2015
DOI: 10.1016/j.enggeo.2015.08.024
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High internal pressure induced fracture patterns in rock masses surrounding caverns: Experimental study using physical model tests

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Cited by 53 publications
(13 citation statements)
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“…ese geological disasters are the macromechanical manifestations of rock instability and failure. As a natural material, the rock contains various defects (e.g., microcracks, pores, joints, and fissures), and the instability and failure of an engineered rock mass are essentially a progressive process from the development of damage of mesoscopic defects to the macroscopic fracture of rock under a stress field [4][5][6]. erefore, it is of great theoretical significance and engineering value to study the fracture mechanism and crack propagation trends of rock under loading to thoroughly understand the failure mechanism of the engineering rock mass as well as to evaluate and predict geological disasters.…”
Section: Introductionmentioning
confidence: 99%
“…ese geological disasters are the macromechanical manifestations of rock instability and failure. As a natural material, the rock contains various defects (e.g., microcracks, pores, joints, and fissures), and the instability and failure of an engineered rock mass are essentially a progressive process from the development of damage of mesoscopic defects to the macroscopic fracture of rock under a stress field [4][5][6]. erefore, it is of great theoretical significance and engineering value to study the fracture mechanism and crack propagation trends of rock under loading to thoroughly understand the failure mechanism of the engineering rock mass as well as to evaluate and predict geological disasters.…”
Section: Introductionmentioning
confidence: 99%
“…Yan Chunhe et al [21][22][23] numerically simulated the time-yield deformation law and the extent of the time-yield damage zone at the top of the cavity in the surrounding rock and rock pillars of salt cavern gas storage reservoirs through the secondary development of ABAQUS. Pornkasem et al [24] investigated the damage behavior of cavern envelopes under high internal pressure, as well as the mechanism of crack generation and development in the rock mass, by using a physical model test method on synthetic rock samples containing cavities. Xia Caichu et al [25][26][27] addressed the stability of surrounding rocks in piezo gas storage in underground chambers operating under high internal pressure; the plastic zone and perimeter strain of the surrounding rocks in piezo gas storage chambers of different structural types and under high internal pressure was obtained through finite element calculations.…”
Section: Introductionmentioning
confidence: 99%
“…In these models, they do not consider the initial stress state of the surrounding ground before excavation and operation, which can lead to unrealistic evaluation. In the last decade, many researchers have performed analyses to suggest a reasonable uplift failure pattern [7][8][9][10][11][12]. According to their study, the initial failure point along the cavern periphery depends on the in-situ stress ratio that can lead to different uplift failure patterns [2,9].…”
Section: Introductionmentioning
confidence: 99%