Titlebook: Biogeochemistry of Global Change; Radiatively Active T Ronald S. Oremland (Chairman) Book 1993 Chapman & Hall, Inc. 1993 Atmospheric chemis

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Models of Oceanic and Terrestrial Sinks of Anthropogenic CO2: A Review of the Contemporary Carbon Cyaints on the partitioning of the CO. sink between land and sea, the conclusions are highly dependent on the δ.C value of the respired CO.. Understanding ecosystem dynamics with turnover times of 10–100 years is, thus, tantamount.

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Sulfur Gas Emissions from African Savanna-Burning thus contributing about 10% to the global COS flux. Concerning SO., emission factor (ΔSO./ΔCO.) ratios ranged from 27 x 10. to 65 x 10. (mean value 47 x 10.) during field experiments. Biomass-burning is estimated to release up to 0.3 Tg S/yr, which do not represent a significant SO. source on a glo

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Production of Methane and Nitrous Oxide by Organic Soils within a Northern Hardwood Forest Ecosystemuxes were negligible for the forest soil and relatively high for the organic soil. Interactions of several processes seemed to control nitrous oxide production by the soils and nitrous oxide fluxes observed .. When fluxes were weighted by the areal extent of these soil types in the forest, the ecosy