Hostname: page-component-848d4c4894-75dct Total loading time: 0 Render date: 2024-05-21T09:39:16.909Z Has data issue: false hasContentIssue false

Three-dimensional oscillatory flow over steep ripples

Published online by Cambridge University Press:  10 June 2000

P. SCANDURA
Affiliation:
Dipartimento di Ingegneria Ambientale, Università di Genova, Via Montallegro 1, 16145, Genova, Italy
G. VITTORI
Affiliation:
Dipartimento di Ingegneria Ambientale, Università di Genova, Via Montallegro 1, 16145, Genova, Italy
P. BLONDEAUX
Affiliation:
Dipartimento di Ingegneria Ambientale, Università di Genova, Via Montallegro 1, 16145, Genova, Italy

Abstract

The process which leads to the appearance of three-dimensional vortex structures in the oscillatory flow over two-dimensional ripples is investigated by means of direct numerical simulations of Navier–Stokes and continuity equations. The results by Hara & Mei (1990a), who considered ripples of small amplitude or weak fluid oscillations, are extended by considering ripples of larger amplitude and stronger flows respectively. Nonlinear effects, which were ignored in the analysis carried out by Hara & Mei (1990a), are found either to have a destabilizing effect or to delay the appearance of three-dimensional flow patterns, depending on the values of the parameters. An attempt to simulate the flow over actual ripples is made for moderate values of the Reynolds number. In this case the instability of the basic two-dimensional flow with respect to transverse perturbations makes the free shear layer generated by boundary layer separation become wavy as it leaves the ripple crest. Then the amplitude of the waviness increases and eventually complex three-dimensional vortex structures appear which are ejected in the irrotational region. Sometimes the formation of mushroom vortices is observed.

Type
Research Article
Copyright
© 2000 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)