Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China; Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Hangzhou 310058, China.
Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China; Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Hangzhou 310058, China.
J Hazard Mater. 2019 Jul 15;374:258-266. doi: 10.1016/j.jhazmat.2019.04.040. Epub 2019 Apr 14.
Methanogenesis is commonly mass-produced under anaerobic conditions and serves as a major terminal electron accepting process driving the degradation of organic biomass. In this study, a cofactor of methanogenesis (coenzyme M, CoM) and a classic methanogensis inhibitor (2-bromoethanesulfonate, BES) were added at different concentrations to investigate how methanogenesis would affect PCP degradation in flooded soil. Strikingly, the processes of methanogenesis and PCP degradation were simultaneously promoted with CoM, or inhibited with BES, significantly (p < 0.05). High-throughput sequencing for soil bacterial and archaeal community structures revealed that members of Desulfitobacterium, Dethiobacter, Sedimentibacter, Bacillus and Methanosarcina might act as the core functional groups jointly perform PCP degradation in flooded soil, possibly through assisting microbial mediated dechlorination in direct organohalide-respiration, and/or indirect co-metabolization in complex anaerobic soil conditions. This study implied an underlying synergistic coupling between methanogenesis and dechlorination, and provided insights into a novel consideration with respect to coordinating methanogenesis while promoting anaerobic degradation of PCP for complex polluted soil environment, which is necessary for the improved all-win remediation.
产甲烷作用通常在厌氧条件下大量产生,是驱动有机生物质降解的主要末端电子接受过程。在本研究中,以不同浓度添加产甲烷作用的辅助因子(辅酶 M,CoM)和经典的产甲烷作用抑制剂(2-溴乙烷磺酸盐,BES),以研究产甲烷作用如何影响水淹土壤中五氯酚的降解。惊人的是,CoM 同时促进了产甲烷作用和五氯酚的降解,BES 则显著抑制了它们的降解(p<0.05)。土壤细菌和古菌群落结构的高通量测序显示,脱硫杆菌、脱硫弧菌、沉积杆菌、芽孢杆菌和产甲烷菌的成员可能作为核心功能群共同在水淹土壤中进行五氯酚的降解,可能通过协助微生物介导的直接有机卤化物呼吸中的脱氯作用,和/或在复杂的厌氧土壤条件下通过间接共代谢作用。本研究暗示了产甲烷作用和脱氯作用之间存在潜在的协同耦合,并为协调产甲烷作用以促进复杂污染土壤环境中五氯酚的厌氧降解提供了新的考虑,这对于改善双赢修复是必要的。