Porous Media: Theory and Experiments 1999
DOI: 10.1007/978-94-011-4579-4_19
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A Linear Theory of Porous Elastic Solids

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Cited by 9 publications
(19 citation statements)
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“…In addition to balances (6)(7)(8) and (10)(11)(12), we need the balance equations at a surface of discontinuity, namely a propagating wave Σ. As it is customary, we assume that the smooth movable surface Σ, that traverses the body B, is oriented and we denote by n the unit normal vector to Σ in the reference placement B * and by υ n the corresponding non-zero normal speed of displacement of Σ at point (x * , τ) in the reference placement.…”
Section: Balance Laws and Jump Conditionsmentioning
confidence: 99%
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“…In addition to balances (6)(7)(8) and (10)(11)(12), we need the balance equations at a surface of discontinuity, namely a propagating wave Σ. As it is customary, we assume that the smooth movable surface Σ, that traverses the body B, is oriented and we denote by n the unit normal vector to Σ in the reference placement B * and by υ n the corresponding non-zero normal speed of displacement of Σ at point (x * , τ) in the reference placement.…”
Section: Balance Laws and Jump Conditionsmentioning
confidence: 99%
“…where the second-order referential microinertia tensor field J * ∈ Sym + is constant (see [3,12,28]). As a consequence of this definition, the left-hand side of Eq.…”
Section: Thermodynamic Restrictions On the Constitutive Assumptionsmentioning
confidence: 99%
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