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Evolution of the microbial community of the biofilm in a methane-based membrane biofilm reactor reducing multiple electron acceptors

机译:甲烷基膜生物膜反应器中生物膜微生物群落的进化,减少了多个电子受体

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Previous work documented complete perchlorate reduction in a membrane biofilm reactor (MBfR) using methane as the sole electron donor and carbon source. This work explores how the biofilm's microbial community evolved as the biofilm stage-wise reduced different combinations of perchlorate, nitrate, and nitrite. The initial inoculum, carrying out anaerobic methane oxidation coupled to denitrification (ANMO-D), was dominated by uncultured Anaerolineaceae and Ferruginibacter sp. The microbial community significantly changed after it was inoculated into the CH4-based MBfR and fed with a medium containing perchlorate and nitrite. Archaea were lost within the first 40 days, and the uncultured Anaerolineaceae and Ferruginibacter sp. also had significant losses. Replacing them were anoxic methanotrophs, especially Methylocystis, which accounted for more than 25 % of total bacteria. Once the methanotrophs became important, methanol-oxidizing denitrifying bacteria, namely, Methloversatilis and Methylophilus, became important in the biofilm, probably by utilizing organic matter generated by the metabolism of methanotrophs. When methane consumption was equal to the maximum-possible electron-donor supply, Methylomonas, also an anoxic methanotroph, accounted for > 10 % of total bacteria and remained a major part of the community until the end of the experiments. We propose that aerobic methane oxidation coupled to denitrification and perchlorate reduction (AMO-D and AMO-PR) directly oxidized methane and reduced NO3- to NO2- or N2O under anoxic condition, producing organic matter for methanol-assimilating denitrification and perchlorate reduction (MA-D and MA-PR) to reduce NO3-. Simultaneously, bacteria capable of anaerobic methane oxidation coupled to denitrification and perchlorate reduction (ANMO-D and ANMO-PR) used methane as the electron donor to respire NO3- or ClO4- directly.
机译:先前的工作记录了使用甲烷作为唯一电子供体和碳源的膜生物膜反应器(MBfR)中的高氯酸盐完全还原。这项工作探索了生物膜的微生物群落如何随着生物膜逐步减少高氯酸盐,硝酸盐和亚硝酸盐的不同组合而演化。最初的接种物进行无氧甲烷氧化与反硝化作用(ANMO-D),主要是未经培养的厌氧杆菌和费氏杆菌属。微生物群落接种到基于CH4的MBfR中并加入含高氯酸盐和亚硝酸盐的培养基后,微生物群落发生了显着变化。在开始的40天内,古细菌消失了,未培养的厌氧杆菌和Ferruginibacter sp.。也有重大损失。替代它们的是缺氧的甲烷营养菌,尤其是甲基囊藻,其占细菌总数的25%以上。一旦甲烷营养生物变得重要,可能通过利用甲烷营养生物的代谢产生的有机物,甲醇氧化反硝化细菌,即甲硫菊酯和嗜甲基菌在生物膜中就变得重要。当甲烷消耗量等于最大可能的电子供体供应量时,也是缺氧的甲烷营养生物的甲基单孢菌占细菌总数的10%以上,并且在实验结束之前仍是群落的主要部分。我们建议将好氧甲烷氧化与脱氮和高氯酸盐还原(AMO-D和AMO-PR)耦合直接氧化甲烷,并在缺氧条件下将NO3-还原为NO2-或N2O,产生有机物用于甲醇同化反硝化和高氯酸盐还原(MA -D和MA-PR)还原NO3-。同时,能够进行厌氧甲烷氧化并结合反硝化和高氯酸盐还原的细菌(ANMO-D和ANMO-PR)使用甲烷作为电子供体,直接吸收NO3-或ClO4-。

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