Van Oost K, Quine T A, Govers G, De Gryze S, Six J, Harden J W, Ritchie J C, McCarty G W, Heckrath G, Kosmas C, Giraldez J V, da Silva J R Marques, Merckx R
Physical and Regional Geography Research Group, Katholieke Universiteit Leuven, 3001 Heverlee, Belgium.
Science. 2007 Oct 26;318(5850):626-9. doi: 10.1126/science.1145724.
Agricultural soil erosion is thought to perturb the global carbon cycle, but estimates of its effect range from a source of 1 petagram per year(-1) to a sink of the same magnitude. By using caesium-137 and carbon inventory measurements from a large-scale survey, we found consistent evidence for an erosion-induced sink of atmospheric carbon equivalent to approximately 26% of the carbon transported by erosion. Based on this relationship, we estimated a global carbon sink of 0.12 (range 0.06 to 0.27) petagrams of carbon per year(-1) resulting from erosion in the world's agricultural landscapes. Our analysis directly challenges the view that agricultural erosion represents an important source or sink for atmospheric CO2.
农业土壤侵蚀被认为会扰乱全球碳循环,但其影响的估计范围从每年1皮克的碳源(-1)到同等规模的碳汇。通过对一项大规模调查中的铯-137和碳储量测量,我们发现了一致的证据,表明侵蚀导致的大气碳汇相当于侵蚀所输送碳的约26%。基于这种关系,我们估计全球农业景观中的侵蚀每年导致0.12(范围为0.06至0.27)皮克碳的碳汇(-1)。我们的分析直接挑战了农业侵蚀是大气二氧化碳的重要源或汇这一观点。