Hostname: page-component-848d4c4894-x5gtn Total loading time: 0 Render date: 2024-05-14T06:45:36.866Z Has data issue: false hasContentIssue false

Linear and nonlinear instabilities of a Blasius boundary layer perturbed by streamwise vortices. Part 2. Intermittent instability induced by long-wavelength Klebanoff modes

Published online by Cambridge University Press:  20 May 2003

XUESONG WU
Affiliation:
Center for Turbulence Research, Stanford University, CA 94305, USA Department of Mathematics, Imperial College, 180 Queens Gate, London SW7 2BZ, UK
MEELAN CHOUDHARI
Affiliation:
Computational Modeling and Simulation Branch, NASA Langley Research Center, Hampton, VA 23681-2199, USA

Extract

This paper presents theoretical results on the instability of a Blasius boundary layer perturbed by Klebanoff modes (i.e. the low-frequency streaks known to be induced by free-stream turbulence). Herein, the Klebanoff distortions are modelled as the signature of a three-dimensional convected gust that may be either isolated or periodic along the spanwise direction. Relatively weak Klebanoff fluctuations can produce $O(1)$ changes tothe near-wall curvature of the base flow profile and, hence, fundamentally alter the nature of its instability characteristics.The perturbed flow is shown to support instabilities that are predominantly inviscid and have significantly larger growth rates and characteristic frequencies than the Tollmien–Schlichting(T–S) modes of an unperturbed Blasius flow. The spanwise mode shape of instabilities in the perturbed flow is determined by theSchrödinger equation, with a potential function that corresponds to the skin friction perturbation due to the Klebanoff distortion. The growth ratesof these modes are determined by the near-wall torsion of the perturbed flow.The unsteadiness of the Klebanoff distortion is shown to be a crucial element in determining the overall instability characteristics.

Type
Research Article
Copyright
© 2003 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)