The Impact of Agricultural Soil Erosion on the Global Carbon Cycle

The Impact of Agricultural Soil Erosion on the Global Carbon Cycle

26 October 2007 | K. Van Oost, T. A. Quine, G. Govers, S. De Gryze, J. Six, J. W. Harden, J. C. Ritchie, G. W. McCarty, G. Heckath, C. Kosmas, J. V. Giraldez, J. R. Marques da Silva, R. Merckx
The article "The Impact of Agricultural Soil Erosion on the Global Carbon Cycle" by K. Van Oost et al. explores the impact of agricultural soil erosion on the global carbon cycle. The authors use caesium-137 and carbon inventory measurements from a large-scale survey to find evidence of an erosion-induced sink of atmospheric carbon, equivalent to approximately 26% of the carbon transported by erosion. Based on this, they estimate a global carbon sink of 0.12 petagrams of carbon per year from erosion in agricultural landscapes. This challenges the view that agricultural erosion is an important source or sink for atmospheric CO2. The study examines three key mechanisms by which soil erosion can affect carbon flux: replacement of SOC at eroding sites, deep burial of SOC, and enhanced decomposition of SOC during transport. The authors conclude that the integrated effect of these processes is more complex than previously thought, and their findings provide new insights into the role of agricultural soil erosion in the global carbon cycle.The article "The Impact of Agricultural Soil Erosion on the Global Carbon Cycle" by K. Van Oost et al. explores the impact of agricultural soil erosion on the global carbon cycle. The authors use caesium-137 and carbon inventory measurements from a large-scale survey to find evidence of an erosion-induced sink of atmospheric carbon, equivalent to approximately 26% of the carbon transported by erosion. Based on this, they estimate a global carbon sink of 0.12 petagrams of carbon per year from erosion in agricultural landscapes. This challenges the view that agricultural erosion is an important source or sink for atmospheric CO2. The study examines three key mechanisms by which soil erosion can affect carbon flux: replacement of SOC at eroding sites, deep burial of SOC, and enhanced decomposition of SOC during transport. The authors conclude that the integrated effect of these processes is more complex than previously thought, and their findings provide new insights into the role of agricultural soil erosion in the global carbon cycle.
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