Search results for "dimensional analysi"

showing 10 items of 68 documents

Testing a theoretical resistance law for overland flow on a stony hillslope

2020

Overland flow, sediments, and nutrients transported in runoff are important processes involved in soil erosion and water pollution. Modelling transport of sediments and chemicals requires accurate estimates of hydraulic resistance, which is one of the key variables characterizing runoff water depth and velocity. In this paper, a new theoretical power–velocity profile, originally deduced neglecting the impact effect of rainfall, was initially modified for taking into account the effect of rainfall intensity. Then a theoretical flow resistance law was obtained by integration of the new flow velocity distribution. This flow resistance law was tested using field measurements by Nearing for the …

010504 meteorology & atmospheric sciencesFlow (psychology)rainfall0207 environmental engineering02 engineering and technology01 natural sciencessymbols.namesakeWetted perimeteroverland flowdimensional analysiFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali020701 environmental engineering0105 earth and related environmental sciencesWater Science and Technologyself-similarityReynolds numberLaminar flowstony hillslopeFlow velocityLawsymbolsvelocity profileEnvironmental scienceSurface runoffflow resistanceIntensity (heat transfer)
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Comments on “Overflow characteristics of streamlined weirs based on model experimentation” by Bagheri S. and Kabiri-Samani A

2021

Abstract In this paper the stage-discharge equation of a streamlined weir is theoretically deduced applying the Π-Theorem of dimensional analysis and the self-similarity theory. The coefficients of the new stage-discharge relationship are estimated using the experimental results by Bagheri and Kabiri-Samani.

0207 environmental engineering02 engineering and technology01 natural sciencesComputer Science Applications010309 opticsDimensional analysis Discharge coefficient Self-similarity Stage-discharge relationship Streamlined weirPhysics::Plasma PhysicsModeling and Simulation0103 physical sciencesWeirApplied mathematicsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliElectrical and Electronic Engineering020701 environmental engineeringInstrumentationMathematics
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Three-dimensional analysis of the physiological foramen geometry of maxillary and mandibular molars by means of micro-CT.

2017

The aim of this study was to investigate the physiological foramen diameter, shape and distance between physiological and anatomical apex of maxillary and mandibular first and second molars. Accurate knowledge of the physiological foramina morphology; thus, inherent mechanical shaping technical hindrances, is decisive when taking the corresponding root canal final preparation decision. The morphological dimensions of a total of 1727 physiological foramina were investigated by means of micro-computed tomography. Mean narrow and wide (to a high number, oval) diameters of the physiological foramen were 0.24, 0.22 and 0.33 mm and 0.33, 0.31 and 0.42 mm in mesiobuccal (MB), distobuccal (DB) and …

0301 basic medicineMolarThree dimensional analysisRoot canalDecision MakingDentistry610 Medicine & healthIn Vitro TechniquesMandibular first molarMandibular second molar03 medical and health sciencesmaxillary and mandibular molars morphology0302 clinical medicineTooth Apexstomatognathic system10066 Clinic of Conservative and Preventive DentistryForamenmedicineHumansapical constrictionphysiological foramenmicro-computed tomography610 Medicine & healthGeneral DentistryMathematicsbusiness.industryDistobuccalX-Ray Microtomography030206 dentistryMolar3500 General DentistryApex (geometry)030104 developmental biologymedicine.anatomical_structureOriginal ArticleDental Pulp Cavitybusinessfinal apical fileRoot Canal Preparation
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Assessing, measuring and modelling erosion in calanchi areas: A review

2016

Calanchi are erosion landforms characterised by a heavily dissected terrain with steep, unvegetated slopes and channels with a dendritic pattern, which rapidly incise and extend headwards. Recent literature focusing on badland systems highlights their similarity with other larger fluvial landforms, stating that these behave as a full size laboratory, due to their rapid development in space and time and to the diversity of geomorphic processes involved. In this paper, a brief review of the most important results on badland research is firstly presented. Then, the morphometric similarity between calanchi and other erosion landforms is discussed. Finally, models quantitatively relating the vol…

BadlandCalanchiDimensional analysi010504 meteorology & atmospheric sciences0208 environmental biotechnologydimensional analysisFluvialTerrainBioengineering02 engineering and technology01 natural sciencesIndustrial and Manufacturing Engineeringlcsh:AgricultureMorphometric analysiself-similarity.TributaryGeotechnical engineeringlcsh:Agriculture (General)Geomorphology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorymorphometric analysisLandformMechanical Engineeringlcsh:Sbadlandslcsh:S1-972020801 environmental engineeringSelf-similarityMorphometric analysisErosionSoil erosionBadlands; Calanchi; Dimensional analysis; Morphometric analysis; Self-similarity; Soil erosion; Bioengineering; Mechanical Engineering; Industrial and Manufacturing EngineeringGeology
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Overland flow hydrodynamic characteristics in rough beds at low Reynolds numbers

2022

This paper considers overland flow resistance at low Reynolds numbers through analysis of experimental runs carried out using water only and water/glycerol mixtures. We first examined the power relationship between the Darcy–Weisbach friction factor f and the Reynolds number Re to obtain the values of the K coefficient and b exponent. These results confirmed the applicability of the values of b suggested in literature, while K required a specific calibration for laminar open-channel flows. The analysis revealed that transition from a laminar to turbulent flow regime for water only flows occurred at a threshold value of Re equal to 500 as described historically. The estimate of f by the powe…

Bed roughneSelf-similarityDimensional analysiMixed flowFlow resistanceVelocity profileSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliWater Science and TechnologyJournal of Hydrology
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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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Testing a theoretical resistance law for overland flow under simulated rainfall with different types of vegetation

2020

Abstract In this paper a recently theoretically deduced flow resistance equation, based on a power-velocity profile, was tested using data collected for overland flow under simulated rainfall carried out in plots with vegetation. The available data were obtained exploring a wide range of rainfall intensities (from 60 to 181 mm h−1) and slopes (from 3.6 to 39.6%), and with four different types of vegetation. The database, including measurements of flow velocity, water depth, cross sectional flow area, wetted perimeter and bed slope, was divided in four datasets (one for each vegetation type), which allowed the calibration of the relationship between the velocity profile parameter Γ, the slop…

Dimensional analysi010504 meteorology & atmospheric sciencesSoil science01 natural sciencessymbols.namesakeWetted perimeterVelocity profileFroude numbermedicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliVegetable cover0105 earth and related environmental sciencesEarth-Surface ProcessesReynolds numberLaminar flow04 agricultural and veterinary sciencesOpen channel flowOpen-channel flowSelf-similarityFlow (mathematics)Flow velocityFlow resistance040103 agronomy & agriculturesymbolsRainfall simulationSoil erosion0401 agriculture forestry and fisheriesEnvironmental sciencemedicine.symptomVegetation (pathology)
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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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