Potassium sulfate 18.60 per cent.
Magnesium sulfate 14.70 “ “
Calcium sulfate 61.00 “ “
Sodium chlorid 1.50 “ “
Water 4.20 “ “
The percentage of potash corresponding to the above formula is 10.05.
It is therefore less valuable than kainit in so far as its content of
potash is concerned. This salt also exists in limited quantities and is
not likely to become an important article of commerce.
=241. Sylvin.=—One of the alteration products of carnallit is a
practically pure potassium chlorid which, as it occurs in the Stassfurt
mines is known as sylvin. The alteration of the carnallit arises from
its solution in water from which, on subsequent evaporation, the
potassium chlorid is deposited alone. This mineral is found in only
limited quantities in the Stassfurt deposits and it therefore does not
have any great commercial importance.
=242. Sylvinit.=—This mineral has been mined in recent years in
considerable quantities. It is, in fact, only common salt carrying
large quantities of potassium chlorid together with certain other
accidental impurities. It was probably formed by the drying up of a
saline mass in such a way as not to permit the complete separation of
its mineral constituents. The average composition of sylvinit as it
comes from the mines is given in the following table:
Potassium chlorid 30.55 per cent.
Sodium chlorid 46.05 “
Potassium sulfate 6.95 “
Magnesium sulfate 4.80 “
Magnesium chlorid 2.54 “
Calcium sulfate 1.80 “
Water and insoluble 7.29 “
This salt is richer in chlorin than any other of the Stassfurt potash
minerals, containing altogether 79.14 per cent of chlorids. Its potash
content amounts to 23.04 per cent, but in proportion to the potash
which it contains, it is relatively poorer in chlorin than kainit and
carnallit. On account of its high content of potash the freights on a
given weight thereof as contained in sylvanit are lower than for kainit
and carnallit.
=243. Kieserit.=—The mineral kieserit is essentially magnesium sulfate
and it does not necessarily contain any potash salts. Under the name
of kieserit, however, or bergkieserit, there is mined a mixture of
carnallit and kieserit, which is a commercial source of potash. The
mixture contains the following average content of the bodies named:
Potassium chlorid 11.80 per cent.
Magnesium sulfate 21.50 “
Magnesium chlorid 17.20 “
Sodium chlorid 26.70 “
Calcium sulfate 0.80 “
Water 20.70 “
Insoluble 1.30 “
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