摘要
随着水库蓄水后水位的变化,其库岸的水文地质环境必然发生改变,水库边坡自然平衡发生破坏,地下水与岩土体之间发生复杂的物理化学作用,从而使库岸边坡有别于其他非水库边坡.从水库边坡的特点出发,对水库边坡的破坏形式、滑坡塌岸的形成机理和预测方法进行了简要的阐述.
During the process of water storing, the rising of water level in reservoirs will cause the change of hydrogeologic environment and then lead to the breakage of natural balance of slopes. Complicated physical and chemical actions take place between the rock-soil mass and underwater. Such effects differentiate the reservoir bank slopes from others. Based on the characters of reservoir bank slope, the shapes of failure forms, mechanism of the slope-collapse and methods of forecast are discussed in this paper.
出处
《地质与资源》
CAS
2005年第3期213-215,共3页
Geology and Resources
关键词
水库
边坡
稳定性
reservoir
bank slope
stability
