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Inclusion of soil carbon lateral movement alters terrestrial carbon budget in China

机译:纳入土壤碳横向运动会改变中国的陆地碳收支

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The lateral movement of soil carbon has a profound effect on the carbon budget of terrestrial ecosystems; however, it has never been quantified in China, which is one of the strongest soil erosion areas in the world. In this study, we estimated that the overall soil erosion in China varies from 11.27 to 18.17?Pg yr?1 from 1982 to 2011, accounting for 7–21% of total soil erosion globally. Soil erosion induces a substantial lateral redistribution of soil organic carbon ranging from 0.64 to 1.04?Pg C yr?1. The erosion-induced carbon flux ranges from a 0.19?Pg C yr?1 carbon source to a 0.24?Pg C yr?1 carbon sink in the terrestrial ecosystem, which is potentially comparable in magnitude to previously estimated total carbon budget of China (0.19 to 0.26?Pg yr?1). Our results showed that the lateral movement of soil carbon strongly alters the carbon budget in China, and highlighted the urgent need to integrate the processes of soil erosion into the regional or global carbon cycle estimates.
机译:土壤碳的横向运动对陆地生态系统的碳收支有着深远的影响。但是,中国从未被量化,中国是世界上土壤侵蚀最严重的地区之一。在这项研究中,我们估计从1982年到2011年,中国的总体土壤侵蚀在11.27至18.17?Pg yr ?1 之间,占全球总土壤侵蚀的7-21%。水土流失引起土壤有机碳在0.64〜1.04?Pg C yr ?1 范围内的大量横向再分布。侵蚀引起的碳通量范围从陆地生态系统中的0.19?Pg C yr ?1 碳源到0.24?Pg C yr ?1 碳汇。规模可能与之前估算的中国总碳预算(0.19至0.26?Pg yr ?1 )相当。我们的结果表明,土壤碳的横向运动极大地改变了中国的碳收支,并强调了将土壤侵蚀过程纳入区域或全球碳循环估算的迫切需要。

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