Mineralogical Changes Occurring During the Decopperizing and Deleading of Kidd Creek Copper Refinery Anode Slimes

The Minerals, Metals and Materials Society
T. T. Chen
Organization:
The Minerals, Metals and Materials Society
Pages:
25
File Size:
969 KB
Publication Date:
Jan 1, 1993

Abstract

Raw anode slimes consisting primarily of PbSO4, AgCuSe, Cu3Se2, Cu2-x Se, Cu2O, CuSO4.5H2O, Sn arsenate and Sb-Bi-As oxide are batch-leached with electrolyte-O2 to dissolve Cu. During this process, Cu2O and CuSO4.5H2O are solubilized and the Cu in the selenides is leached with the formation of Ag2Se and Se. A small amount of Cu remains in the Ag2Se, Sn arsenate and Sb-Bi-As oxide. The decopperized slimes are repulped in Na2CO3 solution to convert most of the PbSO4 to NaPb2(CO3)2(OH). The Sn arsenate and Sb-Bi-As oxide partly react, but the Ag2Se is not significantly affected by the Na2CO3 solution. The NaPb2(CO3)2(OH) intermediate phase is dissolved in acetic acid to leave a final product consisting of Ag2Se, Se, Sn arsenate and Sb-Bi-As oxide, together with small amounts of PbSO4, NaPb2(CO3)2(OH) and various gangue constituents.
Citation

APA: T. T. Chen  (1993)  Mineralogical Changes Occurring During the Decopperizing and Deleading of Kidd Creek Copper Refinery Anode Slimes

MLA: T. T. Chen Mineralogical Changes Occurring During the Decopperizing and Deleading of Kidd Creek Copper Refinery Anode Slimes. The Minerals, Metals and Materials Society, 1993.

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