Journal
ENVIRONMENTAL SCIENCE & TECHNOLOGY
Volume 45, Issue 2, Pages 482-488Publisher
AMER CHEMICAL SOC
DOI: 10.1021/es1032585
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Funding
- NSERC
- CFI-LOF
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In order to gain regulatory approval for source zone natural attenuation (SZNA) at hydrocarbon-contaminated sites, knowledge regarding the extent of the contamination, its tendency to spread, and its longevity is required. However, reliable quantification of biodegradation rates, an important component of SZNA, remains a challenge. If the rate of CO2 gas generation associated with contaminant degradation can be determined, it may be used as a proxy for the overall rate of subsurface biodegradation. Here, the CO2-efflux at the ground surface is measured using a dynamic closed chamber (DCC) method to evaluate whether this technique can be used to assess the areal extent of the contaminant source zone and the depth-integrated rate of contaminant mineralization. To this end, a field test was conducted at the Bemidji, MN, crude oil spill site. Results indicate that at the Bemidji site the CO2-efflux method is able to both delineate the source zone and distinguish between the rates of natural soil respiration and contaminant mineralization. The average CO2-efflux associated with contaminant degradation in the source zone is estimated at 2.6 mu mol m(-2) s(-1), corresponding to a total petroleum hydrocarbon mineralization rate (expressed as C10H22) of 3.3 g m(-2) day(-1).
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