Search results for "Fluid dynamics"

showing 10 items of 1005 documents

Onset of Convection in an Inclined Anisotropic Porous Layer with Internal Heat Generation

2019

The onset of convection in an inclined porous layer which is heated internally by a uniform distribution of heat sources is considered. We investigate the combined effects of inclination, anisotropy and internal heat generation on the linear instability of the basic parallel flow. When the Rayleigh number is sufficiently large, instability occurs and a convective motion is set up. It turns out that the preferred motion at convection onset depends quite strongly on the anisotropy ratio, &xi

ConvectioninclinationMaterials scienceonsetComputingMethodologies_IMAGEPROCESSINGANDCOMPUTERVISION02 engineering and technologyanisotropylcsh:Thermodynamics01 natural sciencesInstability010305 fluids & plasmasPhysics::Fluid Dynamicsporous media0203 mechanical engineeringlcsh:QC310.15-3190103 physical sciencesAstrophysics::Solar and Stellar Astrophysicsheat generationAnisotropyconvectionlcsh:QC120-168.85Fluid Flow and Transfer ProcessesMechanical EngineeringMechanicsRayleigh numberCondensed Matter PhysicsVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410Transverse plane020303 mechanical engineering & transportsTheoryofComputation_MATHEMATICALLOGICANDFORMALLANGUAGESHeat generationComputer Science::Programming Languageslcsh:Descriptive and experimental mechanicsAstrophysics::Earth and Planetary AstrophysicsInternal heatingPorous mediumFluids
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Dye-tracer technique for rill flows by velocity profile measurements

2020

Abstract Water flow on hillslope soil surface supplies energy which is required to detach soil particles, to transport and deposit sediments, therefore flow velocity is a key variable related to hillslope hydrodinamics of soil erosion processes. Among the different methods available for measuring velocity of shallow interrill and rill flow, the trace technique is widely used. Trace technique is applied by adding a material (salt, magnetic material, water isotope, floating object) and then measuring the speed of the material to travel a known distance from the injection point. When flow velocity is measured using a dye-tracing method, the mean velocity is calculated by multiplying the measur…

Correction factorDye method010504 meteorology & atmospheric sciencesWater flowFlow (psychology)Surface finish01 natural sciencesPhysics::GeophysicsPhysics::Fluid DynamicsFlow velocitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorySediment04 agricultural and veterinary sciencesMechanicsPlumeRillFlumeFlow velocityRill flowSoil erosion040103 agronomy & agriculture0401 agriculture forestry and fisheriesInterrill flowGeologyCATENA
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2017

We propose a mesh-free and discrete (particle-based) multi-physics approach for modelling the hydrodynamics in flexible biological valves. In the first part of this study, the method is successfully validated against both traditional modelling techniques and experimental data. In the second part, it is further developed to account for the formation of solid aggregates in the flow and at the membrane surface. Simulations of various types of aggregates highlight the main benefits of discrete multi-physics and indicate the potential of this approach for coupling the hydrodynamics with phenomena such as clotting and calcification in biological valves.

CouplingMultidisciplinaryAggregate (data warehouse)Blood flow01 natural sciencesMesh free010305 fluids & plasmas010101 applied mathematicsFlow (mathematics)Blood vessel prosthesis0103 physical sciencesFluid dynamics0101 mathematicsMembrane surfaceBiological systemPLOS ONE
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Coupling of lattice-Boltzmann solvers with suspended particles using the MPI intercommunication framework

2017

Abstract The MPI intercommunication framework was used for coupling of two lattice-Boltzmann solvers with suspended particles, which model advection and diffusion respectively of these particles in a carrier fluid. Simulation domain was divided into two parts, one with advection and diffusion, and the other with diffusion only (no macroscopic flow). Particles were exchanged between these domains at their common boundary by a direct process to process communication. By analysing weak and strong scaling, it was shown that the linear scaling characteristics of the lattice-Boltzmann solvers were not compromised by their coupling.

CouplingPhysicsadvection-diffusionta114AdvectionGeneral EngineeringLattice Boltzmann methods01 natural sciences010305 fluids & plasmasPhysics::Fluid DynamicsFlow (mathematics)0103 physical sciencesFluid dynamicsLinear scaleMPIStatistical physicsDiffusion (business)coupling010306 general physicsScalingSoftwareLattice-BoltzmannAdvances in Engineering Software
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Experimental and Numerical Validation of a Wind Gust Facility

2013

The study of a vehicle moving through a lateral wind gust has always been a difficult task due to the difficulties in granting the right similitude. The facility proposed by Ryan and Dominy has been one of the best options to carry it out. In this approach, a double wind tunnel is used to send a lateral moving gust on a stationary model. Using this idea as a starting point, the ISAE has built a dedicated test bench for lateral wind studies on transient conditions. Experimental work has been carried out by means of time-resolved PIV, aiming at studying the unsteady interpenetration of the two flows coming from each wind tunnel. Meanwhile, a 3D CFD model based on URANS was set up, faithfully …

