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Description
Delaying the transition from laminar flow to turbulent flow in a boundary layer has many
advantages for aerospace systems, the principal one being a significant reduction in wall shear
stress and thereby skin friction drag. As such, understanding the mechanisms by which this
transition occurs has been of fundamental scientific interest since Osborne Reynolds' classic
dye experiment in the 19th century.
Traditionally, the study of laminar-turbulent transition has focussed on the boundary
layers forming along a nominally zero pressure gradient flat plat immersed in a disturbancefree
flow. In such conditions, the transition process has been viewed as consisting offour steps
(Morkovin et al., 1994; Fasel, 2002; Sarec et al., 2002): (1) receptivity, by which unsteady
disturbances external to the boundary layer enter the boundary layer; (2) linear instability, by
which growth of these disturbances can be determined using the linearized, unsteady, NavierStokes
equations; (3) secondary instability, during which nonlinear interactions occur and
the amplitude of the disturbances grow three-dimensionally; and (4) breakdown, involving
the formation of local bursts and spots of turbulence which rapidly merge to form a fully
turbulent boundary layer.
The transition process described above is only observed under ideal conditions where
the freestream turbulence intensity is quite low, u' jUoo of the order of 0.01%, where u' is
the mean amplitude of the velocity fluctuations and Uoo is the mean velocity of the free
stream. Whereas this magnitude of freestream turbulence is potentially possible in free
flight conditions, in a large majority of engineering flows, freestream turbulence levels can be
considerably higher. Under these conditions, the boundary layer undergoes what is referred
to as "bypass transition" (Morkovin, 1993).
During bypass transition, transition occurs much earlier and the actual transition to
turbulence is often preceded by the appearance of streamwise streaks of low momentum
fluid within the boundary layer (Klebenoff, 1971) associated with spanwise distortion of the
boundary layer thickness. Commonly referred to as "Klebenoff modes" , these structures are
long in the streamwise direction and narrow in the spanwise direction (with a width on the
order of the boundary layer thickness). The amplitude of the fluctuations of the Klebenoff
modes peaks at a location approximately half the boundary layer thickness away from the
wall and grows algebraically in the streamwise direction. As such, these streaks differ from
both the linear disturbances occurring in disturbance-free conditions (a.k.a. the TollmienSchlichting
waves (Schlichting & Gersten, 2000)) and longitudinal streaks observed in fully
turbulent boundary layers (Kline et al., 1967; Hutchins et al., 2009). It as yet, unclear
what role the Klebenoff modes play in the ultimate transition turbulence, although it's been
Status | Finished |
---|---|
Effective start/end date | 1/1/11 → 12/31/11 |
Funding
- KY Council on Postsecondary Education
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Projects
- 1 Finished
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EPSCoR: Match for NASA Kentucky Space Grant
Smith, S. (PI) & Lumpp, J. (CoI)
KY Council on Postsecondary Education
8/1/10 → 6/7/16
Project: Research project