首页> 外文期刊>Journal of Contaminant Hydrology >Methane oxidation in a crude oil contaminated aquifer: Delineation of aerobic reactions at the plume fringes
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Methane oxidation in a crude oil contaminated aquifer: Delineation of aerobic reactions at the plume fringes

机译:原油污染的含水层中的甲烷氧化:羽流边缘的好氧反应的轮廓

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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 C02, and the presence of methanotrophic bacteria. Sharp redox gradients were observed near the water table. Shifts in 813CCH_4 from an average of - 57.6‰ (±1.7‰) in the methanogenic zone to -39.6‰ (±8.7‰) at 105 m downgradient, strongly suggest CH_4 attenuation through microbially mediated degradation. In the downgradient zone the aerobic/anaerobic transition is up to 0.5 m 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.
机译:在短的垂直距离上进行高分辨率直接推压剖面分析,以研究明尼苏达州贝米吉附近被石油污染的含水层中CH_4的衰减。使用溶解的气体,氧化还原敏感组分,主要离子,CH_4和CO2中的碳同位素比以及甲烷营养细菌的存在来描绘污染物羽流。在地下水位附近观察到急剧的氧化还原梯度。 813CCH_4从产甲烷区的平均-57.6‰(±1.7‰)到105 m下降梯度处的转变为-39.6‰(±8.7‰),强烈表明CH_4通过微生物介导的降解而衰减。在降坡区,需氧/厌氧过渡段在地下水位以下达0.5 m,这表明O_2在整个地下水位上的迁移正在导致该界面CH_4的需氧降解。溶解的N_2浓度超过了与大气平衡时水的预期浓度,表明气泡截留,然后通过有氧降解CH_4或其他碳氢化合物优先剥离O_2。多变量和聚类分析被用来区分气泡大量滞留的区域和其他过程(例如富含O_2的补给水的渗透)是重要的O_2输送机制的区域。

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