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2016
DOI: 10.3997/2214-4609.201600412
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Mathematical Simulation of Hydraulic Fracturing of Shale Strata

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“…The flow of fluid in rock mass will change the distribution of seepage volume force and change the original stress state of the rock mass. At the same time, the change in the stress state of rock mass will change the geometric characteristics of cracks, such as the opening or closing of cracks [13,14], change of crack roughness [15,16], and so on, cracks will occur at the tip of the crack, new cracks may occur in rock blocks near the crack surface, and the water permeability pressure will affect the stress distribution and stress redistribution of surrounding rocks. Rock mass seepage behavior will change [17][18][19][20].…”
Section: Introductionmentioning
confidence: 99%
“…The flow of fluid in rock mass will change the distribution of seepage volume force and change the original stress state of the rock mass. At the same time, the change in the stress state of rock mass will change the geometric characteristics of cracks, such as the opening or closing of cracks [13,14], change of crack roughness [15,16], and so on, cracks will occur at the tip of the crack, new cracks may occur in rock blocks near the crack surface, and the water permeability pressure will affect the stress distribution and stress redistribution of surrounding rocks. Rock mass seepage behavior will change [17][18][19][20].…”
Section: Introductionmentioning
confidence: 99%