Hostname: page-component-848d4c4894-ndmmz Total loading time: 0 Render date: 2024-05-31T07:49:31.692Z Has data issue: false hasContentIssue false

Nonlinear instability of plane liquid sheets

Published online by Cambridge University Press:  10 March 2000

SEYED A. JAZAYERI
Affiliation:
Department of Mechanical Engineering, University of Victoria, Victoria, B.C., Canada V8W 3P6
XIANGUO LI
Affiliation:
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1

Abstract

A nonlinear stability analysis has been carried out for plane liquid sheets moving in a gas medium at rest by a perturbation expansion technique with the initial amplitude of the disturbance as the perturbation parameter. The first, second and third order governing equations have been derived along with appropriate initial and boundary conditions which describe the characteristics of the fundamental, and the first and second harmonics. The results indicate that for an initially sinusoidal sinuous surface disturbance, the thinning and subsequent breakup of the liquid sheet is due to nonlinear effects with the generation of higher harmonics as well as feedback into the fundamental. In particular, the first harmonic of the fundamental sinuous mode is varicose, which causes the eventual breakup of the liquid sheet at the half-wavelength interval of the fundamental wave. The breakup time (or length) of the liquid sheet is calculated, and the effect of the various flow parameters is investigated. It is found that the breakup time (or length) is reduced by an increase in the initial amplitude of disturbance, the Weber number and the gas-to-liquid density ratio, and it becomes asymptotically insensitive to the variations of the Weber number and the density ratio when their values become very large. It is also found that the breakup time (or length) is a very weak function of the wavenumber unless it is close to the cut-off wavenumbers.

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.)