=224. Introduction.=—The potash present in unfertilized soils has been
derived from the decay of rocks containing potash minerals. Among
these potash producers feldspars are perhaps the most important. For
a discussion of the nature of their decomposition and the causes
producing it the first part of volume first may be consulted. Potash is
quite as extensively distributed as phosphoric acid and no true soils
are without it in some proportion. Its presence is necessary to plant
growth and it forms, in combination with organic and mineral acids, an
essential part of the vegetable organism, existing in exceptionally
rich quantities in the seeds. It is possible that potash salts, such
as the chlorid, sulfate, and phosphate may be assimilated as such,
but, as with other compounds, we must not deny to the plant the
remarkable faculty of being able to decompose its most stable salts
and to form from the fragments thus produced entirely new compounds.
This is certainly true of the potash compounds existing in plants in
combination with organic acids. The potash which is assimilated by
plants exists in the soil chiefly in a mineral state, and that added as
fertilizer is chiefly in the same condition. That part of the potash in
a soil arising directly from the decomposition of vegetable matters may
exist partly in organic combination, but this portion, in comparison
with the total quantity absorbed by the plant, is insignificant.
It is then safe to assume that at least a considerable part of the
potash absorbed by the plant is decomposed from its original form
of combination by the vegetable biochemical forces, and is finally
incorporated in the plant tissues in forms determined by the same
powerful forces of vegetable metabolism.
The analyst is not often called upon to investigate the forms in
which the potash exists in plants, when engaged in investigation of
fertilizers. It is chiefly found in combination with organic and
phosphoric acids, and on ignition will appear as phosphate or carbonate
in the ash.
=225. Forms in which Potash is Found in Fertilizers.=—The chief
natural sources of potash used in fertilizer fabrication are: First,
organic compounds, such as desiccated mineral matters, tobacco
waste, cottonseed hulls, etc.; second, the ash derived from burning
terrestrial plants of all kinds; third, the natural mineral deposits,
such as Stassfurt salts.
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