Influence of joint location and connectivity on the shear properties of artificial rock samples with non-persistent planar joints

被引:0
作者
Liangxiao Xiong
Haijun Chen
Xiaolong Geng
Zhongyuan Xu
机构
[1] East China Jiaotong University,School of Civil Engineering and Architecture
[2] Guangxi University,Guangxi Key Laboratory of Disaster Prevention and Engineering Safety
[3] China Institute of Water Resources and Hydropower Research,State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin
[4] Nanjing Hydraulic Research Institute,Geotechnical Engineering Department
[5] New Jersey Institute of Technology,Center for Nature Resources
[6] University of Delaware,Department of Earth Sciences
来源
Arabian Journal of Geosciences | 2020年 / 13卷
关键词
Jointed rock specimen; Joint location; Joint connectivity ratio; Shear strength;
D O I
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中图分类号
学科分类号
摘要
In this paper, direct shear tests of cement mortar samples with non-persistent planar joints are reported, to study the effects of joint connectivity ratio k (ratio of the length of the planar joint to the length of the specimen) and locations of a planar joint on the shear properties of artificial jointed rock samples. The test results indicate that (a) the shear stress-shear displacement curve of samples with non-persistent planar joint under direct shear stress consists of five stages. (b) For samples with a non-persistent planar joint, when the joint connectivity ratio k remains unchanged, the shear strength of the specimen increases as the distance s between the left end of the planar joint and the left edge of the specimen increases. When the distance s remains constant, the shear strength of the specimens increases with an increase in the joint connectivity ratio k. When both the joint connectivity ratio k and the distance s remain unchanged, the shear strength increases as higher normal stress is applied. (c) For samples with two non-persistent planar joints and constant joint connectivity ratio k, the shear strength increases as the two planar joints, respectively, are at the two ends of specimen, compared to the scenario where the two planar joints are at the middle of the specimen. The results also demonstrate that the proposed fitting model is suitable for characterizing the shear stress-shear displacement of artificial jointed rock specimens where a non-persistent planar joint is present.
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