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Biotic and abiotic transformation of a volatile organics plume in a semiarid vadose zone

机译:半干旱渗流区中挥发性有机物羽流的生物和非生物转化

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An evaluation of biotic and abiotic attenuation processes potentially important to chlorinated and non-chlorinated volatile organic compound (VOC) fate and transport in the 148 meter thick vadose zone beneath the Chemical Waste Landfill (CWL) was conducted. A unique feature of this evaluation is the comparison of two estimates of VOC mass present in the soil gas, pore-water, and solid phases (but not including mass as non-aqueous phase liquid [NAPL]) of the vadose zone in 1993. One estimate, 1,800 kg, was obtained from vadose zone transport modeling that incorporated molecular diffusion and volatilization to the atmosphere, but not biotic or chemical processes. The other estimate, 2,120 kg, was obtained from the usm of VOC mass physically removed during soil vapor extraction and an estimate of VOC mass remaining in the vadose zone in 1998, both adjusted to exclude NAPL mass. This comparison indicates that biogeochemical processes were at best slightly important to historical VOC plume development. Some evidence of aerobic degradation of non-chlorinated VOCs and abiotic transformation of 1,1,1-Trichloroethane was identified. Despite potentially amenable site conditions, no evidence was found of cometabolic and anaerobic transformation pathways. Relying principally on soil-gas analytical results, an upper-bound estimate of 21 percent mass reduction due to natural biogeochemical processes was developed. Although available information for the CWL indicates that natural atteruation processes other than volatilization to the atmosphere did not effectively enhance groundwater protection, these processes could be important in significantly reducing groundwater contamination and exposure risks at other sites. More laboratory and field research is required to improve our collective ability to characterize and exploit natural VOC attenuation processes, especially with respect to the combination of relatively thick and dry vadose zones and chlorinated VOCs.
机译:对生物和非生物减毒过程进行了评估,这些过程对于氯化废物和非氯化挥发性有机化合物(VOC)的命运以及在化学废物掩埋场(CWL)下148米厚的渗流区中的运输具有潜在的重要性。该评估的一个独特之处是比较了1993年渗流区土壤气体,孔隙水和固相中存在的VOC质量的两个估计值(但不包括非水相液体[NAPL]的质量)。从渗流区迁移模型获得了1,800 kg的估计值,该模型结合了分子向大气的扩散和挥发,但没有结合生物或化学过程。另一个估算值是2,120 kg,是从土壤蒸汽提取过程中物理去除的VOC质量的usm和1998年渗流区中残留的VOC质量估算得出的,两者均进行了调整,以排除NAPL的质量。该比较表明,生物地球化学过程至多对历史VOC羽流的发育至为重要。鉴定出一些证据表明有氧降解了非氯代挥发性有机化合物,以及1,1,1-三氯乙烷的非生物转化。尽管可能存在适宜的场地条件,但未发现有关代谢和厌氧转化途径的证据。主要依靠土壤气体分析结果,对由于自然生物地球化学过程而导致的质量下降21%进行了上限估算。尽管CWL的可用信息表明,除了向大气挥发以外,自然散发过程并不能有效地增强对地下水的保护,但这些过程对于显着减少其他地方的地下水污染和暴露风险可能是重要的。需要更多的实验室和现场研究来提高我们表征和利用天然VOC衰减过程的集体能力,尤其是在相对较厚和干燥的渗流带和氯化VOC组合方面。

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