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在河流岸边带近岸区域,反硝化作用的 NO 还原势较高。

High NO reduction potential by denitrification in the nearshore site of a riparian zone.

机构信息

Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China.

Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.

出版信息

Sci Total Environ. 2022 Mar 20;813:152458. doi: 10.1016/j.scitotenv.2021.152458. Epub 2021 Dec 23.

Abstract

As a potent atmospheric greenhouse gas and a major source of ozone depletion, nitrous oxide (NO) emission has been given increasing attention in aquatic systems, particularly at the aquatic-terrestrial interfaces, such as riparian zones. However, the microbial mechanisms regulating NO emission in riparian zones remain unknown. Here, we measured the contributions of denitrification and ammonium oxidation to NO emission along with the abundance and community structure of nirK-, nirS-, nosZ I- and nosZ II-harbouring bacteria in both surface sediments (0-10 cm) and overlying water along a lake riparian zone (including nearshore sites and offshore sites). Overall, the nearshore sites of the riparian zones emitted less NO than the offshore sites. Nearshore NO emission was dominated by denitrification with a high NO reduction rate, whereas offshore NO emission was driven by ammonium oxidation. Furthermore, NO derived from ammonium oxidation was influenced by the NH-N content, and denitrification NO was modulated by denitrifier communities. The NO-producing community was dominated by nirS-harbouring bacteria, while the NO-reducing community was dominated by nosZ I-harbouring bacteria. The relative abundance of Hydrogenophilales from nirS-denitrifiers and Chloroflexi unclassified from nosZ II-type communities influenced the NO produced by denitrification, according to high-throughput sequencing analysis. Additionally, we also found lower levels of NO production per unit volume in overlying water, which were 3-4 orders of magnitude less than in the surface sediment. Overall, we propose that using riparian zones can be an effective management tool for NO mitigation by enhancing the NO reduction process of denitrification and decreasing ammonium oxidation.

摘要

作为一种强效的大气温室气体和主要的臭氧消耗物质,氧化亚氮(NO)排放越来越受到水生系统的关注,特别是在水陆交界带,如河岸带。然而,河岸带中调节 NO 排放的微生物机制尚不清楚。在这里,我们测量了反硝化作用和氨氧化作用对 NO 排放的贡献,以及在沿湖滨岸带(包括近岸和远岸地点)的表层沉积物(0-10cm)和上覆水中 nirK-、nirS-、nosZ I-和 nosZ II 型细菌的丰度和群落结构。总的来说,湖滨带的近岸地点比远岸地点排放的 NO 更少。近岸 NO 排放主要由反硝化作用驱动,具有较高的 NO 还原速率,而远岸 NO 排放则由氨氧化作用驱动。此外,氨氧化产生的 NO 受 NH-N 含量的影响,而反硝化作用产生的 NO 受反硝化菌群落的调节。产生 NO 的群落主要由携带 nirS 的细菌主导,而还原 NO 的群落主要由携带 nosZ I 的细菌主导。nirS-反硝化菌中的 Hydrogenophilales 和 nosZ II 型群落中的 Chloroflexi unclassified 的相对丰度影响反硝化作用产生的 NO,这是根据高通量测序分析得出的。此外,我们还发现上覆水中单位体积的 NO 生成量较低,比表层沉积物低 3-4 个数量级。总的来说,我们提出利用河岸带可以通过增强反硝化作用的 NO 还原过程和减少氨氧化作用来有效管理 NO 减排。

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