Search results for "turbulent"

showing 10 items of 46 documents

Multiphysical Modeling of Transport Phenomena During Laser Welding of Dissimilar Steels

2016

Abstract The success of new high-strength steels allows attaining equivalent performances with lower thicknesses and significant weight reduction. The welding of new couples of steel grades requires development and control of joining processes. Thanks to high precision and good flexibility, laser welding became one of the most used processes for joining of dissimilar welded blanks. The prediction of the local chemical composition in the weld formed between dissimilar steels in function of the welding parameters is essential because the dilution rate and the distribution of alloying elements in the melted zone determines the final tensile strength of the weld. The goal of the present study i…

010302 applied physicsturbulent flowHeat-affected zoneMaterials scienceLaser beam weldingdissimilar materials02 engineering and technologyMechanicsWeldingPhysics and Astronomy(all)021001 nanoscience & nanotechnology01 natural sciencesFick's laws of diffusiontransport of specieslaw.inventionlaminar flowlaw0103 physical sciencesHeat transferWeld poolLaser weldingDiffusion (business)0210 nano-technologyTransport phenomenaPhysics Procedia
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Geographic and temporal variations in turbulent heat loss from lakes : A global analysis across 45 lakes

2018

Heat fluxes at the lake surface play an integral part in determining the energy budget and thermal structure in lakes, including regulating how lakes respond to climate change. We explore patterns in turbulent heat fluxes, which vary across temporal and spatial scales, using in situ high-frequency monitoring data from 45 glob- ally distributed lakes. Our analysis demonstrates that some of the lakes studied follow a marked seasonal cycle in their turbulent surface fluxes and that turbulent heat loss is highest in larger lakes and those situated at low latitude. The Bowen ratio, which is the ratio of mean sensible to mean latent heat fluxes, is smaller at low lati- tudes and, in turn, the rel…

010504 meteorology & atmospheric sciences0208 environmental biotechnologyta1172ta1171Climate change02 engineering and technologyAquatic ScienceOceanographyAtmospheric sciences01 natural sciencesjärvetLatitudeWater balanceheat fluxesLatent heatparasitic diseaseslakesBowen ratioturbulent heat loss0105 earth and related environmental sciencesthermal structurelake surface15. Life on landilmastonmuutoksetEnergy budget020801 environmental engineeringclimate change13. Climate actionHeat transferarticlesEnvironmental scienceSpatial variabilitylämpötilaenergy budgetlämpöhäviöLimnology and Oceanography
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Turbulent jet through porous obstructions under Coriolis effect: an experimental investigation

2021

AbstractThe present study has the main purpose to experimentally investigate a turbulent momentum jet issued in a basin affected by rotation and in presence of porous obstructions. The experiments were carried out at the Coriolis Platform at LEGI Grenoble (FR). A large and unique set of velocity data was obtained by means of a Particle Image Velocimetry measurement technique while varying the rotation rate of the tank and the density of the canopy. The main differences in jet behavior in various flow configurations were assessed in terms of mean flow, turbulent kinetic energy and jet spreading. The jet trajectory was also detected. The results prove that obstructions with increasing density…

010504 meteorology & atmospheric sciencesComputational MechanicsGeneral Physics and AstronomyRotation01 natural sciencesSettore ICAR/01 - Idraulica010305 fluids & plasmasPhysics::Fluid DynamicsMomentumCorioli0103 physical sciencesMean flow0105 earth and related environmental sciencesFluid Flow and Transfer ProcessesPhysicsJet (fluid)[SDE.IE]Environmental Sciences/Environmental EngineeringTurbulence[SPI.FLUID]Engineering Sciences [physics]/Reactive fluid environmentexperimentsMechanicsParticle image velocimetry13. Climate actionMechanics of MaterialsDragturbulent jetTurbulence kinetic energyExperiments in Fluids
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Existence and Singularities for the Prandtl Boundary Layer Equations

2000

Prandtl's boundary layer equations, first formulated in 1904, resolve the differences between the viscous and inviscid description of fluid flows. This paper presents a review of mathematical results, both analytic and computational, on the unsteady boundary layer equations. This includes a review of the derivation and basic properties of the equations, singularity formation, well-posedness results, and infinite Reynolds number limits.

Applied MathematicsMathematical analysisPrandtl numberComputational MechanicsReynolds numberBoundary layer thicknessPhysics::Fluid Dynamicssymbols.namesakeBoundary layerInviscid flowBlasius boundary layersymbolsTurbulent Prandtl numberReynolds-averaged Navier–Stokes equationsMathematicsZAMM
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Observed versus simulated mountain waves over Scandinavia – improvement of vertical winds, energy and momentum fluxes by enhanced model resolut…

2017

Abstract. Two mountain wave events, which occurred over northern Scandinavia in December 2013 are analysed by means of airborne observations and global and mesoscale numerical simulations with horizontal mesh sizes of 16, 7.2, 2.4 and 0.8 km. During both events westerly cross-mountain flow induced upward-propagating mountain waves with different wave characteristics due to differing atmospheric background conditions. While wave breaking occurred at altitudes between 25 and 30 km during the first event due to weak stratospheric winds, waves propagated to altitudes above 30 km and interfacial waves formed in the troposphere at a stratospheric intrusion layer during the second event. Global an…

