Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface

Turbulent flows over wavy surfaces give rise to the formation of ripples, dunes and other natural bedforms. To predict how much sediment these flows transport, research has focused mainly on basal shear stress, which peaks upstream of the highest topography, and has largely ignored the corresponding...

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Main Authors: Philippe Claudin, Michel Louge, Bruno Andreotti
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-05-01
Series:Frontiers in Physics
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fphy.2021.682564/full
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author Philippe Claudin
Michel Louge
Bruno Andreotti
author_facet Philippe Claudin
Michel Louge
Bruno Andreotti
author_sort Philippe Claudin
collection DOAJ
description Turbulent flows over wavy surfaces give rise to the formation of ripples, dunes and other natural bedforms. To predict how much sediment these flows transport, research has focused mainly on basal shear stress, which peaks upstream of the highest topography, and has largely ignored the corresponding pressure variations. In this article, we reanalyze old literature data, as well as more recent wind tunnel results, to shed a new light on pressure induced by a turbulent flow on a sinusoidal surface. While the Bernoulli effect increases the velocity above crests and reduces it in troughs, pressure exhibits variations that lag behind the topography. We extract the in-phase and in-quadrature components from streamwise pressure profiles and compare them to hydrodynamic predictions calibrated on shear stress data.
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spelling doaj.art-441f5302124640f49e687c4749c0350a2022-12-21T22:46:20ZengFrontiers Media S.A.Frontiers in Physics2296-424X2021-05-01910.3389/fphy.2021.682564682564Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy SurfacePhilippe Claudin0Michel Louge1Bruno Andreotti2Physique et Mécanique des Milieux Hétérogènes, PMMH UMR 7636 CNRS, ESPCI Paris, PSL Research University, Université de Paris, Sorbonne Université, Paris, FranceSibley School of Mechanical and Aerospace Engineering, Cornell University, Ithaca, NY, United StatesLaboratoire de Physique de L’Ecole Normale Supérieure, UMR 8550 CNRS, PSL Research University, Université de Paris, Sorbonne Université, Paris, FranceTurbulent flows over wavy surfaces give rise to the formation of ripples, dunes and other natural bedforms. To predict how much sediment these flows transport, research has focused mainly on basal shear stress, which peaks upstream of the highest topography, and has largely ignored the corresponding pressure variations. In this article, we reanalyze old literature data, as well as more recent wind tunnel results, to shed a new light on pressure induced by a turbulent flow on a sinusoidal surface. While the Bernoulli effect increases the velocity above crests and reduces it in troughs, pressure exhibits variations that lag behind the topography. We extract the in-phase and in-quadrature components from streamwise pressure profiles and compare them to hydrodynamic predictions calibrated on shear stress data.https://www.frontiersin.org/articles/10.3389/fphy.2021.682564/fullpressure modulationbedformssinusoidal topographylinear responselaminar-turbulent transition
spellingShingle Philippe Claudin
Michel Louge
Bruno Andreotti
Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface
Frontiers in Physics
pressure modulation
bedforms
sinusoidal topography
linear response
laminar-turbulent transition
title Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface
title_full Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface
title_fullStr Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface
title_full_unstemmed Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface
title_short Basal Pressure Variations Induced by a Turbulent Flow Over a Wavy Surface
title_sort basal pressure variations induced by a turbulent flow over a wavy surface
topic pressure modulation
bedforms
sinusoidal topography
linear response
laminar-turbulent transition
url https://www.frontiersin.org/articles/10.3389/fphy.2021.682564/full
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AT brunoandreotti basalpressurevariationsinducedbyaturbulentflowoverawavysurface