Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence

The present paper simplifies the naturally formed dunes (riverbeds) as large-scale three-dimensional staggered wavy walls to investigate the features of the accompanying secondary flows and streamwise vortices via large-eddy simulation. A comparison between the swirling strength and the mean velocit...

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Main Authors: Enwei Zhang, Zhan Wang, Wangxia Wu, Xiaoliang Wang, Qingquan Liu
Format: Article
Language:English
Published: Cambridge University Press 2023-01-01
Series:Flow
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S2633425923000132/type/journal_article
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author Enwei Zhang
Zhan Wang
Wangxia Wu
Xiaoliang Wang
Qingquan Liu
author_facet Enwei Zhang
Zhan Wang
Wangxia Wu
Xiaoliang Wang
Qingquan Liu
author_sort Enwei Zhang
collection DOAJ
description The present paper simplifies the naturally formed dunes (riverbeds) as large-scale three-dimensional staggered wavy walls to investigate the features of the accompanying secondary flows and streamwise vortices via large-eddy simulation. A comparison between the swirling strength and the mean velocities suggests where a secondary flow induces upwash or downwash motions. Moreover, we propose a pseudo-convex wall mechanism to interpret the directionality of the secondary flow. The centrifugal instability criterion is then used to reveal the generation of the streamwise vortices. Based on these analytical results, we found that the streamwise vortices are generated in the separation and reattachment points on both characteristic longitudinal–vertical and horizontal cross-sections, which is related to the curvature effect of the turbulent shear layer. Furthermore, the maximum Görtler number characterized by the ratio of centrifugal to viscous effects suggests that, for fixed ratio of spanwise- to streamwise-wavelength cases, the strongest centrifugal instability occurring on the longitudinal–vertical cross-section gradually dominates with the increases in amplitude. A similar trend for the cases with varied spanwise wavelength can also be found. It is also found that the streamwise vortices are generated more readily via transverse flow around the crest near the separation and reattachment points when the ratio of spanwise- to streamwise-wavelength equals 1.
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spelling doaj.art-a17795c6d0ee417abb65fc5df4833e982023-07-04T07:33:21ZengCambridge University PressFlow2633-42592023-01-01310.1017/flo.2023.13Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulenceEnwei Zhang0https://orcid.org/0000-0002-0562-0837Zhan Wang1https://orcid.org/0000-0003-4393-2118Wangxia Wu2https://orcid.org/0000-0001-5548-8312Xiaoliang Wang3Qingquan Liu4https://orcid.org/0000-0002-4472-6626Institute of Mechanics, Chinese Academy of Sciences, Beijing 100190, PR ChinaInstitute of Mechanics, Chinese Academy of Sciences, Beijing 100190, PR ChinaSchool of Aerospace Engineering, Beijing Institute of Technology, Beijing 100081, PR ChinaSchool of Aerospace Engineering, Beijing Institute of Technology, Beijing 100081, PR ChinaSchool of Aerospace Engineering, Beijing Institute of Technology, Beijing 100081, PR ChinaThe present paper simplifies the naturally formed dunes (riverbeds) as large-scale three-dimensional staggered wavy walls to investigate the features of the accompanying secondary flows and streamwise vortices via large-eddy simulation. A comparison between the swirling strength and the mean velocities suggests where a secondary flow induces upwash or downwash motions. Moreover, we propose a pseudo-convex wall mechanism to interpret the directionality of the secondary flow. The centrifugal instability criterion is then used to reveal the generation of the streamwise vortices. Based on these analytical results, we found that the streamwise vortices are generated in the separation and reattachment points on both characteristic longitudinal–vertical and horizontal cross-sections, which is related to the curvature effect of the turbulent shear layer. Furthermore, the maximum Görtler number characterized by the ratio of centrifugal to viscous effects suggests that, for fixed ratio of spanwise- to streamwise-wavelength cases, the strongest centrifugal instability occurring on the longitudinal–vertical cross-section gradually dominates with the increases in amplitude. A similar trend for the cases with varied spanwise wavelength can also be found. It is also found that the streamwise vortices are generated more readily via transverse flow around the crest near the separation and reattachment points when the ratio of spanwise- to streamwise-wavelength equals 1.https://www.cambridge.org/core/product/identifier/S2633425923000132/type/journal_articleTopographic effects
spellingShingle Enwei Zhang
Zhan Wang
Wangxia Wu
Xiaoliang Wang
Qingquan Liu
Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence
Flow
Topographic effects
title Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence
title_full Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence
title_fullStr Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence
title_full_unstemmed Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence
title_short Secondary flow and streamwise vortices in three-dimensional staggered wavy-wall turbulence
title_sort secondary flow and streamwise vortices in three dimensional staggered wavy wall turbulence
topic Topographic effects
url https://www.cambridge.org/core/product/identifier/S2633425923000132/type/journal_article
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AT wangxiawu secondaryflowandstreamwisevorticesinthreedimensionalstaggeredwavywallturbulence
AT xiaoliangwang secondaryflowandstreamwisevorticesinthreedimensionalstaggeredwavywallturbulence
AT qingquanliu secondaryflowandstreamwisevorticesinthreedimensionalstaggeredwavywallturbulence