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Dissolution and passivation mechanisms of chalcopyrite during bioleaching: DFT calculation, XPS and electrochemistry analysis

机译:黄铜矿在生物浸出过程中的溶解和钝化机理:DFT计算,XPS和电化学分析

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In this work, density functional theory (DFT) calculation, X-ray photoelectron spectroscopy (XPS) and electrochemistry analysis were carried out to investigate the dissolution process and passivation mechanisms of chalcopyrite in the presence of sulfur and iron oxidizing microorganisms. Both DFT calculation and XPS analysis indicated that the formula of chalcopyrite should be Cu + Fe-3 + (S2-)(2). Disulfide (S-2(2-)) and polysulfide (S-n(2-)) can be easily formed on the surface of chalcopyrite due to the surface reconstruction. The dissolution process of chalcopyrite in bioleaching was mainly dependent on redox potential. Chalcopyrite was predominantly directly oxidized to polysulfide when redox potential was lower than about 350 mV vs. Ag/AgCl and resulted in low dissolution rate. When redox potential was in the range of about 350-480 mV vs. Ag/AgCl; chalcopyrite was mainly transformed to intermediate species of Cu2S rather than polysulfide, thus resulting in high dissolution rate. When redox potential was higher than about 480 my vs. Ag/AgCl, chalcopyrite was principally directly oxidized to polysulfide which caused the passivation of chalcopyrite. Finally, a model of dissolution and passivation mechanisms of chalcopyrite in the presence of sulfur and iron oxidizing microorganisms was provided. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在这项工作中,进行了密度泛函理论(DFT)计算,X射线光电子能谱(XPS)和电化学分析,以研究在硫和铁氧化微生物存在下黄铜矿的溶解过程和钝化机理。 DFT计算和XPS分析均表明,黄铜矿的分子式应为Cu + Fe-3 +(S2-)(2)。由于表面重构,容易在黄铜矿的表面上形成二硫化物(S-2(2-))和多硫化物(S-n(2-))。黄铜矿在生物浸出过程中的溶解过程主要取决于氧化还原电位。当氧化还原电势相对于Ag / AgCl低于约350 mV时,黄铜矿主要直接氧化为多硫化物,导致溶解速率低。当氧化还原电势相对于Ag / AgCl在约350-480mV的范围内时;黄铜矿主要转化为Cu2S的中间物种,而不是多硫化物,因此具有较高的溶解速率。当氧化还原电势相对于Ag / AgCl高于480 my时,黄铜矿主要直接氧化为多硫化物,从而导致黄铜矿钝化。最后,提供了在硫和铁氧化微生物存在下黄铜矿的溶解和钝化机理模型。 (C)2016 Elsevier Ltd.保留所有权利。

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