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A copper and iron K-edge XANES study on chalcopyrite leached by mesophiles and moderate thermophiles

机译:一种铜和铁k-Edge Xanes在乳铜矿浸出的中温嗜热偶

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To reveal the mechanism of chalcopyrite biooxidation at different temperatures, pure chalcopyrite leached by mesophiles (30°C) and moderate thermophiles (48°C) was characterized by synchrotron X-ray apbsorption near-edge structure (XANES). Solution study shows that elevated temperature significantly promoted the chalcopyrite dissolution. A copper concentration of 1.32g/l was finally achieved in 48°C leaching, while only 0.49g/l copper was released in 30°C bioleaching. Cu AT-edge XANES study shows the formation of a CuSn-like solid phase at early leaching stage and a decrease of this phase at late stage. This result suggests the preferential release of iron, which is followed by the successive dissolution of copper resulting in a metal-deficient sulfur-rich layer (S_n~(2-)) left on the chalcopyrite surface which further hinders chalcopyrite dissolution. In addition, Fe K-edge XANES indicates that no significant amount of jarosite was formed in 30°C bioleaching; however, in 48°C bioleaching jarosite precipitation was profoundly accelerated, which reached a contribution of 50.5% at day 35.
机译:为了揭示不同温度下的黄铜矿生物氧化的机理,通过同步X射线吸收性近边缘结构(Xanes),表征了由中间铬(30℃)和中等嗜热(48℃)浸出的纯炭黄石。解决方案研究表明,升高的温度显着促进了黄铜矿溶解。最终在48℃的浸出中实现1.32g / L的铜浓度,而在30℃的BOO-浸出中仅释放0.49g / l铜。 Cu在边缘Xanes研究表明,在早期浸出阶段形成Cusn样固相的形成,并且在晚期的这种阶段降低。该结果表明铁的优先释放,其次是铜的连续溶解,导致富含金属铜矿表面的金属缺乏硫的层(S_N〜(2-)),其进一步阻碍了黄铜矿溶解。此外,Fe K-Edge Xanes表明在30℃的BOOLEACHING中没有形成大量的碱化合物;然而,在48℃的生物浸硼酸释放中,深入加速,在第35天达到50.5%的贡献。

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