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涎流冰是高寒地区独特的工程地质现象。国外地处高纬度的加拿大北部、苏联远东地区都有分布。在我国大小兴安岭与长白山地区、青藏高原3200米以上地区均有发育,其中又尤以大兴安岭林区最为严重。为此,我们以大兴安岭林区腹地,伊勒呼里山南北坡的松岭、呼中两局的林道干、支线为重点,对涎流冰的危害、成因及地下水的运动规律和特征等进行了调查研究。并从经济、可行角度提出了几项整治方案,仅供专家们商榷与指正。
Salty ice flow is a unique engineering geological phenomenon in the alpine region. Foreign high-latitude is located in northern Canada, the Soviet Union has the distribution of the Far East. In our country, the Hinggan Mountains and Changbai Mountains, there are 3200 meters above the Qinghai-Tibet Plateau, especially the Daxing’anling forest area. To this end, we take the Daxing’anling forest hinterland, the North and South slopes of Mount Ereli Hill Songling, Huzhu Lin Road dry, the focus of the branch, the saliva ice hazards, causes and groundwater movement patterns and characteristics were Research. And from the economic, feasible point of view put forward several remediation programs, only for experts to discuss and correct.