Search results for "porous medium"

showing 10 items of 164 documents

Trapping and mobilization of residual fluid during capillary desaturation in porous media

1998

We discuss the problem of trapping and mobilization of nonwetting fluids during immiscible two-phase displacement processes in porous media. Capillary desaturation curves give residual saturations as a function of capillary number. Interpreting capillary numbers as the ratio of viscous to capillary forces the breakpoint in experimental curves contradicts the theoretically predicted force balance. We show that replotting the data against a novel macroscopic capillary number resolves the problem for discontinuous mode displacement.

Condensed Matter::Soft Condensed MatterPhysics::Fluid DynamicsCapillary pressureMaterials scienceCapillary actionTrappingMechanicsResidualGranular materialPorous mediumDisplacement (fluid)Capillary numberPhysical Review E
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Large time behavior for a porous medium equation in a nonhomogeneous medium with critical density

2014

Abstract We study the large time behavior of solutions to the Cauchy problem for the porous medium equation in nonhomogeneous media with critical singular density | x | − 2 ∂ t u = Δ u m , in R N × ( 0 , ∞ ) , where m > 1 and N ≥ 3 , with nonnegative initial condition u ( x , 0 ) = u 0 ( x ) ≥ 0 . The asymptotic behavior proves to have some interesting and striking properties. We show that there are different asymptotic profiles for the solutions, depending on whether the continuous initial data u 0 vanishes at x = 0 or not. Moreover, when u 0 ( 0 ) = 0 , we show the convergence towards a peak-type profile presenting a jump discontinuity, coming from an interesting asymptotic simplification…

Conservation lawSingularityApplied MathematicsMathematical analysisConvergence (routing)Initial value problemScale (descriptive set theory)Limit (mathematics)Classification of discontinuitiesPorous mediumAnalysisMathematicsNonlinear Analysis: Theory, Methods & Applications
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A fractional order theory of poroelasticity

2019

Abstract We introduce a time memory formalism in the flux-pressure constitutive relation, ruling the fluid diffusion phenomenon occurring in several classes of porous media. The resulting flux-pressure law is adopted into the Biot’s formulation of the poroelasticity problem. The time memory formalism, useful to capture non-Darcy behavior, is modeled by the Caputo’s fractional derivative. We show that the time-evolution of both the degree of settlement and the pressure field is strongly influenced by the order of Caputo’s fractional derivative. Also a numerical experiment aiming at simulating the confined compression test poroelasticity problem of a sand sample is performed. In such a case, …

Constitutive equationPoromechanics02 engineering and technology01 natural sciencesPressure fieldDarcy–Weisbach equationPhysics::Geophysics010305 fluids & plasmas0203 mechanical engineeringFractional operators0103 physical sciencesCaputo's fractional derivative; Fractional operators; PoroelasticityApplied mathematicsGeneral Materials ScienceCaputo's fractional derivative Fractional operators PoroelasticityCaputo's fractional derivativeCivil and Structural EngineeringMathematicsOrder theoryBiot numberMechanical EngineeringPoroelasticityCondensed Matter PhysicsFractional calculus020303 mechanical engineering & transportsMechanics of MaterialsFractional operatorSettore ICAR/08 - Scienza Delle CostruzioniPorous medium
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Onset of convective rolls in a circular porous duct with external heat transfer to a thermally stratified environment

2011

A horizontal circular duct filled with a fluid saturated porous medium is studied. The external wall is assumed to exchange heat with an external environment thermally stratified in the vertical direction. The external heat transfer is modeled through a third kind boundary condition, and a Biot number associated with the external heat transfer coefficient is defined. The linear stability of the basic state where the velocity field is zero is studied numerically. The condition of neutral stability is determined, by solving the system of elliptic governing equations for the disturbances through a Galerkin finite-element method. The neutral stability curves, together with the critical values o…

ConvectionMaterials scienceBiot numberLINEAR STABILITYBIOT NUMBERGeneral EngineeringThermodynamicsCIRCULAR CYLINDERHeat transfer coefficientRayleigh numberMechanicsCondensed Matter PhysicsNusselt numberPhysics::Fluid DynamicsPOROUS MEDIUMConvective instabilityHeat transferCONVECTIVE INSTABILITYLinear stabilityInternational Journal of Thermal Sciences
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Onset of convection in a vertical porous cylinder with a permeable and conducting side boundary

2015

Abstract The onset of natural convection in a vertical porous cylinder saturated by a fluid is studied. The lateral confinement of the porous cylinder is due to an external porous medium having a permeability much smaller than that of the cylinder. Thus, the vertical side boundary of the cylinder is permeable and constrained by given pressure and temperature distributions. The lower and upper plane boundaries of the cylinder are impermeable walls. The lower wall is subject to a uniform heat flux, while the upper wall has a uniform temperature. The basic motionless state displays a uniform and vertical temperature gradient oriented downward. The linear stability analysis is carried out by us…

ConvectionRayleigh–Bénard problemMaterials scienceNatural convectionGeneral EngineeringPorous mediumMechanicsCondensed Matter PhysicsPhysics::Fluid DynamicsTemperature gradientsymbols.namesakeMathieu functionClassical mechanicsHeat fluxNatural convectionDispersion relationsymbolsVertical cylinderLinear stabilityPorous mediumLinear stability
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Viscous dissipation and thermoconvective instabilities in a horizontal porous channel heated from below

