Spatial distribution and failure mechanism of water-induced landslides in the reservoir areas of Southwest China
作者机构:State Key Laboratory of Hydraulics and Mountain River EngineeringSichuan UniversityChengdu610065China College of Water Resources and HydropowerSichuan UniversityChengdu610065China
出 版 物:《Journal of Rock Mechanics and Geotechnical Engineering》 (岩石力学与岩土工程学报(英文版))
年 卷 期:2023年第15卷第2期
页 面:442-456页
核心收录:
学科分类:081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程]
基 金:We gratefully acknowledge the support of the National Key R&D Program of China(Grant No.2017YFC1501102) the National Nat-ural Science Foundation of China(Grant No.41977229) the Sichuan Youth Science and Technology Innovation Research Team Project(Grant No.2020JDTD0006)
主 题:Water-induced landslide Hydropower reservoir Spatial distribution Fundamental control Failure mechanism
摘 要:Water-induced landslides in hydropower reservoirs pose a great threat to both project operation and human *** paper examines three large reservoirs in Sichuan Province,*** surveys,site monitoring data analyses and numerical simulations are used to analyze the spatial distribution and failure mechanisms of water-induced landslides in reservoir ***,the general rules of landslide development in the reservoir area are *** first rule is that most of the landslides have rear edge elevations of 100e500 m above the normal water level of the reservoir,with volumes in the range of 106 e107 m *** the volume exceeds a certain amount,the number of sites at which the landscape can withstand landslides is greatly *** hazards mainly occur in the middle section of the reservoir and less in the annex of the dam site and the latter half of the reservoir *** second rule is that sedimentary rocks such as sandstone are more prone to landslide hazards than other ***,the failure mechanism of changes in the water level that reduces the stability of the slope composed of different geomaterials is analyzed by a proposed slope stability framework that considers displacement and is discussed with the monitoring *** is an essential parameter for understanding the diametrically opposed deformation behavior of landslides experiencing filling-drawdown cycles during *** study seeks to provide inspiration to subsequent researchers,as well as guidance to technicians,on landslide prevention and control in reservoir areas.