  Desorption of H2O films ranging from 53 nanometres to 101 micrometre
thicknesses have been investigated using a quartz-crystal microbalance (QCM)
and temperature-programmed desorption. Three desorption stages are observed
belonging to amorphous solid water (ASW), stacking disordered ice I (ice Isd),
and hexagonal ice I (ice Ih). The desorption of ASW is only visible for the >10
micrometre films and is separated from the ice I desorption by 10-15 K and has
an associated desorption energy of 64 kJ mol-1. The desorption energy of the 53
nanometre film was found to be near 50 kJ mol-1 as also noted in the
literature, but with increasing film thickness the desorption energy of ice I
rises until reaching a plateau around 65-70 kJ mol-1. The reason for the
increased desorption energy is suggested to be due to molecules unable to
desorb due to the thick covering layer of H2O and possibly re-adsorption.
Before complete desorption of ice I which occurs around 220 K for the 100
micrometre film, a two-stage ice I desorption is observed with the QCM for the
10 and 20 micrometre films near 200 K. This event corresponds to the desorption
of ice Isd as corroborated by X-ray diffraction patterns collected upon heating
from 92-260 K at ambient pressure. Cubic ice is not observed as is commonly
stated in the literature as resulting from the crystallisation of ASW.
Therefore, ice Isd is the correct terminology for the initial crystallisation
product of ASW.
