2021
DOI: 10.1007/s00603-021-02539-3
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Numerical Study on the Field-Scale Criterion of Hydraulic Fracture Crossing the Interface Between Roof and Broken Low-Permeability Coal

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Cited by 10 publications
(6 citation statements)
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“…where σ s is the stress vector; E 0 is the stiffness matrix of the solid element; ε s and ε p s are the total and plastic strain vectors, respectively; I is the identity matrix; d is the damage tensor, and its evolution law is determined according to the research results [24].…”
Section: Elastic-plastic Constitutive Relation Of Intact Coal and Rockmentioning
confidence: 99%
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“…where σ s is the stress vector; E 0 is the stiffness matrix of the solid element; ε s and ε p s are the total and plastic strain vectors, respectively; I is the identity matrix; d is the damage tensor, and its evolution law is determined according to the research results [24].…”
Section: Elastic-plastic Constitutive Relation Of Intact Coal and Rockmentioning
confidence: 99%
“…where G is the plastic potential function; δ is a parameter of the control curve in the stretching stage and δ = 0.1; σ U is the tensile strength of coal; ψ is the angle of dilatancy. On this basis, combined with plastic mechanics and its corresponding numerical solution [24], ε p s values can be obtained.…”
Section: Elastic-plastic Constitutive Relation Of Intact Coal and Rockmentioning
confidence: 99%
“…The core idea of this technology is that the horizontal well is drilled in the roof or the floor, and the hydraulic fracture initiating in the roof or floor propagates into the coal seam. To date, the indirect fracturing technology has been successfully applied in Luling mine of Huaibei and in Zhaozhuang mine of Jincheng in China [7].…”
Section: Introductionmentioning
confidence: 99%
“…Huang et al [17][18] using the block discrete element method to explore the influence of engineering parameters on the behaviour process of hydraulic fractures penetrating bedding planes. Li et al [19] studied the propagation law of hydraulic fracture across the coal-rock interface based on Plasticity Fracture-Seepage (PF-S) model, and found that the in-situ stress and the interfacial shear strength are the dominant factor controlling the propagation of hydraulic fracture across the coal-rock interface. Escobar et al [20] studied the effect of stress interference on the penetration ability of multiple fractures using XFEM method, and the results showed that stress shadowing facilitate the propagation of hydraulic fracture from shale into roof rock.…”
Section: Introductionmentioning
confidence: 99%
“…ey found that only when the interface strength is relatively high would HFs will pass through the interface. According to the CT test and the nonlinear mechanicsleakage hypothesis, Li et al [9] developed a three-dimensional discontinuous network model and a plastic-nonlinear fracture-leakage-coupled constitutive formula. According to the numerical simulation results, Oyedere et al [10] believe that in low-permeability media, too high a fracturing fluid injection rate will stop the propagation of hydraulic fractures.…”
Section: Introductionmentioning
confidence: 99%