首页 | 本学科首页   官方微博 | 高级检索  
     检索      

单剪条件下主应力大小及主应力轴方向
引用本文:卢廷浩,周爱兆,刘尧.单剪条件下主应力大小及主应力轴方向[J].岩土力学,2010,31(4):1009-1012.
作者姓名:卢廷浩  周爱兆  刘尧
作者单位:1.河海大学 岩土力学与堤坝工程教育部重点实验室,南京 210098;2.河海大学 岩土工程科学研究所,南京 210098
基金项目:国家自然科学基金委员会、二滩水电开发有限责任公司雅砻江水电开发联合研究基金重点项目 
摘    要:对单剪条件下的应力莫尔圆变化过程进行详细分析,将莫尔圆从初始状态到破坏状态的大、小主应力变化过程看做由若干个等增量步组成,从而推导出任意剪应力状态与初始状态对应的小主应力差值与两者大主应力差值的比为一常数,该常数可以根据初始状态莫尔圆和破坏时对应的莫尔圆确定。推导出单剪条件下任意剪应力对应的大、小主应力及主应力轴方向的表达式。讨论了土体材料参数及法向应力对主应力轴偏转过程的影响以及大、小主应力与剪应力的关系。结果表明:在土体材料参数一定的条件下,主应力轴方向由应力比唯一确定;法向应力一定,土体的摩擦角越小,相同剪应力对应的主应力偏转角越大;剪切起始阶段,主应力变化缓慢,随着剪应力增大,主应力急剧变化至土样破坏时保持不变。

关 键 词:单剪  莫尔圆  主应力  主应力轴方向  影响因素  
收稿时间:2008-07-02

Size and axis direction of principal stress in simple shear
LU Ting-hao,ZHOU Ai-zhao,LIU Yao.Size and axis direction of principal stress in simple shear[J].Rock and Soil Mechanics,2010,31(4):1009-1012.
Authors:LU Ting-hao  ZHOU Ai-zhao  LIU Yao
Institution:1.Key Laboratory for Geomechanics and Embankment Engineering of Ministry of Education, Hohai University, Nanjing 210098, China; 2.Geotechnical Research Institute, Hohai University, Nanjing 210098, China
Abstract:The changing process of stress Mohr circle in simple shear is analyzed in detail. In the analysis, the process is regard as a components of some incremental step in equal; and two variables are difined: one is the difference between two minor principal stresses corresponding to a random shear stress state and the initial state, another is the difference between two major principal stresses corresponding to a random shear stress state and the initial state; Then the ratio value of the two variables is proved to be constant, which can be got by the Mohr circle in initial state and failure state. Furthermore, expressions of the principal stresses and the corresponding axis directions related to a random shear stress in simple shear are deduced. The influence of soil character parameters and normal stress on the principal stress axis directions is discussed. The relationship between principal stress and shear stress is also evaluated. Studying shows that under the same soil character parameters, the direction of principal stress axis are only decided by the stress ratio; for constant normal stress and shear stress, the rotation angle of principal stress axis increases with the decrement of internal friction angle of the soil, the principal stresses change slowly at the beginning of shearing, change sharply with the increament of shear stress, and keep constant in the failure state.
Keywords:simple shear  Mohr circle  principal stress  principal stress axis direction  influence factor
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《岩土力学》浏览原始摘要信息
点击此处可从《岩土力学》下载免费的PDF全文
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