Factors that control the stable carbon isotopic composition of methane produced in an anoxic marine sediment
- 21 September 1992
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 6 (3), 271-291
- https://doi.org/10.1029/92gb01650
Abstract
No abstract availableKeywords
This publication has 64 references indexed in Scilit:
- Isotopic composition of methane released from wetlands: Implications for the increase in atmospheric methaneGlobal Biogeochemical Cycles, 1988
- Measurements and interpretation of δ13C of methane from termites, rice paddies, and wetlands in KenyaGlobal Biogeochemical Cycles, 1988
- Biogeochemical aspects of atmospheric methaneGlobal Biogeochemical Cycles, 1988
- Seasonal variations of D/H and 13C/12C ratios of microbial methane in surface sedimentsNature, 1988
- Natural Abundances of Carbon Isotopes in Acetate from a Coastal Marine SedimentScience, 1987
- Seasonal Variations in the Stable Carbon Isotopic Signature of Biogenic Methane in a Coastal SedimentScience, 1986
- Graham's laws: Simple demonstrations of gases in motion: Part I, TheoryJournal of Chemical Education, 1969
- Fractionation of carbon isotopes and its temperature dependence in the system CO2-Gas-CO2 in solution and HCO3-CO2 in solutionEarth and Planetary Science Letters, 1968
- Graham's Laws of diffusion and effusionJournal of Chemical Education, 1967
- Gas Flow through the Mass Spectrometer Viscous LeakReview of Scientific Instruments, 1950