Search results for " Convection"

showing 10 items of 110 documents

One-dimensional Mixed MHD Convection

2006

The parallel, fully developed flow of an electrically conducting fluid between plane parallel walls under the simultaneous influence of a driving pressure head, buoyancy, and magnetohydrodynamic (MHD) forces is studied. The fluid is assumed to be internally heated and the flow is modeled as one-dimensional and incompressible, while the Boussinesq approximation is adopted for the buoyancy terms. Analytical solutions are obtained for temperature, velocity and electrical potential under different electrical boundary conditions, forced to natural convection intensity ratios and values of the magnetic induction. Generalized working charts are presented which synthetically describe the system''s …

Fluid Flow and Transfer ProcessesPhysicsBuoyancyNatural convectionMagnetohydrodynamic generatorMechanical EngineeringMAGNETIC FIELDMechanicsCUBIC ENCLOSUREengineering.materialCondensed Matter PhysicsOpen-channel flowlaw.inventionPhysics::Fluid DynamicsClassical mechanicslawCombined forced and natural convectionCHANNEL FLOWengineeringMagnetohydrodynamic driveMagnetohydrodynamicsBoussinesq approximation (water waves)LIQUID-METAL
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An experimental investigation on natural convection of air in a vertical channel

1993

Abstract The free convection of air in a vertical channel is studied experimentally in a laboratory model of height H = 2.6 m and rectangular cross-section b × s , with b = 1.2 m and the channel width s variable. One of the channel walls is heated with a uniform heat flux. Tests are made with different values of channel gap and heating power ( s = 7.5, 12.5, 17 cm; q c = 48–317 W m −2 ). On the basis of the results two empirical formulae are found, giving Nu and Re as functions of Ra and the geometrical parameter s/H ; Nu = 0.9282 Ra 0.2035 (s/H) 0.8972 ; Re = 0.5014 Ra 0.3148 (s/H) 0.418 . The mathematical form of these relationships reproduces other previously published formulae, valid fo…

Fluid Flow and Transfer ProcessesPhysicsVertical channelHeating powerNatural convectionMechanical EngineeringReynolds numberGeometryRayleigh numberCondensed Matter PhysicsNusselt numbersymbols.namesakeHeat fluxsymbolsCommunication channelInternational Journal of Heat and Mass Transfer
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Enhancement of heat exchanger thermal hydraulic performance using aluminum foam

2018

Abstract This paper deals with an experimental study of a turbulent forced convection in a rectangular channel partly fitted with aluminum metallic foam blocks. Experiments were carried out on samples having a constant porosity of 93.8%, different grades of 5, 20 and 40 PPI, and three different height ratios of 0.6, 0.8 and 1. The blocks were arranged in a baffle like configuration. A constant heat flux of 2 W/cm2 was applied on the bottom wall of the test section, while air velocity was varied from 1 to 5 m·s−1. Temperatures of the wall along the flow direction as well as those of the inlet and outlet sections have been measured. Additionally, pressure drop measurements across the aluminum…

Fluid Flow and Transfer ProcessesPressure dropMaterials science020209 energyMechanical EngineeringGeneral Chemical EngineeringPlate heat exchangerAerospace EngineeringBaffle02 engineering and technology021001 nanoscience & nanotechnologyForced convectionNuclear Energy and EngineeringHeat fluxHeat transfer0202 electrical engineering electronic engineering information engineeringPlate fin heat exchangerComposite material0210 nano-technologyShell and tube heat exchangerExperimental Thermal and Fluid Science
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Study on heat transfer coefficients during cooling of PET bottles for food beverages

2015

The heat transfer properties of different cooling systems dealing with Poly-Ethylene-Terephthalate (PET) bottles were investigated. The heat transfer coefficient (Ug) was measured in various fluid dynamic conditions. Cooling media were either air or water. It was shown that heat transfer coefficients are strongly affected by fluid dynamics conditions, and range from 10 W/m2 K to nearly 400 W/m2 K. PET bottle thickness effect on Ug was shown to become relevant under faster fluid dynamics regimes.

