Prediction of longitudinal roll cells in rotating plane turbulent Couette flow

Citation
Bap. Reif et Hi. Andersson, Prediction of longitudinal roll cells in rotating plane turbulent Couette flow, TH COMP FL, 14(2), 2000, pp. 89-108
Citations number
42
Categorie Soggetti
Physics,"Mechanical Engineering
Journal title
THEORETICAL AND COMPUTATIONAL FLUID DYNAMICS
ISSN journal
09354964 → ACNP
Volume
14
Issue
2
Year of publication
2000
Pages
89 - 108
Database
ISI
SICI code
0935-4964(200006)14:2<89:POLRCI>2.0.ZU;2-W
Abstract
The ability of a second-moment closure to predict the three-componential me an flow which results when a plane Couette flow is subjected to moderate an ticyclonic system rotation is explored. The counterrotating streamwise-orie nted roll cells, which may occur by the imposition of a destabilizing Corio lis force field, are treated as an integral part of the steady mean motion governed by the Reynolds-averaged Navier-Stokes equations. Near-wall effect s are accounted for by Durbin's elliptic relaxation approach, while system rotation only appears naturally in rotational stress-producing terms and in the mean intrinsic vorticity in the non-linear pressure-strain model. The model predictions mimicked the most striking effects of anticyclonic ro tation, as observed in a series of recent direct numerical simulations. In particular they reproduced the characteristic energetic roll-cell pattern, which inevitably enhanced the cross-sectional mixing. The broadening of the central core region, in which the primary mean velocity profile adjusted i tself to make the absolute mean vorticity negligibly small, was well captur ed by the predictions, together with the remarkable damping of the turbulen t velocity fluctuations. The success of the predictions supports the view t hat such large-scale structures as the rotational-induced roll cells should be treated as a part of the resolved mean flow field, the obvious and phys ically appealing implication being that the turbulence closure is left to r epresent nothing but real turbulence.