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
|
Studies of thermokarst and its effects on ecosystem carbon cycle in the Third Polar regions and the Arctic
|
Lin JIA 1( ), Chengyan FAN 1, Mei MU 1, Xu CHEN 1, Wen ZHONG 1, Jianguo SHANG 2, Feng ZHANG 1, Lili LI 3, Xiaoqing PENG 1, Cuicui MU 1,4,5( ), Tingjun ZHANG 1,5
|
|
图6. 三种常见的坡地热喀斯特地貌对碳氮循环及通量影响的概念模型[16]
|
Fig.6. Conceptual model of the effects of the three types of most common hillslope thermokarst landscapes on carbon and nitrogen cycling and flux[16]
|
|
|
|
|