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

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Verfahrensgrundlagen der Angebotskalkulationnge to the overall cycle are agricultural intensification and land-use change, particularly in tropical regions. These processes should be evaluated carefully as causal factors for imbalances in global budgets of nitrogen-containing trace gases.

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Agriculture, the Global Nitrogen Cycle, and Trace Gas Fluxnge to the overall cycle are agricultural intensification and land-use change, particularly in tropical regions. These processes should be evaluated carefully as causal factors for imbalances in global budgets of nitrogen-containing trace gases.

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Gerhard Girmscheid,Christoph Motzkospheric carbon dioxide can be analyzed in terms of biogeochemical cycles that transfer carbon between reservoirs. The small atmospheric reservoir is closely linked to other small reservoirs, shallow sea and biota. Transfer of carbon between these small reservoirs is rapid; residence times are short.

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Gerhard Girmscheid,Christoph Motzkothe last 150,000 years). Of special interest is the most direct evidence of past changes in radiatively active trace gases found in the ice record. We present here a review of the results concerning three of the main radiatively active gases: CO., CH., and N.O..The record indicates that the three ga