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首页> 外文期刊>Transactions of Nonferrous Metals Society of China >Biofilm forming and leaching mechanism during bioleaching chalcopyrite by Thiobacillus ferrooxidans
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Biofilm forming and leaching mechanism during bioleaching chalcopyrite by Thiobacillus ferrooxidans

机译:铁氧化硫杆菌对黄铜矿生物浸出过程中生物膜的形成和浸出机理

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摘要

The mechanism of attachment and leaching of thiobacillus ferrooxidans (T. f.) on chalcopyrite were studied. The shaking flasks with bacteria were observed by SEM. The process of T. f attached to the surface of the mineral sample and the biofilm forming were described. The promoting role of the biofilm for bioleaching was discussed. The existence of Fe~(2+) in the exopolysaccharide layer of T. f was demonstrated by EM (electronic micro-scope) cell-chemistry analysis. These results show that under the proper growth condition of bacteria, bioleaching of chalcopyrite results in the formation of complete biofilm after 2 - 3 weeks. There are iron ions in the Outer layer polymer of T. f., which provides the micro-environment for themselves, and can guaruntee the energy needed for the bacteria growth in the biofilm. At the same time, Fe~(3+) ions produced oxidize sulfide which brings about the increase of both growth rate of the bacterial and leaching rate of sulfide minerals.
机译:研究了硫氧化杆菌(T. f。)在黄铜矿上的附着和浸出机理。通过SEM观察带有细菌的摇瓶。描述了T. f附着在矿物样品表面的过程和生物膜的形成。讨论了生物膜在生物浸出中的促进作用。 EM(电子显微镜)细胞化学分析证明了T.f胞外多糖层中Fe〜(2+)的存在。这些结果表明,在适当的细菌生长条件下,黄铜矿的生物浸出会在2-3周后形成完整的生物膜。在T.f.的外层聚合物中存在铁离子,铁离子为其自身提供了微环境,并可以确保细菌在生物膜中生长所需的能量。同时,产生的Fe〜(3+)离子氧化了硫化物,使细菌的生长速度和硫化物矿物的浸出速度均增加。

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