The chemical interaction of (i) HCl (ii) NH3, and (iii) HCl + NH3 with crys
talline ice has been examined as a function of temperature (T = 80-150 K) u
tilizing FTIR spectroscopy. The infrared spectra reveal the formation of io
nic hydrates for HCl and molecular hydrates for NH3. The acid-base reaction
leads to the formation of the ammonium ion, NH4+. While it is produced to
a limited extent between 80 and 140 K, NH4+ is a dominant species above 140
K. All species appear as lower amorphous hydrates for T = 80-140 K. Dramat
ic changes in the spectra occur above 140 K as higher crystalline hydrates
are formed. This temperature coincides with the amorphous to crystalline ph
ase transformation of ice. This change appears to be due to a greater numbe
r of water molecules on the surface that are available for hydration and cr
ystallization.