首页> 外文期刊>Journal of Contaminant Hydrology >Identification of abiotic and biotic reductive dechlorination in a chlorinated ethene plume after thermal source remediation by means of isotopic and molecular biology tools
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Identification of abiotic and biotic reductive dechlorination in a chlorinated ethene plume after thermal source remediation by means of isotopic and molecular biology tools

机译:利用同位素和分子生物学工具鉴定热源修复后的氯化乙烯羽流中的非生物和生物还原性脱氯

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摘要

Thermal tetrachloroethene (PCE) remediation by steam injection in a sandy aquifer led to the release of dissolved organic carbon (DOC) from aquifer sediments resulting in more reduced redox conditions, accelerated PCE biodegradation, and changes in microbial populations. These changes were documented by comparing data collected prior to the remediation event and eight years later. Based on the premise that dual C-Cl isotope slopes reflect ongoing degradation pathways, the slopes associated with PCE and TCE suggest the predominance of biotic reductive dechlorination near the source area. PCE was the predominant chlorinated ethene near the source area prior to thermal treatment. After thermal treatment, cDCE became predominant. The biotic contribution to these changes was supported by the presence of Dehalococcoides sp. DNA (Dhc) and Dhc targeted rRNA close to the source area. In contrast, dual C-CI isotope analysis together with the almost absent VC C-13 depletion in comparison to cDCE C-13 depletion suggested that cDCE was subject to abiotic degradation due to the presence of pyrite, possible surface-bound iron (II) or reduced iron sulphides in the downgradient part of the plume. This interpretation is supported by the relative lack of Dhc in the downgradient part of the plume. The results of this study show that thermal remediation can enhance the biodegradation of chlorinated ethenes, and that this effect can be traced to the mobilisation of DOC due to steam injection. This, in turn, results in more reduced redox conditions which favor active reductive dechlorination and/or may lead to a series of redox reactions which may consecutively trigger biotically induced abiotic degradation. Finally, this study illustrates the valuable complementary application of compound-specific isotopic analysis combined with molecular biology tools to evaluate which biogeochemical processes are taking place in an aquifer contaminated with chlorinated ethenes. (C) 2016 Elsevier B.V. All rights reserved.
机译:通过在砂质含水层中注水进行热四氯乙烯(PCE)修复,导致含水层沉积物中溶解有机碳(DOC)的释放,从而导致氧化还原条件进一步降低,PCE生物降解加速以及微生物种群的变化。通过比较修复事件之前和八年后收集的数据来记录这些更改。基于双C-Cl同位素斜率反映了正在进行的降解路径的前提,与PCE和TCE相关的斜率表明源区附近生物还原性脱氯的优势。 PCE是热处理前靠近源区的主要氯化乙烯。热处理后,cDCE占主导地位。 Dehalococcoides sp。的存在支持了这些变化的生物贡献。 DNA(Dhc)和Dhc靶向rRNA靠近源区域。相反,双重C-CI同位素分析以及与cDCE C-13耗尽相比几乎不存在的VC C-13耗尽表明,由于黄铁矿,可能的表面结合铁(II)的存在,cDCE易受非生物降解。或在羽流降级部分还原的硫化铁。羽流降级部分相对缺乏Dhc支持了这种解释。这项研究的结果表明,热修复可以增强氯化乙烯的生物降解作用,这种作用可以追溯到由于注入蒸汽而引起的DOC的动员。反过来,这导致更多的氧化还原条件降低,这有利于活性还原脱氯和/或可能导致一系列氧化还原反应,这些反应可以连续触发生物诱导的非生物降解。最后,这项研究说明了化合物特异性同位素分析与分子生物学工具相结合的有价值的补充应用,以评估在被氯化乙烯污染的含水层中发生了哪些生物地球化学过程。 (C)2016 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2016年第9期|1-19|共19页
  • 作者单位

    Univ Neuchatel, Ctr Hydrogeol & Geotherm CHYN, Rue Emile Argand 11, CH-2000 Neuchatel, Switzerland;

    Tech Univ Denmark DTU, Dept Environm Engn, DTU B113, DK-2800 Lyngby, Denmark;

    Geol Survey Denmark & Greenland GEUS, Dept Geochem, O Voldgade 10, DK-1350 Copenhagen K, Denmark;

    Univ Neuchatel, Ctr Hydrogeol & Geotherm CHYN, Rue Emile Argand 11, CH-2000 Neuchatel, Switzerland;

    SiREM, 130 Res Lane, Guelph, ON N1G 5G3, Canada;

    Univ Neuchatel, Ctr Hydrogeol & Geotherm CHYN, Rue Emile Argand 11, CH-2000 Neuchatel, Switzerland;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Chloroethenes; Stable isotopes; Molecular biology; Thermal treatment;

    机译:叶绿素;稳定同位素;分子生物学;热治疗;

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