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机构地区:[1]中国矿业大学(北京)化学工程系,北京100083 [2]中国科学院过程工程研究所,北京100190
出 处:《过程工程学报》2012年第5期781-784,共4页The Chinese Journal of Process Engineering
基 金:国家重点基础研究发展规划(973)基金资助项目(编号:2010CB630904);国家高技术研究发展计划(863)基金资助项目(编号:2012AA061503);国家自然科学基金资助项目(编号:51174185);北京市自然科学基金资助项目(编号:2112038)
摘 要:研究了Ag+对含砷金精矿生物浸出的影响,测量了浸出液中铁、银、砷浓度及氧化还原电位(Eh)的变化,考察了Ag+对细菌密度的影响,并对浸渣进行了光谱表征.结果表明,Ag+对含砷金精矿的生物浸出有一定的促进作用且在高浓度Fe3+条件下催化作用明显;低Ag+浓度下含砷金精矿的生物浸出率提高约10%,但Ag+浓度过高将影响细菌生长,导致浸出速率下降.Ag+催化含砷金精矿生物浸出是Ag+取代矿物表面的砷并生成Ag2S,之后被Fe3+氧化分解,重新产生Ag+,从而加速矿物的氧化分解.The effect of Ag+ on bioleaching of As-bearing gold concentrate was studied. The concentrations of Fe3+, Ag+ and As in the bioleaching solution were monitored during the leaching process. The effect of Ag+ on the bacterial density was investigated and the leaching residue was characterized by XRD and SEM. The experimental results show that Ag+ can enhance the bioleaching rate especially at the high concentration of Fe3 +, but the growth of bacteria was restrained under at higher concentration of Ag+, leading to the decrease of leaching rate. Based on the leaching results and leaching residue analysis, the catalytic mechanism of Ag+ was that the arsenic on the surface of concentrate was displaced by Ag+, and Ages formed, which could be dissolved by Fe3+, releasing Ag+ again.
分 类 号:TF18[冶金工程—冶金物理化学]
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