Search results for "SIMILARITY"

showing 10 items of 474 documents

Testing the USLE-M family of models at the Sparacia experimental site in south Italy

2017

The modified Universal Soil Loss Equation (USLE-M) was empirically deduced by a statistical analysis of the original data set of soil loss measurements used to derive the Universal Soil Loss Equation (USLE). The USLE-M, including the effect of runoffin the event rainfall-runofferosivity factor, is characterized by a better capacity to predict event soil loss. At first, in this paper, using the soil erosion representative variables of USLE-M and the reference condition adopted in the USLE, the dimensional analysis and the self-similarity theory are applied to theoretically deduce a multiplicative equation similar to the USLE-M. Then using the database of the Sparacia experimental site, the a…

Dimensional analysi23000208 environmental biotechnologySoil science02 engineering and technology020801 environmental engineeringOriginal dataPlot soil loSet (abstract data type)Universal Soil Loss EquationSoil lossSelf-similarity theorySoil erosionUSLE-MUSLE-MMEnvironmental ChemistrySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliStatistical analysisUniversal Soil Loss Equation (USLE)General Environmental ScienceMathematicsCivil and Structural EngineeringWater Science and Technology
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Measuring rill erosion at plot scale by a drone-based technology

2015

The traditional direct method (i.e. metric ruler and rillmeter) of monitoring rill erosion at plot scale is time consuming and invasive since it modifies the surface of the rilled area. Measuring rill features using a drone-based technology is considered a non-invasive method allowing a fast field relief. In the experimental Sparacia area a survey by a quadricopter Microdones md4-200 was carried out and this relief allowed the generation of a Digital Elevation Model (DEM), with a mesh size of 1 cm and a resolution elevation equal to 2 mm, for three plots (L, G and C) affected by rill erosion. At first for the experimental L plot, which is 44 m long, the rill features were surveyed by a “man…

Dimensional analysiErosion modelingSelf-similarity theorySoil erosionRillSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDroneGullyEphemeral gully
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Assessing an overland flow resistance approach under equilibrium sediment transport conditions

2021

Abstract In this study, for the first time, a theoretically deduced flow resistance equation was tested for an overland flow under equilibrium sediment transport conditions using available experimental data by Liu et al. for five Chinese soils. Initially the relationship among the velocity profile parameter Γ, the channel slope, the flow Reynolds number, the Froude number and the sediment concentration was calibrated using 90 measurements of the available database (Loessial, Cinnamon and Black soil) and tested by other 60 measurements (Red and Purple soil). The results proved that the Darcy–Weisbach friction factor can be accurately estimated by the proposed theoretical approach, with error…

Dimensional analysiFlow (psychology)Reynolds numberSoil scienceSediment transportSoil typeScale factorSelf-similaritysymbols.namesakeFlow resistanceVelocity profileSoil waterFroude numbersymbolsEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSurface runoffSediment transportEarth-Surface Processes
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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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Evaluating the Effects of Sediment Transport on Pipe Flow Resistance

2021

In this paper, the applicability of a theoretical flow resistance law to sediment-laden flow in pipes is tested. At first, the incomplete self-similarity (ISS) theory is applied to deduce the velocity profile and the corresponding flow resistance law. Then the available database of measurements carried out by clear water and sediment-laden flows with sediments having a quasi-uniform sediment size and three different values of the mean particle diameter Dm (0.88 mm, 0.41 mm and 0.30 mm) are used to calibrate the Γ parameter of the power-velocity profile. The fitting of the measured local velocity to the power distribution demonstrates that (i) for clear flow the exponent δ can be estimated b…

Dimensional analysiSelf-similarity0208 environmental biotechnologyGeography Planning and Developmentdimensional analysis02 engineering and technologyAquatic ScienceBiochemistrysediment transportPipe flowsymbols.namesakeHydraulic headFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliTD201-500Water Science and TechnologyPhysicsWater supply for domestic and industrial purposesself-similaritySedimentHydraulic engineering04 agricultural and veterinary sciencesMechanics020801 environmental engineeringPower (physics)pipe flowFlow (mathematics)velocity profile040103 agronomy & agriculturesymbols0401 agriculture forestry and fisheriesTC1-978flow resistanceSediment transportWater
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New Theoretical Solution of Stage-Discharge Relationship for Slit Weirs