CrosswindTest benchMeteorologybusiness.industryComputer scienceTurbulenceMécanique des fluidesMechanical EngineeringComputational fluid dynamicsGustSimilitudeExperimentalPoint (geometry)Transient (oscillation)businessWind tunnelMarine engineeringWind tunnelCrosswindJournal of Fluids Engineering
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An improved immersed boundary method for curvilinear grids

2009

Abstract In the present paper we propose an extension of the direct-forcing immersed boundary technique, recently developed and employed by Verzicco and co-authors [Fadlun EA, Verzicco R, Orlandi P, Mohd-Yusof J. Combined immersed-boundary finite-difference methods for three-dimensional complex flow simulations. J Comput Phys 2000;161:35–60; Verzicco R, Fatica M, Iaccarino G, Moin P, Khalighi B. Large eddy simulation of a road vehicle with drag-reduction devices. AIAA J 2002;40(12):2447–55; Cristallo A, Verzicco R. Combined immersed boundary/large-eddy-simulations of incompressible three-dimensional complex flows. Flow Turbul Combust 2006;77(1–4):3–26.] and successively improved by Balaras …

Curvilinear coordinatesGeneral Computer Sciencebusiness.industryNumerical analysisGeneral EngineeringGeometryStokes flowComputational fluid dynamicsImmersed boundary methodGridlaw.inventionImmersed boundary Curvilinear grid Numerical methodsPhysics::Fluid DynamicslawApplied mathematicsPolygon meshCartesian coordinate systembusinessMathematics
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Three-dimensional numerical simulations on wind- and tide-induced currents: The case of Augusta Harbour (Italy)

2014

The hydrodynamic circulation in the coastal area of the Augusta Bay (Italy), located in the eastern part of Sicily, is analysed. Due to the heavy contamination generated by the several chemical and petrochemical industries active in the zone, the harbour was declared a Contaminated Site of National Interest. To mitigate the risks connected with the industrial activities located near the harbour, it is important to analyse the hydrodynamic circulation in the coastal area. To perform such analysis, a parallel 3D numerical model is used to solve the Reynolds-averaged momentum and mass balance, employing the k-e turbulence model for the Reynolds stresses. The numerical model is parallelized usi…

Curvilinear coordinatesMeteorologyTurbulenceDomain decomposition methodsReynolds stressMomentumCurrent (stream)Circulation (fluid dynamics)Free surfaceWind-driven flow MPI 3D hydrodynamicmodel Finite volumemodel ParallelcomputingComputers in Earth SciencesPhysics::Atmospheric and Oceanic PhysicsGeologyInformation SystemsMarine engineering
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Adaptive control of a seven mode truncation of the Kolmogorov flow with drag

2009

Abstract We study a seven dimensional nonlinear dynamical system obtained by a truncation of the Navier–Stokes equations for a two dimensional incompressible fluid with the addition of a linear term modelling the drag friction. We show the bifurcation sequence leading from laminar steady states to chaotic solutions with increasing Reynolds number. Finally, we design an adaptive control which drives the state of the system to the equilibrium point representing the stationary solution.

D'Alembert's paradoxEquilibrium pointTruncationGeneral MathematicsApplied MathematicsMathematical analysisGeneral Physics and AstronomyReynolds numberAdaptive controlStatistical and Nonlinear PhysicsLaminar flowDrag equationFinite dimensional approximationPhysics::Fluid Dynamicssymbols.namesakeClassical mechanicsDragsymbolsBifurcationReynolds-averaged Navier–Stokes equationsMathematics
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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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Interaction between turbulent structures and particles in roughened channel

2016

Abstract The distribution of inertial particles in turbulent flows is highly non-uniform and is driven by the local dynamics of the turbulent structures of the underlying carrier flow field. In the specific context of dilute particle-laden wall-bounded flows, deposition and resuspension mechanisms are dominated by the interaction between inertial particles and coherent turbulent structures characteristic of the wall region. The macroscopic behavior of these two-phase systems is influenced by particle inertia, which plays a role at the microscale of a single dispersed element. These turbulent structures, which control the turbulent regeneration cycles, are strongly affected by the wall rough…

DNSmedia_common.quotation_subjectDirect numerical simulationGeneral Physics and AstronomyContext (language use)Lagrangian particle trackingInertia01 natural sciencesSettore ICAR/01 - Idraulica010305 fluids & plasmasPhysics::Fluid DynamicsPhysics and Astronomy (all)symbols.namesake0103 physical sciences010306 general physicsDispersion (water waves)media_commonFluid Flow and Transfer ProcessesPhysicsTurbulenceMechanical EngineeringParticle-laden flowReynolds numberMechanicsTurbulenceClassical mechanicssymbolsParticleLagrangian trackingParticle mass fluxRoughneInternational Journal of Multiphase Flow
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