摘要
青康公路运行35a后,经沿线调查与钻探表明,在多年冻土区内,凡路堤高度低于08m的富冰地段,历年均有不同程度的热融、翻浆病害发生;凡路堤高度大于08m的路段则基本保持稳定.在全面分析路堤下冻土上限的升降规律基础上,并考虑目前区内冻土明显退化的现实与高级路面对路基变形的要求,提出高原多年冻土区修筑道路时,砂砾路面路堤高度应为16m,水泥混凝土路面路堤高度应为20m.
The survey and drilling investigation in the permafrost regions along the Qinghai-Kangding Highway, which has been operated for 35 years, indicate that the line where the height of the embankment is lower than 08 m suffers from frost boiling and thermokast to different extent every year, and that the line where the height of embankment was over 08 m maintains a steady state. Based on an overall analysis on the change in permafrost table under the embankment, after considering the fact that the permafrost in the area is degrading and the requirement of the deformation of the road surface of high quality, it is suggested that the height of embankment is 16 m for the gravel road, and 20 m for cement concrete road in the plateau permafrost regions.
出处
《冰川冻土》
CSCD
北大核心
1998年第1期36-41,共6页
Journal of Glaciology and Geocryology
基金
国家自然科学基金