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贯通型锯齿状节理岩体的剪切力学行为
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作者单位:

1.重庆大学 土木工程学院;2.库区环境地质灾害防治国家地方联合工程研究中心;3.山地城镇建设与新技术教育部重点实验室，重庆 400045

作者简介:

刘新荣（1969- ），男，教授，博士生导师，主要从事岩石力学及地下工程研究，E-mail：liuxrong@126.com。
LIU Xinrong (1969- ), professor, doctorial supervisor, main research interests: rock mechanics and underground engineering, E-mail: liuxrong@126.com.

通讯作者:

许彬（通信作者），男，博士生，E-mail： geotechnicale2016@163.com。

中图分类号:

TU458

基金项目:

国家自然科学基金（41972266、52074042）；重庆市研究生科研创新项目（CYS21024）；2018年重庆市基础研究与前沿探索项目（cstc2018jcyjAX0453）


Shear mechanical behavior of rock with through-type saw-tooth joints
Author:
  • LIU Xinrong 1,2,3

    LIU Xinrong

    School of Civil Engineering;National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China
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  • ZENG Xi 1,2,3

    ZENG Xi

    School of Civil Engineering;National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China
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  • XU Bin 1,2,3

    XU Bin

    School of Civil Engineering;National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China
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  • ZHOU Xiaohan 1,2,3

    ZHOU Xiaohan

    School of Civil Engineering;National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China
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  • LIU Xinlin 1,2,3

    LIU Xinlin

    School of Civil Engineering;National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China
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  • WANG Jiwen 1,2,3

    WANG Jiwen

    School of Civil Engineering;National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China
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Affiliation:

1.School of Civil Engineering;2.National Joint Engineering Research Center for Prevention and Control of Environmental Geological Hazards in the TGR Area;3.Key Laboratory of New Technology for Construction of Cities in Mountain Area, Ministry of Education, Chongqing University, Chongqing 400045, P. R. China

Fund Project:

National Natural Science Foundation of China (No. 41972266, 52074042); the Graduate Scientific Research and Innovation Foundation of Chongqing, China (No. CYS21024); Basic Research and Frontier Exploration Project of Chongqing in 2018 (No. cstc2018jcyjAX0453)

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    摘要:

    为探究一阶起伏角和法向应力对贯通型锯齿状节理岩体剪切强度及变形的影响规律，在不同法向应力作用下对含不同一阶起伏角的锯齿节理试样进行室内直剪试验，建立一个贯通型锯齿状节理岩体剪切强度估算公式并进行验证。结果表明：相同法向应力作用下，根据其形态特征的不同，剪切应力-位移曲线分为滑动型曲线、滑动-峰值型曲线和峰值型曲线3类，滑动型曲线和滑动-峰值型曲线可分为非线性缓慢上升阶段、线性陡升阶段、“上凸形”缓慢上升阶段、近似平直阶段和平直阶段，峰值型曲线可分为非线性缓慢上升阶段、线性陡升阶段、“微凸型”上升阶段、脆性跌落阶段和波动缓降阶段；根据起伏角的不同，锯齿节理岩体的破坏模式可概化为滑移破坏、爬坡破坏和爬坡啃断破坏，每种破坏模式下节理损伤演化过程均可分为3个阶段，即滑移破坏模式可分为压密阶段、克服摩擦阶段和滑移阶段，爬坡破坏模式可分为压密阶段、爬坡滑移阶段和塑性流动阶段，爬坡啃断破坏模式可分为压密爬坡阶段、爬坡啃断阶段和啃断滑移阶段；含不同一阶起伏角的锯齿节理岩体剪切强度均随法向应力和起伏角的增加而增大，其计算表达式仍然遵循M-C准则。

    Abstract:

    To explore the effect of undulating angle and normal stress on the shear strength and deformation of the rock with regular saw-tooth joints, direct shear tests were carried out on the limestone samples with different undulating angles under different normal stresses. Subsequently, a shear strength estimation formula was established and verified. The results show that,under the same normal stress, according to the morphological characteristics，the shear stress-displacement curves can be divided into three types：the sliding curve, the sliding-peak curve and the peak curve. The sliding curve and the sliding-peak curve can be divided into nonlinearly slow rising, linear steep rising, and “upward convex” slow rising stage, approximately straight and flat stage. The peak type curve can be divided into nonlinearly slow rising, linear steep rising, “slightly convex” rising, brittle falling and gently descending stage. The failure mode of rock with saw-tooth joints with different undulating angles can be generalized into three failure modes: sliding failure, climbing failure and gnawing failure. The evolution of joint damage under each failure mode can be divided into three stages, i.e., the sliding failure mode can be divided into compaction, friction-over-coming and sliding stage. The climbing failure mode can be divided into compaction, climbing-sliding and plastic flow stage. The gnawing failure modes can be divided into compaction-climbing, climbing-gnawing and gnawing-sliding stage. The shear strength increases with the increase of the normal stress and undulating angle, and the evolution of shear strength still follows M-C criterion.

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刘新荣,曾夕,许彬,周小涵,刘馨琳,王继文.贯通型锯齿状节理岩体的剪切力学行为[J].土木与环境工程学报（中英文）,2023,45(5):1-9. LIU Xinrong, ZENG Xi, XU Bin, ZHOU Xiaohan, LIU Xinlin, WANG Jiwen. Shear mechanical behavior of rock with through-type saw-tooth joints[J]. JOURNAL OF CIVIL AND ENVIRONMENTAL ENGINEERING,2023,45(5):1-9.10.11835/j. issn.2096-6717.2021.195

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  • 收稿日期:2021-06-04
  • 在线发布日期: 2023-08-24
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