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Iron-Mediated Microbial Oxidation and Abiotic Reduction of Organic Contaminants under Anoxic Conditions

机译:缺氧条件下铁介导的微生物氧化和非生物还原有机污染物

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In anoxic environments, the oxidation of organic compounds, such as BTEX fuel components, by dissimilatory Fe(III) reduction can generate reactive mineral-bound Fe(II) species, which in turn are able to reduce other classes of organic and inorganic groundwater contaminants. In this study, we designed and evaluated an anaerobic batch reactor that mimicks iron-reducing conditions to investigate the factors that favor the coupling of microbial toluene oxidation and abiotic reduction of nitroaromatic contaminants. We investigated the influence of different Fe(III)-bearing minerals and combinations thereof on the coupling of these two processes. Results from laboratory model systems show that complete oxidation of toluene to CO_2 by Geobacter metallireducens in the presence of Fe(III)-bearing minerals leads to the formation of mineral-bound Fe(II) species capable of the reduction of 4-nitroacetophenone. Whereas significant microbial toluene oxidation was only observed in the presence of amorphous Fe(III) phases, reduction of nitroaromatic compounds only proceeded with Fe(II) species bound to crystalline Fe(III) oxides. Our results suggest that in anoxic soils and sediments containing amorphous and crystalline iron phases simultaneously, coupling of microbial oxidation and abiotic reduction of organic compounds may allow for concurrent natural attenuation of different contaminant classes.
机译:在缺氧环境中,通过异化还原Fe(III)来氧化有机化合物(例如BTEX燃料成分)会生成与矿物结合的反应性Fe(II)物种,从而能够还原其他类别的有机和无机地下水污染物。在这项研究中,我们设计和评估了一个模拟铁还原条件的厌氧间歇式反应器,以研究有利于微生物甲苯氧化与非生物还原硝基芳族污染物耦合的因素。我们研究了不同的含Fe(III)的矿物及其组合对这两个过程的耦合的影响。实验室模型系统的结果表明,在含有Fe(III)的矿物存在下,Geobacter metallireducens将甲苯完全氧化为CO_2导致形成能够还原4-硝基苯乙酮的结合矿物的Fe(II)物种。尽管仅在无定形的Fe(III)相存在下才观察到明显的微生物甲苯氧化,但硝基芳族化合物的还原仅在与结晶的Fe(III)氧化物结合的Fe(II)物种下进行。我们的结果表明,在同时含有无定形和结晶铁相的缺氧土壤和沉积物中,微生物氧化和非生物还原有机化合物的耦合可能允许同时自然衰减不同的污染物类别。

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