人民长江

• 论文 • 上一篇    下一篇

三峡水库水位升降作用下树坪滑坡复活机理研究

张永昌 钱辈贝 郭飞   

  • 出版日期:2015-09-15 发布日期:2015-09-15

Study of revival mechanism of Shuping Landslide under water level fluctuation of Three Gorges Reservoir

  • Online:2015-09-15 Published:2015-09-15

摘要: 树坪古滑坡位于三峡库区内,在库水位周期性涨落作用下,滑坡土体处于饱和与非饱和动态调整状态,籍于此,根据非饱和渗流场与应力场耦合的有限元方程,应用有限元强度折减法,对库水位在不同速率变动情况下树坪古滑坡的复活机理开展了研究。结果表明:树坪滑坡地下水位变动具有一定的滞后性,并与滑体的渗透性系数密切相关;滑坡稳定系数在水位上升时整体呈现先增大后减小的趋势,并随着变动速率的增大而增大;水位下降时整体呈现先减小后增大的趋势,并随着变动速率的增大而减小;树坪滑坡复活的临界水位升降速率为2 m/d,临界水位为降落到165 m左右。

关键词: 库水位升降, 非饱和流固耦合, 滑坡复活, 机理

Abstract:

Shuping Landslide, located in Three Gorges reservoir area, is in dynamic saturated or unsaturated state due to the periodical water level fluctuation of the reservoir. Therefore, based on the finite element equations coupled with the saturated-unsaturated seepage field and stress field, the revival mechanism of Shuping Landslide under the periodical water level fluctuation with different variation rate was researched by using the FEM strength reduction method. The result indicates that the fluctuation of ground water level in the landslide has a hysteretic nature, and is closely related with the permeability of slide body; when the water level rises, the stability coefficient of landslide increases first and decreases then, and the coefficient increases with the rising rate of water level; when the water level falls, the coefficient decreases first and increases later, and the coefficient decreases with the falling rate of water level; the critical water level change speed for Shuping Landslide revival is 2 m/d, and the critical fluctuation level is about falling to 165 m.

Key words: reservoir water level fluctuation, unsaturated seepage-solid coupling, landslide revival, mechanism