摘要
本文根据我国不同地区沙漠化类型的面积、土壤有机碳的含量及沙漠化的正逆转速率,计算了我国沙漠化土地中有机碳的变动。结果表明,我国沙漠化土地0-50cm土层中有机碳的,总贮量为753.143Mt,近40年来因土地沙漠化而释放到大气中的CO2,总量达173.286Mt,而逆转过程中固定的CO2量为59.124Mt碳,所以,近40年来我国沙漠化土地净释放到大气中的CO2量为124.475Mt碳,占全球温带和寒带土地每年释放CO2量133Mt碳的93.5%。
The paper,according to areas and conversion rates( positive and negative)of desertified lands, contents of organic carbon in soils, calculates the quantitative dynamics of China desertified lands, the results show: The organic carbon stored in0-50cm soil layers of national desertified lands amounts to 753.143Mt; over the recent 40 years, 173. 286Mt of CO2 are released from desertified lands, however, only 59.124Mt of CO2 are fixed In the reverse processes to desertificafion; that is, China desertified lands have released 124.475Mt of CO2 into the air over the 40 years.
出处
《干旱区资源与环境》
CSCD
1996年第2期89-94,共6页
Journal of Arid Land Resources and Environment
基金
中国科学院沙坡头开放试验站基金
关键词
沙漠化
大气环境
全球变化
中国
二氧化碳
Desertification, CO_2, atmospheric environment, global change