Rock and Soil Mechanics ›› 2024, Vol. 45 ›› Issue (2): 325-339.doi: 10.16285/j.rsm.2023.0204

• Fundamental Theroy and Experimental Research •     Next Articles

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

ZHANG Pei-sen1, 2, XU Da-qiang1, 2, YAN Wei1, 2, ZHANG Xiao-le1, 2, DONG Yu-hang1, 2, ZHAO Ming1, 2   

  1. 1. National Key Laboratory for Mine Disaster Prevention and Control, Shandong University of Science and Technology, Qingdao, Shandong 266590, China; 2. National Demonstration Center for Experimental Mining Engineering Education, Shandong University of Science and Technology, Qingdao, Shandong 266590, China
  • Received:2023-02-20 Accepted:2023-05-05 Online:2024-02-11 Published:2024-02-06
  • Supported by:
    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).

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.

Key words: rock mechanics, stress-seepage coupling, unloading path, damage characteristics, energy evolution

CLC Number: 

  • TU 447
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