2014
DOI: 10.1016/j.jsg.2014.10.014
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Fracture mechanical behavior of red sandstone containing a single fissure and two parallel fissures after exposure to different high temperature treatments

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Cited by 70 publications
(17 citation statements)
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“…com] information has been reported. For example, Yang et al 43,44 analysed the crack initiation and propagation process of single-flawed sandstone and granite specimens, as well as crack coalescence patterns of twoflawed sandstone specimens under uniaxial compression. However, the crack coalescence behaviour of rocks containing three or more flaws that are exposed to high temperatures has not been investigated comprehensively, which is much more complicated than that with one or two flaws.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…com] information has been reported. For example, Yang et al 43,44 analysed the crack initiation and propagation process of single-flawed sandstone and granite specimens, as well as crack coalescence patterns of twoflawed sandstone specimens under uniaxial compression. However, the crack coalescence behaviour of rocks containing three or more flaws that are exposed to high temperatures has not been investigated comprehensively, which is much more complicated than that with one or two flaws.…”
Section: Introductionmentioning
confidence: 99%
“…However, the crack coalescence behaviour of rocks containing three or more flaws that are exposed to high temperatures has not been investigated comprehensively, which is much more complicated than that with one or two flaws. To investigate the crack coalescence mechanism of preflawed rocks after hightemperature treatments and to extend the previous experimental study of Yang et al, 43,44 uniaxial compression tests on three-flawed sandstone specimens heated to high temperatures were performed in this study. The effects of thermal treatment and flaw inclination angle on the stress-strain curve, peak strength, elastic modulus and peak strain of the preflawed specimens were investigated.…”
Section: Introductionmentioning
confidence: 99%
“…However, the existing studies show that local thermal stress will be generated between mineral particles due to the differences in the thermal expansion coefficient between rock mineral particles at high temperature. In this way, the internal structure of the particles will change substantially, and thermal cracking may occur in the rock, which eventually affects the physical and mechanical properties of the rock [14][15][16][17][18][19]. Besides, it is also well known that the fracture trajectories and fracture roughness and surface morphology are strictly related to the seepage behavior of geofluids.…”
Section: Introductionmentioning
confidence: 99%
“…Based on the experimental research and PFC numerical simulation, Jin et al [2] generalized that, with the increase of flaw angle, the tensile cracks initiate from gentle flaw and shear cracks emerge at tips of steep flaws. Yang [3] argued that the cracking process depended on both the fissure geometry and the heat treatment temperature. Chen et al [4] carried out uniaxial compression experiments on the sandstone samples containing double fissures and a single circular hole and thought that the peak strength, peak strain, and elastic modulus of defected specimens show decreased trend firstly and then increase with changing from 0 ∘ to 90 ∘ .…”
Section: Introductionmentioning
confidence: 99%