4.4 Article

Experimental and numerical study on mechanical and fracture behavior of rock-like specimens containing pre-existing holes flaws

Journal

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/19648189.2019.1657961

Keywords

Pre-existing holes; fracture mode; acoustic emission; progressive failure process; particle flow code

Funding

  1. National Natural Science Foundation of China [51734009, 51704279, 51709260]

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This paper investigates the mechanical behavior of rock containing two pre-existing holes through laboratory tests and numerical simulation. The experimental results reveal significant stress-strain fluctuations and different failure modes caused by the presence of holes in the rock. The numerical simulation further examines the process of crack initiation, propagation, and coalescence, as well as the mechanism of overall instability.
Laboratory tests and numerical simulation are conducted to study mechanical behavior of rock containing two pre-existing holes in this paper. First of all, rock-like specimens containing two pre-existing holes were prepared to investigate mechanical and acoustic emission characteristics in the uniaxial compression. Different geometries were obtained by changing the angle of the center line of holes with respect to the direction of axial loading. Experimental results show that the stress-strain curves present obvious fluctuation, and evolution process of acoustic emission signal can be divided into four stages. There are three kinds of failure modes: only shear failure, mainly shear and auxiliary tensile failure, mainly tensile and auxiliary shear failure. Then, parallel bonded mode (PBM) based on the particle flow code in two dimensions (PFC2D) were established to study strength and failure modes in the biaxial compression. Finally, process of cracks initiation, propagation and coalescence, and fracture mechanism were further discussed. The most important conclusion reached is that the deformation and failure process of rock mass containing holes defects can be divided into two stages: rock bridge penetration and overall instability, which are sequential.

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