2016
DOI: 10.1016/j.ngib.2016.03.008
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Impacts of bedding directions of shale gas reservoirs on hydraulically induced crack propagation

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Cited by 21 publications
(11 citation statements)
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“…However, the main issue with DEM model is the computational cost, which becomes prohibitive if largescale problems need to be analyzed. Classical finite element method (FEM) (Dokhani et al 2016;Zeng and Wei 2017) and extended FEM (Sun et al 2016) have been successfully applied to fracture propagation and fracking simulations on shale rocks. Anisotropy has been included in some of these numerical simulations by decreasing the values of mechanical properties, such as elastic modulus, cohesion coefficients or fracture toughness, in precise locations of the domain in order to create weak layers which affect fracture extents and shapes.…”
Section: Introductionmentioning
confidence: 99%
“…However, the main issue with DEM model is the computational cost, which becomes prohibitive if largescale problems need to be analyzed. Classical finite element method (FEM) (Dokhani et al 2016;Zeng and Wei 2017) and extended FEM (Sun et al 2016) have been successfully applied to fracture propagation and fracking simulations on shale rocks. Anisotropy has been included in some of these numerical simulations by decreasing the values of mechanical properties, such as elastic modulus, cohesion coefficients or fracture toughness, in precise locations of the domain in order to create weak layers which affect fracture extents and shapes.…”
Section: Introductionmentioning
confidence: 99%
“…For the same rock sample, the relaxation rate ρ 2 and pore shape factor F S can be approximated as constants. Hence, the T 2 spectra can be used to determine the distribution of rock pores because rocks with longer relaxation times correspond to larger fractures, and vice versa [52,53].…”
Section: Nuclear Magneticmentioning
confidence: 99%
“…Bedding fractures are related to tectogenesis. Because beddings are the weak surfaces of strata, when the pressure gradient inside a closed system is greater than a critical value, a part of the bedding surface dislocates or opens to form a fracture [52,56]. Bedding fractures are nearly parallel to the bedding surface and cross mineral grains.…”
Section: Genetic Types Of Microfracturesmentioning
confidence: 99%
“…rock mechanics and hydraulic fracturing studies that show the bedding plane direction is generally weaker than the plane perpendicular to the bedding plane (Dyskin et al, 1991;Sun et al, 2016;Zhang et al, 2014), due to anisotropy resulting from the depositional environment and tectonic stresses as coal is formed. developed in coal #2 after EHD stimulation and that the fractures penetrate through the coal cube.…”
Section: Characterisation Of Coal After Ehd Stimulationmentioning
confidence: 99%