Investigations of Aerobic Methane Oxidation in Two Marine Seep Environments: Part 2—Isotopic Kinetics

During aerobic oxidation of methane (CH4) in seawater, a process which mitigates atmospheric emissions, the 12C‐isotopologue reacts with a slightly greater rate constant than the 13C‐isotopologue, leaving the residual CH4 isotopically fractionated. Prior studies have attempted to exploit this system...

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Veröffentlicht in:	Journal of geophysical research. Oceans 2019-11, Vol.124 (11), p.8392-8399
Hauptverfasser:	Chan, E. W., Shiller, A. M., Joung, D. J., Arrington, E. C., Valentine, D. L., Redmond, M. C., Breier, J. A., Socolofsky, S. A., Kessler, J. D.
Format:	Artikel
Sprache:	eng
Schlagworte:	Blooms Canyons Chemical analysis chemical kinetics Cultivation Fractionation Geophysics Incubation period Isotope fractionation Isotope ratios Isotopes Kinetics Leases Marine environment Mesocosms Methane methane oxidation Microorganisms Natural environment Ocean floor Oxidation Ratios Reaction kinetics Seawater Stable isotopes Substrates Water analysis
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