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The effect of ore mineralogy on the speciation of arsenic in bacterial oxidation of refractory arsenical gold ores

机译:矿石矿物质对耐火砷金矿细菌氧化砷的形态

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The bacterial leaching of refractory arsenic-bearing gold ores from different deposits were investigated to determine the effects of mineralogy on the fate of arsenic during processing and to assess the effectiveness of biological pre-treatment on gold extraction. Experiments were conducted using a mixed culture of iron and sulphur oxidising bacteria dominated by Thiobacillus ferrooxidans. The speciation of arsenic during bioleaching was studied using polarography. Leaching of a concentrate which was predominantly arsenopyrite resulted in 80 percent of the leached arsenic reporting in solution as arsenic(III) at the end of the bacterial oxidation stage. Study of the oxidation of concentrates from different ore deposits with various ratios of pyrite to arsenopyrite showed that the amount of pyrite was an important factor in determining the dominating arsenic oxidation state in the leach solutions. Iron(III) alone was found not to be able to oxidise arsenic(III), instead pyrite was needed as a catalyst. It was found that adding pyrite and iron(III) to arsenopyrite concentrates promotes the formation of arsenic(V) leaving less than 1 percent of the extracted arsenic as arsenic(III). Furthermore a strong dependence of pyrite leaching and arsenic(III) oxidation was demonstrated. These results demonstrate the importance of ore composition in terms of pyrite to arsenopyrite ratio in the production of environmentally acceptable biooxidation residues containing arsenic(V).
机译:研究了来自不同沉积物的耐火砷金矿的细菌浸出,以确定矿物学在加工过程中对砷的命运的影响,并评估生物预治疗对金提取的有效性。使用由Thiobacillus ferrooxidans主导的铁和硫氧化细菌的混合培养进行实验。使用极谱法研究了生物浸出过程中砷的形态。浸出浓缩物的浓缩物,主要是亚苯甲酸盐,导致在细菌氧化阶段结束时作为砷(III)的溶液中的80%的浸出砷报告。用不同矿石沉积物与亚苯甲酸盐的不同矿石沉积物氧化的研究表明,黄铁矿的量是测定浸出溶液中占主导砷氧化态的重要因素。仅发现单独的铁(III)不能能够氧化砷(III),而是需要胶铁作为催化剂。发现将硫铁矿和铁(III)加入砷吡啶矿石浓缩物促进砷(V)的形成留下少于1%的砷(III)。此外,证实了硫铁矿浸出和砷(III)氧化的强烈依赖。这些结果证明了矿石组合物在含有砷(V)的环境可接受的生物氧化残基的生产中的氨基吡钛矿比的重要性。

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