Solid layers of interest for the chemistry of polar stratospheric clouds ar
e investigated. Mixtures of covalent N2O5 and water in various molar ratios
are deposited from the vapor phase on a cold 12 K substrate. By repeatedly
recording Fourier transform infrared spectra of the samples during gradual
warmup to 200 K over a period of several hours the hydrolysis process can
be followed. At each concentration the process is found to proceed in sever
al distinct steps with sharp temperature thresholds. In samples containing
only small amounts of water the covalent N2O5 is first, at around 110 K, co
nverted to an ionic nitronium nitrate, and only in a subsequent step does N
O2+NO3- react to form nitric acid. (C) 2001 American Institute of Physics.