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Soil Organic Carbon Changes for Croplands across China from 1991 to 2012

文献类型： 外文期刊

作者： He, Wentian 1 ; He, Ping 2 ; Jiang, Rong 2 ; Yang, Jingyi 4 ; Drury, Craig F. 4 ; Smith, Ward N. 3 ; Grant, Brian B. 3 ;

作者机构： 1.Beijing Acad Agr & Forestry Sci, Inst Plant Nutr & Resources, Beijing 100097, Peoples R China

2.Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Key Lab Plant Nutr & Fertilizer, Minist Agr & Rural Affairs, Beijing 100081, Peoples R China

3.Agr & Agri Food Canada, Ottawa Res & Dev Ctr, 960 Carling Ave, Ottawa, ON K1A 0C6, Canada

4.Agr & Agri Food Canada, Harrow Res & Dev Ctr, 2585 Cty Rd 20, Harrow, ON N0R 1G0, Canada

关键词： soil organic carbon; carbon stock; China's croplands; global climate change; CO2 emissions

期刊名称：AGRONOMY-BASEL （ 影响因子：3.417； 五年影响因子：3.64 ）

ISSN：

年卷期： 2021 年 11 卷 7 期

页码：

收录情况： SCI

摘要： Accurate estimates of soil organic carbon (SOC) are critical for evaluating the impacts of crop and nutrient management practices on soil sustainability and global climate change. Temporal and spatial variations in topsoil (0-0.20 m) SOC were analyzed using 43,743 soil samples in China's croplands. The soil database in our study was collected from the International Plant Nutrition Institute (IPNI) China Program. The results showed an increasing trend in SOC density (SOCD) for both grain and cash crops from 1991 to 2012. The average SOCD increased by 16.8, 17.4, 11.8 and 8.7% in the north central, northwest, southeast and southwest regions, respectively, whereas average SOCD decreased by 1.3% for the northeast region between the 1991-2001 and 2002-2012 periods. For both grain and cash crops, the SOCD frequency distribution (%) increased in the ranges of 10-20, 20-30 and 30-40 Mg C ha(-1) from the 1991-2001 to the 2002-2012, but decreased in the ranges of 0-10 and 50-60 Mg C ha(-1). Additionally, SOCD increased in most major soil types across China's cropland regions, except in phaeozems, chernozems and umbrisols, where it decreased by 8.6-18.7% mainly due to water runoff, soil erosion, and low C input. The overall SOC stock (SOCS) in China's cropland increased by 260 Tg C (23.7 Tg C yr(-1)) from 1991-2001 to 2002-2012, which was partially due to the increased crop residue return, improved fertilization and adopted conservation tillage over the period. This SOC increase represents a potential offset in carbon dioxide (CO2) emissions that could help reduce the overall net CO2 emissions in China.

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