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甲烷相关微生物生态过程可显著提升林丹污染稻田的自净能力。

Methane-associated micro-ecological processes crucially improve the self-purification of lindane-polluted paddy soil.

机构信息

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.

出版信息

J Hazard Mater. 2021 Apr 5;407:124839. doi: 10.1016/j.jhazmat.2020.124839. Epub 2020 Dec 14.

Abstract

Reductive dechlorination, an efficient pathway for complete removal of organic chlorinated pollutants (OCPs), is commonly reported to be coupled to oxidation of methane (CH) or methanogenesis in anaerobic environments. However, the relationship between dechlorination and CH-associated bioprocesses is unclear. Based on the hypothesis that CH supplementation could facilitate OCP dechlorination, we investigated the role of CH-associated bioprocesses in the self-purification of flooded lindane-spiked paddy soils. Four treatments were conducted for up to 28 days: sterilized soil (S), sterilized soil + CH (SC), non-sterilized soil (NS), and non-sterilized soil + CH (NSC). Results indicated that both sterilization and addition of CH promoted lindane degradation and CH emissions in the flooded paddy soils. In the NS treatment, lindane had the lowest degradation rate when CH emissions were barely detected; while in the SC treatment, lindane had the highest degradation rate when CH achieved its highest emissions from anaerobic soil. Also, sterilization led to microbial diversity loss and functional recession, but increased ferrous ion [Fe(II)] concentrations compared to non-sterilized soils. Methanogenic communities and mcrA gene recovered faster than the majority of microorganisms (e.g., Fe bacteria, Bdellovibrionaceae, Rhizobiaceae, Dehalogenimonas) or functional genes (e.g., Dhc, Geo, narG, nirS). Collectively, we assume the enhanced removal of lindane may partly be due to both abiotic dechlorination promoted by chemical Fe redox processes and methanogenesis-derived biotic dechlorination. Revealing the coupling between dechlorination and CH-associated bioprocesses is helpful to resolve both pollution remediation and mitigation of CH emissions in anaerobic contaminated sites.

摘要

还原脱氯是一种有效去除有机氯化污染物(OCPs)的途径,通常与甲烷(CH)或厌氧环境中的产甲烷作用的氧化耦合。然而,脱氯与 CH 相关生物过程之间的关系尚不清楚。基于 CH 补充可以促进 OCP 脱氯的假设,我们研究了 CH 相关生物过程在受污染的水淹林丹污染稻田的自净化中的作用。进行了四个处理,时间长达 28 天:灭菌土壤(S)、灭菌土壤+CH(SC)、非灭菌土壤(NS)和非灭菌土壤+CH(NSC)。结果表明,灭菌和添加 CH 都促进了水淹稻田中林丹的降解和 CH 的排放。在 NS 处理中,当几乎检测不到 CH 排放时,林丹的降解率最低;而在 SC 处理中,当从厌氧土壤中 CH 排放达到最高时,林丹的降解率最高。此外,灭菌导致微生物多样性丧失和功能衰退,但与非灭菌土壤相比,亚铁离子[Fe(II)]浓度增加。与大多数微生物(如 Fe 细菌、Bdellovibrionaceae、根瘤菌科、Dehalogenimonas)或功能基因(如 Dhc、Geo、narG、nirS)相比,产甲烷群落和 mcrA 基因恢复得更快。总的来说,我们假设林丹的去除增强可能部分归因于化学 Fe 氧化还原过程促进的非生物脱氯和产甲烷衍生的生物脱氯。揭示脱氯与 CH 相关生物过程之间的耦合有助于解决厌氧污染场地的污染修复和 CH 排放缓解问题。

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