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Pyrite biooxidation: electrochemical and kinetic data

机译:黄铁矿生物氧化:电化学和动力学数据

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Studies on pyrite oxidation by Thiobacillus ferrooxidans, using a compact pyrite electrode, resulted in detection of 14 exchanged electrons. This indicates that the pyrite biooxidation to sulfate ions occurred at the pyrite surface without the formation of any sulfur intermediates. Exchange current density showed that the pyrite biooxidation rate was higher by one order of magnitude as compared to conditions without bacteria. Assuming sulfate is the final product, the initial rate of pyrite concentrate oxidation by ferric iron (up to 180 mM) was similar to the rate of pyrite concentrate oxidation by T.ferrooxidans in the absence of any significant ferric iron. Electrochemical and kinetic studies supported the indirect mechanism of pyrite oxidation based on iron-oxidizing activity of T.ferrooxidans.
机译:使用紧凑的黄铁矿电极对氧化亚铁硫杆菌进行黄铁矿氧化的研究导致检测到14个交换电子。这表明黄铁矿在黄铁矿表面发生了生物氧化为硫酸根离子,没有形成任何硫中间体。交换电流密度表明,与没有细菌的条件相比,黄铁矿的生物氧化速率高出一个数量级。假设硫酸盐是最终产物,则在没有任何明显三价铁的情况下,三价铁的黄铁矿精矿的初始氧化速率(最高180 mM)与三氧化二铁的黄铁矿精矿的氧化速率相似。电化学和动力学研究支持基于铁三氧化二铁的铁氧化活性的黄铁矿氧化的间接机理。

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