Issue |
J. Phys. II France
Volume 7, Number 9, September 1997
|
|
---|---|---|
Page(s) | 1225 - 1243 | |
DOI | https://doi.org/10.1051/jp2:1997183 |
J. Phys. II France 7 (1997) 1225-1243
Statics and Kinetics at the Nematic-Isotropic Interface: Effects of Biaxiality
V. Popa-Nita, T.J. Sluckin and A.A. WheelerFaculty of Mathematical Studies, University of Southampton, Southampton S017 1BJ, UK
(Received 2 December 1996, received in final form 9 May 1997, accepted 27 May 1997)
Abstract
We use the Landau-de Gennes theory of a nematic liquid crystal to investigate anew aspects of the properties of the interface
between the isotropic and nematic liquid crystal phases of the same fluid. The equations of the static interface have been
solved, both numerically and using asymptotic analysis, with an emphasis on the effect of inclusion of the order parameter
biaxiality on the physical properties. We have compared the results of the exact solutions to the commonly used de Gennes
ansatz, which assumes positive and uniform unixiality through the interface. Although the de Gennes ansatz in general gives good results, when bend and splay elastic constants dominate over the twist constants, it can lead to errors
of up to 10% in the surface energy. The asymptotic analysis also shows that, by contrast with the de Gennes ansatz, the order parameter wings in the isotropic phase exhibit negative order parameter, with principal axis perpendicular to
the surface. For moving interfaces, using an approximation which at this stage does not yet include hydrodynamic coupling,
we have compared our results with the analogue of the de Gennes ansatz used by the present authors in an earlier paper. We find that including biaxiality leads to larger effects in the dynamic
than in the static properties, and that whereas this is essentially a perturbation to the energy, the velocity of the moving
interface can be significantly slowed down. The slowing down effects are strongly correlated with surface biaxiality, but
both effects seem to be diminished when the isotropic phase is advancing.
© Les Editions de Physique 1997