Search results for " Velocity profile"

showing 10 items of 16 documents

Flow resistance law under equilibrium bed-load transport conditions

2018

Abstract The uniform flow resistance equation, in the form due to Manning or Darcy-Weisbach, is often applied to determine the stage-discharge relationship of a river cross-section. The application of this equation, namely the slope-area method, allows to indirectly measure by water level readings the corresponding river discharge. In this paper, a recently deduced flow resistance equation for open channel flow was tested during conditions of equilibrium bed-load transport. First the flow resistance equation was determined by dimensional analysis and applying the condition of incomplete self-similarity for the flow velocity profile. Then the analysis was developed by the following steps: (i…

Dimensional analysi010504 meteorology & atmospheric sciences0208 environmental biotechnology02 engineering and technology01 natural sciencesShields parametersymbols.namesakeFroude numberElectrical and Electronic EngineeringInstrumentation0105 earth and related environmental sciencesBed loadPhysicsFlow velocity profileComputer Science Applications1707 Computer Vision and Pattern Recognition020801 environmental engineeringComputer Science ApplicationsOpen-channel flowFlumeSelf-similarityFlow conditionsFlow velocityFlow resistanceLawModeling and SimulationsymbolsPotential flowBed-load
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Assessing flow resistance in gravel bed channels by dimensional analysis and self-similarity

2018

Abstract In this paper a new flow resistance equation for open channel flow, based on the integration of a power velocity profile, was tested for gravel bed channels. First this flow resistance equation, theoretically deduced by dimensional analysis and incomplete self-similarity condition, was reported. Then a relationship between the Γ function of the velocity profile, the channel slope and the Froude number was calibrated by the available laboratory measurements of flow velocity, water depth and bed slope carried out in 416 flume experimental runs with a gravel bed. Then the relationship for estimating Γ function and the theoretical resistance equation was tested by 83 independent flume …

Dimensional analysiFlow velocity profile010504 meteorology & atmospheric sciencesSelf-similarity0208 environmental biotechnology02 engineering and technologyMechanicsFunction (mathematics)Scale factor01 natural sciences020801 environmental engineeringOpen-channel flowPower (physics)FlumeSelf-similaritysymbols.namesakeGravel bedFlow velocityFlow resistanceFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Experimental study of boulder concentration effect on flow resistance in gravel bed channels

2021

Abstract Previous studies demonstrated that for open channel flows the power velocity profile can be integrated to obtain the flow resistance law. In this paper the relationship between Γ coefficient of the power velocity distribution, the channel slope and Froude number (Eq. (9) ) is firstly presented. Then the measurements carried out in a laboratory flume covered by hemispheric elements for two different hydraulic conditions (partially inundated and inundated) are used to calibrate this relationship. These elements are placed with a square arrangement and have a concentration range 4–64%. For the two investigated hydraulic conditions, this analysis demonstrates that the relationship to e…

Dimensional analysiFlow velocity profileMaterials scienceConcentration effectSoil scienceSurface finishScale factorOpen-channel flowSelf-similarityFlumeGravel bedsymbols.namesakeFlow resistanceCalibrationRange (statistics)Froude numbersymbolsBoulder concentrationEarth-Surface ProcessesCATENA
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Flow Resistance in Step-Pool Rills

2017

Rills evolve morphologically, and the adjustment of rill channel geometry to flow affects the relationships among velocity, discharge, and slope. The resistance to flow in step-pool rills is mainly due to form-induced mechanisms and, in comparison, grain resistance is of minor significance. Previous studies on rill flow resistance have been performed exclusively for grainresistance conditions and use a stream flow equation. In this study, a new flow resistance equation, deduced by applying dimensional analysis and self-similarity theory, was applied to rill flow in step-pool channels. First, the incomplete self-similarity hypothesis was used for establishing a power flow velocity profile wh…

Flow resistanceMorphology (linguistics)010504 meteorology & atmospheric sciences0208 environmental biotechnologySoil Science02 engineering and technologySTREAMSMechanics01 natural sciences020801 environmental engineeringFlow (mathematics)Dimensional analysis Flow resistance equations Friction factors Resistance equations Self-similarities Theoretical approach Theoretical expression Velocity profilesStream flowSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeology0105 earth and related environmental sciencesVadose Zone Journal
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Flow resistance in mobile bed rills shaped in soils with different texture

2021

Rill erosion is considered one of the most important soil processes because of the large amount of soil loss due to the development of a rill network able to promote an efficient transport of both rill flow-detached particles and those delivered from the inter-rill areas. Rill flow experiments are useful to overcome the gap in rill hydraulics knowledge and to test the reliability of currently applied uniform open channel flow equations for mobile bed rills. In this paper the applicability of a theoretical flow resistance equation, based on a power-velocity profile, to rill channels shaped on soils having different textures was investigated. The measurements (437 runs) of water depth, cross-…

