Search results for "flow [Keywords]"

showing 10 items of 469 documents

Flow resistance in gravel-bed channels with large-scale roughness

2003

A previously published mixing length (ML) model for evaluating the Darcy–Weisbach friction factor for a large-scale roughness condition (depth to sediment height ratio ranging from 1 to 4) is briefly reviewed and modified (MML). Then the MML model and a modified drag (MD) model are experimentally tested using laboratory measurements carried out for gravel-bed channels and large-scale roughness condition. This analysis showed that the MML gives accurate estimates of the Darcy–Weisbach coefficient and for Froude number values greater than 0·5 the MML model coincides with the ML one. Testing of the MD model shows limited accuracy in estimating flow resistance. Finally, the MML and MD models are com…

Flow resistanceScale (ratio)Depth to sediment height ratioGeography Planning and DevelopmentLarge-scale roughnessSurface finishMechanicsScale factorsymbols.namesakeFlow resistanceDragGravel-bed channelEarth and Planetary Sciences (miscellaneous)ExponentFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineeringConstant (mathematics)Earth-Surface ProcessesMathematicsEarth Surface Processes and Landforms
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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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Applying Hypothesis of Self-Similarity for Flow-Resistance Law in Calabrian Gravel-Bed Rivers

2018

In this paper, the results of an investigation carried out to test the applicability of a flow-resistance law on gravel-bed rivers in southern Italy (fiumare) are reported. First, dimensional analysis and self-similarity theory are applied for deducing the flow-resistance law (i.e., relationship among friction factor, mean velocity, shear stress, and physical properties) for gravel-bed rivers with a high boulder concentration. The proposed approach is calibrated and tested using two independent data sets (104 reaches of some Calabrian fiumare). Then, the incomplete self-similarity hypothesis is also applied to theoretically deduce the flow-velocity profile, which was integrated for obtainin…

Flow resistanceVelocity measurement010504 meteorology & atmospheric sciencesSelf-similarityGravel-bed riverMechanical Engineering0208 environmental biotechnology02 engineering and technology01 natural sciences020801 environmental engineeringSelf-similarityFlow resistanceDimension (vector space)LawSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSouthern Italy0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringMathematicsJournal of Hydraulic Engineering
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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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Testing a new rill flow resistance approach using the Water Erosion Prediction Project experimental database

2018

In this paper, a recently theoretically deduced rill flow resistance equation, based on a power‐velocity profile, was tested using the Water Erosion Prediction Project database. This database includes measurements of flow velocity, water depth, cross section area, wetted perimeter, and bed slope that were made in rills shaped on experimental sites distributed across the continental United States. In particular, three different experimental conditions (only rainfall, only flow, and rain with flow) were examined, and for each condition, the theoretically based relationship for estimating the Γ function of the power velocity profile was calibrated. The results established that (a) the Darcy‐We…

Flow resistancegeographyWater erosiongeography.geographical_feature_categorysoil erosionself-similarity0208 environmental biotechnology04 agricultural and veterinary sciences02 engineering and technology020801 environmental engineeringRill040103 agronomy & agriculture0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineeringrill erosionflow resistanceGeologyWater Science and Technology
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Slope threshold in rill flow resistance

2022

The applicability of a theoretical rill flow resistance equation, based on the integration of a power velocity distribution, was tested using measurements carried out in mobile and fixed bed rills, shaped on plots having different slopes (9, 14, 15, 18, 22, 24, 25 and 26%) and soil textures (clay fractions ranging from 32.7% to 73% and silt of 19.9–30.9%), and flume measurements available in the literature. The Darcy–Weisbach friction factor resulted dependent on the slope, Froude number, Reynolds number and clay and silt percentages, used as variables representative of soil transportability and detachability, respectively. This theoretical approach was applied to two different databases di…

Flow resistancegeographygeography.geographical_feature_categoryFixed bedSoil textureRill hydraulicReynolds numberSoil scienceSiltGentle hillslopeFlumeRillsymbols.namesakeFlow resistancesymbolsFroude numberSoil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSteep hillslopesGeologyEarth-Surface Processes
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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 in Channels with Flexible Submerged Vegetation

2005

In this paper, experimental data collected in a straight flume having a bed covered by grasslike vegetation have been used to analyze flow resistance for flexible submerged elements. At first, the measurements are used to test the applicability of Kouwen’s method. Then, a calibration of two coefficients appearing in the semilogarithmic flow resistance equation is carried out. Finally, applying the P-theorem and the incomplete self-similarity condition, a flow resistance equation linking the friction factor with the shear Reynolds number, the depth-vegetation height ratio and the inflection degree is deduced.

Flow resistanceopen-channel flow flow resistance vegetatiom dimension analysisMechanical EngineeringShear resistanceReynolds numberMechanicsOpen channel flow; Flow resistance; Vegetation; Dimensional analysisOpen-channel flowPhysics::Fluid DynamicsFlumesymbols.namesakeFriction factorsymbolsGeotechnical engineeringGeologyWater Science and TechnologyCivil and Structural EngineeringJournal of Hydraulic Engineering
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Testing slope effect on flow resistance equation for mobile bed rills

2018

In this paper, a recently theoretically deduced rill flow resistance equation, based on a power-velocity profile, is tested experimentally on plots of varying slopes in which mobile bed rills are incised. Initially, measurements of flow velocity, water depth, cross-sectional area, wetted perimeter and bed slope conducted in 106 reaches of rills incised on an experimental plot having a slope of 14% were used to calibrate the flow resistance equation. Then, the relationship between the velocity profile parameter Γ, the channel slope, and the flow Froude number, which was calibrated using the 106 rill reach data, was tested using measurements carried out in plots having slopes of 22% and 9%. …

Flow resistancesoil erosion010504 meteorology & atmospheric sciences0208 environmental biotechnology02 engineering and technology01 natural sciencesplot measurement020801 environmental engineeringvelocity profileSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineeringflow resistancerill hydraulicGeology0105 earth and related environmental sciencesWater Science and TechnologyHydrological Processes
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Estimating flow resistance in steep slope rills

2021

Recent research recognized that the slope of 18% can be used to distinguish between the ‘gentle slope’ case and that of ‘steep slope’ for the detected differences in hydraulic variables (flow depth, velocity, Reynolds number, Froude number) and those representatives of sediment transport (flow transport capacity, actual sediment load). In this paper, using previous measurements carried out in mobile bed rills and flume experiments characterized by steep slopes (i.e., slope greater than or equal to 18%), a theoretical rill flow resistance equation to estimate the Darcy-Weisbach friction factor is tested. The main aim is to deduce a relationship between the velocity profile parameter Γ, the c…

Flow resistancesoil erosionSoil texturesteep hillslopesSteep slopeSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil sciencesoil textureflow resistancerill hydraulicGeologyplot measurementWater Science and Technology
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