Abstract

The study on hydromechanical coupling properties of rocks is of great importance for rock engineering. It is closely related to the stability analysis of structures in rocks under seepage condition. In this study, a series of conventional triaxial tests under drained condition and hydrostatic compression tests under drained or undrained condition on sandstones were conducted. Moreover, complex cyclic loading and unloading tests were also carried out. Based on the experimental results, the following conclusions were obtained. For conventional triaxial tests, the elastic modulus, peak strength, crack initiation stress, and expansion stress increase with increased confining pressure. Pore pressure weakened the effect of the confining pressure under drained condition, which led to a decline in rock mechanical properties. It appeared that cohesion was more sensitive to pore pressure than to the internal friction angle. For complex loading and unloading cyclic tests, in deviatoric stress loading and unloading cycles, elastic modulus increased obviously in first loading stage and increased slowly in next stages. In confining pressure loading and unloading cycles, the Biot coefficient decreased first and then increased, which indicates that damage has a great impact on the Biot coefficient.

Highlights

  • IntroductionGeological materials are mostly saturated, and pores and fissures are filled with one or several kinds of fluids

  • For underground engineering, geological materials are mostly saturated, and pores and fissures are filled with one or several kinds of fluids

  • In order to study the mechanical characteristics of the rock under the complex stress conditions, hydrostatic pressure test and complex cycle loading and unloading test were done on samples SY-11 to SY-13

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Summary

Introduction

Geological materials are mostly saturated, and pores and fissures are filled with one or several kinds of fluids. The research of Yin and Chen [12] concerned the influences of seepage pressure on joint stressseepage coupling characteristics, changing trends of rock stress, displacement, joint hydraulic apertures, and conductivity along with shear displacement Their results indicated that shear stress, displacement, hydraulic apertures, and conductivity of joint specimens were distinctly related to seepage. Oda et al and Schulze et al [13, 14] conducted some relevant research on permeability evolution under triaxial compression which showed that rock deformation damage had a large effect on permeability characteristics, and we could obtain the conclusion that there is currently an understanding of stressstrain characteristics under seepage pressure.

GPa μ8 σci : σc SY-1
Experimental Preparations
Results of Triaxial Compression Test of the Drained Samples
Results of Complex Cyclic Loading and Unloading Tests
Analysis of Confining Pressure Loading-Unloading
Conclusions
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