Search results for "Fluid dynamic"

showing 10 items of 1034 documents

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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In-flight temperature of solid micrometric powders during cold spray additive manufacturing

2020

Abstract During cold dynamic gas spray additive manufacturing, the thermal field within particles is generally simplified by a state of an instantaneous uniform distribution over the particle's media at any position inside and outside the De-Laval nozzle. This paper addresses critical discussions using analytical and computational analysis of the transient heat transfer within the solid particles due to the convective exchange with the flowing gas. An analytical criterion depicts conditions of instantaneous uniform temperature over the range of typical cold spray data including various particle thermal conductivity, particle size range, dragging velocities, gas nature and gas setting condit…

ConvectionRange (particle radiation)Materials science020209 energyGeneral EngineeringGas dynamic cold spray02 engineering and technologyMechanicsCondensed Matter PhysicsResidence time (fluid dynamics)01 natural sciences010305 fluids & plasmasTemperature gradient[SPI]Engineering Sciences [physics]Thermal conductivity0103 physical sciences0202 electrical engineering electronic engineering information engineeringParticleParticle size
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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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