The Principles of Chemistry, Volume IIMendeleyev, Dmitry Ivanovich
Science
The Principles of Chemistry, Volume II
Mendeleyev, Dmitry Ivanovich
Argon; Chemistry; Periodic law
so important for a knowledge of the natural conditions for the
application of fertilisers, belongs, strictly speaking, to the
province of agriculture. In Russia the first foundation of a
scientific fertilisation has been laid by Dokuchaeff. As an
example only, we will give the composition of four soils; (1) The
black earth of the Simbirsk Government; (2) a clay soil from the
Smolensk Government; (3) a more sandy soil from the Moscow
Government; and (4) a peaty soil from near St. Petersburg. These
analyses were made in the laboratory of the St. Petersburg
University about 1860, in connection with experiments on
fertilisation (conducted by me) by the Imperial Free Economical
Society. 10,000 grams of air-dried soil contain the following
quantities (in grams) of substances capable of dissolving in
acids, and of serving for the nourishment of plants.
(1) (2) (3) (4)
Na_{2}O 11 5 4 4
K_{2}O 58 10 7 5
MgO 92 33 19 7
CaO 134 17 14 11
P_{2}O_{5} 7 1 7 3
N 44 11 13 16
S 13 7 7 6
Fe_{2}O_{3} 341 155 111 46
By chemical and mechanical analysis, the chief component parts per
100 parts of air-dried soil are
Clay 46 29 12 10
Sand 40 67 86 84
Organic matter 3·7 1·7 0·6 4·1
Hygroscopic water 6·3 1·3 0·8 1·9
Weight of a litre in grams 1150 1270 1350 960
The black earth excels the other soils in many respects, but
naturally its stores are also exhausted by cultivation if nothing
be returned to it in the form of fertilisers; and the improvement
of a soil (for instance, by the addition of marl or peat, and by
drainage and watering), and its fertilisation, if carried on in
conformity with its composition and with the properties of the
plants to be cultivated, are capable of rendering not only every
soil fit for cultivation, but also of improving its value, so that
in the course of time whole countries (like Holland) may clearly
improve their agricultural position, whilst under the ordinary
_régime_ of continued exhaustion of the soil, entire regions (as,
for instance, many parts of Central Asia) may be rendered unfit
for any agriculture.
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