1998
DOI: 10.1006/jcph.1998.5858
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An Efficient Boundary Integral Formulation for Flow Through Fractured Porous Media

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Cited by 82 publications
(60 citation statements)
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“…The hydrofractures are extremely permeable with respect to other structural features and define the domain from which shale gas will be produced. In general, the aperture size of fractures is much smaller than the length scale of matrix block fractures, and the hydrofractures can be modelled as two-dimensional planes in an asymptotic approximation (Lough, Lee & Kamath 1998). …”
Section: Hydraulic Fracturesmentioning
confidence: 99%
“…The hydrofractures are extremely permeable with respect to other structural features and define the domain from which shale gas will be produced. In general, the aperture size of fractures is much smaller than the length scale of matrix block fractures, and the hydrofractures can be modelled as two-dimensional planes in an asymptotic approximation (Lough, Lee & Kamath 1998). …”
Section: Hydraulic Fracturesmentioning
confidence: 99%
“…In order to homogenize small-scale fractures, Oda (1985) derived a simple analytical expression for enhanced matrix permeability for gridblocks that contain very short fractures. Likewise, Lough et al (1997Lough et al ( , 1998 developed a boundary element method (with uniform pressure and periodic boundary conditions) to calculate effective conductivity for gridblocks containing multiple fractures.…”
Section: Overview Of Edfmmentioning
confidence: 99%
“…The previous cell was used as a means to study porous media or fractures, in the same way as a Hele-Shaw cell can be used for such a study (e.g., Lough et al 1998;Oltean et al 2004). As the macroscopic flow is globally directed along x 1 , we can define both macroscopic 1D-pressure P and 1D-velocity V as follows: (1) where S(x 1 ) is the vertical cross-section, |S(x 1 )| is the cross-section area and e 1 is the unit vector along x 1 .…”
Section: Macroscopic Flow Equationmentioning
confidence: 99%