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Compressibility Effect on Darcy Porous Convection

Giuseppe Arnone, Florinda Capone, Roberta De Luca, Giuliana Massa

2023Transport in Porous Media10 citationsDOIOpen Access PDF

Abstract

Abstract Perfectly incompressible materials do not exist in nature but are a useful approximation of several media which can be deformed in non-isothermal processes but undergo very small volume variations. In this paper, the linear analysis of the Darcy-Bénard problem is performed in the class of extended-quasi-thermal-incompressible fluids, introducing a factor $$\beta$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mi>β</mml:mi> </mml:math> which describes the compressibility of the fluid and plays an essential role in the instability results. In particular, in the Oberbeck-Boussinesq approximation, a more realistic constitutive equation for the fluid density is employed in order to obtain more thermodynamically consistent instability results. The critical Rayleigh-Darcy number for the onset of convection is determined, via linear instability analysis of the conduction solution, as a function of a dimensionless parameter $$\widehat{\beta }$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mover> <mml:mi>β</mml:mi> <mml:mo>^</mml:mo> </mml:mover> </mml:math> proportional to the compressibility factor $$\beta$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mi>β</mml:mi> </mml:math> , proving that $$\widehat{\beta }$$ <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> <mml:mover> <mml:mi>β</mml:mi> <mml:mo>^</mml:mo> </mml:mover> </mml:math> enhances the onset of convective motions. Article Highlights The onset of convection in fluid-saturated porous media is analyzed, taking into account fluid compressibility effect. The critical Rayleigh-Darcy number is determined in a closed algebraic form via linear instability analysis. The critical Rayleigh-Darcy number is shown to be a decreasing function of the dimensionless compressibility factor.

Topics & Concepts

CompressibilityThermodynamicsConvectionRayleigh numberDimensionless quantityPorous mediumPhysicsMaterials scienceNatural convectionPorosityComposite materialFluid Dynamics and Turbulent FlowsNavier-Stokes equation solutionsNanofluid Flow and Heat Transfer