Options to Control Acid Generation in Existing Pyritic Mine Waste Dumps

Society for Mining, Metallurgy & Exploration
D. K. Gibson A. I. M. Ritchie
Organization:
Society for Mining, Metallurgy & Exploration
Pages:
4
File Size:
601 KB
Publication Date:
Jan 1, 1991

Abstract

The phenomenon of acid drainage is likely to occur whenever pyritic rock is broken up, permitting access of air and water. The basic chemistry of the oxidation process is described by the equations below:- FeS 2 +1120 + 7 02 ➔FeS04 +112S04 +1440k.J This reaction proceeds rather slowly, although believed to be bacterially catalysed to some extent. Once sufficient ferrous ions and acidity have been established the following two reactions take over, yielding the same net result but at a much greater rate. First, ferrous ions are oxidised to ferric; this is an extremely slow reaction unless bacterially catalysed.
Citation

APA: D. K. Gibson A. I. M. Ritchie  (1991)  Options to Control Acid Generation in Existing Pyritic Mine Waste Dumps

MLA: D. K. Gibson A. I. M. Ritchie Options to Control Acid Generation in Existing Pyritic Mine Waste Dumps. Society for Mining, Metallurgy & Exploration, 1991.

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