Search results for "Rayleigh number"

showing 2 items of 22 documents

Linear instability of the vertical throughflow in a horizontal porous layer saturated by a power-law fluid

2016

Abstract The effects of the vertical throughflow of a non-Newtonian power-law fluid on the onset of convective instability in a horizontal porous layer are investigated. The extended Darcy’s model of momentum diffusion is employed together with the Oberbeck–Boussinesq approximation. A stationary basic solution for the vertical throughflow is determined analytically. The basic velocity and temperature fields turn out to be independent of the non-Newtonian rheology. A linear stability analysis is carried out, leading to a fourth-order eigenvalue problem. A numerical solution of the eigenvalue problem is employed to obtain the neutral stability curves and the critical Rayleigh number for the o…

Power-law fluid0208 environmental biotechnologyThermodynamics02 engineering and technologyPéclet numberCondensed Matter Physic01 natural sciencesInstability010305 fluids & plasmasMomentum diffusionPhysics::Fluid Dynamicssymbols.namesakeConvective instability0103 physical sciencesPhysicsFluid Flow and Transfer ProcessesThroughflowConvective instabilityMechanical EngineeringNon-Newtonian fluidRayleigh numberPorous mediumRayleigh numberMechanicsCondensed Matter PhysicsNon-Newtonian fluid020801 environmental engineeringsymbolsVertical throughflow
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Stability of Flow with Viscous Dissipation in a Horizontal Porous Layer with an Open Boundary Having a Prescribed Temperature Gradient

2010

Published version of an article in the journal: Transport in Porous Media. The original publication is available at www.springerlink.com, http://dx.doi.org/10.1007/s11242-010-9588-6 A buoyancy-induced stationary flow with viscous dissipation in a horizontal porous layer is investigated. The lower boundary surface is impermeable and subject to a uniform heat flux. The upper open boundary has a prescribed, linearly varying, temperature distribution. The buoyancy-induced basic velocity profile is parallel and non-uniform. The linear stability of this basic solution is analysed numerically by solving the disturbance equations for oblique rolls arbitrarily oriented with respect to the basic velo…

VDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413PhysicsBuoyancyOPEN BOUNDARYGeneral Chemical EngineeringBoundary (topology)MechanicsRayleigh numberPOROUS LAYERengineering.materialCritical valueVISCOUS DISSIPATIONInstabilityCatalysisTHERMAL INSTABILITYPhysics::Fluid DynamicsTemperature gradientClassical mechanicsHeat fluxPRESCRIBED TEMPERATURE GRADIENTengineeringVDP::Technology: 500::Materials science and engineering: 520Linear stabilityTransport in Porous Media
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