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The effect of surface roughness on the convective instability of the BEK family of boundary-layer flows

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posted on 2016-02-25, 13:34 authored by Burhan Alveroglu, A. Segalini, Stephen J. Garrett
A Chebyshev polynomial discretisation method is used to investigate the effect of both anisotropic (radially and azimuthally) and isotropic surface roughnesses on the convective instability of the BEK family of rotating boundary-layer flows. The mean-flow profiles for the velocity components are obtained by modelling surface roughness with a partial-slip approach. A linear stability analysis is then performed to investigate the effect of roughness on the convective instability characteristics of the inviscid Type I (cross-flow) instability and the viscous Type II instability. It is revealed that all roughness types lead to a stabilisation of the Type I mode in all flows within the BEK family, with the exception of azimuthally-anisotropic roughness (radial grooves) within the Bödewadt layer which causes a mildly destabilising effect. In the case of the Type II mode, the results reveal the destabilising effect of radially-anisotropic roughness (concentric grooves) on all the boundary layers, whereas both azimuthally-anisotropic and isotropic roughnesses have a stabilising effect on the mode for Ekman and von Kármán layers. Complementary results are also presented by considering the effects of roughness on the growth rates of each instability mode within the Ekman layer.

History

Citation

European Journal of Mechanics B/Fluids, 2015, pp. 178-187

Author affiliation

/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Mathematics

Version

  • AM (Accepted Manuscript)

Published in

European Journal of Mechanics B/Fluids

Publisher

Elsevier for European Mechanics Society (Euromech)

issn

0997-7546

eissn

1873-7390

Acceptance date

2015-11-24

Copyright date

2015

Available date

2017-12-22

Publisher version

http://www.sciencedirect.com/science/article/pii/S0997754615301898

Notes

The file associated with this record is under a 24-month embargo from publication in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.

Language

en

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