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在膜生物膜反应器中,微生物铬酸盐还原与甲烷厌氧氧化偶联。

Microbial chromate reduction coupled with anaerobic oxidation of methane in a membrane biofilm reactor.

机构信息

Advanced Water Management Centre, The University of Queensland, St Lucia, Queensland 4072, Australia; School of Environmental and Chemical Engineering, Shanghai University, 333 Nanchen Road, Shanghai 200444, PR China.

Advanced Water Management Centre, The University of Queensland, St Lucia, Queensland 4072, Australia.

出版信息

Environ Int. 2019 Sep;130:104926. doi: 10.1016/j.envint.2019.104926. Epub 2019 Jun 20.

Abstract

It has been reported that microbial reduction of sulfate, nitrite/nitrate and iron/manganese could be coupled with anaerobic oxidation of methane (AOM), which plays a significant role in controlling methane emission from anoxic niches. However, little is known about microbial chromate (Cr(VI)) reduction coupling with AOM. In this study, a microbial consortium was enriched via switching nitrate dosing to chromate feeding as the sole electron acceptor under anaerobic condition in a membrane biofilm reactor (MBfR), in which methane was continuously provided as the electron donor through bubble-less hollow fiber membranes. According to long-term reactor operation and chromium speciation analysis, soluble chromate could be reduced into Cr(III) compounds by using methane as electron donor. Fluorescence in situ hybridization and high-throughput 16S rRNA gene amplicon profiling further indicated that after feeding chromate Candidatus 'Methanoperedens' (a known nitrate-dependent anaerobic methane oxidation archaeon) became sole anaerobic methanotroph in the biofilm, potentially responsible for the chromate bio-reduction driven by methane. Two potential pathways of the microbial AOM-coupled chromate reduction were proposed: (i) Candidatus 'Methanoperedens' independently utilizes chromate as electron acceptor to form Cr(III) compounds, or (ii) Candidatus 'Methanoperedens' oxidizes methane to generate intermediates or electrons, which will be utilized to reduce chromate to Cr(III) compounds by unknown chromate reducers synergistically. Our findings suggest a possible link between the biogeochemical chromium and methane cycles.

摘要

据报道,硫酸盐、亚硝酸盐/硝酸盐和铁/锰的微生物还原可以与甲烷的厌氧氧化(AOM)耦合,这在控制缺氧生境中甲烷的排放方面起着重要作用。然而,对于微生物铬酸盐(Cr(VI))还原与 AOM 的偶联知之甚少。在这项研究中,通过在膜生物膜反应器(MBfR)中作为唯一电子受体将硝酸盐剂量切换为铬酸盐进料,在厌氧条件下富集微生物共生物,其中甲烷通过无泡空心纤维膜连续作为电子供体提供。根据长期反应器运行和铬形态分析,甲烷可用作电子供体,将可溶性铬酸盐还原成 Cr(III)化合物。荧光原位杂交和高通量 16S rRNA 基因扩增谱进一步表明,在进料铬酸盐后,Candidatus 'Methanoperedens'(一种已知的依赖硝酸盐的厌氧甲烷氧化古菌)成为生物膜中唯一的厌氧甲烷氧化细菌,可能负责由甲烷驱动的铬酸盐生物还原。提出了微生物 AOM 偶联铬酸盐还原的两种可能途径:(i) Candidatus 'Methanoperedens' 独立地将铬酸盐用作电子受体形成 Cr(III)化合物,或 (ii) Candidatus 'Methanoperedens' 将甲烷氧化生成中间体或电子,这些中间体或电子将被未知的铬酸盐还原剂协同用于将铬酸盐还原为 Cr(III)化合物。我们的发现表明,生物地球化学铬和甲烷循环之间可能存在联系。

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