2011
DOI: 10.1007/s11242-011-9781-2
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Poroelasticity-II: On the Equilibrium State of the Fluid-Filled Penetrable Poroelastic Body

Abstract: Part-II of the paper titled "Poroelasticity-II" is devoted to defining the joint equilibrium state of a fluid and elastic penetrable material, encapsulated in a rigid volume, . One can ask different questions in respect to such an equilibrium state, such as: (1) In what physical state will the fluid be, if the porous volume of the poroelastic material is filled with a given mass of fluid? (2) What is the capacity of a volume filled with a penetrable sponge in respect to the fluid being in specific state? etc. … Show more

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Cited by 10 publications
(3 citation statements)
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“…Other recent considerations can be found in [39,204,260]. An elegant approach based on a Lagrangian formulation and representative elementary volume averaging can be found in [177][178][179]. The authors state that their final set of equations is equivalent to Biot's equations for homogeneous, consolidated (nondegenerated) materials with negligible porosity dynamics if at most linear waves are considered [178].…”
Section: Literature On Rock Mechanics and Geomechanicsmentioning
confidence: 99%
See 1 more Smart Citation
“…Other recent considerations can be found in [39,204,260]. An elegant approach based on a Lagrangian formulation and representative elementary volume averaging can be found in [177][178][179]. The authors state that their final set of equations is equivalent to Biot's equations for homogeneous, consolidated (nondegenerated) materials with negligible porosity dynamics if at most linear waves are considered [178].…”
Section: Literature On Rock Mechanics and Geomechanicsmentioning
confidence: 99%
“…An elegant approach based on a Lagrangian formulation and representative elementary volume averaging can be found in [177][178][179]. The authors state that their final set of equations is equivalent to Biot's equations for homogeneous, consolidated (nondegenerated) materials with negligible porosity dynamics if at most linear waves are considered [178]. Consequently, the considerations in this thesis are based on Biot's equations as we are interested in consolidation phenomena.…”
Section: Literature On Rock Mechanics and Geomechanicsmentioning
confidence: 99%
“…The first studies of poroelasticity are due to Biot [9][10][11][12][13] in which a linear mathematical model of poroelasticity theory was introduced. Subsequently, more sophisticated models of poroelasticity have been proposed, these include, various nonlinear models, and models with physically feasible boundary conditions and interface conditions, see, for example, [14][15][16].…”
Section: Introductionmentioning
confidence: 99%