Lu Fei, Wang Xiao-Ke, Han Bing, Ouyang Zhi-Yun, Zheng Hua
State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
Ying Yong Sheng Tai Xue Bao. 2010 Jan;21(1):99-108.
Based on the long-term datasets of soil organic matter content and the observation data of rice paddies' methane (CH4) emission collected from the agricultural experiment stations across the country, the rice paddies in China were divided into single cropping and double cropping regions. The soil carbon sequestration potential of straw return in three types of rice paddies in the two regions, i. e., single cropping rice paddies, upland/paddy alternated rice paddies, and double cropping rice paddies, was evaluated, based on the datasets of soil organic matter content; and the total CH4 emission from rice paddies without straw return was estimated, with reference to the experimental data of paddies' CH4 emission and by the method of mean emission coefficient. The total CH4 emission from our paddies after straw return and the global warming potential of the increased CH4 emission were also estimated by using the related methods and parameters given by IPCC. It was estimated that the full popularization of straw return to China's rice paddies would sequester 10.48 Tg x a(-1) of C, and the contribution to the global warming mitigation was 38.43 Tg CO2-eqv x a(-1). In the meanwhile, the CH4 emission from our rice paddies would be increased from 5.796 Tg x a(-1) to 9.114 Tg x a(-1), and the increased 3.318 Tg x a(-1) of CH4 emission would lead to a global warming potential of 82.95 Tg CO2 -eqv x a(-1), which was 2.158 times of the mitigation from carbon sequestration in rice paddies. Therefore, the increased CH4 emission due to straw return should be regarded as an important greenhouse gas leakage, since it could greatly offset the mitigation benefits of soil carbon sequestration in China's rice paddies.
基于全国农业试验站收集的土壤有机质含量长期数据集以及稻田甲烷(CH4)排放观测数据,将中国稻田划分为单季稻区和双季稻区。基于土壤有机质含量数据集,评估了这两个区域三种类型稻田(即单季稻田、旱田/水田轮作稻田和双季稻田)秸秆还田的土壤固碳潜力;参照稻田CH4排放实验数据并采用平均排放系数法,估算了无秸秆还田稻田的CH4总排放量。利用IPCC给出的相关方法和参数,还估算了秸秆还田后我国稻田的CH4总排放量以及CH4排放增加的全球升温潜势。据估算,秸秆还田在我国稻田全面推广将固碳10.48 Tg x a(-1),对全球变暖减缓的贡献为38.43 Tg CO2-eqv x a(-1)。同时,我国稻田的CH4排放量将从5.796 Tg x a(-1)增至9.114 Tg x a(-1),增加排放的3.318 Tg x a(-1) CH4将导致全球升温潜势达82.95 Tg CO2 -eqv x a(-1),是稻田固碳减缓作用的2.158倍。因此,秸秆还田导致的CH4排放增加应被视为重要的温室气体泄漏,因为它会极大抵消我国稻田土壤固碳带来的减缓效益。