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Turbulent channel flow over heterogeneous roughness at oblique angles
by
Anderson, W.
in
Angles (geometry)
/ Boundary layers
/ Cells
/ Channel flow
/ Computational fluid dynamics
/ Computer simulation
/ Dependence
/ Direction
/ Engineering
/ Equilibrium
/ Heterogeneity
/ Large eddy simulation
/ Momentum
/ Oceanic eddies
/ Patchiness
/ Reynolds number
/ Roughness
/ Skewness
/ Spatial heterogeneity
/ Turbulent flow
/ Viscosity
2020
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Turbulent channel flow over heterogeneous roughness at oblique angles
by
Anderson, W.
in
Angles (geometry)
/ Boundary layers
/ Cells
/ Channel flow
/ Computational fluid dynamics
/ Computer simulation
/ Dependence
/ Direction
/ Engineering
/ Equilibrium
/ Heterogeneity
/ Large eddy simulation
/ Momentum
/ Oceanic eddies
/ Patchiness
/ Reynolds number
/ Roughness
/ Skewness
/ Spatial heterogeneity
/ Turbulent flow
/ Viscosity
2020
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While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Turbulent channel flow over heterogeneous roughness at oblique angles
by
Anderson, W.
in
Angles (geometry)
/ Boundary layers
/ Cells
/ Channel flow
/ Computational fluid dynamics
/ Computer simulation
/ Dependence
/ Direction
/ Engineering
/ Equilibrium
/ Heterogeneity
/ Large eddy simulation
/ Momentum
/ Oceanic eddies
/ Patchiness
/ Reynolds number
/ Roughness
/ Skewness
/ Spatial heterogeneity
/ Turbulent flow
/ Viscosity
2020
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Turbulent channel flow over heterogeneous roughness at oblique angles
Journal Article
Turbulent channel flow over heterogeneous roughness at oblique angles
2020
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Overview
Large-eddy simulation has been used to model turbulent channel flow over a range of surfaces featuring a prominent spatial heterogeneity; the flow streamwise direction is aligned relative to the heterogeneity at a range of angles, defined herein with
$\\unicode[STIX]{x1D703}$
. Prior work has established that a sharp roughness heterogeneity orthogonal to the flow streamwise direction (
$\\unicode[STIX]{x1D703}=0$
) induces formation of an internal boundary layer, which originates at the heterogeneity and thickens in the downflow direction before being homogenized via ambient shear. In contrast, more-recent studies have shown that a sharp roughness heterogeneity parallel to the flow streamwise direction (
$\\unicode[STIX]{x1D703}=\\unicode[STIX]{x03C0}/2$
) induces streamwise-aligned, Reynolds-averaged secondary cells, where the spacing between adjacent surface heterogeneities regulates the spatial extent of secondary cells. No prior study has addressed intermediate (oblique) cases,
$0\\leqslant \\unicode[STIX]{x1D703}\\leqslant \\unicode[STIX]{x03C0}/2$
. Results presented herein show that the momentum penalty exhibits a nonlinear dependence upon obliquity, where internal boundary layer-like flow processes persist over a range of obliquity angles before abruptly vanishing for spanwise roughness heterogeneity (
$\\unicode[STIX]{x1D703}=\\unicode[STIX]{x03C0}/2$
). This result manifests itself within effective roughness lengths recovered
a posteriori
: the traditional approach to roughness modelling – predicated upon dependence with surface geometric arguments including height root-mean-square, skewness, frontal- and plan-area index, effective slope. and combinations thereof – is insufficient. A revised model incorporating dependence upon roughness frontal area index and flow-heterogeneity obliquity angle is able to accurately predict effective roughness length
a priori
.
Publisher
Cambridge University Press
Subject
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