Stability of a self-similar adverse pressure gradient turbulent boundary layer

Conference Paper (2018)
Author(s)

M. P. Eisfelder (Monash University)

J. S. Müller (Technical University of Berlin)

A. Sekimoto (Osaka University, Monash University)

A. J. Buchner (Monash University, TU Delft - Mechanical Engineering)

V. Kitsios (Monash University, CSIRO Oceans and Atmosphere)

C. Atkinson (Monash University)

K. Oberleithner (Technical University of Berlin)

J. Soria (Monash University)

Research Group
Fluid Mechanics
More Info
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Publication Year
2018
Language
English
Research Group
Fluid Mechanics
ISBN (electronic)
9780646597843
Event
21st Australasian Fluid Mechanics Conference, AFMC 2018 (2018-12-10 - 2018-12-13), Adelaide, Australia
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Abstract

Linear stability analysis (LSA) of a self-similar adverse pressure gradient (APG) turbulent boundary layer (TBL) is explored in order to identify coherent structures. An eddy viscosity model (EV) is implemented via the Boussinesq hypothesis [8] to model the nonlinear coherent-turbulent interactions. Direct numerical simulations (DNS) by Kitsios et al. [3, 6] are used for the database of this study. A weak APG and strong APG (on the verge of separation) are studied with dimensionless streamwise pressure gradients (β) of 1 and 39 respectively. Their Reynolds numbers based on the momentum thickness (δ2) within their respective regions of interest are 3, 100 − 3, 400 and 10, 000 − 12, 300. For the strong APG, the most unstable eigen-solution produces a wave resembling a Kelvin-Helmholtz (KH) instability located near the displacement thickness (δ1) height. This position coincides with the inflection point (IP) in the mean flow profile. The IP satisfies Rayleigh’s and Fjortoft’s criterion for the existence of an inviscid instability [9]. Positive growth rate is seen for non-dimensional angular frequencies of 0.08 ≤ ω ≤ 0.51, with the maximum growth occurring at ω = 0.26. The weak APG also contains a KH like wave, however for all ω, the growth rates are negative. Spanwise wavenumber kxr and phase velocity ĉr increase monotonically for both β cases. Comparisons with a quasi-laminar analysis are also made.

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