The Story of the Soil; from the Basis of Absolute Science and Real LifeHopkins, Cyril G. (Cyril George)
Science
The Story of the Soil; from the Basis of Absolute Science and Real Life
Hopkins, Cyril G. (Cyril George)
Soils
"Yes, that is the rule under general or average conditions, but it
should be stated that the amount of sulfur required by plants is
very small as compared with phosphorus, a difference which places a
great distinction between them. Besides considerable quantities of
sulfur are returned to the air in the combustion of coal and organic
matter, and this returns to the soil in rain. The information thus
far secured shows that sulfur rarely if ever limits the crop yields
under field conditions; and the same may be said of iron, which is
required by plants in very small amount and is contained in
practically all soils in enormous quantities.
"While normal soils contain abundance of potassium, with about half
as much calcium and one-fourth as much magnesium; yet, when measured
by crop requirements for plant food, the supplies of these three
elements are not markedly different. On the other hand, about 300
pounds of calcium are lost per acre per annum by leaching from good
soils in humid climates, compared with about 10 pounds of potasssium
and intermediate amounts of magnesium; so that, of these three
elements, calcium requires by far the most consideration and
potassium the least, even aside from the use of limestone to correct
or prevent soil acidity.
"Among the conditions essential for nitrification may be mentioned
the presence of free oxygen and limestone; and of course all
bacteria require certain food materials, resembling other plants in
this respect."
"Are they plants?" asked Mrs. Thornton. "I thought they were tiny
little animals."
"No, they are classified as plants," replied Percy; "but the
scientists have difficulty with some of the lower organism to decide
whether they are plants or animals. The college boys used to say
that some animals were plants in the botanical department and
animals again when they studied zoology. Orton says it is easy to
tell a cow from a cabbage, but impossible to assign any absolute,
distinctive character which will divide animal life from plant life.
"The oxygen is essential for nitrification, because that is an
oxidation process. That is, it is a kind of combustion, so to speak.
The organic matter is oxidized or converted into substances
containing more oxygen than in the original form. In ammonification
the carbon is separated or divorced from the nitrogen and united
with oxygen. Some of the hydrogen of the organic matter remains
temporarily with the carbon, and some is held temporarily with the
nitrogen in the form of ammonia.
"The nitrite bacteria replace two of the hydrogen atoms in ammonia
with one of oxygen, and insert another oxygen atom between the
nitrogen and the remaining hydrogen, thus forming nitrous acid;
H-O-N=O, or HNO2.
"The nitrate bacteria then cause the direct addition of another
oxygen atom, which is held by the two extra bonds of the nitrogen
atom, which you will remember is a five-handed atom.
Public-domain text, read in full here on John Shaqi.
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