A viscous froth model for dry foams in the Surface Evolver

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dc.contributor.author Cox, Simon
dc.date.accessioned 2007-08-13T15:26:49Z
dc.date.available 2007-08-13T15:26:49Z
dc.date.issued 2005-08
dc.identifier.citation Cox , S 2005 , ' A viscous froth model for dry foams in the Surface Evolver ' pp. 81-89 . en
dc.identifier.other PURE: 72186
dc.identifier.other dspace: 2160/322
dc.identifier.uri http://hdl.handle.net/2160/322
dc.description Cox, S.J. (2005) A Viscous Froth Model for Dry Foams in the Surface Evolver. Coll. Surf. A 263:81-89. Sponsorship: Partial support from both the Ulysses France–Ireland Exchange Scheme and the European Space Agency, Contract 14308/00/NL/SH (AO-99-031) CCN 002 MAP Project AO-99-075. en
dc.description.abstract An implementation of the recent viscous froth model of Kern et al. [N.Kern, D.Weaire, A. Martin, S. Hutzler, S.J. Cox, The two-dimensional viscous froth model for foam dynamics, Phys. Rev. E 70 (2004) 041411.] in the Surface Evolver is described, along with examples of the simulations that can be achieved. In particular, results are given for steady shear of both periodic and confined staircase structures, and contrasted with the quasi-static case. Also discussed are the case of Couette shear and the relaxation due to coarsening after an initial stepstrain. It is shown how the viscous froth model allows the investigation of strain-rate dependent effects and that it gives improved resolution of the topological events which govern the foam’s evolution, leading to structures that could not previously have been predicted. en
dc.format.extent 9 en
dc.language.iso eng
dc.relation.ispartof en
dc.title A viscous froth model for dry foams in the Surface Evolver en
dc.type Text en
dc.type.publicationtype Conference paper en
dc.identifier.doi http://dx.doi.org/10.1016/j.colsurfa.2004.12.061
dc.contributor.institution Institute of Mathematics & Physics (ADT) en
dc.contributor.institution Mathematical Modelling of Structures, Solids and Fluids en
dc.description.status Non peer reviewed en


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