Wedge filling, cone filling and the strong-fluctuation regime

Citation
Ao. Parry et al., Wedge filling, cone filling and the strong-fluctuation regime, J PHYS-COND, 13(21), 2001, pp. 4591-4613
Citations number
38
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
JOURNAL OF PHYSICS-CONDENSED MATTER
ISSN journal
09538984 → ACNP
Volume
13
Issue
21
Year of publication
2001
Pages
4591 - 4613
Database
ISI
SICI code
0953-8984(20010528)13:21<4591:WFCFAT>2.0.ZU;2-Z
Abstract
Interfacial fluctuation effects occurring at wedge- and cone-filling transi tions are investigated and shown to exhibit very different characteristics. For both geometries we argue that the conditions for observing critical (c ontinuous) filling are much less restrictive than for critical wetting, whi ch is known to require the fine tuning of the Haamaker constants. Wedge fil ling is critical if the wetting binding potential does not exhibit a local maximum, whilst conic filling is critical if the line tension is negative. This latter scenario is particularly encouraging for future experimental st udies. Using mean-field and effective Hamiltonian approaches, which allow for brea ther-mode fluctuations which translate the interface up and down the sides of the confining geometry, we are able to completely classify the possible critical behaviours (for purely thermal disorder).. For the three-dimension al wedge, the interfacial fluctuations are very strong and characterized by a universal roughness critical exponent nu (W)(perpendicular to) = 1/4 ind ependent of the range of the forces. For the physical dimensions d = 2 and d = 3, we show that the effect of the cone geometry on the fluctuations at critical filling is to mimic the analogous interfacial behaviour occurring at critical wetting in the strong-fluctuation regime. In particular, for d = 3 and for quite arbitrary choices of the intermolecular potential, the fi lling height and roughness show the same critical properties as those predi cted for three-dimensional critical wetting with short-ranged forces in the large-wetting-parameter (omega > 2) regime.