A text-book of assaying : $b for the use of those connected with mines.Beringer, C. (Cornelius)
Science
A text-book of assaying : $b for the use of those connected with mines.
Beringer, C. (Cornelius)
Assaying
Tungstic acid 50.1%
Cassiterite 10.9
Ferrous oxide 24.6
Manganous oxide 5.4
Niobic oxide, alumina, &c. 3.5
Silica 1.2
Copper oxide 2.7
Zinc oxide 0.22
Arsenic 0.51
Sulphur 0.20
-----
99.33
NIOBIC AND TANTALIC OXIDES.
These oxides are commonly met with in samples of wolfram and tinstone,
especially niobic. They are probably present in the form of columbite, a
niobate of iron and manganese; and tantalite, a tantalate of the same
metals.
On boiling with hydrochloric acid they are both liberated, and remain
for the greater part (all the niobic) in the insoluble residue with the
tungstic acid. On removing the latter with dilute ammonia they remain as
a white insoluble precipitate, very prone to run through the filter on
washing. They may be dissolved in hydrofluoric acid either at once or
after fusion with bisulphate of potash, and extraction with cold water.
To the solution in hydrofluoric acid gradually add a boiling solution of
acid potassium fluoride (HF, KF.). Potassic fluotantalate (soluble in
200 parts of water) separates out first, and afterwards potassic
fluoniobate (soluble in 12 parts of water). The separated salts (after
heating with sulphuric acid and washing out the potassium sulphate
formed) are ignited with ammonic carbonate, and weighed as tantalic
oxide (Ta_{2}O_{5}) and niobic oxide (Nb_{2}O_{5}) respectively.
They are both white powders. The oxide of niobium dissolved in a bead of
microcosmic salt gives a bluish colour in the reducing flame. The oxide
of tantalum dissolves in the bead, but gives no colour.
FOOTNOTES:
[76] This will give almost the whole of the tin; a further portion will
be got in subsequent work, and must be added to this result.
[77] Published by P. Holland, in the _Chemical News_, vol. lix. p. 27.
CHAPTER XIII.
MANGANESE, CHROMIUM, &c.
MANGANESE.
Manganese occurs mainly as black oxide (MnO_{2}) in the mineral
pyrolusite; and, in a less pure form, in psilomelane and wad. The value
of the ore depends rather on the percentage of available oxygen than on
the proportion of metal present. The results of assays are generally
reported as so much per cent. of the dioxide (MnO_{2}). In smaller
quantities it is very widely distributed. Manganese itself has a value
for steel-making; or, rather, for the making of spiegeleisen and
ferro-manganese, which are used in the Bessemer and Siemens processes.
For this purpose the percentage of the metal (Mn) is required.
Consequently the minerals of manganese may be considered in two
aspects--(1) as a source of oxygen; and (2) as a source of manganese.
These will require separate consideration.
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