Assessment of Soil Organic Carbon Stock in the Upper Yangtze River Basin  

作　　者：WANG Xiao-guo ZHU Bo HUA Ke-ke LUO Yong ZHANG Jian ZHANG An-bang 

机构地区：[1]Key Laboratory of Mountain Surface Processes and Ecological Regulation,Chinese Academy of Sciences [2]Henan Institute of Science and Technology

出　　处：《Journal of Mountain Science》2013年第5期866-872,共7页山地科学学报（英文）

基　　金：funded by Special Program of Strategic Science and Technology of Chinese Academy of Sciences (Grant No. XDA05050506);State Key and Basic Research Development Planning (Grant No. 2012CB417101);Project of Natural Science Foundation of China (Grant No. 40901134);West Light Foundation of Chinese Academy of Sciences

摘　　要：Soil organic carbon is of great importance to terrestrial ecosystems. Studies on the amount and spatial distribution of soil organic carbon stock in various types of soil can help to better understand the role of soil in the global carbon cycle and provide a scientific basis for the assessment of the magnitude of carbon stored in a given area. Here we present estimates of soil organic carbon stock in soils in the upper reaches of the Yangtze River based on soil types as defined by Chinese Soil Taxonomy and recently compiled into a digital soil database. The results showed that the total soil organic carbon stock of the upper Yangtze River to a depth of 100 cm was 1.452x1013 kg. The highest soil organic carbon stock was found in felty soils （2.419x10TM kg）, followed by dark brown soils （1.269x10=kg）, and dark feltysoils （L139x10=kg）. Chernozems and irrigation silting soils showed the lowest soil organic carbon stock, mainly due to the small total area of such soils. The soil organic carbon density of these major soil types ranged from 5.6 to 26.1 kg m2- The average soil organic carbon density of the upper reaches of the Yangtze River was 16.4 kg m-2, which was higher than that of the national average. Soil organic carbon density indicated a distinct decreasing trend from west to east, which corresponds to the pattern of increasing temperature from cold to subtropical.

关 键 词：SOIL Organic carbon Carbon stock YangtzeRiver 

分 类 号：S153.6[农业科学—土壤学]