Search results for "Physics::Fluid Dynamics"

showing 10 items of 662 documents

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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History and results of the Riga dynamo experiments

2008

On 11 November 1999, a self-exciting magnetic eigenfield was detected for the first time in the Riga liquid sodium dynamo experiment. We report on the long history leading to this event, and on the subsequent experimental campaigns which provided a wealth of data on the kinematic and the saturated regime of this dynamo. The present state of the theoretical understanding of both regimes is delineated, and some comparisons with other laboratory dynamo experiments are made.

Astrophysics (astro-ph)Fluid Dynamics (physics.flu-dyn)General EngineeringFOS: Physical sciencesEnergy Engineering and Power TechnologyChamp magnetiqueGeophysicsPhysics - Fluid DynamicsAstrophysicsPhysics::GeophysicsPhysics::Fluid DynamicsNuclear magnetic resonanceDynamo theoryMagnetohydrodynamicsGeologyDynamo
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ASYMPTOTIC ANALYSIS OF THE LINEARIZED NAVIER–STOKES EQUATION ON AN EXTERIOR CIRCULAR DOMAIN: EXPLICIT SOLUTION AND THE ZERO VISCOSITY LIMIT

2001

In this paper we study and derive explicit formulas for the linearized Navier-Stokes equations on an exterior circular domain in space dimension two. Through an explicit construction, the solution is decomposed into an inviscid solution, a boundary layer solution and a corrector. Bounds on these solutions are given, in the appropriate Sobolev spaces, in terms of the norms of the initial and boundary data. The correction term is shown to be of the same order of magnitude as the square root of the viscosity. Copyright © 2001 by Marcel Dekker, Inc.

Asymptotic analysisApplied MathematicsMathematical analysisAsymptotic analysis; Boundary layer; Explicit solutions; Navier-Stokes equations; Stokes equations; Zero viscosity; Mathematics (all); Analysis; Applied MathematicsMathematics::Analysis of PDEsAnalysiStokes equationDomain (mathematical analysis)Navier-Stokes equationPhysics::Fluid DynamicsSobolev spaceAsymptotic analysiBoundary layersymbols.namesakeBoundary layerSquare rootExplicit solutionInviscid flowStokes' lawsymbolsMathematics (all)Zero viscosityNavier–Stokes equationsAnalysisMathematicsCommunications in Partial Differential Equations
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The Role of Wind Speed and Wind Shear for Banner Cloud Formation

2019

Abstract Banner clouds are clouds that appear to be attached to the leeward face of a steep mountain. This paper investigates the role of wind speed and wind shear for the formation of banner clouds. Large-eddy simulations are performed to simulate the flow of dry air past an idealized pyramid-shaped mountain. The potential for cloud formation is diagnosed through the Lagrangian vertical parcel displacement, which in the case of a banner cloud shows a plume of large values in the lee of the mountain. In addition, vortical structures are visualized through streamlines and their curvature. A series of sensitivity experiments indicates that both the flow and the banner cloud occurrence are lar…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologybusiness.industryCloud computing010501 environmental sciences01 natural sciencesVertical motionWind speedPhysics::Fluid DynamicsAtmosphereBoundary layerWind shearBannerbusinessPhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesJournal of the Atmospheric Sciences
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The Effect of Turbulence on the Accretional Growth of Graupel

2019

Abstract Wind tunnel experiments were carried out to investigate the influence of turbulence on the collection kernel of graupel. The collection kernel defines the growth rate of a graupel accreting supercooled droplets as it falls through a cloud. The ambient conditions were similar to those occurring typically in the mixed-phase zone of convective clouds, that is, at temperatures between −7° and −16°C and with liquid water contents from 0.5 to 1.3 g m−3. Tethered spherical collectors with radii between 220 and 340 μm were exposed in a flow carrying supercooled droplets with a mean volume radius of 10 μm. The vertical root-mean-square fluctuation velocity, the dissipation rate, and the Tay…

Atmospheric Science010504 meteorology & atmospheric sciencesTurbulence01 natural sciences010305 fluids & plasmasPhysics::Fluid DynamicsKernel (statistics)0103 physical sciencesGrowth ratePrecipitationStatistical physicsGraupel0105 earth and related environmental sciencesMathematicsJournal of the Atmospheric Sciences
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Experimental modeling of viscous inclusions in a circular high-strain shear rig: Implications for the interpretation of shape fabrics and deformed en…

2002

[1] Deformation experiments with initially spherical and prolate viscous inclusions suspended in a viscous Newtonian matrix in a circular high strain annular shear rig provide insights on the shape development of inclusions in high strain shear zones during progressive deformation. Inclusions with a specific viscosity ratio with respect to the matrix material show distinct types of three-dimensional shape development. For instance, at a high viscosity ratio between matrix and inclusion a pulsating ellipsoid develops, which both continuously rotates and changes its shape from a sphere to an ellipsoid and back to a sphere. The experiments show that the shape of an inclusion that has a viscosi…

