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The Alteration Mechanism of Copper-bearing Biotite and Leachable Property of Copper-bearing Minerals in Mulyashy Copper Mine Zambia

机译:赞比亚Mulyashy铜矿中含铜黑云母的蚀变机理和含铜矿物的浸出特性

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摘要

The XRF, XRD, polarizing microscopy and SEM-EDS were used to study the alteration mechanism of copper-bearing biotite and the leachable property of copper-bearing minerals in Mulyashy Copper Mine, Zambia. It was found that biotite can be divided into copper-bearing biotite and copper-free biotite. Some copper-bearing biotite existed in the form of monomer, and others aggregated with copper-bearing chlorite, malachite or copper-bearing limonite. The main reason for the occurrence of biotite aggregations was that copper-bearing biotite underwent two kinds of alteration mechanisms as follows: altering into copper-bearing chlorite and malachite, and altering into copper-bearing chlorite and copper-bearing limonite. The order of factors effecting the copper leaching rate of the ores in acid leaching experiments was temperature > sample size > H2SO4 concentration > leaching time > stirring speed. In addition, the copper leaching rate of copper-bearing minerals at different temperatures was in the following order: malachite, chrysocolla and pseudomalachite > copper-bearing chlorite > copper-bearing muscovite > copper-bearing biotite > copper-bearing limonite. The leachable property of biotite is closely related to its special structure.
机译:利用XRF,XRD,偏光显微镜和SEM-EDS研究了赞比亚穆利亚希铜矿中含铜黑云母的蚀变机理和含铜矿物的浸出特性。发现黑云母可以分为含铜黑云母和无铜黑云母。一些含铜的黑云母以单体形式存在,另一些则与含铜的亚氯酸盐,孔雀石或含铜的褐铁矿聚集。发生黑云母团聚的主要原因是,含铜黑云母经历了两种蚀变机理,即变为含铜绿泥石和孔雀石,以及变为含铜绿泥石和含铜褐铁矿。在酸浸实验中,影响矿石铜浸出率的因素依次为温度>样品量> H2SO4浓度>浸出时间>搅拌速度。此外,不同温度下含铜矿物的铜浸出率依次为:孔雀石,温石棉和假孔雀石>含铜亚氯酸盐>含铜白云母>含铜黑云母>含铜褐铁矿。黑云母的可浸出性与其特殊结构密切相关。

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