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基于微生物生态学理解单室微生物燃料电池中完全氨氮去除的机制。

Understanding complete ammonium removal mechanism in single-chamber microbial fuel cells based on microbial ecology.

机构信息

Korea Testing & Research Institute, Ulsan 44412, Republic of Korea.

Department of Civil and Environmental Engineering, Pusan National University, Busan 46241, Republic of Korea.

出版信息

Sci Total Environ. 2021 Apr 10;764:144231. doi: 10.1016/j.scitotenv.2020.144231. Epub 2020 Dec 24.

Abstract

The removal of organics and ammonium from domestic wastewater was successfully achieved by a flat-panel air-cathode microbial fuel cell (FA-MFC). To elucidate the reason for complete ammonium removal in the single-chamber MFCs, microbial communities were analyzed in biofilms on the surface of each anode, separator, and cathode of separator-electrode assemblies (SEAs). The spatial distribution of bacterial families related to the nitrogen cycle varied based on local conditions. Since oxygen diffusing from the air-cathode created a locally aerobic condition, ammonia-oxidizing bacteria (AOB) Nitrosomonadacea and nitrite-oxidizing bacteria (NOB) Nitrospiraceae were present near the cathode. NOB (12.1%) was more abundant than AOB (4.4%), suggesting that the nitrate produced by NOB may be reduced back to nitrite by heterotrophic denitrifiers such as Rhodocyclaceae (21.7%) and Comamonadaceae (5%) in the anoxic zone close to the NOB layer. Near that zone, the "nitrite loop" also substantially enriched two nitrite-reducing bacterial families: Ignavibacteriaceae (18.1%), facultative heterotrophs, and Brocadiaceae (11.2%), anaerobic ammonium oxidizing autotrophs. A larger inner area of biofilm contained abundant heterotrophic denitrifiers and fermentation bacteria. These results indicate that the large-surface SEA of FA-MFC allows counter-diffusion between substrates and oxygen, resulting in interactions of bacteria involved in the nitrogen cycle for complete ammonium removal.

摘要

采用平板式空气阴极微生物燃料电池(FA-MFC)成功实现了生活污水中有机物和铵的去除。为了阐明单室 MFC 中完全去除铵的原因,对分离-电极组件(SEA)各阳极、分离器和阴极表面生物膜中的微生物群落进行了分析。与氮循环有关的细菌家族的空间分布因局部条件而异。由于从空气阴极扩散的氧气形成局部好氧条件,因此氨氧化菌(AOB)硝化单胞菌和亚硝酸盐氧化菌(NOB)硝化螺旋菌科存在于阴极附近。NOB(约 12.1%)比 AOB(约 4.4%)更丰富,这表明由 NOB 产生的硝酸盐可能被靠近 NOB 层的缺氧区中的异养反硝化菌(如红环菌科(约 21.7%)和贪铜菌科(约 5%))还原回亚硝酸盐。在该区域附近,“亚硝酸盐循环”还大量富集了两种亚硝酸盐还原细菌家族:Ignavibacteriaceae(约 18.1%),兼性异养菌和Brocadiaceae(约 11.2%),厌氧氨氧化自养菌。生物膜的较大内区含有丰富的异养反硝化菌和发酵菌。这些结果表明,FA-MFC 的大表面积 SEA 允许底物和氧气的反向扩散,从而导致参与氮循环的细菌相互作用,实现完全去除铵。

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