Atmospheric Science010504 meteorology & atmospheric sciencesairborne observationsFlow (psychology)Mesoscale meteorologygravity waves010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesPhysics::GeophysicsTropospherelcsh:ChemistryGW-LCYCLE IPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesMomentum (technical analysis)Institut für Physik der AtmosphäreLidarTurbulent diffusionVerkehrsmeteorologieBreaking wavelcsh:QC1-999WavelengthAmplitudenumerical modelinglcsh:QD1-999Geologylcsh:PhysicsAtmospheric Chemistry and Physics
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Investigating marine shallow waters dynamics to explore the role of turbidity on ecological responses

2009

The ecological tangible effect of the complex interaction between sediments and water column in shallow waters is represented by turbidity which is a common feature of most aquatic ecosystems: it varies both temporally and spatially; it can cover a huge area and persist for a long period or it can be very localized and temporary. Among many factors able to generate turbidity, wind generated wave action and water mass movements due to tides seem important in causing resuspension of sediments. Although there is much research spent in last decades on this topic and many models to explain the complexity of the wind-water-sediment interaction, some interactive aspects are too site specific and t…

Biological-physical interaction ecological responses hydrodynamics resuspension shallow water turbulent kinetic energy turbidity.
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Nonequilibrium effective temperature of superfluid vortex tangle

2006

An effective nonequilibrium temperature in counterflow superfluid turbulence is proposed, as a parameter characterizing a canonical probability distribution function of vortex orientation, and relating the diffusion coefficient of vortex lines to the vortex friction through an Einstein relation.

Condensed Matter::Quantum GasesPhysicsCondensed matter physicsNonequilibrium temperatureTurbulent superfluidsCondensed Matter::OtherTurbulenceGeneral Physics and AstronomyNon-equilibrium thermodynamicsProbability density functionVortexSuperfluidityDistribution functionCondensed Matter::SuperconductivityEinstein relationDiffusion (business)Settore MAT/07 - Fisica Matematica
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High Reynolds number Navier-Stokes solutions and boundary layer separation induced by a rectilinear vortex

2013

Abstract We compute the solutions of Prandtl’s and Navier–Stokes equations for the two dimensional flow induced by a rectilinear vortex interacting with a boundary in the half plane. For this initial datum Prandtl’s equation develops, in a finite time, a separation singularity. We investigate the different stages of unsteady separation for Navier–Stokes solution at different Reynolds numbers Re = 103–105, and we show the presence of a large-scale interaction between the viscous boundary layer and the inviscid outer flow. We also see a subsequent stage, characterized by the presence of a small-scale interaction, which is visible only for moderate-high Re numbers Re = 104–105. We also investi…

D'Alembert's paradoxGeneral Computer SciencePrandtl numberMathematics::Analysis of PDEsFOS: Physical sciencesPhysics::Fluid Dynamicssymbols.namesakeMathematics - Analysis of PDEsHagen–Poiseuille flow from the Navier–Stokes equationsFOS: MathematicsSettore MAT/07 - Fisica MatematicaMathematical PhysicsMathematicsMathematical analysisGeneral EngineeringFluid Dynamics (physics.flu-dyn)Reynolds numberPhysics - Fluid DynamicsMathematical Physics (math-ph)Non-dimensionalization and scaling of the Navier–Stokes equationsBoundary layersymbolsTurbulent Prandtl numberReynolds-averaged Navier–Stokes equationsBoundary layer Unsteady separation Navier Stokes solutions Prandtl’s equation High Reynolds number flows.Analysis of PDEs (math.AP)
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Reciprocating Flow in a Plane Channel: Comparison of RANS Turbulence Models and Direct Numerical Simulation

2009

Direct Numerical SimulationUnsteady Turbulent FlowRANS Turbulence ModelsCFDHeat TransferSettore ING-IND/19 - Impianti Nucleari
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A study of turbulent heat transfer in curved pipes by numerical simulation

2013

Abstract Turbulent heat transfer in curved pipes was studied by numerical simulation. Two curvatures δ (pipe radius a/curvature radius c) were considered, 0.1 and 0.3; results were also obtained for a straight pipe (δ = 0) for comparison purposes. A tract of pipe 5 diameters in length was chosen as the computational domain and was discretized by finite volume multiblock-structured grids of ∼5.3 × 106 hexahedral cells. Fully developed conditions were assumed; the friction velocity Reynolds number was 500, corresponding to bulk Reynolds numbers between 12 630 and ∼17 350 according to the curvature, while the Prandtl number was 0.86 (representative of saturated liquid water at 58 bar). Simulat…

Fluid Flow and Transfer ProcessesPhysicsTurbulenceMechanical EngineeringPrandtl numberDirect numerical simulationReynolds numberMechanicsHeat transfer coefficientCondensed Matter PhysicsCurvaturePhysics::Fluid Dynamicssymbols.namesakeClassical mechanicsTurbulent heat transfer curved pipe Direct Numerical Simulation Computational Fluid Dynamics Finite Volume MethodHeat transfersymbolsShear velocitySettore ING-IND/19 - Impianti Nucleari
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