Flow resistanceSoil textureSoil waterflow resistance plot measurements rill hydraulics soil erosion soil texture velocity profileSoil ScienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil scienceTexture (geology)Geology
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Rill flow resistance law under sediment transport

2021

Abstract Purpose In this paper, a deduced flow resistance equation for open-channel flow was tested using measurements carried out in mobile bed rills with sediment-laden flows and fixed bed rills. The main aims were to (i) assess the effect of sediment transport on rill flow resistance, and (ii) test the slope-flow velocity relationship in fixed bed rills. Methods The following analysis was developed: (i) a relationship between the Γ function of the velocity profile, the rill slope and the Froude number was calibrated using measurements carried out on fixed bed rills; (ii) the component of Darcy-Weisbach friction factor due to sediment transport was deduced using the corresponding measurem…

Flow resistancegeographyDimensional analysiFlow velocity profilegeography.geographical_feature_categoryFixed bedStratigraphyFlow (psychology)Soil scienceSediment transportSelf-similarityRillsymbols.namesakeFriction factorFlow velocityFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSediment transportGeologyRill flow resistanceEarth-Surface ProcessesJournal of Soils and Sediments
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Rill flow resistance law under equilibrium bed‐load transport conditions

2019

In this paper, a recently deduced flow resistance equation for open channel flow was tested under equilibrium bed-load transport conditions in a rill. First, the flow resistance equation was deduced applying dimensional analysis and the incomplete self-similarity condition for the flow velocity distribution. Then, the following steps were carried out for developing the analysis: (a) a relationship (Equation) between the Γ function of the velocity profile, the rill slope, and the Froude number was calibrated by the available measurements by Jiang et al.; (b) a relationship (Equation) between the Γ function, the rill slope, the Shields number, and the Froude number was calibrated by the same …

Flow resistancegeographygeography.geographical_feature_categoryflow velocity profileself-similarityrill flow resistanceMechanicsbed-loadRilldimensional analysiSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeologyWater Science and TechnologyBed loadHydrological Processes
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Large Eddy Simulations of Rough Turbulent Channel Flows Bounded by Irregular Roughness: Advances Toward a Universal Roughness Correlation

2020

The downward shift of the mean velocity profile in the logarithmic region, known as roughness function, $$\Delta U^+$$ , is the major macroscopic effect of roughness in wall bounded flows. This speed decrease, which is strictly linked to the friction Reynolds number and the geometrical properties which define the roughness pattern such as roughness height, density, shape parameters, has been deeply investigated in the past decades. Among the geometrical parameters, the effective slope (ES) seems to be suitable to estimate the roughness function at fixed friction Reynolds number, Re $$_{\tau }$$ . In the present work, the effects of several geometrical parameters on the roughness function, i…

FrictionLogarithmGeneral Chemical EngineeringGeometryGeneral Physics and AstronomyTurbulent channel flows Large eddy simulation02 engineering and technologySurface finishMacroscopic effects01 natural sciencesReynolds numberSettore ICAR/01 - Idraulica010305 fluids & plasmasRoot mean squaresymbols.namesakeSinusoidal functions0203 mechanical engineering0103 physical sciencesPhysical and Theoretical ChemistryChannel flowEffective slopePhysicsRoughness correlationTurbulenceMathematical analysisReynolds numberTexturesMean velocity profilesRoughnessOpen-channel flowWall flow Geometrical property020303 mechanical engineering & transportsAmplitudeLESLogarithmic regionsMean absolute deviationssymbolsLarge eddy simulationFlow, Turbulence and Combustion
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Large eddy simulations on the effect of the irregular roughness shape on turbulent channel flows

2019

Abstract Large Eddy Simulations (LES) are carried out to investigate on the mean flow in turbulent channel flows over irregular rough surfaces. Here the attention is focused to selectively investigate on the effect induced by crests or cavities of the roughness. The irregular shape is generated through the super-imposition of sinusoidal functions having random amplitude and four different wave-lengths. The irregular roughness profile is reproduced along the spanwise direction in order to obtain a 2D rough shape. The analysis of the mean velocity profiles shows that roughness crests induce higher effect in the outer-region whereas roughness cavities cause the highest effects in the inner-reg…

Higher order statisticMaterials scienceTurbulence simulationTurbulent channel flows Large eddy simulation02 engineering and technologyReynolds stressSurface finish01 natural sciencesReynolds numberSettore ICAR/01 - Idraulica010305 fluids & plasmasPhysics::Fluid Dynamicssymbols.namesake0203 mechanical engineering0103 physical sciencesMean flowReynolds equationAnisotropyChannel flowFluid Flow and Transfer ProcessesTurbulenceMean velocity profileMechanical EngineeringIrregular roughneReynolds numberSinusoidal functionMechanicsCondensed Matter PhysicsOpen-channel flowShear stre020303 mechanical engineering & transportsAmplitudeReynolds streTurbulence Irregular shapeTurbulence intensityLESsymbolsTurbulence modulationInternational Journal of Heat and Fluid Flow
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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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