. (2013) 'Gravity-driven thin lm ow : the in uence of topography and surface tension gradient on rivulet formation.', Chemical engineering and processing : process intensi cation., 68 . pp. 7-12. Further information on publisher's website:http://dx.doi.org/10.1016/j.cep.2012.07.003Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Chemical Engineering and Processing: Process Intensi cation. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be re ected in this document. Changes may have been made to this work since it was submitted for publication. A de nitive version was subsequently published in Chemical Engineering and Processing: Process Intensi cation, 68, June 2013, 10.1016/j.cep.2012.07.003.
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AbstractThe evolution of an advancing fluid front formed by a gravity-driven thin film flowing down a planar substrate is considered, with particular reference to the presence of Marangoni stresses and/or surface topography. The system is modelled using lubrication theory and solved via an efficient, adaptive multigrid method that incorporates automatic, errorcontrolled grid refinement/derefinement and time stepping. The detailed three dimensional numerical results obtained reveal that, for the problems investigated, while both of the above features affect the merger of rivulets by either delaying or promoting the same, topography influences the direction of growth.