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青藏高原腹地各拉丹冬南北坡多年冻土考察初步结果
刘广岳1,2(), 邹德富1, 杨斌3, 杜二计1,2, 周华云1,2, 肖瑶1, 赵林2,4(), 谭昌海3, 胡国杰1, 庞强强1, 王武1, 孙哲1,2, 朱小凡1, 殷秀峰1, 汪凌霄4, 李智斌4, 谢昌卫1
Preliminary results of permafrost investigation on northern and southern slopes of Mt. Geladandong, interior Qinghai-Tibet Plateau
Guangyue LIU1,2(), Defu ZOU1, Bin YANG3, Erji DU1,2, Huayun ZHOU1,2, Yao XIAO1, Lin ZHAO2,4(), Changhai TAN3, Guojie HU1, Qiangqiang PANG1, Wu WANG1, Zhe SUN1,2, Xiaofan ZHU1, Xiufeng YIN1, Lingxiao WANG4, Zhibin LI4, Changwei XIE1

图2. 色林错上游扎加藏布源区和长江上游沱沱河源区重点考察区域及勘察点位、剖面布设
注:活动层是指仅安装了水热监测设备的点位,综合场是指同时布设了钻孔地温和活动层水热观测的场地,坑探采样工作在活动层水热监测场地开挖时进行;扎加藏布源区测温时间为2020年11月19日,沱沱河源区测温时间为2020年11月20—21日,由于钻孔完成不久,数值略有偏高

Fig. 2. Key investigation area, profiles and sites in source area of the Zhaga Zangbo River, a tributary of upper Selin Co Lake (a) and in source area of the Tuotuo River, upper reaches of the Yangtze River (b)