Search results for "Flow velocity"

showing 10 items of 227 documents

Flow velocity profile and turbulence characteristics in a vegetated straight flume

2008

Vegetation affects the hydrodynamic conditions of an open channel flow with direct implications in physical and biophysical processes. In this paper, the vertical flow velocity distribution of a vegetated flow has been analyzed using experimental data collected in a straight flume. The experimental velocity distributions are positively compared with the hyperbolic tangent profile of a pure mixing layer previously verified by Ghisalberti and Nepf (2002). Peculiarly, for different flow and vegetative conditions, fitting of the hyperbolic tangent profile to the experimental velocity distributions has allowed the localization of the inflection point of the velocity profile at a distance from th…

Rivers flow resistance vegetation flow velocity mixing layerSettore ICAR/01 - Idraulica
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Roughness effect on the correction factor of surface velocity for rill flows

2021

Flow velocity is one of the most important hydrodynamic variables for both channelized (rill and gullies) and interrill erosive phenomena. The dye tracer technique to measure surface flow velocity Vs is based on the measurement of the travel time of a tracer needed to cover a known distance. The measured Vs must be corrected to obtain the mean flow velocity V using a factor αv = V/Vs which is generally empirically deduced. The Vs measurement can be influenced by the method applied to time the travel of the dye-tracer and αv can vary in different flow conditions. Experiments were performed by a fixed bed small flume simulating a rill channel for two roughness conditions (sieved soil, gravel)…

Roughness effectgeographysoil erosiongeography.geographical_feature_categoryrill flowSoil scienceSurface velocitycorrection factorflow velocityRilldye methodFlow velocitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliinterrill flowGeologyWater Science and TechnologyHydrological Processes
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Dissipative scaling of step-pool features

2021

Abstract This paper focuses on the dissipative similarity of step-pool units at rill, flume and stream scale. This investigation is carried out using recent advances in open channel flow resistance, applications of close-range photogrammetry to rill erosion, available published data on step-pool features in flumes and streams and a new dataset of measurements in fixed bed step-pool rills. A theoretically-based equation for calculating the Darcy-Weisbach friction factor obtained by integration of a power velocity profile is presented. The scale factor Γ of this power velocity profile, which is included in the flow resistance equation, was previously calibrated (Eq. 10) for mobile bed rills w…

Scale (ratio)0207 environmental engineering02 engineering and technology01 natural sciences010309 opticsFlow velocity0103 physical sciencesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliElectrical and Electronic Engineering020701 environmental engineeringInstrumentationScalinggeographygeography.geographical_feature_categoryMechanicsScale factorComputer Science ApplicationsOpen-channel flowFlumeRillFlow resistanceModeling and SimulationDissipative systemStep-poolSediment transportGeologyFlow Measurement and Instrumentation
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Assessing flow resistance law in vegetated channels by dimensional analysis and self-similarity

2019

Abstract In this paper experimental data collected by Kouwen et al., Wilson and Horrit, Raffaelli et al. and Carollo et al., using straight flumes having a bed covered by grass-like vegetation with different stem concentrations, were used to analyze flow resistance for flexible submerged elements. At first, the dimensional analysis and the incomplete self-similarity hypothesis was applied to deduce the flow velocity distribution and the resulting theoretical expression of the Darcy-Weisbach friction factor. Then, a relationship between the Γ function of the velocity profile and the biomechanical characteristics of vegetation, the channel slope, the Reynolds number and the flow Froude number…

Self-similarity0207 environmental engineering02 engineering and technology01 natural sciences010309 opticssymbols.namesakeOpen channel0103 physical sciencesFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliElectrical and Electronic Engineering020701 environmental engineeringInstrumentationMathematicsVegetationReynolds numberFunction (mathematics)VegetationMechanicsComputer Science ApplicationsDistribution (mathematics)Flow resistanceFlow velocityFlow (mathematics)Modeling and SimulationsymbolsFlow Measurement and Instrumentation
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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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On the variation of the correction factor of surface velocity with the measurement vertical for shallow flows over rough beds

2023

Considering that water flow energy affects the detachment of soil particles, the transport and deposit of the detached particles, the flow velocity is a key variable governing the soil erosion processes at the hillslope scale. The simple dye-tracer technique for measuring mean flow velocity can be applied in non-controlled field applications for which some measurement difficulties (e.g. due to sediment transport, and shallow flows) can occur. The correction factor is usually obtained as the ratio between the mean velocity, deriving from measurements of flow discharge and water depth, and surface velocity. Alternatively, the possibility of using the velocity profile in a given vertical to de…

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalicorrection factor dye method flow velocity measurement vertical open channel flow soil erosion surface velocity velocity distributionWater Science and Technology
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Numerical experiments for defining criteria for the use of LS-PIV based techniques in river monitoring.

