Conventional triaxial compression test I of altered rock: study of classification of strain-stress curve before and after destruction and brittle-ductile diversion confining pressure
|更新时间:2026-06-25
|
Conventional triaxial compression test I of altered rock: study of classification of strain-stress curve before and after destruction and brittle-ductile diversion confining pressure
Vol. 29, Issue 10, (2008)
作者机构:
1. 贵州大学 资源与环境工程学院,贵州,贵阳,550003
2. 成都理工大学地质灾害防治与地质环境保护国家专业实验室,成都,610059
作者简介:
基金信息:
DOI:
CLC:TU458+.3
Online First:03 August 2013,
Published:2008
稿件说明:
移动端阅览
YANG Gen-lan, HUANG Run-qiu, CAI Guo-jun, et al. Conventional triaxial compression test I of altered rock: study of classification of strain-stress curve before and after destruction and brittle-ductile diversion confining pressure[J]. 2008, 29(10).
DOI:
YANG Gen-lan, HUANG Run-qiu, CAI Guo-jun, et al. Conventional triaxial compression test I of altered rock: study of classification of strain-stress curve before and after destruction and brittle-ductile diversion confining pressure[J]. 2008, 29(10).DOI:
Conventional triaxial compression test I of altered rock: study of classification of strain-stress curve before and after destruction and brittle-ductile diversion confining pressure
The altered rock is the soft rock which is scarce in the engineering. For a major engineering project in Southwest China
the altered rock is located in the key position of the project. In order to guarantee the project for long-term stability
the mechanical property of the altered rock should be deeply and fully studied. On the basis of systematic conventional triaxial compression test for the saturated altered rock under different porosities
the test results are analyzed and summarized. It has been put forward that there are three types of stress-strain curve before rock destruction and three types of stress-strain curves after rock destruction. The conclusions have been proposed that the altered rock destruction is effected by both confining pressure and porosity. When the confining pressure is 12 MPa
the brittle failure is dominating. Only when the porosity is more than 16 % and the confining pressure is more than 4 MPa
the brittle-ductile fracture diversion state is possibly found. Furthermore
the confining pressure of brittle-ductile fracture state diversion decreases along with the porosity increases; and the critical state stress ratio increases along with the porosity increases.
Study of creep characteristics and constitutive relation of briquette under confining pressure
Testing study of dynamic shear modulus and damping ratio of typical soils in Fuzhou area
A new method of testing rock properties
2-D multiscale numerical simulation of rock failure subjected to confining pressure based on virtual multi-dimensional internal bonds
Numerical test on failure process of rock subjected to dynamic loading
Related Author
ZHAO Hong-bao
YIN Guang-zhi
ZHANG Wei-zhong
CAI Hui-teng
LI Ying-min
OU Bing-song
WANG Wei
XU Wei-ya
Related Institution
Zhongnan University of Economics and Law
Key Laboratory for the Exploitation of Southwest Resources and the Environmental Disaster Control Engineering of Education Ministry, Chongqing University, Chongqing 400044, Chnia
College of Resources and Environmental Science, Chongqing University
Earthquake Administration of Fujian Province
College of Civil Engineering, Chongqing University