2010

Accepted version of av article from the journal: International Journal of Thermal Sciences. Published version available on Science Direct: http://dx.doi.org/10.1016/j.ijthermalsci.2009.10.010 A linear stability analysis of the basic uniform flow in a horizontal porous channel with a rectangular cross section is carried out. The thermal boundary conditions at the impermeable channel walls are: uniform incoming heat flux at the bottom wall, uniform temperature at the top wall, adiabatic lateral walls. Thermoconvective instabilities are caused by the incoming heat flux at the bottom wall and by the internal viscous heating. Linear stability against transverse or longitudinal roll disturbances …

ConvectionVDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413Darcy's lawMaterials scienceLINEAR STABILITYGeneral EngineeringThermodynamicsMechanicsCondensed Matter PhysicsInstabilityVISCOUS DISSIPATIONPhysics::Fluid DynamicsHeat fluxPOROUS MEDIUMCONVECTIVE ROLLSHeat transferPotential flowVDP::Technology: 500::Materials science and engineering: 520Adiabatic processDARCY'S LAWLinear stability
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Onset of convection in a porous rectangular channel with external heat transfer to upper and lower fluid environments

2012

Published version of an article in the journal: Transport in Porous Media. Also available from the publisher at: http://dx.doi.org/10.1007/s11242-012-0018-9 The conditions for the onset of convection in a horizontal rectangular channel filled with a fluid saturated porous medium are studied. The vertical sidewalls are assumed to be impermeable and adiabatic. The horizontal upper and lower boundary walls are considered as impermeable and subject to external heat transfer, modelled through a third-kind boundary condition on the temperature field. The external fluid environments above and below the channel, kept at different temperatures, provide the heating-from-below mechanism which may lead…

ConvectionVDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413Materials scienceDarcy's lawBiot numberGeneral Chemical EngineeringThermodynamicsMechanicsCatalysisPhysics::Fluid Dynamicsanalytical solutionDarcy’s lawHeat transferBoundary value problemVDP::Technology: 500::Materials science and engineering: 520Porous mediumAdiabatic processrectangular porous channelDarcy–Bénard problemLongitudinal wavelinear stabilitythird-kind temperature conditions
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Onset of Convection in an Inclined Anisotropic Porous Layer with Internal Heat Generation

2019

The onset of convection in an inclined porous layer which is heated internally by a uniform distribution of heat sources is considered. We investigate the combined effects of inclination, anisotropy and internal heat generation on the linear instability of the basic parallel flow. When the Rayleigh number is sufficiently large, instability occurs and a convective motion is set up. It turns out that the preferred motion at convection onset depends quite strongly on the anisotropy ratio, &xi

ConvectioninclinationMaterials scienceonsetComputingMethodologies_IMAGEPROCESSINGANDCOMPUTERVISION02 engineering and technologyanisotropylcsh:Thermodynamics01 natural sciencesInstability010305 fluids & plasmasPhysics::Fluid Dynamicsporous media0203 mechanical engineeringlcsh:QC310.15-3190103 physical sciencesAstrophysics::Solar and Stellar Astrophysicsheat generationAnisotropyconvectionlcsh:QC120-168.85Fluid Flow and Transfer ProcessesMechanical EngineeringMechanicsRayleigh numberCondensed Matter PhysicsVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410Transverse plane020303 mechanical engineering & transportsTheoryofComputation_MATHEMATICALLOGICANDFORMALLANGUAGESHeat generationComputer Science::Programming Languageslcsh:Descriptive and experimental mechanicsAstrophysics::Earth and Planetary AstrophysicsInternal heatingPorous mediumFluids
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Reconstruction of random media using Monte Carlo methods.

1998

A simulated annealing algorithm is applied to the reconstruction of two-dimensional porous media with prescribed correlation functions. The experimental correlation function of an isotropic sample of Fontainebleau sandstone and a synthetic correlation function with damped oscillations are used in the reconstructions. To reduce the numerical effort we follow a proposal suggesting the evaluation of the correlation functions only along certain directions. The results show that this simplification yields significantly different microstructures as compared to a full evaluation of the correlation function. In particular, we find that the simplified reconstruction method introduces an artificial a…

Correlation function (statistical mechanics)Mathematical optimizationIsotropySimulated annealingMonte Carlo methodStatistical physicsFunction (mathematics)Granular materialAnisotropyPorous mediumMathematicsPhysical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics
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Lower semicontinuity of weak supersolutions to the porous medium equation

2013

Weak supersolutions to the porous medium equation are defined by means of smooth test functions under an integral sign. We show that nonnegative weak supersolutions become lower semicontinuous after redefinition on a set of measure zero. This shows that weak supersolutions belong to a class of supersolutions defined by a comparison principle.

Degenerate diffusion35K55 31C45Applied MathematicsGeneral MathematicsMathematical analysista111Mathematics::Analysis of PDEscomparison principlelower semicontinuitysupersolutionsMathematics - Analysis of PDEsporous medium equationFOS: MathematicsPorous mediumdegenerate diffusionSign (mathematics)MathematicsAnalysis of PDEs (math.AP)
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