Search results for "Flow velocity profile"

showing 9 items of 9 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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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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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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Entropic approach to estimate the mean flow velocity: experimental investigation in laboratory flumes

2015

The paper deals with the linear entropic relationship between the maximum velocity, u max , and the mean flow velocity, u m , through a dimensionless parameter Φ(M), in open-channel flow. The analysis is conducted with the aid of experimental data collected in straight laboratory flumes under different bed and side-walls roughness conditions. In particular, rough/vegetated beds and smooth/rough side-walls conditions have been investigated. The results show that, in the investigated conditions (with exception of low-submergence vegetated bed—h/k v  < 2), Φ(M) can be assumed equal to a value that is very close to that found in natural channels. This demonstrates that Φ(M) is able to implicitl…

Physics::Fluid DynamicsFlow resistanceHydrogeologyEnvironmental ChemistryThermodynamicsGeometrySurface finishMean flow velocityFlow discharge entropy flow velocity profile experimental dataSettore ICAR/01 - IdraulicaWater Science and TechnologyDimensionless quantityMathematicsEnvironmental Fluid Mechanics
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Assessing theoretical flow velocity profile and resistance in gravel bed rivers by field measurements

2018

Previous studies showed that integrating a power velocity profile, deduced applying dimensional analysis and the incomplete self-similarity condition, the flow resistance equation for open channel flow can be obtained. At first, in this paper the relationship between the Gamma function of the power velocity profile, the channel slope and the Froude number, which was already empirically introduced in a previous paper, is now theoretically deduced. Then this relationship is calibrated using the field measurements of flow velocity, water depth and bed slope carried out in 101 reaches of gravel bed rivers available by literature. The proposed relationship for estimating Gamma function and the t…

Self-similarityField (physics)0208 environmental biotechnologydimensional analysisBioengineering02 engineering and technologyIndustrial and Manufacturing Engineeringlcsh:Agriculturesymbols.namesakedimensional analysiRange (statistics)Froude numberflow velocity profile.lcsh:Agriculture (General)self-similarityflow velocity profileMechanical Engineeringlcsh:SFunction (mathematics)Mechanicslcsh:S1-972020801 environmental engineeringPower (physics)Open-channel flowFlow resistanceFlow velocitysymbolsGeologygravel bedJournal of Agricultural Engineering
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Effects of Boulder Arrangement on Flow Resistance Due to Macro-Scale Bed Roughness

2023

Flow resistance in gravel-bed channels is not only affected by the shape and size of the roughness elements, but also by their arrangement on the channel bed surface (position to flow streamlines, spacing between elements, and their protrusion from the channel bed). Many investigations proved that open channel flow resistance can be obtained by integrating the power velocity profile. For a macro-scale roughness condition, this study aims to investigate the effect of different boulder arrangements on flow resistance. First, for each arrangement, the equation relating &Gamma; function of the power velocity profile, the Froude number, and the channel slope was calibrated using available measur…

flow velocity profileself-similarityflow resistance; gravel bed; boulder arrangement; dimensional analysis; flow velocity profile; self-similaritydimensional analysiGeography Planning and DevelopmentSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliboulder arrangementAquatic Scienceflow resistanceBiochemistrygravel bedWater Science and TechnologyWater; Volume 15; Issue 2; Pages: 349
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