Studies of the Mechanism of Rock Mineral Flotation at Clarabelle Mill

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چکیده

At the Clarabelle mill, significant amounts of rock minerals float inadvertently during nickel and copper sulfide flotation, causing poor concentrate grades. It is known that the rock minerals that report to the concentrates are amphiboles and phyllosilicates. However, the latter are found only on concentrates obtained by processing highly altered ores. The amphiboles, which occur as both primary and secondary minerals in the Sudbury basin ores are double-chain ionosilicates containing hydroxyl (-OH) groups. The chemical composition of amphiboles may be represented by a general formula [1]: A0-1B2C5T8O22(OH,F)2, where: A = Na or K, B = Ca, Mn, Fe, Mg, or Li, C = Mn, Fe, Mg, Fe, Al, or Ti, and T = Si or Al.

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تاریخ انتشار 1999