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Wave propagation in poroelastic media: A velocity-stress staggered-grid finite-difference method with perfectly matched layers
Date
2003-01-01
Author
Sheen, Dong-Hoon
Tuncay, Kağan
Baag, Chang-Eob
Ortoleva, Peter J.
Metadata
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URI
https://hdl.handle.net/11511/36221
Journal
SEG Technical Program Expanded Abstracts
DOI
https://doi.org/10.1190/1.1817810
Collections
Department of Civil Engineering, Article
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Wave propagation in poroelastic media: A velocity-stress staggered-grid finite-difference method with perfectly matched layers
Sheen, Dong-hoon; Tuncay, Kağan; Baag, Chang-eob; Ortoleva, Peter J. (2003-01-01)
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<jats:p>A theory of wave propagation in isotropic poroelastic media saturated by two immiscible Newtonian fluids is presented. The macroscopic constitutive relations, and mass and momentum balance equations are obtained by volume averaging the microscale balance and constitutive equations and assuming small deformations. Momentum transfer terms are expressed in terms of intrinsic and relative permeabilities assuming the validity of Darcy’s law. The coefficients of macroscopic constitutive relations are expr...
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A study of wave propagation in fractured porous media saturated by two immiscible fluids is presented, based on the double-porosity concept. The macroscopic constitutive relations and mass and momentum balance equations are obtained by volume averaging the microscale balance and constitutive equations, and assuming small deformations. Momentum transfer terms are expressed in terms of intrinsic and relative permeabilities assuming the validity of Darcy's law in fractured porous media. In the simplest case, t...
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D.-H. Sheen, K. Tuncay, C.-E. Baag, and P. J. Ortoleva, “Wave propagation in poroelastic media: A velocity-stress staggered-grid finite-difference method with perfectly matched layers,”
SEG Technical Program Expanded Abstracts
, pp. 2295–2298, 2003, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/36221.