人民长江 ›› 2023, Vol. 54 ›› Issue (10): 189-195.doi: 10.16232/j.cnki.1001-4179.2023.10.027

• • 上一篇    

基于离心模型试验的水动力型滑坡失稳机制研究

朱军威 张强 卢晓春 陈鸿杰 程伟   

  • 收稿日期:2022-09-20 出版日期:2023-10-28 发布日期:2023-10-26

Instability mechanism of hydrodynamic landslide based on centrifugal model test

ZHU Junwei ZHANG Qiang LU Xiaochun CHEN Hongjie CHENG Wei   

  • Received:2022-09-20 Online:2023-10-28 Published:2023-10-26

摘要: 水动力型滑坡是中国西南高坝大库库区常见的滑坡类型,是影响库区安全的重要因素。为厘清库水位下降和降雨两种作用在水动力型滑坡变形中的主次关系,及此类滑坡变形失稳机理,以云南黄登水电站库区车邑坪滑坡为研究对象,设计了一套试验系统,利用大型土工离心机开展不同方案下大型滑坡离心模型试验,分析其变形失稳机制。结果表明:(1)库水位上升阶段,孔压的增长表现出一定的滞后性;库水位下降阶段,孔压消散速率小于库水位降落速率;降雨阶段,有裂缝的滑坡其孔压迅速增长。(2)库水位下降是导致车邑坪滑坡变形的主要因素,降雨为激发因素;库水位下降使滑坡产生指向坡体外的动水压力,致使滑坡失稳,产生裂缝;裂缝为降雨入渗提供了通道,加剧裂缝的发展。(3)车邑坪滑坡治理相对困难,建议对车邑坪小村进行搬迁处理,同时编制应急预案。

关键词: 水动力型滑坡;离心模型试验;降雨;库水位变动;失稳机制;

Abstract: Hydrodynamic landslides are the most common type of landslides in high-dam and large-scale reservoir areas in southwest China and are an important factor affecting the safety of reservoir areas.After the water storage operation in the Huangdeng Reservoir area, a series of ancient landslides on the reservoir banks were revived due to the change in hydrodynamic conditions.Taking the Cheyiping landslide in the Huangdeng Reservoir area as the research object, a set of test systems was independently designed, and a large-scale geotechnical centrifuge was used to carry out centrifugal model tests for these large landslides under different schemes to clarify the primary and secondary effects of reservoir water level drop and rainfall in landslide deformation, The deformation and instability mechanism was revealed.The results showed that in the rising stage of the reservoir water level, the growth of pore pressure showed a certain hysteresis; in the stage of reservoir water level decline, the dissipation rate of pore pressure was less than the falling rate of the reservoir water level; in the rainfall stage, for landslides with cracks, the pore pressure increased rapidly.(2) The decline of the reservoir water level is the main factor for the deformation of the Cheyiping landslide, and rainfall is a triggering factor.The drop in the reservoir water level causes the landslide to generate dynamic water pressure pointing to the outside of the slope, resulting in the instability of the landslide and the formation of cracks; the cracks provide a channel for rainfall infiltration and aggravate the development of cracks.(3) It is relatively difficult to control the Cheyiping landslide.It is suggested to relocate the small village of Cheyiping and prepare an emergency plan at the same time.

Key words: hydrodynamic landslide; centrifugal model test; rainfall; reservoir water level fluctuation; instability mechanism;