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Modeling of vapor intrusion from hydrocarbon-contaminated sources accounting for aerobic and anaerobic biodegradation

机译:建模从碳氢化合物污染源的蒸汽入侵,考虑到好氧和厌氧生物降解

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摘要

A one-dimensional steady state vapor intrusion model including both anaerobic and oxygen-limited aerobic biodegradation was developed. The aerobic and anaerobic layer thickness are calculated by stoichiometrically coupling the reactive transport of vapors with oxygen transport and consumption. The model accounts for the different oxygen demand in the subsurface required to sustain the aerobic biodegradation of the compound(s) of concern and for the baseline soil oxygen respiration. In the case of anaerobic reaction under methanogenic conditions, the model accounts for the generation of methane which leads to a further oxygen demand, due to methane oxidation, in the aerobic zone. The model was solved analytically and applied, using representative parameter ranges and values, to identify under which site conditions the attenuation of hydrocarbons migrating into indoor environments is likely to be significant. Simulations were performed assuming a soil contaminated by toluene only, by a BTEX mixture, by Fresh Gasoline and by Weathered Gasoline. The obtained results have shown that for several site conditions oxygen concentration below the building is sufficient to sustain aerobic biodegradation. For these scenarios the aerobic biodegradation is the primary mechanism of attenuation, i.e. anaerobic contribution is negligible and a model accounting just for aerobic biodegradation can be used. On the contrary, in all cases where oxygen is not sufficient to sustain aerobic biodegradation alone (e.g. highly contaminated sources), anaerobic biodegradation can significantly contribute to the overall attenuation depending on the site specific conditions.
机译:建立了包括厌氧和氧受限的需氧生物降解的一维稳态蒸气入侵模型。需氧和厌氧层的厚度是通过化学计量地将蒸汽的反应性传输与氧气的传输和消耗耦合来计算的。该模型说明了维持所关注化合物的有氧生物降解所需的地下不同的氧气需求,以及基线土壤的氧气呼吸。在产甲烷条件下进行厌氧反应的情况下,该模型考虑了甲烷的产生,由于在好氧区中甲烷的氧化,甲烷的产生进一步导致了氧气需求。该模型经过解析求解,并使用代表性的参数范围和值进行了应用,以识别在哪种场所条件下迁移到室内环境的碳氢化合物的衰减可能很显着。假设土壤仅被甲苯,BTEX混合物,新鲜汽油和风化汽油污染,则进行模拟。获得的结果表明,在几个场所条件下,建筑物以下的氧气浓度足以维持需氧生物降解。对于这些情况,好氧生物降解是衰减的主要机制,即厌氧影响可忽略不计,可以使用仅考虑好氧生物降解的模型。相反,在所有氧气不足以单独维持需氧生物降解的情况下(例如,高污染源),厌氧生物降解可显着促进总衰减,具体取决于场所的具体条件。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2011年第4期|p.167-180|共14页
  • 作者单位

    Department of Civil Engineering, University of Rome 'Tor Vergata', Via del Politecnico, 1, 00133 Rome, Italy;

    Department of Civil Engineering, University of Rome 'Tor Vergata', Via del Politecnico, 1, 00133 Rome, Italy;

  • 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

    vapor intrusion; modeling; natural attenuation; contaminated sites;

    机译:蒸气侵入造型;自然衰减受污染的地点;

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