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National Scale Analysis of Soil Organic Carbon Storage in China Based on Chinese Soil Taxonomy

机译:基于中国土壤分类学的中国土壤有机碳储量国家规模分析

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摘要

Patterns of soil organic carbon (SOC) storage and density in various soil types or locations are the foundation for examining the role of soil in the global carbon cycle. An assessment of SOC storage and density patterns in China based on soil types as defined by Chinese Soil Taxonomy (CST) and the recently compiled digital 1:1000000 Soil Database of China was conducted to generate a rigorous database for the future study of SOC storage. First, SOC densities of 7 292 soil profiles were calculated and linked by soil type to polygons of a digital soil map using geographic information system resulting in a 1:1000 000 SOC density distribution map of China. Further results showed that soils in China covered 9 281 x 10~3 km~2 with a total SOC storage of 89.14 Gt and a mean SOC density 96.0 t ha~(-1). Among the 14 CST orders, Cambosols and Argosols constituted high percentage of China's total SOC storage, while Andosols, Vertosols, and Spodsols had a low percentage. As for SOC density, Histosols were the highest, while Primosols were the lowest. Specific patterns of SOC storage of various soil types at the CST suborder, group, and subgroup levels were also described. Results obtained from the study of SOC storage and density of all CST soil types would be not only useful for international comparative research, but also for more accurately estimating and monitoring of changes of SOC storage in China.
机译:各种土壤类型或位置中土壤有机碳(SOC)的存储方式和密度模式是检验土壤在全球碳循环中的作用的基础。根据中国土壤分类法(CST)定义的土壤类型以及最近编辑的数字1:1000000中国土壤数据库,对中国的SOC储存和密度模式进行了评估,以建立一个严格的数据库,以供将来研究SOC储存。首先,使用地理信息系统计算了7 292个土壤剖面的SOC密度,并通过土壤类型将其链接到数字土壤图的多边形,从而得出了1:100 000的中国SOC密度分布图。进一步的结果表明,中国土壤覆盖面积为9 281 x 10〜3 km〜2,总SOC储量为89.14 Gt,平均SOC密度为96.0 t ha〜(-1)。在这14批CST订单中,Cambosol和Argosols在中国的SOC总存储量中所占的比例很高,而Andosols,Vertosols和Spodsols所占的比例却较低。就SOC密度而言,组织溶胶最高,而Primosol最低。还描述了CST子阶,群和子群级别的各种土壤类型的SOC的特定存储模式。通过研究所有CST土壤类型的SOC储量和密度获得的结果不仅可用于国际比较研究,而且还可用于更准确地估算和监测中国SOC储量的变化。

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