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首页|期刊导航|岩土力学|应力-渗流耦合作用下不同卸荷路径对砂岩损伤特性及能量演化规律的影响研究

应力-渗流耦合作用下不同卸荷路径对砂岩损伤特性及能量演化规律的影响研究

张培森 许大强 颜伟 张晓乐 董宇航 赵铭

岩土力学2024,Vol.45Issue(2):325-339,15.
岩土力学2024,Vol.45Issue(2):325-339,15.DOI:10.16285/j.rsm.2023.0204

应力-渗流耦合作用下不同卸荷路径对砂岩损伤特性及能量演化规律的影响研究

Influence of unloading paths on sandstone damage characteristics and energy evolution law under stress-seepage coupling

张培森 1许大强 1颜伟 1张晓乐 1董宇航 1赵铭1

作者信息

  • 1. 山东科技大学矿山灾害预防控制国家重点实验室培育基地,山东青岛 266590||山东科技大学矿业工程国家级实验教学示范中心,山东青岛 266590
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摘要

Abstract

Rock mass disasters are caused by instability driven by energy within the rock mass.The excavation and unloading disturbance can lead to fractures and instability in the rock mass structure,which is a major cause of dynamic disasters such as water inrush in stopes.To understand the influence of excavation unloading on rock mass structure fractures and to clarify the degradation law of surrounding rock and the mechanism of dynamic disasters like water inrush,this study focuses on the characteristics of rock damage and the evolution of energy under stress-seepage coupling factors.Using the Rock Top multi-field coupling tester,the study investigates the rock damage characteristics and energy evolution under three stress paths:conventional triaxial compression(group C),conventional unloading confining pressure with different initial damage degrees(group W),and cyclic loading and unloading confining pressure(group X)under the influence of stress-seepage coupling.Based on the evolution characteristics of rock elastic strain energy,the stress-strain curve of rock under conventional triaxial compression(group C)is divided into five stages,and the characteristics of U1,U3,Ue,Ud and permeability change in each stage are explained in detail(Ue is the elastic strain energy,Ud is the dissipated energy,U1 is the strain energy of the rock transformed by the positive work done by the axial stress on the rock,and U3 is the strain energy released by the negative work).During the conventional confining pressure unloading process,the evolution law of U1 and U3 is similar to that of group C rock,but the negative growth of U3 is more significant.The rock input energy gradually shifts from Ue to Ud,and the initial damage degree has no significant influence on the law.During the confining pressure unloading process,the permeability shows a fluctuating upward trend,and the confining pressure is negatively correlated with the permeability.In the process of cyclic loading and unloading confining pressure,the energy evolution law is similar to that of group W rock,with energy accumulation differing only due to time effects.On the whole,regardless of the stress path,the pre-peak rock is dominated by Ue,representing energy storage,while post-peak rock is dominated by energy release and dissipation.Axial stress loading is the main influencing factor for rapid accumulation of Ue,while the change in confining pressure is not enough to cause a large change in Ue.Axial load is the primary factor influencing engineering disasters.Furthermore,there is a significant negative correlation between rock damage variable and confining pressure.The larger the confining pressure is,the smaller the Ue release ratio of rock is,and the smaller the rock damage is.Confining pressure restraint effectively enhances the energy storage capacity of rock and inhibits the dissipation and release of rock energy.

关键词

岩石力学/应力-渗流耦合/卸荷路径/损伤特性/能量演化

Key words

rock mechanics/stress-seepage coupling/unloading path/damage characteristics/energy evolution

分类

建筑与水利

引用本文复制引用

张培森,许大强,颜伟,张晓乐,董宇航,赵铭..应力-渗流耦合作用下不同卸荷路径对砂岩损伤特性及能量演化规律的影响研究[J].岩土力学,2024,45(2):325-339,15.

基金项目

国家重点研发计划(No.2018YFC0604702) (No.2018YFC0604702)

国家自然科学基金(No.51379119) (No.51379119)

山东省自然科学基金(No.ZR2021ME086).This work was supported by the National Key Research and Development Program of China(2018YFC0604702),the National Natural Science Foundation of China(51379119)and the Natural Science Foundation of Shandong Province(ZR2021ME086). (No.ZR2021ME086)

岩土力学

OA北大核心CSTPCD

1000-7598

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