Search results for "Channel flow"

showing 10 items of 77 documents

Flow Velocity Measurements in Vegetated Channels

2002

Understanding of the hydraulics of flow over vegetation is very important to support the management of fluvial processes. In this paper the flow over flexible bottom vegetation is experimentally studied. A two-dimensional-acoustic doppler velocimeter is used to measure the local flow velocities for different vegetation concentrations, discharges, and flume slopes. The influence of vegetation concentration and the depth/vegetation height ratio on the measured velocity profiles is analyzed. All measured velocity distributions are S-shaped and exhibit a three-zone profile. The relationship between the velocity distribution and the turbulence intensity distribution is also analyzed. The charact…

HydrologyTurbulenceMechanical EngineeringPrandtl numberGeometryFlow measurementPhysics::GeophysicsOpen-channel flowPhysics::Fluid DynamicsFlumesymbols.namesakeFlow velocityTurbulence kinetic energysymbolsmedicineTURBULENCEmedicine.symptomVegetation (pathology)RESISTANCEGeologyCOEFFICIENTSWater Science and TechnologyCivil and Structural EngineeringJournal of Hydraulic Engineering
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Testing the Outflow Process over a Triangular Labyrinth Weir

2017

In this paper, the dimensionless stage-discharge relation for a sharp-crested triangular labyrinth weir, determined in a previous study, is initially tested by some experimental runs carried out in a laboratory flume. According to this relationship, the flow magnification is affected by the length-magnification ratio and the head to one cycle width ratio. The measurements allowed to test the applicability of this dimensionless relation for different values of both the angle of the sidewall to the main flow direction and the weir height. Finally, the proposed dimensionless equation was also tested by using experimental measurements carried out for broad-crested triangular labyrinth weir.

Hydrologyanimal structures010504 meteorology & atmospheric sciences0208 environmental biotechnologyGeometry02 engineering and technology01 natural sciencesAgricultural and Biological Sciences (miscellaneous)020801 environmental engineeringOpen-channel flowPhysics::Fluid Dynamicsembryonic structuresWeirOpen-channel flowSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDischargeOutflowWeirHeadNonlinear Sciences::Pattern Formation and SolitonsGeology0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Flow resistance ofPosidonia oceanicain shallow water

2006

Management of coastal waters and lagoons by mathematical circulation models requires determination of the hydraulic resistance of submerged vegetation. A plant typical of sandy coastal bottoms in the Mediterranean Sea is Posidonia oceanica, which is constituted by very thin and flexible ribbon-like leaves, about 1 cm wide and up to 1.5 m long, and usually covers the bottom with a density of 500-1000 plants/ m2. From the hydraulic viewpoint, P. oceanica constitutes a particular roughness, because, as the velocity increases, the leaves bend more and more until they lie down on the bottom. Although P. oceanica is widespread, in the technical literature it is difficult to find indications about…

HydrologybiologyHydraulicsVegetationSMOOTHbiology.organism_classificationVELOCITY DISTRIBUTIONlaw.inventionOpen-channel flowFlumeWaves and shallow waterMediterranean seaLAYERlawAquatic plantPosidonia oceanicaOPEN-CHANNEL FLOWTURBULENCEEnvironmental scienceVEGETATIONHYDRAULIC RESISTANCEWater Science and TechnologyCivil and Structural EngineeringJournal of Hydraulic Research
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Diffusive Modeling of Aggradation and Degradation in Artificial Channels

2008

The unsteady flow and solid transport simulation problem in artificial channels is solved using a three-equation model, coupled with a local erosion law. The three equations are the water mass and momentum balance equations, as well as the total solid load balance equation. It is shown that even during severe hydrological events inertial terms can be neglected in the momentum equation without any substantial change in the solution sought. Empirical equilibrium formulas were used to estimate the solid load as a function of the flow variables. Local erosion, due to the scour generated at the jump between two channels connected at different bottom elevations, was estimated adapting a literatur…

Inertial frame of referenceSpacetimeMechanical EngineeringFunction (mathematics)MechanicsSettore ICAR/01 - IdraulicaOpen-channel flowFlow (mathematics)JumpGeotechnical engineeringDiffusion (business)sediment transport shallow waters solid load unsteady flow numerical models local scourSediment transportWater Science and TechnologyCivil and Structural EngineeringMathematicsJournal of Hydraulic Engineering
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Large eddy simulation of inertial particles dispersion in a turbulent gas-particle channel flow bounded by rough walls

2020

The purpose of this paper is to understand the capability and consistency of large eddy simulation (LES) in Eulerian–Lagrangian studies aimed at predicting inertial particle dispersion in turbulent wall-bounded flows, in the absence of ad hoc closure models in the Lagrangian equations of particle motion. The degree of improvement granted by LES models is object of debate, in terms of both accurate prediction of particle accumulation and local particle segregation; therefore, we assessed the accuracy in the prediction of the particle velocity statistics by comparison against direct numerical simulation (DNS) of a finer computational mesh, under both one-way and two-way coupling regimes. We p…

Lagrange multipliersLagrangian equationsParticle statisticsParticle statisticsVelocity controlComputational MechanicsDirect numerical simulationWall flow Accurate prediction02 engineering and technology01 natural sciencesReynolds numberSettore ICAR/01 - Idraulica010305 fluids & plasmasPhysics::Fluid Dynamicssymbols.namesake0203 mechanical engineeringEquations of motion0103 physical sciencesParticle velocityDispersionsPhysicsTurbulence modificationTurbulenceMechanical EngineeringLarge eddy simulationTwo phase flowReynolds numberMechanicsTurbulent wall-bounded flows Segregation (metallography)Open-channel flow020303 mechanical engineering & transportsParticle accumulationQuay wallssymbolsParticle segregationParticleForecastingParticle velocitiesLarge eddy simulationActa Mechanica
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Flow resistance law under suspended sediment laden conditions

