Atmospheric CH 4 oxidation by Arctic permafrost and mineral cryosols as a function of water saturation and temperature

Stackhouse, B.; Lau, M. C.  Y.; Vishnivetskaya, T.; Burton, N.; Wang, R.; Southworth, A.; Whyte, L.; Onstott, T. C.

doi:10.1111/gbi.12193

Title: Atmospheric CH ₄ oxidation by Arctic permafrost and mineral cryosols as a function of water saturation and temperature

Journal Article · Fri Jul 29 00:00:00 EDT 2016 · Geobiology

DOI:https://doi.org/10.1111/gbi.12193· OSTI ID:1536727

Stackhouse, B. ^[1]; Lau, M. C. Y. ^[1]; Vishnivetskaya, T. ^[2]; Burton, N. ^[1]; Wang, R. ^[1]; Southworth, A. ^[1]; Whyte, L. ^[3]; Onstott, T. C. ^[1]

Department of Geosciences, Princeton University, Princeton NJ USA
The Center for Environmental Biotechnology, University of Tennessee, Knoxville TN USA
Department of Natural Resource Sciences, McGill University, Montreal QC Canada

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Research Organization:: Princeton Univ., NJ (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

DOE Contract Number:: SC0004902

OSTI ID:: 1536727

Journal Information:: Geobiology, Vol. 15, Issue 1; ISSN 1472-4677

Publisher:: Wiliey

Country of Publication:: United States

Language:: English

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