Theoretical Analysis of Some Thin-Film Flows over Complex Surfaces
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Saudi Digital Library
Abstract
In this thesis, three different aspects of thin-film
flow over complex surfaces are investigated.
First, locally-unidirectional rivulet
flow on a slippery surface is considered. We
study rivulets with prescribed
flux and either fixed semi-width or fixed contact angle. In
both cases we determined the effect of varying the slip length on the rivulet. We found
that in the limit of strong slip, for a rivulet of a perfectly wetting
fluid and a rivulet
with constant width, the velocity becomes large and plug-like, and the rivulet becomes
shallow, while for a rivulet with positive constant contact angle, the velocity becomes
large and plug-like, and the rivulet becomes narrow and shallow. Second, rivulet
flow
over and through a permeable membrane is considered. We study rivulets with prescribed
flux and either fixed semi-width or fixed contact angle. We found that whereas
there is a physically realisable pendant rivulet solution only if the semi-width does not
exceed a critical value, there are physically realisable sessile and vertical rivulet solutions
for all values of the semi-width; moreover, a sessile rivulet with fixed semi-width
has a finite maximum possible length which is attained in the limit of a wide rivulet.
Lastly, patterns formed in a two-dimensional thin film with a Derjaguin-type disjoining
pressure on a planar substrate with periodic wettability stripes is considered. Using
Liapunov-Schmidt reduction, we study the local bifurcation structure of the problem
for spatially homogeneous disjoining pressure and how the structure depends on the
average film thickness. Using methods of local bifurcation theory and the continuation
software package AUTO, we perform a continuation analysis of the steady state
solutions and establish the existence of both nucleation and metastable regimes. The
dependence of the steady state solutions on the wettability contrast are investigated
for two forms of spatially non-homogeneous disjoining pressure.