2021
DOI: 10.1016/j.egyr.2021.05.029
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Theoretical and experimental investigation on fracture response of coal impacted by high-velocity water jet

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Cited by 21 publications
(4 citation statements)
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“…Certain representative parameters, such as the shear stress and principal stress, were selected for the analysis, and the propagation law of stress wave in rock under water jet impinging and failure response of coal was investigated. 29 In this phase, researchers payed attention not only to the stress state of rock but also to the damage distribution and failure mechanism. They explained the mechanism of rock breakage by exploring the variation of different parameters, which is the prevailing analytical method.…”
Section: Introductionmentioning
confidence: 99%
“…Certain representative parameters, such as the shear stress and principal stress, were selected for the analysis, and the propagation law of stress wave in rock under water jet impinging and failure response of coal was investigated. 29 In this phase, researchers payed attention not only to the stress state of rock but also to the damage distribution and failure mechanism. They explained the mechanism of rock breakage by exploring the variation of different parameters, which is the prevailing analytical method.…”
Section: Introductionmentioning
confidence: 99%
“…High-pressure water jet technology is an effective method for cutting or breaking targets due to many operational advantages, such as selective removal capability, heatfree, dust-free, and high efficiency. [1][2][3][4][5][6][7][8][9] Due to its unique characteristic, it has been widely used in related engineering fields including oil and gas drilling, rock cutting, mining, machining, cleaning, and rotary jet grouting, and so on. A submerged environment is an important working condition for high-pressure water jet.…”
Section: Introductionmentioning
confidence: 99%
“…In the jet-breaking mechanism, the impact stress wave is the main form of action. When the water jet impacts the rock, the high pressure generated in the liquid-solid contact area is transmitted in the form of a stress wave in the rock as a sphere (Lesser 1981;Lesser and Field 1983;Xiao et al 2021) and generates tangential and radial tensile stresses, which subjects the rock to tension followed by compression. When the tensile action exceeds the tensile limit of the rock, the rock cracks (NI et al 2003;Lu et al 2015) and ruptures in the direction of the stress wavefront, forming a circular cracking surface and resulting in laminar cracking of the rock (Xue et al 2017).…”
Section: Introductionmentioning
confidence: 99%