Search results for "Laminar Flow"

showing 10 items of 78 documents

Numerical simulation of reciprocating turbulent flow in a plane channel

2009

Direct numerical simulation results were obtained for oscillatory flow with zero time mean (reciprocating flow) in a plane channel using a finite volume method, Crank-Nicolson time stepping and central approximation of the advection terms. A pressure gradient varying co-sinusoidally in time was imposed as the forcing term, and its frequency and amplitude were made to vary so as to span a range of regimes from purely laminar to fully turbulent. For the limiting cases of reciprocating laminar flow and steady-state turbulent flow, numerical results were validated against analytical solutions and classic experimental literature data, respectively. For general reciprocating flows, predictions we…

Fluid Flow and Transfer ProcessesPhysicsChézy formulaTurbulenceMechanical EngineeringComputational MechanicsDirect numerical simulationThermodynamicsLaminar sublayerLaminar flowMechanicsReciprocating Flow Channel flow transition to turbulence Direct Numerical SimulationCondensed Matter PhysicsPipe flowOpen-channel flowPhysics::Fluid DynamicsFlow separationMechanics of MaterialsSettore ING-IND/19 - Impianti NucleariPhysics of Fluids
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On the influence of gravitational and centrifugal buoyancy on laminar flow and heat transfer in curved pipes and coils

2015

Abstract The effects of gravitational and centrifugal buoyancy on laminar flow and heat transfer in curved and helical pipes were investigated by numerical simulation. Six dimensionless numbers characterizing the problem were identified, and an analysis was conducted on the possible combinations of signs of the gravitational and centrifugal buoyancy effects. Two distinct Richardson numbers were introduced in order to quantify the importance of the two types of buoyancy, and it was shown that, in the case of heating from the wall, a maximum realizable value of the centrifugal Richardson number exists which is a linear function of the curvature δ (ratio of pipe radius a to curvature radius c)…

Fluid Flow and Transfer ProcessesPhysicsRichardson numberBuoyancyMechanical EngineeringCentrifugal buoyancyCurved pipeTorsion (mechanics)ThermodynamicsLaminar flowMechanicsengineering.materialGravitational buoyancyCondensed Matter PhysicsCurvatureNusselt numberPhysics::Fluid DynamicsComputational fluid dynamics Laminar flowHeat transferHeat transferengineeringHelical coilSettore ING-IND/19 - Impianti NucleariDimensionless quantity
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Route to chaos in the weakly stratified Kolmogorov flow

2019

We consider a two-dimensional fluid exposed to Kolmogorov’s forcing cos(ny) and heated from above. The stabilizing effects of temperature are taken into account using the Boussinesq approximation. The fluid with no temperature stratification has been widely studied and, although relying on strong simplifications, it is considered an important tool for the theoretical and experimental study of transition to turbulence. In this paper, we are interested in the set of transitions leading the temperature stratified fluid from the laminar solution [U∝cos(ny),0, T ∝ y] to more complex states until the onset of chaotic states. We will consider Reynolds numbers 0 < Re ≤ 30, while the Richardson numb…

Fluid Flow and Transfer ProcessesPhysicsRichardson numberTurbulenceMechanical EngineeringMathematical analysisComputational MechanicsReynolds numberLaminar flowCondensed Matter Physics01 natural sciences010305 fluids & plasmasPhysics::Fluid Dynamicssymbols.namesakeTemperature gradientMechanics of Materials0103 physical sciencessymbolsBifurcation Computational complexity Reynolds number Boussinesq approximations Chaotic solutions Richardson number Stabilizing effects Stratified fluid Temperature stratification Transition to turbulence Weak stratificationStratified flowBoussinesq approximation (water waves)010306 general physicsSettore MAT/07 - Fisica MatematicaBifurcation
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Inflow/outflow pressure boundary conditions for smoothed particle hydrodynamics simulations of incompressible flows

2017

Abstract Open Boundary treatment is a well-known issue in the Smoothed Particle Hydrodynamics (SPH) method, mainly when the truly Incompressible (ISPH) approach is employed. In the paper a novel method is proposed to set pressure boundary conditions in the computational domain inlets and outlets, without requiring the velocity profile assignment. The new technique allows to treat in the same way inflow and outflow sections, effectively dealing with the release of new particles at inlets and the deactivation of the ones leaving the domain through the outlets. Several 3D numerical tests, both in the laminar and turbulent regimes, are carried out to validate the proposed numerical scheme consi…

