4.7 Article

Discrete element modeling of transversely isotropic rocks with non-continuous planar fabrics under Brazilian test

Journal

ACTA GEOTECHNICA
Volume 15, Issue 8, Pages 2277-2304

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11440-020-00919-7

Keywords

Brazilian test; Fracture pattern; Non-continuous planar fabrics; Particle discrete element method; Transverse isotropy

Funding

  1. U.S. Department of Transportation (DOT) [69A3551747118]
  2. National key research and development program of China [2016YFC08022010]

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A new numerical approach based on the particle discrete element method (PDEM) is developed to investigate the mechanical behavior of transversely isotropic rocks with non-continuous planar fabrics. In this numerical model, micro-cracks and interactions between grains are represented as flat joint contact, and the contacts with certain dipping angles are assigned as smooth joint contacts to simulate the non-continuous fabrics. The following are studied using the numerical model: (1) the effects of the micro-structure of the rock matrix and the fabric micro-parameters on the tensile and shear strength and the fracture patterns of rocks under Brazilian tests, and (2) the model calibration process for determining the micro-parameters and the failure process of rocks influenced by the micro-structure of the rock matrix. The results show that: (1) based on the Brazilian test results of 20 kinds of transversely isotropic rocks with non-continuous planar fabrics, six patterns regarding the relationship between the normalized failure strength (NFS) and fabric-loading angles are obtained; and (2) the patterns of the NFS curves are slightly affected by the contact state of particles in the rock matrix, while greatly affected by the amount of preexisting micro-cracks in rock matrix, and the stiffness, strength and distributed region of the fabrics; (3) the calibrated results of six typical rocks with different patterns agreed well with the experimental results with regards to failure strength and fracture patterns; and (4) during the failure process, micro-cracks the in rock matrix are mainly formed as the tensile and shear breakage of preexisting cracks, and micro-cracks on fabrics appear mostly at the aggregated region of preexisting cracks.

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