We have shown that water adsorbed to the (001) plane of muscovite mica has
an infrared spectrum consistent with a bonding network that is more structu
red than that found in bulk water. Isotherms taken at temperatures ranging
from near the ice melting point to room temperature suggest that water wets
mica incompletely. Additionally, we find that the enthalpy and entropy of
the adsorbed water molecules imply a strongly bound first layer. Both entha
lpy and entropy approach the bulk values as the thickness of the adsorbed l
ayer increases.