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Isotope fractionation in the systems CH4–H2O and CH4–CO2 during microbial methane genesis in the Earth's crust

✍ Scribed by L.K. Gutsalo


Book ID
116869102
Publisher
Siberian Branch of the Russian Academy of Sciences
Year
2008
Tongue
English
Weight
388 KB
Volume
49
Category
Article
ISSN
1068-7971

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Emissions ofN20, CH 4, and CO2 from soils at two sites in the tropical savanna of central Venezuela were determined during the dry season in February 1987. Measured arithmetic mean fluxes of N20, CH4, and CO2 from undisturbed soil plots to the atmosphere were 2.5 x 109, 4.3 x 10 I°, and 3.0 x 1013 m