Structure and phase transitions of monolayers of intermediate-length n -alkanes on graphite studied by neutron diffraction and molecular dynamics simulation

• Published in: The Journal of chemical physics 2009-08, Vol.131 (8), p.084707-084707-10
• Main Authors: Diama, A., Matthies, B., Herwig, K. W., Hansen, F. Y., Criswell, L., Mo, H., Bai, M., Taub, H.
• Format: Article
• Language: English
• Subjects: ALKANES; CARBON; CHAINS; DEFECTS; GRAPHITE; HEATING; INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY; MELTING; NEUTRON DIFFRACTION; ORIENTATION; SIMULATION; TRANSITION TEMPERATURE
• ISSN: 0021-9606; 1089-7690
• DOI: 10.1063/1.3212095

We present evidence from neutron diffraction measurements and molecular dynamics (MD) simulations of three different monolayer phases of the intermediate-length alkanes tetracosane ( n -C 24 H 50 denoted as C24) and dotriacontane ( n -C 32 H 66 denoted as C32) adsorbed on a graphite basal-plane surface. Our measurements indicate that the two monolayer films differ principally in the transition temperatures between phases. At the lowest temperatures, both C24 and C32 form a crystalline monolayer phase with a rectangular-centered (RC) structure. The two sublattices of the RC structure each consists of parallel rows of molecules in their all - trans conformation aligned with their long axis parallel to the surface and forming so-called lamellas of width approximately equal to the all - trans length of the molecule. The RC structure is uniaxially commensurate with the graphite surface in its [110] direction such that the distance between molecular rows in a lamella is 4.26   Å = 3 a g , where a g = 2.46   Å is the lattice constant of the graphite basal plane. Molecules in adjacent rows of a lamella alternate in orientation between the carbon skeletal plane being parallel and perpendicular to the graphite surface. Upon heating, the crystalline monolayers transform to a "smectic" phase in which the inter-row spacing within a lamella expands by ∼ 10 % and the molecules are predominantly oriented with the carbon skeletal plane parallel to the graphite surface. In the smectic phase, the MD simulations show evidence of broadening of the lamella boundaries as a result of molecules diffusing parallel to their long axis. At still higher temperatures, they indicate that the introduction of gauche defects into the alkane chains drives a melting transition to a monolayer fluid phase as reported previously.