Viscous froth simulations with surfactant mass transfer and Marangoni effects: Deviations from Plateau's rules

Embley, B.; Grassia, P.

Abstract

The viscous froth model is a theological model for dry, "two-dimensional" foams, such as a monolayer of bubbles confined between two glass plates. The model is typically out of mechanical equilibrium due to viscous dissipation by drag along the confining plates. By introducing variable local surfactant coverages and variable local surface tensions, we modify the model such that, in addition to being out of mechanical equilibrium, foam structures can also be out of physicochemical equilibrium. We include effects accounting for spatially and temporally varying Marangoni forces and surfactant transport, and we investigate the effects on a simple, periodic honeycomb lattice under shear. It is found that surfactant coverage can vary substantially between and within films, with surfactant becoming highly depleted on film edges that are subjected to rapid direct shear. Moreover substantial deviations from Plateau's laws occur at flowing three-fold vertices an effect previously noted in experiments but without any definitive explanation in theory or models. For large enough values of the governing dimensionless groups (capillary, Deborah, and Marangoni numbers), angles may locally vary from 120 degrees by 10 degrees or more. Correspondingly, the change in surface tensions at a three-fold vertex leads to a change in the time required to induce a topological rearrangement (T1) in a sheared foam sample. In this sense, variable surfactant coverage effects help to preserve the structure of a flowing foam, but also lead to an increase in energy storage within the foam. (C) 2011 Elsevier B.V. All rights reserved.

Más información

Título según WOS: ID WOS:000291917000003 Not found in local WOS DB
Título de la Revista: COLLOIDS AND SURFACES A-PHYSICOCHEMICAL AND ENGINEERING ASPECTS
Volumen: 382
Número: 1-3
Editorial: Elsevier
Fecha de publicación: 2011
Página de inicio: 8
Página final: 17
DOI:

10.1016/j.colsurfa.2011.01.013

Notas: ISI