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Mechanism of Silver-Catalyzed Bioleaching of Enargite Concentrate

机译:银催化浓缩精矿的生物浸出机理

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Silver-catalyzed bioleaching of enargite concentrate with three bacteria (Acidimicrobium ferrooxidans ICP, Sulfobacillus sibiricus NI, Acidithiobacillus caldus KU) and one archaeon (Ferroplasma acidiphilum Y) was conducted in order to elucidate the catalytic mechanism of silver sulfide in enargite bioleaching. Whereas Cu recovery remained relatively low (43%) and Fe dissolved completely without silver sulfide, Cu recovery was greatly enhanced (96%) and Fe dissolution was suppressed (29%) in the presence of 0.04% silver sulfide. In the latter case, 52% of the solubilized As was re-immobilized, in contrast to only 14% As re-immobilization in the former. The silver-catalyzed bioleaching (at 0.04% silver sulfide) proceeded at low redox potentials within the optimal range, which likely promoted enargite dissolution via formation of intermediate CU_2S. XAFS analysis revealed that As was mainly immobilized as As(V), which was in agreement with the EPMA results detecting ferric arsenate passivation on some enargite grains. Furthermore, formation of trisilver arsenic sulfide (Ag_3AsS_4) was detected by XRD and EPMA, covering the surface of enargite particles. An intermediate layer, consisting of (Cu,Ag)_3AsS_4, was also observed between the enargite grain and trisilver arsenic sulfide layer, implying that Cu in enargite may be gradually substituted by solubilized Ag. Kinetic study suggested that these secondary minerals do not rate-limit the enargite dissolution. The overall mechanism of silver-catalyzed bioleaching of enargite concentrate will be proposed.
机译:为了阐明银硫化物在银矿生物浸出中的催化机理,进行了银催化的3种细菌(铁氧化亚铁微杆菌ICP,西伯利亚硫杆菌,酸度硫杆菌KU)的生物浸出。在没有硫化银的情况下,Cu的回收率仍然较低(43%),Fe完全溶解,而在有0.04%的硫化银的情况下,Cu的回收率大大提高(96%),Fe的溶解受到抑制(29%)。在后一种情况下,52%的溶解砷被重新固定,而在前者中只有14%的砷被重新固定。银催化的生物浸出(硫化银含量为0.04%)在最佳范围内的低氧化还原电势下进行,这很可能通过形成中间CU_2S促进了辉石的溶解。 XAFS分析表明,As主要被固定为As(V),这与EPMA在某些硬质合金晶粒上检测砷酸铁钝化的结果一致。此外,通过XRD和EPMA检测到三银硫化砷(Ag_3AsS_4)的形成,覆盖了硬辉石颗粒的表面。在镁辉石晶粒与三银硫化砷层之间还观察到由(Cu,Ag)_3AsS_4组成的中间层,这意味着辉镁岩中的Cu可能会逐渐被溶解的Ag取代。动力学研究表明,这些次生矿物质不对钠辉石的溶出速率进行限制。提出了银催化辉绿精矿生物浸出的整体机理。

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