A Model Of The Chemistry Of The Dump Leaching Of Chalcopyrite

The American Institute of Mining, Metallurgical, and Petroleum Engineers
KNona C. Liddell Renato G. Bautista
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
6
File Size:
295 KB
Publication Date:
Jan 1, 1981

Abstract

A model of the reaction of chalcopyrite, CuFeS2, with Fe3+ and with 02 is considered. Homogeneous solution phase reactions are assumed to be always at equilibrium throughout the dissolution of the mineral. The dissociation of USOb- and several complexation reactions involving cu2+, Fez+ and Fe3+ are incorporated in the model equations. The relative importance of Fe3+, 02, and H+ as oxidants and the role of solution equilibria are assessed and the implications for leaching practice discussed.
Citation

APA: KNona C. Liddell Renato G. Bautista  (1981)  A Model Of The Chemistry Of The Dump Leaching Of Chalcopyrite

MLA: KNona C. Liddell Renato G. Bautista A Model Of The Chemistry Of The Dump Leaching Of Chalcopyrite. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1981.

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