Seismic responses of slopes with different angles in coral sand
有在珊瑚沙的不同角度的斜坡的地震回答作者机构:College of Civil EngineeringTaiyuan University of TechnologyTaiyuan 030024China College of Civil EngineeringChongqing UniversityChongqing400045China Key Laboratory of New Technology for Construction of Cities in Mountain AreaChongqing UniversityChongqing400045China
出 版 物:《Journal of Mountain Science》 (山地科学学报(英文))
年 卷 期:2021年第18卷第9期
页 面:2475-2485页
核心收录:
学科分类:07[理学] 0708[理学-地球物理学]
基 金:supported by the National Natural Science Foundation of China(Grant Nos.41831282,51878103) the Fundamental Research Funds for the Central Universities(Grant No.2021CDJQY-042) the Postdoctoral innovative talents support program,Chongqing
主 题:Coral sand Slope angle Shaking table tests Seismic response Liquefaction
摘 要:This paper investigates the seismic responses of slopes in coral sand taken from a reef island in the South China Sea.A series of shaking table model tests were conducted to explore the responses of soil acceleration,excess pore pressure,and slope displacement for three slope angles(5°,10°,and 15°).The results show that the excess pore pressure ratio of the slope decreases due to an increase in the initial shear stress when the slope angle *** acceleration response of the soil increases with the increase of the slope *** slope displacement presents substantial increments as the excess pore pressure ratio *** addition,the lateral movement,and slope settlement present substantial increments as the slope angle *** liquefaction is observed under a dynamic excitation of 0.2 g in the coral sand *** a dynamic excitation of 0.4 g,the site liquefies quickly,the acceleration amplification factor decreases,and the lateral movement and the settlement of the slope surface both increase compared with that under 0.2 g *** the slope with an angle of 15°at 0.4 g,the flow distance of the sand strip increase by 289.47%compared with that in the 5°*** lateral movement of the slope surface near the water level line is substantially larger than that away from the water *** largest settlement is observed near the middle section of the slope(below the water level)under a dynamic excitation of 0.2 *** contrast,the largest settlement under a dynamic excitation of 0.4 g occurs at the top of the slope.