首页> 外文会议>Clay Minerals Society Annual Meeting >MICROBES, Mn OXYHYDROXIDES AND METALS: MICROBIAL BIOGEOCHEMISTRY IN ACID ROCK DRAINAGE
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MICROBES, Mn OXYHYDROXIDES AND METALS: MICROBIAL BIOGEOCHEMISTRY IN ACID ROCK DRAINAGE

机译:微生物,Mn羟基氧化物和金属:酸岩排水中的微生物生物地球化学

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Reactive metal transport in acid rock drainage (ARD) environments is increasingly appreciated as a microbially mediated process. Understanding the linkages amongst microbial function, system geochemical conditions and metal behaviour, will help to provide a mechanistic foundation from which to design mitigative and/or bioremediation approaches for ARD. My group has been investigating the biogeochemical processes controlling metal dynamics in tailings derived streams in an ARD environment (Sudbury, ON), using an integrated approach combining geochemical, microbiological and microscopic techniques. These tailings associated streams are acidic (pH < 3.5) with high metal loads (nMolar - mMolar) and flourishing microbial biofilms. Whilst microbial biofilms are thin layer structures (typically hundreds of microns, to a few millimeters in thickness), their role in controlling overall system metal transport may be significant, due to the high rates of microbial activity and attendant geochemical reactivity, concentrated within these structures. Investigation by my group, of the biogeochemical processes controlling biofilm metal behaviour has identified associated biominerals of Mn oxyhydroxides, as key metal sorbents.
机译:在酸岩排水(ARD)环境反应性金属运输日益理解为微生物介导的过程。了解微生物之间的功能,系统地球化学条件和金属的行为,的联系将有助于提供一个机制的基础,从中设计出减缓和/或ARD生物修复方法。我的群组已调查生物地球化学过程控制尾矿金属动力学衍生流在ARD环境(萨德佰里,ON),使用集成的办法,结合地球化学,微生物和显微镜技术。相关联的流中。这些尾矿是酸性的(pH值<3.5)具有高金属负载(毫微摩尔 - 毫摩尔)和繁荣的微生物生物膜。尽管微生物生物膜薄层结构(通常几百微米,以便在厚度为几个毫米),它们在控制整个系统的金属运输作用可能是显著,由于微生物的活动和伴随的地球化学反应性的高速率,浓缩这些结构内。通过我的调查组的生物地球化学过程控制生物膜金属的行为,已经确定相关联的Mn羟基氧化物的生物矿物,如关键金属吸附剂。

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