Search results for "Physics::Fluid Dynamics"

showing 10 items of 662 documents

Heat and mass transfer phenomena in magnetic fluids

2007

In this article the influence of a magnetic field on heat and mass transport phenomena in magnetic fluids (ferrofluids) will be discussed. The first section is dealing with a magnetically driven convection, the so called thermomagnetic convection while in the second section the influence of a temperature gradient on the mass transport, the Soret effect in ferrofluids, is reviewed. (© 2007 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim)

ConvectionMass transportFerrofluidMaterials scienceCondensed matter physicsApplied MathematicsGeneral Physics and AstronomyThermomagnetic convectionThermophoresisMagnetic fieldPhysics::Fluid DynamicsTemperature gradientMass transferGeneral Materials ScienceNonlinear Sciences::Pattern Formation and SolitonsGAMM-Mitteilungen
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A three-dimensional study of the onset of convection in a horizontal, rectangular porous channel heated from below

2012

Author's version of an article published in the journal: International Journal of Thermal Sciences. Also available from the publisher at: http://dx.doi.org/10.1016/j.ijthermalsci.2011.12.012 The onset of convection is studied in a rectangular channel filled with a fluid saturated porous medium, bounded above and below by impermeable isothermal walls at unequal temperatures and laterally by partially conducting walls. A three-dimensional linear stability analysis is carried out under the assumption of an infinite longitudinal channel length. Then, this assumption is relaxed in order to determine the threshold length for the three-dimensional convection to be the preferred mode at onset. Sens…

ConvectionMaterials scienceBiot number Darcy-Bénard problem lateral confinement linear stability method of weighted residuals rectangular channelAspect ratioBiot numberLINEAR STABILITYBIOT NUMBERGeneral EngineeringThermodynamicsMechanicsCondensed Matter PhysicsInstabilityVDP::Mathematics and natural science: 400::Mathematics: 410Physics::Fluid DynamicsTransverse planeDARCY-BÉNARD PROBLEMHeat transferMETHOD OF WEIGHTED RESIDUALSRECTANGULAR CHANNELLongitudinal waveLinear stability
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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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Simulation of turbulent metal flows

2007

Comprehensive knowledge of the heat and mass transfer processes in turbulent metal flows is required to realize efficient and reliable melting and casting processes. Experimental and numerical studies of the melt flow in induction furnaces show that the flow pattern, which comprise several vortexes of the mean flow, and the temperature distribution in the melt are significantly influenced by low-frequency large scale flow oscillations. Two- and three-dimensional hydrodynamic calculations of the melt flow, using two-equation turbulence models based on Reynolds Averaged Navier-Stokes approach, do not predict the large scale periodic flow instabilities obtained from the experimental data. That…

ConvectionMaterials scienceComputer simulationTurbulenceApplied MathematicsGeneral Physics and AstronomyMechanical engineeringMechanicsPhysics::Fluid DynamicsFlow (mathematics)Mass transferGeneral Materials ScienceMean flowMelt flow indexLarge eddy simulationGAMM-Mitteilungen
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Geoid effects in a convecting system with lateral viscosity variations

1992

The geoid signal and the flow patterns of two-dimensional steady state convection models with exponential temperature- and depth dependent viscosity are compared with results for an equivalent stratified viscosity structure. In analogy to Richards and Hager [1989], the latter are computed by a “dynamic response” approach. The flow fields obtained with this approach are quite different from the full solution; the geoid signals are similar but the amplitudes differ significantly. The differences are analysed in the horizontal wavenumber domain and in the spatial domain. They may lead to an overestimation of the viscosity contrast of the earth's mantle derived by modeling the earth's geoid wit…

ConvectionMechanicsGeodesyMantle (geology)Physics::GeophysicsExponential functionPhysics::Fluid DynamicsGeophysicsAmplitudeDownwellingGeoidGeneral Earth and Planetary SciencesWavenumberConvection–diffusion equationGeologyGeophysical Research Letters
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Heat transfer calculation in a free convection air solar collector

1998

This paper deals with the free convective air flow developing in a vertical channel with a rectangular cross-section heated on one side. The channel geometric and physical properties are such as to simulate an air solar collector suitable for building heating. A calculation method that can be applied to the transient combined heat transfer by conduction through the wall and by convection from the wall to the air stream is presented. The conduction across the wall is computed with a one-dimensional, time-dependent finite difference scheme, with convective boundary conditions at both wall surfaces. For the free convective flow along the channel, the air flow rate and the mean convective coeff…

