首页 | 本学科首页   官方微博 | 高级检索  
     

基于三维形貌分析的结构面剪切试验研究
引用本文:胡伟,邬爱清,陈胜宏.基于三维形貌分析的结构面剪切试验研究[J].长江科学院院报,2017,34(9).
作者姓名:胡伟  邬爱清  陈胜宏
作者单位:1. 长江科学院 水利部岩土力学与工程重点实验室,武汉,430010;2. 武汉大学 水资源与水电工程科学国家重点实验室,武汉,430072
基金项目:国家自然科学基金项目,中央级公益性科研院所基本科研业务费项目
摘    要:为研究结构面表面形貌、正应力及剪切历史对岩石结构面剪切特性及强度的影响规律,利用近景摄影测量技术测量试验前后结构面三维形貌数据,对影响结构面剪切特性的因素开展定性与半定量的分析。分析结果表明:(1)结构面形貌对剪切特性的影响具有方向性,视倾角0°的凸起体才可能在剪切过程中起抵触作用;(2)起伏粗糙对剪切特性的影响随正压力增大而降低,相应的剪胀效应也随正压力增大而减小;(3)在低正压力条件下,结构面表面的起伏凸起体即可被磨损剪断,首先出现磨损剪断的是视倾角较大的凸起,在经历1次正应力条件下剪切变形后,剪切曲线便不再出现峰值现象;(4)摩擦角随正压力增大而减小,而黏聚力随正压力增大而增大;(5)单块试样反复剪切试验中,取第1次残余值与后续剪切强度值拟合得到的剪切强度参数可代表具有剪切运动历史的结构面剪切强度。

关 键 词:岩体结构面  三维形貌  直剪试验  近景摄影  剪切强度

Shear Test of Rock Discontinuity Based on 3-D Morphologic Analysis
HU Wei,WU Ai-qing,CHEN Sheng-hong.Shear Test of Rock Discontinuity Based on 3-D Morphologic Analysis[J].Journal of Yangtze River Scientific Research Institute,2017,34(9).
Authors:HU Wei  WU Ai-qing  CHEN Sheng-hong
Abstract:The shear failure characteristics of rock mass discontinuities are influenced by surface morphology, normal stress and shear history.Close range photogrammetry is a quick and accurate approach to obtain the 3-D morphology of surface features.In this paper, the 3-D surface morphology of the discontinuities is analyzed before and after the multiple normal pressure repeated shear test, and the factors that affect the shear characteristics are analyzed in qualitative and semi-quantitative sense.Results reveal that 1) the influence of morphology on the shear behavior is directional, and only the asperity with the apparent inclination greater than 0 degree could resist each other in the shearing process, but the actual contact surface is quite smaller than potential resistant surface;2) the effect of roughness on the shear behavior decreases with the increase of normal pressure, and so does shear dilation behavior;3) the asperity is easily worn and cut even under low normal stress, in particular, asperity with large apparent inclination will be primarily damaged, and peak value of the shear curve does not occur in subsequent shear after the first shear;4) friction angle increases with the decrease of positive pressure, while cohesion displays an opposite trend;5) the shear strength parameters fitted from the first residual value and the subsequent shear strength value can be used to represent the shear strength of the discontinuities with the shear movement history.
Keywords:rock discontinuity  3-D morphology  direct shear test  close range photogrammetry  shear strength
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号