2022
DOI: 10.1016/j.tust.2022.104624
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Experiments on three-dimensional flaw dynamic evolution of transparent rock-like material under osmotic pressure

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Cited by 15 publications
(8 citation statements)
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“…Ashby [ 32 ] and Nemat-Nasser [ 33 ] performed physical model compression tests using similar materials with single and multiple cracks, observing the initiation and propagation shapes of surface-penetrating cracks and rock bridge penetration patterns, revealing the evolution of crack propagation. Zhu et al [ 34 ] conducted biaxial experiments under water pressure using transparent resin-based rock-like materials, revealing the evolution patterns of prefabricated crack expansion.…”
Section: Discussionmentioning
confidence: 99%
“…Ashby [ 32 ] and Nemat-Nasser [ 33 ] performed physical model compression tests using similar materials with single and multiple cracks, observing the initiation and propagation shapes of surface-penetrating cracks and rock bridge penetration patterns, revealing the evolution of crack propagation. Zhu et al [ 34 ] conducted biaxial experiments under water pressure using transparent resin-based rock-like materials, revealing the evolution patterns of prefabricated crack expansion.…”
Section: Discussionmentioning
confidence: 99%
“…Clay minerals with loose structure and low strength will be pulled apart before quartz during loading, then the sandstone tensile strength will be primarily borne by quartz particles. The complete quartz particles were strong and cannot be easily broken directly, hence, the final tensile surface may present the following two forms [26]: (1) When passing through the unbroken quartz particles, cracks will expand along the weak part of the quartz boundary; and (2) when passing through the broken quartz grains, the cracks will pass directly through the quartz interior. When the quartz in the sandstone was relatively complete, the tensile strength of the sandstone will be significantly greater than that of the sandstone with relatively broken quartz particles.…”
Section: Evolution Process Of Sandstone Strength Deteriorationmentioning
confidence: 99%
“…Based on this material, Zhu, Lin and Sun et al revealed the effects of fissure length, inclination, spacing, and rock bridge angle on the crack expansion and coalescence modes of single or multiple three-dimensional fissure and the strength of the specimens under uniaxial compression 16 – 18 . Zhu et al 19 used this material to conduct hydraulic fracturing experiments on single fracture specimens under uniaxial and biaxial compression conditions, and revealed the effects of different osmotic pressures and crack forms on the initiation, coalescence, and peak strength of elliptical opening-type cracks. Fu et al 20 developed a rock-like material formed by the reaction of a new type of unsaturated polyacrylate resin and hardener, which exhibits good brittle fracture characteristics at lower temperatures.…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, with the emergence of problems like water inrush and instability in rock bodies in water-rich geological environments, and the improvement of experimental conditions, many scholars have embarked on more in-depth explorations of the failure mechanisms of fractured rock bodies under the coupled effects of high water pressure and engineering excavation disturbances. Based on transparent rock-like materials, Zhu et al 19 and Fu et al 25 studied the progressive damage mechanisms and patterns of three-dimensional crack tips under hydromechanical coupling. Regarding the shear-flow coupling characteristics of fractures, some researchers 29 , 30 used transparent acrylic resin and gypsum to create the upper and lower parts of shear samples with the same surface morphology as natural fractures.…”
Section: Introductionmentioning
confidence: 99%