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在膜生物膜批式反应器中甲烷氧化偶联到高氯酸盐还原。

Methane oxidation coupled to perchlorate reduction in a membrane biofilm batch reactor.

机构信息

College of Environmental and Resource Science, Zhejiang University, Hangzhou, China; Zhejiang Province Key Lab Water Pollut Control & Envi, Zhejiang University, Hangzhou, Zhejiang, China; MOE Key Lab of Environmental Remediation and Ecosystem Health, College of Environmental and Resource Science, Zhejiang University, Hangzhou 310058, China.

Biodesign Swette Center for Environmental Biotechnology, Arizona State University, P.O. Box 875701, Tempe, AZ 85287-5701, USA.

出版信息

Sci Total Environ. 2019 Jun 1;667:9-15. doi: 10.1016/j.scitotenv.2019.02.330. Epub 2019 Feb 23.

Abstract

A specially designed CH-based membrane biofilm batch reactor (MBBR) was applied to investigate anaerobic methane oxidation coupled to perchlorate reduction (AnMO-PR). The 0.21 mM ClO added in the first stage of operation was completely reduced in 28 days, 0.40 mM ClO was reduced within 23 days in stage 2, and 0.56 mM of ClO was reduced within 30 days in stage 3. Although some chlorate (ClO) accumulated, the recovery of Cl was over 92%. Illumina sequencing of the 16S rRNA gene documented that the bacterial community was mainly composed by perchlorate-reducing bacteria (PRB), methanotrophic bacteria, and archaea. Real-time quantitative PCR showed the archaeal 16S rRNA and mcrA genes increased as more ClO was reduced, and the predominant archaea belonged to Methanosarcina mazei, which is related to ANME-3, an archaeon able to perform reverse methanogenesis. Several pieces of evidence support that ClO reduction by the MBBR biofilm occurred via a synergism between Methanosarcina and PRB: Methanosarcina oxidized methane through reverse methanogesis and provided electron donor for PRB to reduce ClO. Because methanotrophs were present, we cannot rule out that they also were involved in AnMO-PR if they received O generated by disproportionation of ClO from the PRB.

摘要

专门设计的基于 CH 的膜生物膜批式反应器 (MBBR) 被用于研究甲烷厌氧氧化偶联高氯酸盐还原 (AnMO-PR)。在运行的第一阶段添加的 0.21mM ClO 在 28 天内完全还原,在第二阶段 0.40mM ClO 在 23 天内还原,在第三阶段 0.56mM ClO 在 30 天内还原。尽管有一些氯酸盐 (ClO) 积累,但 Cl 的回收率超过 92%。16S rRNA 基因的 Illumina 测序记录表明,细菌群落主要由高氯酸盐还原菌 (PRB)、甲烷氧化菌和古菌组成。实时定量 PCR 显示,随着更多 ClO 的减少,古菌的 16S rRNA 和 mcrA 基因增加,主要的古菌属于 Methanosarcina mazei,它与能够进行反向产甲烷作用的 ANME-3 有关。有一些证据支持 MBBR 生物膜中的 ClO 还原是通过 Methanosarcina 和 PRB 之间的协同作用发生的:Methanosarcina 通过反向产甲烷作用氧化甲烷,并为 PRB 提供电子供体来还原 ClO。由于存在甲烷氧化菌,我们不能排除如果它们从 PRB 接收由 ClO 歧化产生的 O,它们也可能参与 AnMO-PR。

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