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干旱区科学  2016, Vol. 8 Issue (3): 364-374    DOI: wuxq@bjfu.edu.cn
  学术论文 本期目录 | 过刊浏览 | 高级检索 |
SOC storage and potential of grasslands from 2000 to 2012 in central and eastern Inner Mongolia, China
TIAN Zheng1, WU Xiuqin1*, DAI Erfu2, ZHAO Dongsheng2
1 Yanchi Research Station, College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;
2 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
SOC storage and potential of grasslands from 2000 to 2012 in central and eastern Inner Mongolia, China
TIAN Zheng1, WU Xiuqin1*, DAI Erfu2, ZHAO Dongsheng2
1 Yanchi Research Station, College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;
2 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
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摘要 Grassland ecosystem is an important component of the terrestrial carbon cycle system. Clear comprehension of soil organic carbon (SOC) storage and potential of grasslands is very important for the effective management of grassland ecosystems. Grasslands in Inner Mongolia have undergone evident impacts from human activities and natural factors in recent decades. To explore the changes of carbon sequestration capacity of grasslands from 2000 to 2012, we carried out studies on the estimation of SOC storage and potential of grasslands in central and eastern Inner Mongolia, China based on field investigations and MODIS image data. First, we calculated vegetation cover using the dimidiate pixel model based on MODIS-EVI images. Following field investigations of aboveground biomass and plant height, we used a grassland quality evaluation model to get the grassland evaluation index, which is typically used to represent grassland quality. Second, a correlation regression model was established between grassland evaluation index and SOC density. Finally, by this regression model, we calculated the SOC storage and potential of the studied grasslands. Results indicated that SOC storage increased with fluctuations in the study area, and the annual changes varied among different sub-regions. The SOC storage of grasslands in 2012 increased by 0.51×1012 kg C compared to that in 2000. The average carbon sequestration rate was 0.04×1012 kg C/a. The slope of the values of SOC storage showed that SOC storage exhibited an overall increase since 2000, particularly for the grasslands of Hulun Buir city and Xilin Gol League, where the typical grassland type was mainly distributed. Taking the SOC storage under the best grassland quality between 2000 and 2012 as a reference, this study predicted that the SOC potential of grasslands in central and eastern Inner Mongolia in 2012 is 1.38×1012 kg C. This study will contribute to researches on related methods and fundamental database, as well as provide a reference for the protection of grassland ecosystems and the formulation of local policies on sustainable grassland development.
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TIAN Zheng
WU Xiuqin
DAI Erfu
ZHAO Dongsheng
关键词:  alfalfa grassland  long-term fertilization  nitrogen  organic carbon  semi-arid Loess Plateau    
Abstract: Grassland ecosystem is an important component of the terrestrial carbon cycle system. Clear comprehension of soil organic carbon (SOC) storage and potential of grasslands is very important for the effective management of grassland ecosystems. Grasslands in Inner Mongolia have undergone evident impacts from human activities and natural factors in recent decades. To explore the changes of carbon sequestration capacity of grasslands from 2000 to 2012, we carried out studies on the estimation of SOC storage and potential of grasslands in central and eastern Inner Mongolia, China based on field investigations and MODIS image data. First, we calculated vegetation cover using the dimidiate pixel model based on MODIS-EVI images. Following field investigations of aboveground biomass and plant height, we used a grassland quality evaluation model to get the grassland evaluation index, which is typically used to represent grassland quality. Second, a correlation regression model was established between grassland evaluation index and SOC density. Finally, by this regression model, we calculated the SOC storage and potential of the studied grasslands. Results indicated that SOC storage increased with fluctuations in the study area, and the annual changes varied among different sub-regions. The SOC storage of grasslands in 2012 increased by 0.51×1012 kg C compared to that in 2000. The average carbon sequestration rate was 0.04×1012 kg C/a. The slope of the values of SOC storage showed that SOC storage exhibited an overall increase since 2000, particularly for the grasslands of Hulun Buir city and Xilin Gol League, where the typical grassland type was mainly distributed. Taking the SOC storage under the best grassland quality between 2000 and 2012 as a reference, this study predicted that the SOC potential of grasslands in central and eastern Inner Mongolia in 2012 is 1.38×1012 kg C. This study will contribute to researches on related methods and fundamental database, as well as provide a reference for the protection of grassland ecosystems and the formulation of local policies on sustainable grassland development.
Key words:  alfalfa grassland    long-term fertilization    nitrogen    organic carbon    semi-arid Loess Plateau
收稿日期:  2015-08-14      修回日期:  2015-11-12           出版日期:  2016-06-01      发布日期:  2015-12-10      期的出版日期:  2016-06-01
基金资助: 

The National Technology & Science Support Program of China (2012BAD16B02)

通讯作者:  WU Xiuqin    E-mail:  wuxq@bjfu.edu.cn
引用本文:    
TIAN Zheng, WU Xiuqin, DAI Erfu, ZHAO Dongsheng. SOC storage and potential of grasslands from 2000 to 2012 in central and eastern Inner Mongolia, China[J]. 干旱区科学, 2016, 8(3): 364-374.
TIAN Zheng, WU Xiuqin, DAI Erfu, ZHAO Dongsheng. SOC storage and potential of grasslands from 2000 to 2012 in central and eastern Inner Mongolia, China. Journal of Arid Land, 2016, 8(3): 364-374.
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http://jal.xjegi.com/CN/wuxq@bjfu.edu.cn  或          http://jal.xjegi.com/CN/Y2016/V8/I3/364
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