Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

[sup 13]C/[sup 12]C fractionation of methane during oxidation in a temperate forested soil

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
 [1];  [2];  [3]
  1. Univ. of California, Irvine, CA (United States)
  2. Institute for the Study of Earth, Oceans and Space, Univ. of New Hampshire, Durham, NH (United States)
  3. National Institute of Water and Atmospheric Research, Lower Hutt (New Zealand)
The authors have made measurements of the [sup 13]C/[sup 12]C fractionation of methane (CH[sub 4]) during microbial oxidation by an upland temperate soil from College Woods, New Hampshire, using both in situ and laboratory incubation measurements. Uptake rates of 1-4.8 mg CH[sub 4]/m[sup 2]/d were measured during the active season in New Hampshire while rates of uptake were 2.6-6.8 mg CH[sub 4]/m[sup 2]/d in jars used for incubation studies. The fractionation factor, calculated from field measurements, was [alpha] = 0.978 [+-] .004. This corresponds to a kinetic isotope effect (KIE) of K[sub 12]/k[sub 13] = 1.022 [+-] .004. Only a small dependence on temperature was noted for air temperatures between 281 and 296 K. The results indicate that the KIE of soil CH[sub 4] oxidation is controlled by physical parameters based on gaseous diffusion into the soil. The implications of these results are discussed with respect to the global CH[sub 4] budget, and balancing CH[sub 4] sources and sinks through the use of [delta][sup 13]CH[sub 4] measurements.
OSTI ID:
7183197
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Journal Name: Geochimica et Cosmochimica Acta; (United States) Vol. 58:6; ISSN GCACAK; ISSN 0016-7037
Country of Publication:
United States
Language:
English