Abstract
A new mechanism is proposed for the generation of Tollmien–Schlichting (T–S)
waves by free-stream turbulence. For definiteness and self-consistency, the mechanism is
described mathematically by using a triple-deck formalism. The free-stream turbulence
is represented by convecting gusts consisting of the so-called vortical and entropy
waves of small amplitude. We show that suitable convecting gusts can interact with
sound waves in the free stream to produce a forcing that has the same time and
length scales as those of the T–S waves, thereby exciting such waves in the vicinity
of the lower branch of the neutral stability curve. The T–S waves so produced
have the order of magnitude of ε2R5/16,
where ε is the amplitude of the free-stream
disturbance and R the global Reynolds number. The scale conversion is achieved
without resorting to any non-homogeneity on the wall, and hence the mechanism
operates in a flat boundary layer. Furthermore, the T–S waves so generated do not
undergo any immediate decay, as they may do in some other receptivity processes.
For homogeneous isotropic free-stream turbulence, the spectrum of the T–S waves
is obtained. The efficiency of the receptivity mechanism is assessed by parametric
studies.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
48 articles.
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