Titlebook: Recarbonization of the Biosphere; Ecosystems and the G Rattan Lal,Klaus Lorenz,Joachim von Braun Book 2012 Springer Science+Business Media

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Potential Carbon Emission Trajectories of Shanghai, China from 2007 to 2050,

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Soil Carbon and Nitrogen Interactions and Biosphere-Atmosphere Exchange of Nitrous Oxide and Methan

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atlands, tropical rainforests, tropical savannas, grasslands, degraded/desertified lands, agricultural lands, and urban lands. However, land-based sinks require long-term management and a protection strategy because C stocks grow with a progressive improvement in ecosystem health.978-94-007-9907-3978-94-007-4159-1

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Book 2012, degraded/desertified lands, agricultural lands, and urban lands. However, land-based sinks require long-term management and a protection strategy because C stocks grow with a progressive improvement in ecosystem health.

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es in carbon dioxide and for recarbonization of the biospherHuman activities are significantly modifying the natural global carbon (C) cycles, and concomitantly influence climate, ecosystems, and state and function of the Earth system. Ever increasing amounts of carbon dioxide (CO2) are added to the

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Book 2012tion of the Earth system. Ever increasing amounts of carbon dioxide (CO2) are added to the atmosphere by fossil fuel combustion but the biosphere is a potential C sink. Thus, a comprehensive understanding of C cycling in the biosphere is crucial for identifying and managing biospheric C sinks. Ecosy

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