2020

Abstract The uniform flow resistance equation, in the form due to Manning or Darcy-Weisbach, is widely applied to establish the stage-discharge relationship of a river cross-section. The application of this equation, namely the slope-area method, allows to indirectly measure the corresponding river discharge by measurements of bed slope, water level, cross-section area, wetted perimeter and an estimate of channel roughness. In this paper, a recently deduced flow resistance equation for open channel flow was tested during conditions of suspended sediment-laden flow. First, the flow resistance equation was determined by dimensional analysis and by applying the condition of incomplete self-sim…

Materials science0207 environmental engineeringSediment02 engineering and technologyMechanicsDimensional analysis Flow resistance Flow velocity profile Self-similarity Suspended-load01 natural sciencesComputer Science ApplicationsOpen-channel flow010309 opticssymbols.namesakeWetted perimeterFlow conditionsFlow velocityFlow (mathematics)Modeling and Simulation0103 physical sciencesFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliPotential flowElectrical and Electronic Engineering020701 environmental engineeringInstrumentationFlow Measurement and Instrumentation
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Turbulence structures over irregular rough surfaces

2010

Turbulent flow in a channel with irregular two-dimensional rough surfaces is analysed through wall-resolving large eddy simulation (LES). Both walls of the channel are roughened through the superimposition of sinusoidal functions having random amplitude and four different wavelengths. The downward shift of the velocity profile in the log region due to the roughness, known as roughness function, is well captured in the simulations. The spanwise and wall-normal turbulence intensities are found to increase with the roughness height, while the streamwise component decreases. The analysis of the Reynolds stress anisotropy tensor highlights a tendency towards isotropisation, confirmed by the vort…

Materials scienceComputational MechanicsGeneral Physics and Astronomyturbulence; irregular rough wall; LESSurface finishReynolds stresschannel flowSettore ICAR/01 - IdraulicaPhysics::Fluid Dynamicsirregular rough wallOpticsirregular roughneAnisotropyturbulence structureTurbulencebusiness.industryturbulenceMechanicsVorticityCondensed Matter PhysicsOpen-channel flowRoughness lengthMechanics of MaterialsLESbusinessLarge eddy simulation
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Anisotropic flow in striped superhydrophobic channels

2012

We report results of dissipative particle dynamics simulations and develop a semi-analytical theory of an anisotropic flow in a parallel-plate channel with two superhydrophobic striped walls. Our approach is valid for any local slip at the gas sectors and an arbitrary distance between the plates, ranging from a thick to a thin channel. It allows us to optimize area fractions, slip lengths, channel thickness and texture orientation to maximize a transverse flow. Our results may be useful for extracting effective slip tensors from global measurements, such as the permeability of a channel, in experiments or simulations, and may also find applications in passive microfluidic mixing.

Materials scienceMicrofluidicsDissipative particle dynamicsFluid Dynamics (physics.flu-dyn)General Physics and AstronomyFOS: Physical sciencesRangingMechanicsSlip (materials science)Physics - Fluid DynamicsCondensed Matter - Soft Condensed MatterOpen-channel flowPhysics::Fluid DynamicsTransverse planeSoft Condensed Matter (cond-mat.soft)WettingPhysical and Theoretical ChemistryCommunication channel
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Explicit equations for uniform flow depth

2017

Conventional approach in uniform open channel flow is to express the resistance coefficient in the Manning, Darcy-Weisbach or Chezy form. However, for practical cross-sections, including rectangular and trapezoidal ones, the governing equation is implicit in the uniform water depth. For these sections the water depth, corresponding to known values of the flow discharge, slope channel and resistance coefficient, is presently obtained by trial and error procedure. In this paper exact analytical solutions of uniform flow depth for rectangular and trapezoidal section have been obtained in the form of fast converging power series.

Mathematical optimization010504 meteorology & atmospheric sciences0208 environmental biotechnologyOpen channel flow unifrom flow water depth discharge02 engineering and technologyMechanics01 natural sciencesAgricultural and Biological Sciences (miscellaneous)Energy–depth relationship in a rectangular channel020801 environmental engineeringOpen-channel flowWater depthSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliResistance coefficientPotential flow0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringMathematics
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Experimental Analysis of Horizontal Turbulence of Flow over Flat and Deformed Beds

2015

Abstract Laboratory experiments in a straight flume were carried out to examine the evolution of large-scale horizontal turbulent structures under flat-bed and deformed-bed conditions. In this paper, the horizontal turbulence of flow under these conditions is analyzed and compared. The conditioned quadrant method is applied to verify the occurrence of turbulent events. The distributions of horizontal Reynolds shear stress and turbulent kinetic energy are also presented and discussed. Results show the occurrence of an “initial” sequence of horizontal vortices whose average spatial length scales with the channel width. Under deformed-bed conditions, this spatial length does not change.

MeteorologyTurbulenceK-epsilon turbulence modelFlow (psychology)Bed formBurst cycleMechanicsLaboratory experimentVortexOpen-channel flowQuadrant (plane geometry)Physics::Fluid DynamicsFlumeFlow turbulence structureTurbulence kinetic energyOpen-channel flowGeologyWater Science and TechnologyCivil and Structural EngineeringArchives of Hydro-Engineering and Environmental Mechanics
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