Fluid Flow and Transfer ProcessesRange (particle radiation)Natural convectionMaterials sciencebusiness.product_category020209 energyThermodynamics02 engineering and technologyHeat transfer coefficientCondensed Matter PhysicCondensed Matter PhysicsHeat transfer0202 electrical engineering electronic engineering information engineeringFluid dynamicsBottlebusiness
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Constraining lithospheric flow.

2016

The motion of Earth's tectonic plates—the lithosphere—is driven by the subduction of relatively cold and dense oceanic plates into the mantle. The resulting forces drive the motions of continental plates, but the manner in which this happens depends on the effective viscosities of the lithosphere and mantle. On page 1515 of this issue, Liu and Hasterok ( 1 ) discuss a novel method of constraining viscosities of the lithosphere from geophysical data.

Gene FlowMultidisciplinary010504 meteorology & atmospheric sciencesSubductionGeophysics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Plate tectonicsTectonicsMantle convectionLithosphereOceanic crustHumansGeologyBlood Flow Velocity0105 earth and related environmental sciencesScience (New York, N.Y.)
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Effects of Rayleigh number length thickness of continent on time of mantle flow reversal

1998

Abstract Numerical experiments are carried out to study the effects of continents on the structure of thermal convection in the mantle. The mantle is modelled by a viscous fluid occupying a horizontally extended rectangular 2-D region of aspect ratio 10:1. Continents are treated as thick rigid heat-conducting plates placed in the mantle, with free-slip and with no-slip conditions. Continents restrict the heat release from the underlying mantle; the mantle material heats up and becomes lighter; as a result, a hot upwelling flow replaces downwelling. We calculate the characteristic time τ of this restructuring for various values of model parameters and obtain analytical approximations for τ a…

GeophysicsMantle wedgeMantle convectionConvective heat transferDownwellingRayleigh numberGeophysicsViscous liquidGeologyMantle (geology)Earth-Surface ProcessesEarth's internal heat budgetJournal of Geodynamics
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Lithospheric stresses in Rayleigh–Bénard convection: effects of a free surface and a viscoelastic Maxwell rheology

2015

GeophysicsRheologyGeochemistry and PetrologyLithosphereFree surfaceLithospheric flexureGeophysicsGeologyViscoelasticityRayleigh–Bénard convectionGeophysical Journal International
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A reversible hydrogen‐bond isomerization triggered by an abrupt spin crossover near room temperature.

2020

The spin crossover salt [Fe(bpp) 2 ](isonicNO) 2 ·2.4H 2 O ( 1 ·2.4H 2 O) (bpp = 2,6‐bis(pyrazol‐3‐yl)pyridine; isonicNO = isonicotinate N‐oxide anion) exhibits a very abrupt spin crossover at T 1 /2 = 274.4 K. This triggers a supramolecular linkage (H‐bond) isomerization that responds reversibly towards light irradiation or temperature change. Isotopic effects in the thermomagnetic behaviour reveal the importance of hydrogen bonds in defining the magnetic state. Further, the title compound can be reversibly dehydrated to afford 1 , a material that also exhibits spin crossover coupled to H‐bond isomerization, leading to strong kinetic effects in the thermomagnetic properties.

Hydrogen bondChemistryOrganic ChemistrySupramolecular chemistryGeneral ChemistryThermomagnetic convectionKinetic energyCatalysisIonCrystallographychemistry.chemical_compoundSpin crossoverPyridineIsomerization
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Natural Convection Heat Transfer in a Partially- or Completely-Partitioned Vertical Rectangular Enclosure

1991

Laminar FlowNatural ConvectionEnclosureHeat TransferCFDSettore ING-IND/19 - Impianti Nucleari
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Natural Convection in Liquid Metal-Filled Rectangular Enclosures with Volumetric Heating

1998

Low Prandtl number FluidNatural ConvectionRectangular EnclosureCFDLiquid MetalSettore ING-IND/19 - Impianti NucleariInternal Heating
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