GORTLER VORTICES PROMOTED BY WALL ROUGHNESS

Authors
Citation
A. Bottaro et A. Zebib, GORTLER VORTICES PROMOTED BY WALL ROUGHNESS, Fluid dynamics research, 19(6), 1997, pp. 343-362
Citations number
28
Categorie Soggetti
Phsycs, Fluid & Plasmas",Mechanics
Journal title
ISSN journal
01695983
Volume
19
Issue
6
Year of publication
1997
Pages
343 - 362
Database
ISI
SICI code
0169-5983(1997)19:6<343:GVPBWR>2.0.ZU;2-B
Abstract
Numerical experiments are conducted to investigate spatially developin g Gortler vortices and the way in which wall roughness promotes their formation and growth. Several different types of walls are examined an d their relative merits as vortex promoters assessed. The only disturb ances of the flow are due to the rough wall; hence, at each downstream station the local field feels (1) the upstream flow distribution (pro duced by the upstream wall conditions) and (2) the local forcing at th e wall. Rapid vortex formation and growth, like in the case of riblete d walls, can be qualitatively explained by the positive combination of these two effects; when the two influences on the local flow field co mpete, e.g. for randomly distributed wall roughness, the equations wit h the boundary conditions filter the disturbances over some streamwise length, function of the roughness amplitude, to create coherent patch es of vorticity out of the random noise. These patches can then be amp lified by the instability mechanism. If a thin rough strip is aligned along the span of an otherwise smooth wall to trip the boundary layer, the filtering region is shorter and growth of the vortices starts ear lier. Also for the case of an isolated three-dimensional hump a rapid disturbance amplification is produced, but in this case the vortices r emain confined and a very slow spanwise spreading of the perturbation occurs. In all naturally developing cases, where no specific wavelengt hs are explicitly favored, the average spanwise wavelengths computed a re very close to those of largest growth from the linear stability the ory.