6533b86efe1ef96bd12cbe7d

RESEARCH PRODUCT

Flow resistance equation for rills

Vincenzo PampaloneVincenzo PalmeriVito FerroCostanza Di Stefano

subject

010504 meteorology & atmospheric sciences0208 environmental biotechnology02 engineering and technology01 natural sciencesPlot (graphics)Physics::Fluid Dynamicssymbols.namesakeWetted perimeterFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineering0105 earth and related environmental sciencesWater Science and TechnologyFlow resistancegeographysoil erosiongeography.geographical_feature_categoryrill flowMechanicsplot measurement020801 environmental engineeringRillDistribution (mathematics)Flow resistanceFlow velocityFlow (mathematics)velocity profilesymbolsGeology

description

In this paper, a new flow resistance equation for rill flow was deduced applying dimensional analysis and self‐similarity theory. At first, the incomplete self‐similarity hypothesis was used for establishing the flow velocity distribution whose integration gives the theoretical expression of the Darcy–Weisbach friction factor. Then the deduced theoretical resistance equation was tested by some measurements of flow velocity, water depth, cross section area, wetted perimeter, and bed slope carried out in 106 reaches of some rills shaped on an experimental plot. A relationship between the velocity profile, the channel slope, and the flow Froude number was also established. The analysis showed that the Darcy–Weisbach friction factor can be accurately estimated by the proposed theoretical approach based on a power–velocity profile.

https://doi.org/10.1002/hyp.11221