Abstract
We investigate analytically the anchoring of a nematic liquid crystal on a two-dimensionally grooved surface of arbitrary shape, induced by the elastic distortions of a liquid crystal adjacent to the surface. Our theoretical framework applied to a surface with square grooves reveals that such a surface can exhibit bistable anchoring, while a direct extension of a well-known theory of Berreman [Phys. Rev. Lett. 28, 1683 (1972)] results in no azimuthal anchoring in the so-called one-constant case (, with , , and being the splay, twist, and bend elastic constants, respectively). We show under the assumption of that the direction of the bistable easy axes and the anchoring strength crucially depend on the ratios and , where is the saddle-splay surface elastic constant. To demonstrate the applicability of our theory to general cases and to elucidate the effect of surface shape and the elastic constants on the properties of surface anchoring, we also consider several specific cases of interest; one-dimensional grooves of arbitrary shape, rhombic grooves, and surfaces possessing -fold symmetry, including hexagonal grooves, and show the following: (i) The rescaled anchoring energy of one-dimensional grooves, with being the angle between the director and the groove direction, is independent of the groove shape. (ii) Whether two diagonal axes of rhombic grooves can become easy axes depends sensitively on , and the angle between the grooves. The angle yielding the maximum anchoring strength for given groove pitch and amplitude depends again on and ; in some cases (one-dimensional grooves), and in other cases , gives the maximum anchoring strength. Square grooves do not necessarily exhibit the largest anchoring strength. (iii) A surface possessing -fold symmetry can yield -stable azimuthal anchoring. However, when and , azimuthal anchoring is totally absent irrespective of the value of . The direction of the easy axes depends on , , and whether is even or odd.
12 More- Received 20 June 2007
DOI:https://doi.org/10.1103/PhysRevE.77.011702
©2008 American Physical Society