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Royal Society of Chemistry, Physical Chemistry Chemical Physics, 19(5), p. 4157-4169, 2003

DOI: 10.1039/b308422c

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The nature of the interface and the diffusion coefficient of HCl/ice and HBr/ice in the temperature range 190–205 K

Journal article published in 2003 by Arnaud Aguzzi, Benoît Flückiger, Michel J. Rossi
This paper is available in a repository.
This paper is available in a repository.

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Abstract

We have investigated the structural properties of the near-surface region of various types of HX (X=Cl, Br)-doped H2O ice from a kinetic point of view by monitoring the time dependent [HX] in the interface region using the fast titration reaction XONO2+HX→X2+HNO3. These “dope and probe” experiments reveal that HX is located throughout a well-defined region of thickness I readily available for titration. At 190 K and a dose of 1016 molecules corresponding to one HCl monolayer condensed onto a typically 1 μm thick ice sample, we measured IHCl=90±9, 120±15 and 90±30 nm for single crystalline (SC), condensed (C) and frozen liquid water or bulk (B) ices, respectively, with IHCl increasing by up to a factor of two with a tenfold increase in HCl dose. The corresponding values for HBr at the same temperature are IHBr=20±2, 30±4 and 30±4 nm. In addition, we have determined the bulk diffusion coefficient in bulk ice for HX, DHX, by applying Fick's second law of diffusion that results in values for DHCl and DHBr in the range 5.1·10−14–4.3·10−13 cm2 s−1 and 2.5·10−15–7.0·10−14 cm2 s−1, respectively, depending on the type of ice in the temperature range 190–205 K. The consequences of these results for heterogeneous reactions on ice particles such as Cirrus clouds, contrails and PSC's type II are discussed.