Studies of translational diffusion in the smectic A phase of a Gay-Berne mesogen using molecular dynamics computer simulation
Bates, Martin A. and Luckhurst, Geoffrey R. (2004) Studies of translational diffusion in the smectic A phase of a Gay-Berne mesogen using molecular dynamics computer simulation. Journal of Chemical Physics, 120, (1), 394-403. (doi:10.1063/1.1630014).
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Molecular dynamics computer simulations are used to determine the self-diffusion coefficients for a Gay-Berne model mesogen GB (4.4,20,1,1) in the isotropic, nematic and smectic A phases along two isobars. The values of the parallel and perpendicular diffusion coefficients, D-parallel to and D-perpendicular to, are calculated and compared in the different phases. For the phase sequence isotropic-smectic A, D-perpendicular to*greater than or equal toD(parallel to)* over the whole smectic A range with the ratio D-parallel to */D-perpendicular to* decreasing with decreasing temperature. At a higher pressure, a nematic phase is observed between these two phases and we find that D-parallel to *D-perpendicular to* throughout the nematic region and the inequality D-parallel to *D-perpendicular to* remains on entering the smectic A phase. However, the ratio D-parallel to*/D-perpendicular to* decreases with decreasing temperature within the smectic A range and eventually this ratio inverts such that D-perpendicular to *D-parallel to* at low temperatures. The temperature dependence of the parallel diffusion coefficient in the smectic A phase for this model mesogen is compared to that predicted by a theoretical model for diffusion subject to a cosine potential.
|Keywords:||x-ray-scattering, anisotropic systems, liquid-crystals, self-diffusion, model, relaxation, behavior|
|Subjects:||Q Science > QA Mathematics > QA75 Electronic computers. Computer science
Q Science > QD Chemistry
Q Science > QC Physics
|Divisions:||University Structure - Pre August 2011 > School of Chemistry
|Date Deposited:||23 Feb 2006|
|Last Modified:||27 Mar 2014 18:09|
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
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