2006
DOI: 10.1016/j.soildyn.2006.01.006
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A few remarks on Biot's model and linear acoustics of poroelastic saturated materials

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Cited by 60 publications
(52 citation statements)
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“…Note that a comparable relation of the porosity can also be found for the fully compressible model of Biot as pointed out in a recent contribution [40]. Wilmański's porosity balance for the linear compressible model can be also discussed for the rigid grain limit…”
Section: Kinematical Assumptionssupporting
confidence: 53%
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“…Note that a comparable relation of the porosity can also be found for the fully compressible model of Biot as pointed out in a recent contribution [40]. Wilmański's porosity balance for the linear compressible model can be also discussed for the rigid grain limit…”
Section: Kinematical Assumptionssupporting
confidence: 53%
“…As remarked earlier in this contribution, this could only be achieved by a more realistic physically based approach for the non-equilibrium momentum interaction (inertia coupling), cf. the remarks in a recent work of Wilmański [40]. In the low-frequency range, viscous coupling locks the bone matrix and the bone marrow and prevents a travelling slow wave.…”
Section: Effective Stress Of the Solid Skeletonmentioning
confidence: 92%
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“…This makes it possible to match the additive stress decomposition (effective stress plus pore pressure) with the multiplicative decomposition of the deformation gradient (instead of the additive strain decomposition adopted in small-strain theory). In contrast with Wilmanski (2006), the free energy proves to be a potential for the stresses in the solid and fluid phases, and-extending Biot's linear theory-the volume fractions are obviously not considered constant. As a by-product, the proposed method provides the extension to large strains of the effective stress formulated by Nur & Byerlee (1971) for small strains and compressible solid constituents.…”
Section: Introductionmentioning
confidence: 99%
“…Following [28], we consider the case α ≈ 1, B ≈ 1, K u → ∞ and a linear dependence between the fluid pressure and the pore pressure, p l = (1 − φ)p [30]. Furthermore, we assume that the coupling is instantaneous.…”
Section: Incompressibility Conditionsmentioning
confidence: 99%