Use of stable isotopes to determine methane oxidation in landfill cover soils

Abstract

The mean isotopic composition of CH 4 emitted from six New England (United States) landfills was 13 C and D enriched (−48.1 to −50.4‰ and −273 to −281‰) relative to anoxic zone landfill CH 4 (mean values of −55.9 to −56.2‰ and −296 to −300‰) owing to the oxidation of methane as it was transported from the landfill to the atmosphere through the soil cap. The fraction of methane oxidized f 0 during its passage through the soil cap was calculated from the degree of 13 C enrichment in emitted CH 4 relative to anoxic zone CH 4 in conjunction with values determined for the preference of soil methane oxidizing bacteria for 12 CH 4 over 13 CH 4 (α = 1.022 ± 0.008). Mean values for methane oxidation in six landfills were from 24 to 35% of the total flux through the soil during the warm season, depending upon how the data were grouped. Our results bracket recent estimates of methane oxidation of about 30% in the warm summer period produced using a model with the input terms of soil temperature, moisture, depth, and oxygen concentration. Because of variations in the response of methane oxidation to temperature at these New England sites, our study is consistent with the modeling results of Czepiel et al. [1996b] that the best estimate for the annual value for methane oxidation in the landfills considered is about 10%.