Human 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 atmosphere by fossil fuel combustion but the biosphere is a
Recarbonization of the Biosphere || Cropland Soil Carbon Dynamics
✍ Scribed by Lal, Rattan; Lorenz, Klaus; Hüttl, Reinhard F.; Schneider, Bernd Uwe; von Braun, Joachim
- Book ID
- 118050803
- Publisher
- Springer Netherlands
- Year
- 2012
- Tongue
- Dutch
- Weight
- 459 KB
- Edition
- 2012
- Category
- Article
- ISBN
- 9400741596
No coin nor oath required. For personal study only.
✦ Synopsis
Human 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 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. Ecosystems with large C stocks which must be protected and sustainably managed are wetlands, peatlands, 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.
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Human 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 atmosphere by fossil fuel combustion but the biosphere is a
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