摘要
据野外调查和室内试验证明,在青藏高原岛状多年冻土区内,年平均地温高于-0.5℃、未饱和的“高温”冻结粗粒土(岩)层既可透水,也可释水,是一种特殊的含水层,这类含水层中的水名曰“冻结层内水”。
Field investigation and indoov experiments havediscovered from the island permafrost areas in Qin-ghai-Xizang (Tibet) plateau the 'high-temperature'unsaturated coarse-grained soil (rock)layers of aver-age annual temperature above-0.5℃ Which ate ca-pable of both water permeation and water releasing.They belong to a special kind of aquifer whosewater is called 'intrapermafrost water' .
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1990年第1期46-47,15,共3页
Hydrogeology & Engineering Geology
