2022
DOI: 10.1061/(asce)gm.1943-5622.0002372
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The Influence of Joint Inclination and Opening Width on Fracture Characteristics of Granite under Triaxial Compression

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Cited by 29 publications
(14 citation statements)
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“…It is found that the number of microseismic events was significantly reduced and the rockbursts were well controlled. From the explanation of rockburst mechanism, optimizing the construction scheme was to reduce the unloading or disturbance effect and the release of strain energy of surrounding rock, thereby reducing the risk of rockbursts [29][30][31]. Strengthening support was to improve the energy storage limit of surrounding rock and prevent the occurrence of rockbursts.…”
Section: Temporal Distribution Law Of Microseismic Eventsmentioning
confidence: 99%
“…It is found that the number of microseismic events was significantly reduced and the rockbursts were well controlled. From the explanation of rockburst mechanism, optimizing the construction scheme was to reduce the unloading or disturbance effect and the release of strain energy of surrounding rock, thereby reducing the risk of rockbursts [29][30][31]. Strengthening support was to improve the energy storage limit of surrounding rock and prevent the occurrence of rockbursts.…”
Section: Temporal Distribution Law Of Microseismic Eventsmentioning
confidence: 99%
“…ere are many factors leading to the formation of different types of strain rock burst. However, no matter how complex its internal mechanism is, rock burst is mainly controlled by two factors, namely lithological conditions and stress field conditions [9][10][11][12][13]. It is found that the deep rock mass is mostly hard brittle rock mass, which generally meets the requirements of lithological conditions when rock burst occurs.…”
Section: Influencing Factors Of Tunnel Surrounding Rock Failurementioning
confidence: 99%
“…The method mainly divides the volumetric strain of rocks into the elastic volumetric strain and volumetric strain of cracks. Under uniaxial compression, the volumetric strain of cracks, c v  , in the rock can be calculated thus [36,37]: Existing methods used for calculating characteristic stresses mainly include strain measurement, AC measurement, and an approach based on the volumetric strain of cracks. Among these, the one based on the volumetric strain of cracks has been widely used due to its definite concept and convenience of determination [34,35].…”
Section: Stress Analysismentioning
confidence: 99%
“…The method mainly divides the volumetric strain of rocks into the elastic volumetric strain and volumetric strain of cracks. Under uniaxial compression, the volumetric strain of cracks,ε v c , in the rock can be calculated thus [36,37]:…”
Section: Stress Analysismentioning
confidence: 99%