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在受原油污染的含水层中进行甲烷氧化:在羽流边缘描绘好需氧反应。

Methane oxidation in a crude oil contaminated aquifer: Delineation of aerobic reactions at the plume fringes.

机构信息

Dept. of Earth and Environmental Sciences, Univ. Waterloo, Waterloo, ON, N2L 3G1, Canada.

出版信息

J Contam Hydrol. 2011 Jul 1;125(1-4):13-25. doi: 10.1016/j.jconhyd.2011.04.003. Epub 2011 Apr 27.

DOI:10.1016/j.jconhyd.2011.04.003
PMID:21612840
Abstract

High resolution direct-push profiling over short vertical distances was used to investigate CH(4) attenuation in a petroleum contaminated aquifer near Bemidji, Minnesota. The contaminant plume was delineated using dissolved gases, redox sensitive components, major ions, carbon isotope ratios in CH(4) and CO(2), and the presence of methanotrophic bacteria. Sharp redox gradients were observed near the water table. Shifts in δ(13)C(CH4) from an average of -57.6‰ (±1.7‰) in the methanogenic zone to -39.6‰ (±8.7‰) at 105m downgradient, strongly suggest CH(4) attenuation through microbially mediated degradation. In the downgradient zone the aerobic/anaerobic transition is up to 0.5m below the water table suggesting that transport of O(2) across the water table is leading to aerobic degradation of CH(4) at this interface. Dissolved N(2) concentrations that exceeded those expected for water in equilibrium with the atmosphere indicated bubble entrapment followed by preferential stripping of O(2) through aerobic degradation of CH(4) or other hydrocarbons. Multivariate and cluster analysis were used to distinguish between areas of significant bubble entrapment and areas where other processes such as the infiltration of O(2) rich recharge water were important O(2) transport mechanisms.

摘要

采用高分辨率直接推送剖面技术,对明尼苏达州贝米吉附近受石油污染的含水层中的 CH(4)衰减进行了研究。利用溶解气体、氧化还原敏感成分、主要离子、CH(4)和 CO(2)中的碳同位素比值以及甲烷营养细菌的存在来描绘污染物羽流。在接近地下水位的地方观察到明显的氧化还原梯度。δ(13)C(CH4)从产甲烷区的平均-57.6‰(±1.7‰)向 105m 下游的-39.6‰(±8.7‰)的偏移强烈表明 CH(4)通过微生物介导的降解而衰减。在下向区,好氧/厌氧过渡区位于地下水位以下 0.5m 以内,这表明 O(2)通过地下水位的传输导致在该界面处有氧降解 CH(4)。溶解 N(2)浓度超过了与大气平衡的水的预期浓度,表明存在气泡捕获,随后通过 CH(4)或其他烃类的有氧降解优先去除 O(2)。多元和聚类分析用于区分显著气泡捕获区和其他过程(如富含 O(2)的补给水的渗透)重要的 O(2)传输机制的区域。

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