冻结季沱沱河源多年冻土区活动层土壤水分含量分析
李智斌1(
), 赵林1,2(), 刘广岳2,3, 邹德富3, 汪凌霄1, 杨斌4, 杜二计2,3, 胡国杰3, 周华云2,3, 王翀1, 幸赞品2,3, 赵建婷1, 殷秀峰3, 迟鸿飞5, 谭昌海4, 陈文4
), 赵林1,2(), 刘广岳2,3, 邹德富3, 汪凌霄1, 杨斌4, 杜二计2,3, 胡国杰3, 周华云2,3, 王翀1, 幸赞品2,3, 赵建婷1, 殷秀峰3, 迟鸿飞5, 谭昌海4, 陈文4
Analysis of soil moisture content in the active layer in the permafrost region of the Tuotuo River source in frozen season
Zhibin LI1(), Lin ZHAO1,2(), Guangyue LIU2,3, Defu ZOU3, Lingxiao WANG1, Bin YANG4, Erji DU2,3, Guojie HU3, Huayun ZHOU2,3, Chong WANG1, Zanpin XING2,3, Jianting ZHAO1, Xiufeng YIN3, Hongfei CHI5, Changhai TAN4, Wen CHEN4
), Lin ZHAO1,2(), Guangyue LIU2,3, Defu ZOU3, Lingxiao WANG1, Bin YANG4, Erji DU2,3, Guojie HU3, Huayun ZHOU2,3, Chong WANG1, Zanpin XING2,3, Jianting ZHAO1, Xiufeng YIN3, Hongfei CHI5, Changhai TAN4, Wen CHEN4
图5. 不同冻土类型土壤含水量
Fig.5. Soil moisture content of different frozen ground types： 0~350 cm total soil moisture content of different types of frozen soil （a）； the soil moisture content of soil profile in permafrost region （b）； the soil moisture content of soil profile in seasonally frozen ground （c）
