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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Biogeochemical characterization of bacterial assemblages in relation to release of arsenic from South East Asia (Bangladesh) sediments
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Biogeochemical characterization of bacterial assemblages in relation to release of arsenic from South East Asia (Bangladesh) sediments

机译:与东南亚(孟加拉国)沉积物中砷释放相关的细菌组合的生物地球化学特征

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摘要

Arsenic release experiments using natural indigenous microbial assemblages and natural sediment samples in Bangladesh have been performed. The As release appears to be facilitated by moderate organic input. Addition of some nutrients caused reducing conditions, which may generate the appropriate environment for Fe-reducing bacteria to become active. Detailed cellular phospholipid fatty acid (PLFA) analysis suggests the presence of SO4-reducing and Fe-reducing bacteria in the sediments. These Fe-reducing bacteria may serve as the agents catalyzing As release in the organic-rich sediments. 16S rDNA analysis of one cultured sample suggests the presence of clostridia, some of which are known to mediate Fe reduction. Based on new PLFA analyses, it is proposed that combined microbial processes of SO4 reduction to generate anaerobic conditions and Fe reduction to co-reduce As are important biogeochemical factors for As release in the Bangladesh sediments. (C) 2008 Published by Elsevier Ltd.
机译:在孟加拉国使用天然的原生微生物组合和天然沉积物样品进行了砷释放实验。适度的有机输入似乎促进了As的释放。某些营养素的添加会导致还原条件的产生,这可能会为还原铁的细菌活化提供适当的环境。详细的细胞磷脂脂肪酸(PLFA)分析表明,沉积物中存在SO4还原菌和Fe还原菌。这些还原铁的细菌可以作为催化As在富有机沉积物中释放的媒介。对一个培养样品的16S rDNA分析表明存在梭状芽胞杆菌,其中一些已知可介导铁还原。基于新的PLFA分析,建议将微生物的SO4还原过程产生厌氧条件,将Fe还原过程共同减少As,这是孟加拉国沉积物中As释放的重要生物地球化学因素。 (C)2008由Elsevier Ltd.发布

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