ConvectionNatural convectionMaterials scienceConvective heat transferbusiness.industryMechanical EngineeringAirflowThermodynamicsBuilding and ConstructionMechanicsThermal conductionPhysics::Fluid DynamicsHeat transferTransient (oscillation)Electrical and Electronic EngineeringbusinessPhysics::Atmospheric and Oceanic PhysicsSolar powerCivil and Structural EngineeringEnergy and Buildings
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Magnetic field driven micro-convection in the Hele-Shaw cell

2013

AbstractMicro-convection caused by ponderomotive forces of the self-magnetic field of a magnetic fluid in the Hele-Shaw cell under the action of a vertical homogeneous magnetic field is studied both experimentally and numerically. It is shown that a non-potential magnetic force at magnetic Rayleigh numbers greater than the critical value causes fingering at the interface between the miscible magnetic and non-magnetic fluids. The threshold value of the magnetic Rayleigh number depends on the smearing of the interface between fluids. Fingering with its subsequent decay due to diffusion of particles significantly increases the mixing at the interface. Velocity and vorticity fields at fingering…

ConvectionPhysicsField (physics)Mechanical EngineeringMechanicsRayleigh numberVorticityequipment and suppliesCondensed Matter PhysicsCritical valueMagnetic fieldPhysics::Fluid DynamicsHele-Shaw flowParticle image velocimetryMechanics of Materialshuman activitiesNonlinear Sciences::Pattern Formation and SolitonsJournal of Fluid Mechanics
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The onset of convection in a two-layered porous medium with anisotropic permeability

2019

We consider convection in a horizontal porous layer of uniform thickness which is heated from below and which is composed of two anisotropic sublayers with principal axes lying in the three coordinate directions. The aim is to determine criteria for the onset of convection by finding the critical Rayleigh number, wavenumber and roll orientation relative to the coordinate axes. The full set of nondimensional parameters has at least six members even when the sublayers are considered to be thermally isotropic, and therefore, we select some special cases in order to illuminate the type of qualitative behaviour which may be expected. One such case is where the anisotropic sublayers are identical…

ConvectionPhysicsGeneral Chemical Engineering0208 environmental biotechnologyIsotropyGeometry02 engineering and technologyRayleigh number010502 geochemistry & geophysics01 natural sciencesVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410Catalysis020801 environmental engineeringVortexPhysics::Fluid DynamicsOrientation (geometry)WavenumberAnisotropy0105 earth and related environmental sciencesPrincipal axis theorem
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Mixed MHD convection and Tritium transport in fusion-relevant configurations

2005

Mixed MHD flow and Tritium transport were computed for a slender poloidal duct, representative of a DEMO HCLL blanket element. 2-D flow and temperature fields were computed in the duct's cross section under the assumption of parallel, fully developed flow, while Tritium concentration C was found by solving a fully 3-D problem with simplifying assumptions at the duct's ends. The spatial distribution of C depended on the intensity and direction of the forced flow. Significant peak factors were obtained if the net flow rate was so low that re-circulation occurred; C maxima were attained near the walls for upward flow, in the core region for downward flow.

ConvectionPhysicsMechanical EngineeringHCLL blanketMechanicsBlanketFusion powerMagnetohydrodynamicVolumetric flow ratePhysics::Fluid DynamicsNuclear physicsNuclear Energy and EngineeringCombined forced and natural convectionFlow conditioningGeneral Materials ScienceDuct (flow)Mixed convectionMagnetohydrodynamicsSettore ING-IND/19 - Impianti NucleariCivil and Structural Engineering
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Magnetic field driven micro-convection in the Hele-Shaw cell: the Brinkman model and its comparison with experiment

2015

International audience; The micro-convection caused by the ponderomotive forces of the self-magnetic field in a magnetic fluid is studied here both numerically and experimentally. The theoretical approach based on the general Brinkman model substantially improves the description with respect to the previously proposed Darcy model. The predictions of both models are here compared to finely controlled experiments. The Brinkman model, in contrast to the Darcy model, allows us to describe the formation of mushrooms on the plumes of the micro-convective flow and the width of the fingers. In the Brinkman approach, excellent quantitative agreement is also obtained for the finger velocity dynamics …

ConvectionPhysics[PHYS.PHYS.PHYS-FLU-DYN]Physics [physics]/Physics [physics]/Fluid Dynamics [physics.flu-dyn]Field (physics)Mechanical EngineeringFlow (psychology)Field strengthMechanicsRayleigh numberCondensed Matter PhysicsMagnetic fieldPhysics::Fluid DynamicsHele-Shaw flowMechanics of Materials[PHYS.COND.CM-MS]Physics [physics]/Condensed Matter [cond-mat]/Materials Science [cond-mat.mtrl-sci]Diffusion (business)[PHYS.COND]Physics [physics]/Condensed Matter [cond-mat]
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