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高边坡节理岩体地质力学模型试验研究
引用本文:袁大祥,朱子龙,朱乔生.高边坡节理岩体地质力学模型试验研究[J].三峡大学学报(自然科学版),2001,23(3):193-197.
作者姓名:袁大祥  朱子龙  朱乔生
作者单位:1. 三峡大学经济与管理学院,
2. 三峡大学发展规划处,
3. 三峡大学土木水电学院,
基金项目:国家八五重点科技攻关项目(85-16-03-05(3))
摘    要:按弹塑性体相似判据和破坏阶段相似判据确立相似常数,模拟山体形态、结构面和岩石物理力学性质、地应力、边界条件和埋设测点,建立三维模型,模拟开挖卸荷过程,监测边坡形态、地应力释放和山体应变,认识到边坡变形的主要因素、变形延时和变形量、变形与就算力释放的关系及山体应力应变明显变化的范围

关 键 词:陡高边坡  节理岩体  模型试验
文章编号:1007-7081(2001)03-0193-05
修稿时间:2001年3月8日

Experimental Research on Geomechanics Model of Jointed Rock Mass of High Slope
Yuan Daxiang,Zhu Zilong,Zhu Qiaosheng.Experimental Research on Geomechanics Model of Jointed Rock Mass of High Slope[J].Journal of China Three Gorges University(Natural Sciences),2001,23(3):193-197.
Authors:Yuan Daxiang  Zhu Zilong  Zhu Qiaosheng
Abstract:According to simularity criteria of elastoplastic body and simularity criteria of its damage stage,the simularity constants are determined. By simulating mountain body shape, structural sarface, physico-mechanical properties of rock, ground(initial) stress, boundary conditions and embedded measured points;a 3-dimensional model of jointed rock mass of high-steep slope is established. Through simulating load-off process due to excaration; monitoring slope deformation, ground stress-release and strain of mountain body; the recognitions obtained are as follows: main factors of slope deformation, deformation delay and deformation value, relationship between deformation and stress-release,obvious change scope of stress-strain of the mountain body.
Keywords:high and steep slope rock  jointed rock mass  model experiments  
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