2019

The developing of new image-based techniques for environmental monitoring is opening new frontiers for remote streamflow measurements in natural environments, since they allow for non-intrusive measurements even in adverse circumstances, such as high flow conditions that often hinder the use of traditional approaches and instruments. Methods based on the acquisition, analysis and elaboration of images for streamflow observation, such as the large scale particle image velocimetry (LSPIV) and the particle tracking velocimetry (PTV) techniques, are rapidly evolving also in consideration of the growing availability of a new generation of optical sensors, digital cameras and methodologies. A num…

Settore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaPIV river flow measurments flow velocity
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Fluid-structure interaction and flow redistribution in membrane-bounded channels

2019

The hydrodynamics of electrodialysis and reverse electrodialysis is commonly studied by neglecting membrane deformation caused by transmembrane pressure (TMP). However, large frictional pressure drops and differences in fluid velocity or physical properties in adjacent channels may lead to significant TMP values. In previous works, we conducted one-way coupled structural-CFD simulations at the scale of one periodic unit of a profiled membrane/channel assembly and computed its deformation and frictional characteristics as functions of TMP. In this work, a novel fluid&ndash

Settore ING-IND/26 - Teoria Dello Sviluppo Dei Processi ChimiciControl and OptimizationMaterials scienceFluid structure interactionEnergy Engineering and Power Technologycomputational fluid dynamics02 engineering and technologyComputational fluid dynamicsComputational fluid dynamicslcsh:TechnologyNumerical modelElectromembrane process020401 chemical engineeringComputational fluid dynamicHydraulic permeabilityReversed electrodialysisFluid–structure interactionMembrane deformationSDG 7 - Affordable and Clean Energy0204 chemical engineeringElectrical and Electronic EngineeringElectromembrane proceEngineering (miscellaneous)Profiled membraneSettore ING-IND/19 - Impianti NucleariIon exchange membraneDarcy's lawSuperficial velocitylcsh:TRenewable Energy Sustainability and the Environmentbusiness.industryFlow maldistributionMechanicsElectrodialysisDarcy flow021001 nanoscience & nanotechnologyelectromembrane processFlow velocity0210 nano-technologyPorous mediumbusinessSettore ICAR/08 - Scienza Delle CostruzioniEnergy (miscellaneous)
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Examination of the shock wave regular reflexion phenomenon in a rarefied supersonic plasma flow

2005

The flow properties of a low-pressure weakly ionized supersonic argon plasma jet are examined using Fabry–Perot interferometry and laser induced fluorescence spectroscopy. The flow velocity and equilibrium temperature measured at the torch nozzle exit are in close agreement with computational fluid dynamics calculations. The model also predicts the plasma flow to be in a rarefied regime. Departure from thermal equilibrium is indeed observed behind the nozzle where the parallel temperature differs significantly from the perpendicular temperature. The development of the axial velocity component along the jet center stream line reveals the occurrence of the shock wave regular reflexion phenome…

Shock wavePhysicsJet (fluid)business.industryNozzleMechanicsCondensed Matter PhysicsPhysics::Fluid DynamicsOpticsFlow velocityShock diamondOblique shockSupersonic speedbusinessChoked flowPhysics of Plasmas
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Physical modelling of the melt flow during large-diameter silicon single crystal growth

2003

Abstract The reported investigations concern physical modelling of Czochralski growth of silicon large-diameter single crystals. InGaSn eutectic was used as a modelling liquid, employing actual criteria of the real process (Prandtl, Reynolds, Grashof numbers, etc.) and geometric similarity. A multi-channel measuring system was used to collect and process the temperature and flow velocity data. The investigations were focused on the study of heat transfer, in particular, the instability of the “cold zone” of the melt at the crystallization front.

SiliconChemistryPrandtl numberGrashof numberMineralogychemistry.chemical_elementMechanicsCondensed Matter Physicslaw.inventionPhysics::Fluid DynamicsInorganic Chemistrysymbols.namesakeFlow velocitylawHeat transferMaterials ChemistrysymbolsCrystallizationMelt flow indexEutectic systemJournal of Crystal Growth
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