Title
Convection in stable and unstable fronts
Date Issued
18 January 2012
Access level
metadata only access
Resource Type
journal article
Publisher(s)
American Physical Society
Abstract
Density gradients across a reaction front can lead to convective fluid motion. Stable fronts require a heavier fluid on top of a lighter one to generate convective fluid motion. On the other hand, unstable fronts can be stabilized with an opposing density gradient, where the lighter fluid is on top. In this case, we can have a stable flat front without convection or a steady convective front of a given wavelength near the onset of convection. The fronts are described with the Kuramoto-Sivashinsky equation coupled to hydrodynamics governed by Darcy's law. We obtain a dispersion relation between growth rates and perturbation wave numbers in the presence of a density discontinuity accross the front. We also analyze the effects of this density change in the transition to chaos. © 2012 American Physical Society.
Volume
85
Issue
1
Number
016207
Language
English
OCDE Knowledge area
Física de plasmas y fluídos
Scopus EID
2-s2.0-84856643513
Source
Physical Review E - Statistical, Nonlinear, and Soft Matter Physics
ISSN of the container
15502376
Sources of information: Directorio de Producción Científica Scopus