STRUCTURE AND EQUATION OF STATE OF A LONG-CHAIN AMPHIPHILE MONOLAYER ADSORBED ON ICE IH - A MOLECULAR-DYNAMICS STUDY

Authors
Citation
Kp. Bell et Sa. Rice, STRUCTURE AND EQUATION OF STATE OF A LONG-CHAIN AMPHIPHILE MONOLAYER ADSORBED ON ICE IH - A MOLECULAR-DYNAMICS STUDY, The Journal of chemical physics, 104(4), 1996, pp. 1684-1692
Citations number
25
Categorie Soggetti
Physics, Atomic, Molecular & Chemical
ISSN journal
00219606
Volume
104
Issue
4
Year of publication
1996
Pages
1684 - 1692
Database
ISI
SICI code
0021-9606(1996)104:4<1684:SAEOSO>2.0.ZU;2-O
Abstract
We report the results of molecular dynamics simulations of the structu re of the rotator phase of a monolayer of a long chain alkyl carboxyli c acid, H(CH2)(15)COOH, supported on the 0001 face of ice Ih, as a fun ction of area per molecule. The potential field generated by this surf ace has an ordered component arising from the lattice of oxygens and a n irregular component arising from the disordered distribution of hydr ogens. Consequently, the many possible head group pinning sites of the ice Ih 0001 surface are irregularly distributed and not commensurate with the oxygen lattice. Our results, which are derived from simulatio ns that use a pseudoatom model of the amphiphile molecule and a rigid lattice model of the ice surface, show that the constraint imposed by the potential field of the rigid ice Ih 0001 surface generates propert ies of the ice supported monolayer that are different from those of th e corresponding liquid water supported monolayer. As expected, we find that the head groups are pinned and that as the area per molecule is increased the monolayer develops a collective tilt; the collective til t increases as the area per molecule increases. More striking, we find that the projection of the unit cell of the monolayer in the plane of the surface remains, on average, hexagonal for all collective tilt an gles and all surface coverages. In contrast, the introduction of a col lective tilt of the molecules in the L(2) (rotator) phase of a liquid water supported monolayer is always accompanied by a distortion of the projection of the unit cell in the plane of the surface, typically fr om hexagonal at zero tilt to centered rectangular for all nonzero tilt . Despite this difference in packing structure, and the pinning of the head groups, the surface pressure as a function of area per molecule, and the collective tilt as a function of area per molecule of a monol ayer supported on ice Ih closely resemble those for the L(2) phase of a monolayer supported at the air/water interface. The only structural data available for monolayers of long chain molecules on ice Ih refer to a low-temperature (similar to 100 K) and high surface density (simi lar to 18 Angstrom(2) per molecule), under which conditions the amphip hile molecules pack in a herringbone structure with a rectangular unit cell in the interface plane. The difference between the properties of this low-temperature monolayer on ice Ih, which is not in a rotator p hase, and the properties of the rotator phase we have simulated is bri efly discussed. (C) 1996 American Institute of Physics.