Abstract

The elastic energy stored in deep rock in three-dimensional stress environment is the energy source of rockburst. To investigate the energy storage characteristics of deep rock under different confining pressures, a series of triaxial single-cyclic loading-unloading compression tests were conducted on red sandstone specimens under eight confining pressures. The input energy density, elastic energy density, and dissipative energy density of the specimen in axial, circumferential, and total directions can be obtained by the area diagram integration method. The results show that the input energy density in the axial direction accounts for the largest logarithmic proportion of the total input energy density, and the relationship between all energy density parameters and unloading level can be described by quadratic function. In the axial direction, there is a linear function relationship among elastic energy density, dissipative energy density, and input energy density. In the circumferential direction, there is a quadratic function relationship among elastic energy density, dissipative energy density, and input energy density. For the total energy density parameters of the rock specimen, the relationship among elastic energy density, dissipative energy density, and input energy density conforms to the quadratic function. According to the above correlation function, the elastic energy stored in deep rock under different confining pressures can be accurately obtained, which provides a foundation for studying the mechanism of rockburst under three-dimensional unloading from the energy perspective.

Highlights

  • With the development of deep engineering, more and more rockburst disasters are encountered in the process of deep rock excavation [1,2,3,4,5,6]

  • Rockburst is a kind of disaster caused by the violent release of elastic energy stored in deep rocks [4,5,6,7,8,9,10,11], and the elastic energy accumulated in deep rock under high confining pressure is the energy source of rockburst

  • [19,20,21]. e energy storage, dissipation, and release during the rock deformation process are closely related to the damage state [19, 22,23,24,25,26,27,28,29,30,31,32]. erefore, it is necessary to study the internal mechanism of rock deformation from the perspective of energy storage and dissipation

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Summary

Introduction

With the development of deep engineering, more and more rockburst disasters are encountered in the process of deep rock excavation [1,2,3,4,5,6]. E energy storage, dissipation, and release during the rock deformation process are closely related to the damage state [19, 22,23,24,25,26,27,28,29,30,31,32]. On the basis of uniaxial cyclic loading-unloading compressive tests, Meng et al [30, 31] investigated the characteristics of energy accumulation and dissipation during rock deformation and implied that with the increase of axial load stress, Shock and Vibration the total absorbed energy density increased the fastest, followed by the elastic energy density, and the dissipative energy density increased the slowest. Zhang and Gao [33] studied the energy evolution of red sandstone under different confining pressures and found that with the increase of confining pressure, the energy storage limit of rock increased in the form of power index

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