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Aerobic Biodegradation of Chlorinated Ethenes in a Fractured Bedrock Aquifer: Quantitative Assessment by Compound-Specific Isotope Analysis (CSIA) and Reactive Transport Modeling

机译:断裂基岩含水层中氯化乙烯的有氧生物降解:通过化合物特异性同位素分析(CSIA)和反应性运输模型进行定量评估

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摘要

A model-based analysis of concentration and isotope data was carried out to assess natural attenuation of chlorinated ethenes in an aerobic fractured bedrock aquifer. Tetrachlo-roethene (PCE) concentrations decreased downgradient of the source, but constant δ~(13)C signatures indicated the absence of PCE degradation. In contrast, geochemical and isotopic data demonstrated degradation of trichloroethene (TCE) and cis-1,2-dichloroethene (DCE) under the prevailing oxic conditions. Numerical modeling was employed to simulate isotopic enrichment of chlorinated ethenes and to evaluate alternative degradation pathway scenarios. Existing field information on groundwater flow, solute transport, geochemistry, and δ~(13)C signatures of the chlorinated ethenes was integrated via reactive transport simulations. The results provided strong evidence for the occurrence of aerobic TCE and DCE degradation. The chlorinated ethene concentrations together with stable carbon isotope data allowed us to reliably constrain the assessment of the extent of biodegradation at the site and plume simulations quantitatively linked aerobic biodegradation with isotope signatures in the field. Our investigation provides the first quantitative assessment of aerobicrnbiodegradation of chlorinated ethenes in a fractured rock aquifer based on compound specific stable isotope measurements and reactive transport modeling.
机译:对浓度和同位素数据进行了基于模型的分析,以评估需氧裂隙基岩含水层中氯化乙烯的自然衰减。四氯乙烯(PCE)浓度降低了源的降级,但是恒定的δ〜(13)C标记表明没有PCE降解。相反,地球化学和同位素数据表明,在普遍的含氧条件下,三氯乙烯(TCE)和顺式1,2-二氯乙烯(DCE)降解。数值模型被用来模拟氯化乙烯的同位素富集并评估替代降解途径的情景。通过反应输运模拟综合了有关地下水流动,溶质运移,地球化学和氯化乙烯的δ〜(13)C标记的现有现场信息。该结果为有氧TCE和DCE降解的发生提供了有力的证据。氯化乙烯的浓度以及稳定的碳同位素数据使我们能够可靠地限制对现场生物降解程度的评估,并且羽流模拟将好氧生物降解与现场同位素特征定量联系起来。我们的研究提供了基于化合物特定的稳定同位素测量值和反应性输运模型,对裂隙含水层中的氯乙烯进行好氧生物降解的定量评估。

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  • 来源
    《Environmental Science & Technology》 |2009年第19期|7458-7464|共7页
  • 作者单位

    Center for Applied Geoscience (ZAG), Eberhard-Karls University of Tuebingen, Sigwartstr. 10,D-72076 Tuebingen, Germany WorleyParsons, Infrastructure & Environment, 10240-124 Street,Edmonton AB, Canada.;

    Center for Applied Geoscience (ZAG), Eberhard-Karls University of Tuebingen, Sigwartstr. 10,D-72076 Tuebingen, Germany BRGM, 3 avenue Claude Guillemin, BP36009,45060 Orleans cedex 2, France.;

    Center for Applied Geoscience (ZAG), Eberhard-Karls University of Tuebingen, Sigwartstr. 10,D-72076 Tuebingen, Germany Instrumental Analytical Chemistry, University Duisburg-Essen,Lotharstr. 1, D-47048 Duisburg, Germany.;

    Center for Applied Geoscience (ZAG), Eberhard-Karls University of Tuebingen, Sigwartstr. 10,D-72076 Tuebingen, Germany;

    Department of Civil Engineering & Canadian Rivers Institute, University of New Brunswick, Fredericton NB, Canada;

    CSIRO Land and Water, Private Bag No. 5, Wembley WA 6913, Australia School of Earth and Environment, University of Western Australia, Crawley, Western Australia.;

  • 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
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  • 入库时间 2022-08-17 14:04:56

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