Classical trajectory calculations of (H2O)(n) (n less than or equal to
123) scattering from rigid model surfaces are presented. Three differ
ent intramolecular water potentials are employed together with both fl
at and corrugated surfaces. Clusters with an internal temperature of 1
80 K are scattered from the surface with incident velocities of 400-20
00 m/s, and energy conversion during surface interaction is followed b
y probing the temperatures of various degrees of freedom. Molecular tr
anslation within the cluster couples strongly to the surface potential
resulting in a compression phase of the cluster and a temperature pea
k at impact. Energy then dissipates to molecular rotation and further
on to intramolecular vibration in the bending mode. The choice of the
intramolecular potential has a strong effect only on the coupling to t
he stretch modes. Cluster fragmentation is very low up to 1300 m/s and
thereafter increases with velocity. The energy redistribution at impa
ct depends only weakly on cluster size and the surface potential emplo
yed. The total energy transfer efficiency is largely determined by the
maximum surface potential energy during the scattering event.