Gd. Miller et Chk. Williamson, TURBULENT STRUCTURES IN THE TRAILING VORTEX WAKE OF A DELTA-WING, Experimental thermal and fluid science, 14(1), 1997, pp. 2-8
In the present study, we investigate the near- and far-wake instabilit
ies in the wake of a delta wing with a view to understanding the basic
instabilities, mixing, and decay rate of the wake. Extensive visualiz
ation of the wake as a delta wing glides in free flight through water
reveals a ''braid wake'' between the primary vortex pair and shows it
imposing its structure on the primary pair. Hot-wire measurements of t
he fluctuating velocity in the immediate near wake not only demonstrat
e the periodic shedding of the spanwise vortices in this ''braid wake,
'' but also reveal a low-frequency oscillation nearer to the core of e
ach primary vortex. The subsequent evolution of the wake is remarkable
, as the scales of disturbances grow in what appear to be almost discr
ete steps, until a large-scale instability of the primary pair develop
s into a sequence of large-scale interconnecting vortex loops. Ultimat
ely, the appearance is similar to a series of vortex rings. The stream
wise wavelength of the ring-like structure was measured for these free
-flight tests and for tests with the wing towed through water at a var
iety of speeds and angles of attack, yielding a wavelength between 4 a
nd 5 spans (intervortex spacing of the primary pair). Further investig
ation is required before the relation of these results to theoretical
analyses can be ascertained. Experiments in which the incident velocit
y is perturbed at selected wavelength and amplitude reveal that the wa
velength of the final structure is reasonably insensitive to either pa
rameter unless the forcing becomes as large as 5% of free-stream veloc
ity, provided the forcing wavelength is far from the natural wavelengt
h. While investigating the vertical mixing of the fluid due to the des
cending vortices, we found that the vertical extent of mixing is surpr
isingly large owing to the formation of a ''curtain'' of vortical flui
d left above the descending vortex pair. (C) Elsevier Science Inc., 19
97.