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冰川冻土  2013 

祁连山区黑河上游多年冻土分布考察

DOI: 10.7522/j.issn.1000-0240.2013.0003, PP. 19-29

Keywords: 多年冻土下界,活动层,海拔,年平均地温,黑河流域

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Abstract:

高山多年冻土的分布及土壤季节冻融过程对地表水文过程、生态系统、碳循环及寒区工程建设等都有很大的影响.黑河上游地处祁连山中东部,属于高原亚寒带半干旱气候,研究黑河流域多年冻土分布对于系统理解该区域的生态-水文过程、气候与环境变化以及水资源评价、工程建设等非常重要.2011年6-8月对黑河干流源头西支开展了多年冻土调查,沿二尕公路(S204)在热水大坂垭口至石棉矿岔口之间区域,完成测温孔7眼,并布设测温管进行地温监测.根据勘察、钻探及测温资料,确定了黑河源头地区山地多年冻土下界为海拔3650~3700m之间.受高度地带性的控制,随着海拔的降低,活动层厚度由在海拔4132m时的1.6m增加至在多年冻土下界处的约4.0m,多年冻土年平均地温也相应的由-1.7℃增加到0.0℃左右,而多年冻土厚度由100m以上减小到多年冻土下界处的0.0m.同时,坡度和坡向、岩性、含水(冰)量、地下水、河水等局地因素对多年冻土温度和厚度也有重要的作用.

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