Elements of Agricultural ChemistryAnderson, Thomas
Science
Elements of Agricultural Chemistry
Anderson, Thomas
Agricultural chemistry
MICA.
|----------------|
Potash. Magnesia.
Silica 46.36 42.65
Alumina 36.80 12.96
Peroxide of iron 4.53 ---
Protoxide of iron --- 7.11
Oxide of manganese 0.02 1.06
Magnesia --- 25.75
Potash 9.22 6.03
Hydrofluoric acid 0.70 0.62
Water 1.84 3.17
---- ----
99.47 99.35
Mica undergoes decomposition with extreme slowness, as is at once
illustrated by the fact that its shining scales may frequently be met
with entirely unchanged in the soil. Its persistence is dependent on the
small quantity of alkaline constituents which it contains; and for this
reason it is observed that the magnesian micas undergo decomposition
less rapidly than those containing the larger quantity of potash.
Eventually, however, both varieties become converted into clay, their
magnesia and potash passing gradually into soluble forms.
Hornblende and augite are two widely distributed minerals, which are so
similar in composition and properties that they may be considered
together. Of the former two varieties, basaltic and common have been
distinguished, and their composition is given below:--
Hornblende.
|----------------|
Common. Basaltic. Augite.
Silica 41.50 42.24 50.12
Alumina 15.75 13.92 4.20
Protoxide of iron 7.75 14.59 11.60
Oxide of manganese 0.25 0.33 --
Lime 14.09 12.24 20.55
Magnesia 19.40 13.74 13.70
Water 0.50 -- --
---- ---- ----
99.24 97.05 99.67
In these minerals alkalies are entirely absent, and their decomposition
is due to the presence of protoxide of iron, which readily absorbs
oxygen from the air, when the magnesia is separated and a ferruginous
clay left.
The minerals just referred to, constitute the great bulk of the mountain
masses, but they are associated with many others which take part in the
formation of the soil. Of these the most important are the zeolites
which do not occur in large masses but are disseminated through the
other rocks in small quantity. They form a large class of minerals of
which Thomsonite and natrolite may be selected as examples--
Thomsonite. Natrolite.
Silica 38.73 48.68
Alumina 30.84 26.36
Lime 13.43 --
Potash 0.54 0.23
Soda 3.85 16.00
Water 13.09 9.55
---- ----
100.48 100.83
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