A New Method for Determining Silica in Iron Ores

The American Institute of Mining, Metallurgical, and Petroleum Engineers
C. C. Hawes
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
2
File Size:
193 KB
Publication Date:
Jan 1, 1936

Abstract

SILICA is the main impurity in iron ore. It is intimately associated with the iron oxide, sometimes free but more often in the combined state, as a mineral silicate. Its separation and purification sometimes present difficult problems to the analyst. In the absence of any definite knowledge to the contrary, orthosilicic acid. H4SiO4, is supposed to be the only silicic acid made, all other forms, such as metasilicic acid, H2SiO3, representing different degrees of its dehydration. These acids are exceedingly weak but form the most stable compounds found in nature. They are known as the silicate minerals and are formed by the combination of the different metallic oxides
Citation

APA: C. C. Hawes  (1936)  A New Method for Determining Silica in Iron Ores

MLA: C. C. Hawes A New Method for Determining Silica in Iron Ores. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1936.

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