Abstract
This paper investigates the receptivity of boundary layers due to distributed roughness
interacting with free-stream disturbances. Both acoustic and vortical perturbations
are considered. An asymptotic approach based on the triple-deck formulation has
been developed to determine the initial amplitude of the Tollmien–Schlichting wave to
the O(R−1/8) accuracy, where R is the global
Reynolds number. In the case of vortical
disturbances, we show that the dominant contribution to the receptivity comes from
the upper deck as well as from the so-called edge layer centred at the outer reach of
the boundary layer. It is found that for certain forms of disturbances, the receptivity
is independent of their vertical structure and can be fully characterized by their slip
velocity at the edge of the boundary layer. A typical case is the vortical disturbance
in the form of a convecting wake, for which the same conclusion as above has been
reached by Dietz (1999) on the basis of measurements. Our theoretical predictions
are compared with the experimental data of Dietz (1999), and a good quantitative
agreement has been found. Such a comparison is the first to be made for distributed
vortical receptivity. Further calculations indicate that the vortical receptivity in general
is much stronger than was suggested previously. In the case of acoustic disturbances,
it is found that our first-order theory is in good agreement with experiments as well
as with previous theoretical results. But the second-order theory over-predicts, and
the possible reasons for this are discussed.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
69 articles.
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