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一种缓释基质可长期刺激地下水微生物群落原位还原六价铬。

A Slow-Release Substrate Stimulates Groundwater Microbial Communities for Long-Term in Situ Cr(VI) Reduction.

机构信息

Institute for Environmental Genomics, and Department of Microbiology and Plant Biology, University of Oklahoma , Norman, Oklahoma 73019, United States.

Earth Science Division, Lawrence Berkeley National Laboratory , Berkeley, California 94270, United States.

出版信息

Environ Sci Technol. 2015 Nov 3;49(21):12922-31. doi: 10.1021/acs.est.5b00024. Epub 2015 Oct 23.

Abstract

Cr(VI) is a widespread environmental contaminant that is highly toxic and soluble. Previous work indicated that a one-time amendment of polylactate hydrogen-release compound (HRC) reduced groundwater Cr(VI) concentrations for >3.5 years at a contaminated aquifer; however, microbial communities responsible for Cr(VI) reduction are poorly understood. In this study, we hypothesized that HRC amendment would significantly change the composition and structure of groundwater microbial communities, and that the abundance of key functional genes involved in HRC degradation and electron acceptor reduction would increase long-term in response to this slowly degrading, complex substrate. To test these hypotheses, groundwater microbial communities were monitored after HRC amendment for >1 year using a comprehensive functional gene microarray. The results showed that the overall functional composition and structure of groundwater microbial communities underwent sequential shifts after HRC amendment. Particularly, the abundance of functional genes involved in acetate oxidation, denitrification, dissimilatory nitrate reduction, metal reduction, and sulfate reduction significantly increased. The overall community dynamics was significantly correlated with changes in groundwater concentrations of microbial biomass, acetate, NO3-, Cr(VI), Fe(II) and SO4(2-). Our results suggest that HRC amendment primarily stimulated key functional processes associated with HRC degradation and reduction of multiple electron acceptors in the aquifer toward long-term Cr(VI) reduction.

摘要

六价铬是一种广泛存在的环境污染物,具有高度毒性和可溶性。先前的工作表明,一次性添加聚乳酸氢释放化合物(HRC)可将受污染含水层中的地下水中六价铬浓度降低 3.5 年以上;然而,负责还原六价铬的微生物群落仍知之甚少。在这项研究中,我们假设 HRC 添加剂会显著改变地下水微生物群落的组成和结构,并且与 HRC 降解和电子受体还原相关的关键功能基因的丰度会长期增加,以应对这种缓慢降解的复杂底物。为了验证这些假设,我们使用综合功能基因微阵列监测了 HRC 添加剂添加后超过 1 年的地下水微生物群落。结果表明,HRC 添加后,地下水微生物群落的整体功能组成和结构经历了连续的转变。特别是,参与乙酸氧化、反硝化、异化硝酸盐还原、金属还原和硫酸盐还原的功能基因的丰度显著增加。总体群落动态与微生物生物量、乙酸、NO3-、Cr(VI)、Fe(II)和 SO4(2-)在地下水中的浓度变化显著相关。我们的结果表明,HRC 添加剂主要刺激了与 HRC 降解和含水层中多种电子受体还原相关的关键功能过程,以实现长期的 Cr(VI)还原。

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