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降雨及库水位作用下碎石土岸坡变形破坏机制模型试验研究

DING Jun-ling JI Feng WEI Song ZHANG Bo ZENG Rui LI Zhuo LU Yu-peng

岩土力学2025,Vol.46Issue(12):3740-3756,17.
岩土力学2025,Vol.46Issue(12):3740-3756,17.DOI:10.16285/j.rsm.2024.00589

降雨及库水位作用下碎石土岸坡变形破坏机制模型试验研究

Model test of deformation and failure mechanism of gravel soil bank slope under rainfall and reservoir water level

DING Jun-ling 1JI Feng 1WEI Song 1ZHANG Bo 2ZENG Rui 1LI Zhuo 1LU Yu-peng1

作者信息

  • 1. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu,Sichuan 610059,China
  • 2. China Railway Changjiang Transport Design Group Co.,Ltd.,Chongqing 401121,China
  • 折叠

摘要

Abstract

Deformation of the deposit bank slope is intensified due to reservoir water regulation and rainfall,threatening reservoir operation.To investigate the deformation and failure mechanisms of bank slopes,as well as their infiltration characteristics,a large-scale physical model test was conducted to simulate rainfall and its interactions with water level fluctuations at the Sanbanxi Reservoir in Guizhou Province.The parameters such as pore water pressure in slope and the whole process of slope deformation evolution are obtained.The results show that:(1)The final shape of the modeled wetting front is determined by the slope shape,and the different infiltration effects are mainly manifested in the change of migration depth,and the seepage field characteristics and slope gradient have a greater influence on the migration rate.(2)The soil pressure curve changes gently under both conditions,the pore water pressure changes with a lag,and the soil pressure and pore water pressure in the deeper layers of the slope body fluctuate more than those in the shallower layers in the saturated state.(3)Slope deformation during rainfall is dominated by erosion pits and localized slides,while erosion channels dominate during coupling,and the scale of slope erosion during coupling is about twice as large as that during rainfall,but multi-stage slip traction damage occurs at the foot of the slopes in both conditions.(4)Based on the experimental results,the deformation and damage mechanism of the modeled bank slope under the coupled rainfall and water level is summarized into five stages:softening and settling of the slope surface,development and expansion of erosion gullies,and development of erosion channels and collapse at the foot of the slope.The results of this study fill the gap in the study of bank slope stability under the above conditions in Sanbanxi Reservoir area,and it is useful for the study of similar deformation damage of gravel soil bank slopes and their prevention and control.

关键词

降雨与库水位/碎石土岸坡/模型试验/变形破坏机制/入渗特性

Key words

rainfall and reservoir water level/gravel soil bank slope/model test/deformation and failure mechanism/infiltration features

分类

建筑与水利

引用本文复制引用

DING Jun-ling,JI Feng,WEI Song,ZHANG Bo,ZENG Rui,LI Zhuo,LU Yu-peng..降雨及库水位作用下碎石土岸坡变形破坏机制模型试验研究[J].岩土力学,2025,46(12):3740-3756,17.

基金项目

国家自然科学基金(No.41977273). This work was supported by the National Natural Science Foundation of China(41977273). (No.41977273)

岩土力学

OA北大核心

1000-7598

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