Search results for "VISCOUS DISSIPATION"

showing 5 items of 5 documents

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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Linear instability of mixed convection of cold water in a porous layer induced by viscous dissipation

2009

Accepted version of an article published in the journal: International Journal of Thermal Sciences, Elsevier Published version available on Science Direct: http://dx.doi.org/10.1016/j.ijthermalsci.2008.06.012 An analysis of linear stability of the stationary laminar Darcy flow in a horizontal porous layer is performed. The porous layer is saturated with cold water. The upper plane boundary is assumed to be subject to heat transfer with finite conductance to an environment at the temperature of maximum density of cold water. The lower plane boundary is adiabatic. Convective instabilities are caused by flow viscous dissipation, inducing a basic temperature distribution that decreases in the u…

VDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413Materials scienceDarcy's lawLINEAR STABILITYGeneral EngineeringThermodynamicsLaminar flowCondensed Matter PhysicsInstabilityVISCOUS DISSIPATIONVDP::Mathematics and natural science: 400::Physics: 430Physics::Fluid DynamicsDARCY LAWPOROUS MEDIUMCombined forced and natural convectionHeat transferThermalPorous mediumBUOYANT FLOWLinear stability
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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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Darcy–Forchheimer Magnetized Nanofluid flow along with Heating and Dissipation Effects over a Shrinking Exponential Sheet with Stability Analysis

2022

Nanoparticles have presented various hurdles to the scientific community during the past decade. The nanoparticles dispersed in diverse base fluids can alter the properties of fluid flow and heat transmission. In the current examination, a mathematical model for the 2D magnetohydrodynamic (MHD) Darcy–Forchheimer nanofluid flow across an exponentially contracting sheet is presented. In this mathematical model, the effects of viscous dissipation, joule heating, first-order velocity, and thermal slip conditions are also examined. Using similarity transformations, a system of partial differential equations (PDEs) is converted into a set of ordinary differential equations (ODEs). The problem is …

Darcy–Forchheimer; nanofluid; viscous dissipation; joule heating; duality; stabilityControl and Systems EngineeringMechanical EngineeringElectrical and Electronic EngineeringMicromachines
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Modeling Atmospheric Turbulence via Rapid Distortion Theory: Spectral Tensor of Velocity and Buoyancy

2017

Abstract A spectral tensor model is presented for turbulent fluctuations of wind velocity components and temperature, assuming uniform vertical gradients in mean temperature and mean wind speed. The model is built upon rapid distortion theory (RDT) following studies by Mann and by Hanazaki and Hunt, using the eddy lifetime parameterization of Mann to make the model stationary. The buoyant spectral tensor model is driven via five parameters: the viscous dissipation rate ε, length scale of energy-containing eddies L, a turbulence anisotropy parameter , gradient Richardson number (Ri) representing the local atmospheric stability, and the rate of destruction of temperature variance . Model outp…

Length scaleAtmospheric Science010504 meteorology & atmospheric sciencesK-epsilon turbulence modelFLOWVelocityTensorsWind01 natural sciencesWind speedAtmospheric temperature010305 fluids & plasmasPhysics::Fluid DynamicsEnergy-containing eddiesConvergence of numerical methodsMonin-Obukhov similarity theorySCALEPhysicsTurbulenceAtmospheric turbulenceMechanicsBuoyancySURFACE-LAYER TURBULENCEClassical mechanicsFluxesStratified turbulenceSIMILARITYSIMULATIONBoundary layersStabilityBuoyancyMETEOROLOGYengineering.materialPROFILEAtmospheric thermodynamics0103 physical sciencesAtmospheric instabilityWind shearsSTABLY STRATIFIED TURBULENCETensorRapid distortion theory0105 earth and related environmental sciencesWind shearBoundary layer flowRichardson numberAtmospheric observationsViscous dissipation rateHorizontal array turbulence study field programsTurbulenceBoundary layerengineeringJournal of the Atmospheric Sciences
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