从第三极到北极： 热喀斯特及其对碳循环影响研究进展
贾麟1(
), 范成彦1, 母梅1, 陈旭1, 仲文1, 尚建国2, 张凤1, 李丽丽3, 彭小清1, 牟翠翠1,4,5(), 张廷军1,5
), 范成彦1, 母梅1, 陈旭1, 仲文1, 尚建国2, 张凤1, 李丽丽3, 彭小清1, 牟翠翠1,4,5(), 张廷军1,5
Studies of thermokarst and its effects on ecosystem carbon cycle in the Third Polar regions and the Arctic
Lin JIA1(), Chengyan FAN1, Mei MU1, Xu CHEN1, Wen ZHONG1, Jianguo SHANG2, Feng ZHANG1, Lili LI3, Xiaoqing PENG1, Cuicui MU1,4,5(), Tingjun ZHANG1,5
), Chengyan FAN1, Mei MU1, Xu CHEN1, Wen ZHONG1, Jianguo SHANG2, Feng ZHANG1, Lili LI3, Xiaoqing PENG1, Cuicui MU1,4,5(), Tingjun ZHANG1,5
图5. 多年冻土退化对土壤水分、 溶解性有机碳和温室气体（CO2、 CH4、 N2O）释放过程影响的示意， 箭头代表生长季节生态系统温室气体交换方向和潜力［
Fig.5. Impacts of permafrost degradation on soil moisture， dissolved organic carbon and the release of greenhouse gases （CO2， CH4 and N2O）， and the arrows indicate the direction and potential of ecosystem greenhouse gas exchange during the growing seasons［
