Abstract

The strength and failure characteristics for granite specimen with a set of cross-joints of different lengths were studied using PFC2D software. The results show that when the included angle of α between the main joint and loading direction is 30° or 45°, no matter what the included angle of β between main and secondary joints is, the main joint controls crack propagation and failure of granite specimen, which occurs the shear failure propagating from main joint tips, and the corresponding uniaxial compressive strength is low. Meanwhile, the secondary joint is the key joint for crack propagation and failure at α of 0° and 90° except when β is 90°. The granite specimen occurs the shear failure propagating from secondary joint tips. And, the shear failure crossing upper tips of main and secondary joints is found at α of 0° or 90° and β of 90°. Their uniaxial compressive strengths are large. Also, the combined actions of main and secondary joints determine crack propagation and failure at α of 60° except when β is 90°. The granite specimen occurs the hybrid failure, including shear failure propagating from main joint tips and tensile failure propagating from main and secondary joints center or secondary joint tips. And, when α is 60° and β is 90°, the granite specimen occurs the shear failure along secondary joint plane direction, and its uniaxial compressive strength is small. Generally, when α or β is a fixed value, the uniaxial compressive strength firstly decreases and then increases with the increase of β or α. Additionally, when α is 60° and β>45°, the uniaxial compressive strength represents a decreasing trend. The uniaxial compressive strength at α and β between 30° and 60° is generally small. Finally, the microdisplacement field distributions of granite specimen were discussed.

Highlights

  • Under the effects of geological tectonic stress field, there are a significant amount of native defects in a natural rock mass, such as joints, fractures, faults, various microinclusions, and pores. ese native defects play an important role in the mechanical properties of the rock mass, further influencing the stability of underground engineering [1,2,3]

  • Main joint tips and tensile failure propagating from the joint center or the secondary joint tips. eir shear crack propagation paths are similar

  • When β ranges from 30° to 60°, the secondary joint is the key joint for crack propagation and failure of the granite specimen. e granite specimens are mainly destroyed by the shear failure propagating from the secondary joint tips

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Summary

Introduction

Under the effects of geological tectonic stress field, there are a significant amount of native defects in a natural rock mass, such as joints, fractures, faults, various microinclusions, and pores. ese native defects play an important role in the mechanical properties of the rock mass, further influencing the stability of underground engineering [1,2,3]. Li et al performed the conventional triaxial compression tests on the marble specimens containing natural joints, and the effects of joint angle (between the joint plane and major principal stress) varying from 29.3° to 56.0° on the strength and failure model were studied [4]. E strength and failure characteristics of the rock specimen containing two sets of cross-joints with equal lengths were studied by Kulatilake et al [20] and Huang and Yang [21]. In this paper, the uniaxial compression tests for granite specimens containing a set of cross-joints with different lengths were simulated by PFC2D software. Lower wall 70 mm Figure 3: Simulation model for the granite specimen with a set of cross-joints with di erent lengths. Α and β were all taken as 0°, 30°, 45°, 60°, and 90°, respectively. en, α and β were combined with each other, and there are 25 test simulation conditions, as shown in Table 3. e simulation test conditions of 1, 6, 11, 16, and 21 are single jointed granite specimens

Strength Characteristics
Failure Characteristic Analysis
Conclusions
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