Search results for "Flow resistance"

showing 10 items of 57 documents

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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Slope threshold for overland flow resistance on sandy soils

2021

Recent research on rill flows recognised that an 18% slope can be used to distinguish between ‘gentle’ and ‘steep’ slope cases for the detected differences in hydraulic (flow depth and velocity) and sediment transport variables (flow transport capacity, actual sediment load). The effects of slope on flow velocity, friction factor and transport capacity and their interactions affect process-based erosion modelling. The main aim of this paper is to investigate, for the first time, how slope affects the overland flow resistance on sandy soils, which are characterised by loose particles readily available to be transported and deposited. Using literature measurements carried out in sandy soils f…

Flow resistanceResistance (ecology)Soil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil ScienceSoil scienceflow resistance gentle hillslopes overland flow hydraulics soil erosion steep hillslopesSurface runoffGeologyEuropean Journal of Soil Science
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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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