Global Potential Energy Minima of (H$_{2}$O)$_{n}$ Clusters on Graphite
| dc.creator | Gonzalez, B. S. | |
| dc.creator | Hernandez-Rojas, J. | |
| dc.creator | Breton, J. | |
| dc.creator | Llorente, J. M. Gomez | |
| dc.date | 2007-06-08 | |
| dc.date.accessioned | 2026-07-07T08:34:53Z | |
| dc.date.available | 2026-07-07T08:34:53Z | |
| dc.description | Likely candidates for the global potential energy minima of (H$_{2}$O)$_{n}$ clusters with $n\leq21$ on the (0001)-surface of graphite are found using basin-hopping global optimization. The potential energy surfaces are constructed using the TIP4P intermolecular potentials for the water molecules (the TIP3P is also explored as a secondary choice), a Lennard-Jones water-graphite potential, and a water-graphite polarization potential that is built from classical electrostatic image methods and takes into account both the perpendicular and parallel electric polarizations of graphite. This potential energy surface produces a rather hydrophobic water-graphite interaction. As a consequence, the water component of the lowest graphite-(H$_{2}$O)$_{n}$ minima is quite closely related to low-lying minima of the corresponding TIP4P (H$_{2}$O)$_{n}$ clusters. In about half of the cases the geometrical substructure of the water molecules in the graphite-(H$_{2}$O)$_{n}$ global minimum coincides with that of the corresponding free water cluster. Exceptions occur when the interaction with graphite induces a change in geometry. A comparison of our results with available theoretical and experimental data is performed. | |
| dc.identifier | https://arxiv.org/abs/0706.1152 | |
| dc.identifier | http://arxiv.org/abs/0706.1152 | |
| dc.identifier | J. Phys. Chem. C 111, 14862 (2007) | |
| dc.identifier.uri | http://salesiana.dossiersoluciones.com/handle/123456789/139593 | |
| dc.subject | Atomic and Molecular Clusters | |
| dc.title | Global Potential Energy Minima of (H$_{2}$O)$_{n}$ Clusters on Graphite | |
| dc.type | text |