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