2018

In this paper, the flow-process of a slit weir was analyzed on the basis of a theorem of dimensional analysis and incomplete selfsimilarity theory. The theoretically deduced stage-discharge formula then was calibrated using experimental data obtained for a ratio between the weir and the channel width, ranging from 0.05 to 0.25. The deduced stage-discharge relationship allowed measuring discharge values characterized by errors that, for 98% of the measured values, were less than or equal to 5%. The performance of the proposed theoreticalstage-discharge formula also was improved by introducing the Reynolds number (for 98.5% of the measured values the error was less than or equal to 5%, and th…

Dimensional analysiSelf-similarityBasis (linear algebra)0208 environmental biotechnologyDischarge measurements02 engineering and technologyMechanics01 natural sciencesAgricultural and Biological Sciences (miscellaneous)SlitOpen channel flow010305 fluids & plasmas020801 environmental engineeringOpen-channel flowSelf-similarity0103 physical sciencesWeirSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliStage (hydrology)Discharge measurementWeirWater Science and TechnologyCivil and Structural EngineeringMathematicsJournal of Irrigation and Drainage Engineering
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Comments on “Mean velocity and turbulent characteristics of flow over half-cycle cosine sharp-crested weirs” by Salehi S., Esmaili K., Azimi A.H.

2019

Abstract In this paper the stage-discharge equation of a half-cycle cosine weir is theoretically deduced applying the Π-Theorem of dimensional analysis and the self-similarity theory. The coefficients of the new stage-discharge relationships are estimated using the results of the experimental runs by Salehi et al..

Dimensional analysiSelf-similarityHalf cycleTurbulenceMathematical analysis0207 environmental engineering02 engineering and technologySharp-crested weirs01 natural sciencesFlow measurementComputer Science ApplicationsFlow measurementSelf-similarity010309 opticsFlow (mathematics)Physics::Plasma PhysicsModeling and SimulationCosine weir0103 physical sciencesWeirTrigonometric functionsElectrical and Electronic Engineering020701 environmental engineeringInstrumentationMathematicsFlow Measurement and Instrumentation
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Testing a theoretically-based overland flow resistance law by Emmett’s database

2021

Abstract The main aim of this paper was to test a recently theoretically deduced flow resistance equation, based on a power-velocity profile, using a wide database of available measurements carried out in laboratory and field experimental runs with overland flow under simulated rainfall. In comparison with previous calibrations and validations of this theoretically deduced flow resistance equation, the used database by Emmett is characterized by a wide range of rainfall intensities (from 79.2 to 303.5 mm h−1 for laboratory runs and from 178.3 to 215.9 mm h−1 for field investigations) and bed slopes (from 0.33 to 17% for laboratory runs and from 2.9 to 33.2% for field investigations). For th…

Dimensional analysiVegetationDatabaseReynolds numberLaminar flowcomputer.software_genreSelf-similaritysymbols.namesakeWetted perimeterOverland flowVelocity profileFlow (mathematics)Flow velocityLawRainfall simulationFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSurface runoffcomputerIntensity (heat transfer)Water Science and TechnologyJournal of Hydrology
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Random analysis of geometrically non-linear FE modelled structures under seismic actions

1990

Abstract In the framework of the finite element (FE) method, by using the “total Lagrangian approach”, the stochastic analysis of geometrically non-linear structures subjected to seismic inputs is performed. For this purpose the equations of motion are written with the non-linear contribution in an explicit representation, as pseudo-forces, and with the ground motion modelled as a filtered non-stationary white noise Gaussian process, using a Tajimi-Kanai-like filter. Then equations for the moments of the response are obtained by extending the classical Ito's rule to vectors of random processes. The equations of motion, and the equations for moments, obtained here, show a perfect formal simi…

Discrete mathematicsHermite polynomialsSimilarity (geometry)Random excitation; non-linear structuresStochastic processMathematical analysisEquations of motionBuilding and ConstructionWhite noiseFinite element methodRandom excitationNonlinear systemsymbols.namesakesymbolsnon-linear structuresSafety Risk Reliability and QualityGaussian processCivil and Structural EngineeringMathematics
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