Abstract

The study of the mechanical properties and cracking behaviors of jointed rock masses is important in rock engineering projects. In the present study, a series of uniaxial compression experiments were conducted on intact rock, and rock masses with single or double preexisting flaws, and then the strength, deformability, and fracture behavior of samples are investigated. Moreover, photographic monitoring technique and emission monitoring technique are introduced to explore the fracturing mode and the acoustic emission (AE) evolution characteristic of fractured rock during the whole loading process. The obtained results show that the preexisting flaw has a strong influence on the mechanical properties, fracture behavior, and AE characteristic of sandstone specimens. In detail, the stress‐strain curves show that no significant stress jump occurs at prepeak and postpeak points for intact sandstone specimens; however, the flaw‐contained sandstone specimens exhibit distinct stress jump during the entire loading process. Meanwhile, the strength parameters of the the rock specimen is obviously weakened by the preexisting fissures, and the uniaxial compression strength of rock specimens generally decreases with the increase in the number of preexisting fissure as well as the peak strain and the elastic modulus. The failure modes of intact and flaw‐contained sandstone specimens exhibit the splitting failure and the mixed failure modes of shear and tension, respectively. Similarly, the maximum AE counts and AE energy both decrease with the increasing number of preexisting flaw. The present research can enhance the understanding of mechanical properties, cracking behaviors, and failure mechanism of jointed rock mass.

Highlights

  • Faults, joints, and fractures are widely distributed in natural rocks, and the existence of these discontinuous surfaces greatly deteriorates the strength and deformability behavior of rock masses [1,2,3,4,5]

  • Under the effect of dead and live load, primary fractures initiate, propagate, and coalesce with each other, which results in a number of geological hazards, such as landslide, instability of slope, and tunnel face. erefore, better understanding of the mechanical properties and failure mechanism of jointed rock mass is pressing

  • In order to reduce the effect of the end friction on the experimental results, the length-diameter ratio of the sandstone specimen should be in the range of 2.0-3.0. erefore, the standard cylinder specimen is adopted in the experiment and the size of the sandstone specimen is 100 mm long and 50 mm in diameter

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Summary

Introduction

Joints, and fractures are widely distributed in natural rocks, and the existence of these discontinuous surfaces greatly deteriorates the strength and deformability behavior of rock masses [1,2,3,4,5]. Considering the influence of discontinuity on properties of rock mass, failure process regarding flaw-contained rock specimens under compression was experimentally and numerically studied by numerous scholars. Morgan et al [32] and Lu et al [33] carried out uniaxial compression tests on sandstone and granite to investigate the influence of the flaw geometry, crack coalescence on failure behavior of rock. The influences of the number of preexisting flaws on the mechanical behavior, fracture mechanism, and failure mode under uniaxial compressive loads have not systematically been investigated for the original rock material. A series of uniaxial compression tests were conducted on intact rocks and rocks containing different number of flaws to simulate the cracking processes of sandstone.

Experimental Preparation and Procedure
Mechanical Properties of Rock Specimens
Cracking Mechanism and Acoustic
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