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Comparative study of S, Fe and Cu speciation transformation during chalcopyrite bioleaching by mixed mesophiles and mixed thermophiles

机译:用混合中硫酸盐和混合嗜热偶乙二醇淀粉生物浸浸料S,Fe和Cu形状转化的对比研究

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The bioleaching experiments of chalcopyrite were conducted with mixed mesophilic cultures (30°C), moderate thermophilic cultures (45°C) and extreme thermophilic cultures (65°C), respectively. During bioleaching, the S/Fe/Cu speciation were analyzed by synchrotron radiation (SR) based X-ray diffraction (XRD) and S, Fe and Cu K-edge X-ray absorption near edge structure (XANES) spectroscopy. The results showed that the chalcopyrite dissolution could be significantly promoted by these mixed cultures, and the promotion effects were enhanced with the increase of leaching temperature. The formation of intermediates S , jarosite and secondary minerals (chalcocite, bornite and covellite) was detected during bioleaching, in which the formation of bornite, chalcocite and covellite was just related with the redox potential. The formation of bornite could accelerate chalcopyrite dissolution, while the decreasing of bioleaching microorganisms could reduce chalcopyrite dissolution.
机译:用混合的中抚化培养物(30℃),中等嗜热培养物(45℃)和极端嗜热培养物(65℃)进行醋壳的生物浸出实验。在生物浸渍期间,通过同步辐射(SR)基于Syschrotron辐射(SR)的X射线衍射(XRD)和S,Fe和Cu K边缘X射线吸收分析S / Fe / Cu形状,靠近边缘结构(Xanes)光谱。结果表明,通过这些混合培养物可以显着促进黄铜矿溶解,随着浸出温度的增加而增强了促进效应。在生物浸渍期间检测中间体S,jar二和二次矿物质(Chalcocite,Bigrite和Covelite)的形成,其中Bigrite,Chalcocite和Covellite的形成与氧化还原潜力有关。 Bigrite的形成可以加速黄铜矿溶解,而生物浸入微生物的降低可以降低硫代铜矿溶解。

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