General Computer ScienceSPHInflow01 natural sciencesDomain (mathematical analysis)Settore ICAR/01 - Idraulica010305 fluids & plasmasPhysics::Fluid DynamicsSmoothed-particle hydrodynamicsEngineering (all)0103 physical sciencesBoundary value problem0101 mathematicsPressure Poisson EquationPhysicsTurbulenceOpen-boundaryComputer Science (all)General EngineeringLaminar flowMechanicsComputational physics010101 applied mathematicsIncompressible SPHCompressibilityOutflowPressure boundary conditionComputers &amp; Fluids
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Group analysis and similarity solutions of the compressible boundary layer equations

1989

In this paper the application of Lie's methods to the equations of the laminar boundary layer is discussed. The momentum and energy equations in Prandtl's form are considered for a steady, viscous, compressible laminar flow with non zero pressure gradient, variable viscosity and thermal conductivity. Group analysis yields similarity solutions for given pressure distributions and particular values of the invariance group parameters (group classification). Crocco's transformation is obtained for the infinite-dimensional group of the Lie's algebra admitted by the equations.

Group (mathematics)Mechanical EngineeringMathematical analysisPrandtl numberLie groupLaminar flowCondensed Matter PhysicsBoundary layer thicknessSimilarity solutionPhysics::Fluid Dynamicssymbols.namesakeBoundary layerMechanics of MaterialsBlasius boundary layersymbolsMathematicsMeccanica
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PGC1α Regulates the Endothelial Response to Fluid Shear Stress via Telomerase Reverse Transcriptase Control of Heme Oxygenase-1

2021

AbstractFluid shear stress (FSS) is known to mediate multiple phenotypic changes in the endothelium. Laminar FSS (undisturbed flow) is known to promote endothelial alignment to flow that is key to stabilizing the endothelium and rendering it resistant to atherosclerosis and thrombosis. The molecular pathways responsible for endothelial responses to FSS are only partially understood. Here we have identified peroxisome proliferator gamma coactivator-1α (PGC-1α) as a flow-responsive gene required for endothelial flow alignment in vitro and in vivo. Compared to oscillatory FSS (disturbed flow) or static conditions, laminar FSS (undisturbed flow) increased PGC-1α expression and its transcription…

Heme oxygenasechemistry.chemical_compoundmedicine.anatomical_structureHMOX1EndotheliumKLF4In vivoChemistrymedicineLaminar flowTelomerase reverse transcriptaseHemeCell biology
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A laboratory and theoretical study on the uptake of sulfur dioxide gas by small water drops containing hydrogen peroxide under laminar and turbulent …

2000

Abstract Laboratory experiments are described where the uptake of SO2 gas by water drops containing H2O2 is investigated where the taken up S(IV) is quickly converted to S(VI). During the gas uptake the drops were freely suspended at their terminal velocity by means of the Mainz vertical wind tunnel. Two series of experiments were carried out, one with a laminar air flow in the wind tunnel, one with a turbulent air flow in the wind tunnel. Afterwards, the experimental results were compared against model computations using the so-called fully mixed convective diffusion model. The experimental results for laminar flow conditions showed that the fully mixed convective diffusion model for the u…

HydrologyAtmospheric ScienceTerminal velocityTurbulenceChemistryAirflowSulfuric acidLaminar flowMechanicsPhysics::Fluid Dynamicschemistry.chemical_compoundAtmospheric chemistryPhysics::Atmospheric and Oceanic PhysicsSulfur dioxideGeneral Environmental ScienceWind tunnelAtmospheric Environment
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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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Theoretical prediction of rainfall intensity for a small rainfall simulator

2022

In this contribution, a theoretical approach was developed for predicting rainfall intensity for a small rainfall simulator. The developed equation was tested for two different devices and different pressure head and water temperature values. The proposed relationship was found to have a good predictive ability of rainfall intensity. The proposed theoretical approach could be usable with other devices that operate on the same principles of the simulator considered in this investigation.

Laminar flow regimeKamphorst simulatorRainfall simulationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliRainfall intensity2022 IEEE Workshop on Metrology for Agriculture and Forestry (MetroAgriFor)
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Morphometry of microstromatolites in calcrete laminar crusts and a fractal model of their growth

1996

The laminar crust, constituting the upper part of calcretes (terrestrial CaCO3 accumulations inside surficial sediments), is a succession of thin layers of various colors and shapes resembling micro-stromatolites. The crust structure and its diagenetic evolution are similar to stromatolites. A quantitative study of its structure was made using image analysis. Euclidian parameters were calculated to describe lamina shape. Eight hundred and eighty-six laminae were divided into six classes from the flatest forms to columnar shapes. The geometrical relationships between the shapes are interpreted as steps in the growth process of the microstromatolite. A fractal model of laminar crust growth wa…

Lamination (geology)Mathematics (miscellaneous)FractalThin sectionDiffusion-limited aggregationEarth and Planetary Sciences (miscellaneous)Dilation (morphology)MineralogyCrustLaminar flowGeologyDiagenesisMathematical Geology
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