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

被引:24
作者
Amos, Richard T. [1 ]
Bekins, Barbara A. [2 ]
Delin, Geoffrey N. [3 ]
Cozzarelli, Isabelle M. [4 ]
Blowes, David W. [1 ]
Kirshtein, Julie D. [4 ]
机构
[1] Univ Waterloo, Dept Earth & Environm Sci, Waterloo, ON N2L 3G1, Canada
[2] US Geol Survey, Menlo Pk, CA 94025 USA
[3] US Geol Survey, Denver, CO 80225 USA
[4] US Geol Survey, Natl Ctr 431, Reston, VA 20192 USA
基金
加拿大自然科学与工程研究理事会;
关键词
Methane oxidation; Natural attenuation; Direct push profiling; Gas bubble entrapment; Dissolved gases; NATURAL ATTENUATION PROCESSES; SPILL SITE; BIOGEOCHEMICAL GRADIENTS; ISOTOPE RATIOS; GRAVEL AQUIFER; SHALLOW SAND; WATER; STREAMS; SYSTEM; CARBON;
D O I
10.1016/j.jconhyd.2011.04.003
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
High resolution direct-push profiling over short vertical distances was used to investigate CH4 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 CH4 and CO2, and the presence of methanotrophic bacteria. Sharp redox gradients were observed near the water table. Shifts in delta C-13(CH4) from an average of -57.6% (+/- 1.7 parts per thousand) in the methanogenic zone to -39.6 parts per thousand (+/- 8.7 parts per thousand) at 105 m downgradient, strongly suggest CH4 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 CH4 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 CH4 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. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:13 / 25
页数:13
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