Reaction rates for the conversion of ice nanocrystals within 3-D arrays to
mono-, tetra- and hexahydrates of HCl have been determined for different HC
l(g) exposure levels and reaction temperatures. The extent of reaction was
monitored and the hydrate product identified, using transmission FT-IR spec
troscopy. The direct method of observation provides evidence that HCl diffu
sion through the hydrate encrusting the ice particles is often the rate-lim
iting factor in the conversion of ice to a hydrate phase. Values for the HC
l diffusion coefficient for the mono- and tetrahydrate are reported. By com
parison, diffusion of HCl in ice is considered to be a nonfactor in most ic
e-HCl interactions.