Atmospheric ScienceEcologyPaleontologySoil ScienceMineralogyForestryMechanicsAquatic ScienceOceanographyEllipsoidPower lawPhysics::Fluid DynamicsViscosityGeophysicsShear (geology)RheologySpace and Planetary ScienceGeochemistry and PetrologyFinite strain theoryEarth and Planetary Sciences (miscellaneous)Newtonian fluidShear zoneGeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Solid Earth
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Experimental Observations of Flow and Bed Processes in Large-Amplitude Meandering Flume

2009

Meanders of large amplitude often exhibit asymmetric planform shape or subsidiary bends. The present work is aimed at improving on understanding of the morphodynamic phenomena affecting the bed evolution of large amplitude meandering channels. Attention is focused on the development of the steady point bar-pool configuration and of the superimposed large-scale migrating bed forms; of particular interest is the role of the changing channel curvature and bed topography variation on flow pattern. A series of experiments was carried out in a sine-generated large-amplitude meandering flume, for two values of width-to-depth ratio. Maps documenting the bed topography and the flow pattern along the…

BedformMechanical EngineeringFlow (psychology)MechanicsCurvatureFlow measurementOpen-channel flowPhysics::Fluid DynamicsFlumeAmplitudeMeanderGeotechnical engineeringGeologyWater Science and TechnologyCivil and Structural EngineeringJournal of Hydraulic Engineering
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A Derivation of the Vlasov-Stokes System for Aerosol Flows from the Kinetic Theory of Binary Gas Mixtures

2016

In this short paper, we formally derive the thin spray equation for a steady Stokes gas, i.e. the equation consists in a coupling between a kinetic (Vlasov type) equation for the dispersed phase and a (steady) Stokes equation for the gas. Our starting point is a system of Boltzmann equations for a binary gas mixture. The derivation follows the procedure already outlined in [Bernard-Desvillettes-Golse-Ricci, arXiv:1608.00422 [math.AP]] where the evolution of the gas is governed by the Navier-Stokes equation.

Binary numberKinetic energy01 natural sciencesBoltzmann equationPhysics::Fluid Dynamics35Q20 35B25 82C40 76T15 76D07symbols.namesakeMathematics - Analysis of PDEshydrodynamic limitPhase (matter)FOS: Mathematics[MATH.MATH-AP]Mathematics [math]/Analysis of PDEs [math.AP][PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph]sprays0101 mathematicsSettore MAT/07 - Fisica MatematicaVlasov-Stokes systemPhysicsNumerical Analysisgas mixture.010102 general mathematicsMSC Primary: 35Q20 35B25; Secondary: 82C40 76T15 76D07.Stokes flowBoltzmann equationAerosol010101 applied mathematicsClassical mechanicsModeling and SimulationBoltzmann constantKinetic theory of gasessymbolsVlasov-Stokes system Boltzmann equation Hydrodynamic limit Aerosols Sprays Gas mixtureaerosolsAnalysis of PDEs (math.AP)
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Liquid-vapour phase behaviour of a symmetrical binary fluid mixture

1998

Using Monte-Carlo simulation and mean field calculations, we study the liquid-vapour phase diagram of a square well binary fluid mixture as a function of a parameter $\delta$ measuring the relative strength of interactions between particles of dissimilar and similar species. The results reveal a rich variety of liquid-vapour coexistence behaviour as $\delta$ is tuned. Specifically, we uncover critical end point behaviour, a triple point involving a vapour and two liquids of different density, and tricritical behaviour. For a certain range of $\delta$, the mean field calculations also predict a `hidden' (metastable) liquid-vapour binodal.

BinodalPhysicsStatistical Mechanics (cond-mat.stat-mech)Triple pointMonte Carlo methodThermodynamicsFOS: Physical sciencesFunction (mathematics)Condensed Matter::Soft Condensed MatterPhysics::Fluid DynamicsTricritical pointMetastabilityPhase (matter)Condensed Matter - Statistical MechanicsPhase diagram
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The droplet evaporation/condensation transition in a finite volume

2003

A fluid in the NVT ensemble at T less than the critical temperature T_c and rho = N/V somewhat in excess of rho_coex (density of the saturated gas in the gas-liquid transition) is considered. For V->infinity, a macroscopic liquid droplet coexists with surrounding saturated gas according to the lever rule. For finite V, droplets can only exist if they exceed a minimum size. A (rounded) first order transition of the system occurs when the droplet evaporates into the supersaturated gas.Simulation evidence for this transition is given for a Lennard-Jones model and interpreted by a phenomenological theory. At the transition, the chemical potential difference mu_t-mu_coex scales like L^(-d/(d+…

BinodalPhysicsSupersaturationFinite volume methodStatistical Mechanics (cond-mat.stat-mech)CondensationThermodynamicsFOS: Physical sciencesStatistical mechanicsCondensed Matter - Soft Condensed MatterPhysics::Fluid DynamicsVolume (thermodynamics)Vapor–liquid equilibriumSoft Condensed Matter (cond-mat.soft)Lever ruleCondensed Matter - Statistical Mechanics
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