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

- 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:
(1993) Mineralogical Changes Occurring During the Decopperizing and Deleading of Kidd Creek Copper Refinery Anode SlimesMLA: Mineralogical Changes Occurring During the Decopperizing and Deleading of Kidd Creek Copper Refinery Anode Slimes. The Minerals, Metals and Materials Society, 1993.