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Interaction of hydrogen chloride with an ultrathin ice film. Observation of adsorbed and absorbed states

Journal Article · · Journal of Physical Chemistry; (United States)
DOI:https://doi.org/10.1021/j100074a026· OSTI ID:7267319
;  [1]
  1. Univ. of Minnesota, Minneapolis, MN (United States)

With the objective of gaining insight into how heterogeneous reactions occur in the Antarctic stratosphere, we have initiated a program to study the adsorption and reaction of simple molecules on model polar stratospheric cloud surfaces. In this work, the temperature-programmed desorption of hydrogen chloride from ultrathin (5-20 monolayers thick) water films is described. Two distinct HCl desorption states, designated [alpha]- and [beta]-HCl, are observed at 140 and 180 K, respectively. Water sublimation occurs at 180 K and is concurrent with [beta]-HCl evolution. [beta]-HCl, which is formed exclusively at low HCl exposures, is derived from the thin film bulk, while [alpha]-HCl is associated with an adsorbed state. [beta]-HCl is assigned to the sublimation of a stoichiometric phase of HCl and water, probably HCl-6H[sub 2]O, and [alpha]-HCl is assigned to the thermal desorption of HCl from the hexahydrate surface. Desorption spectra of HCl from ice-d[sub 2] show that H-D exchange between HCl and D[sub 2]O is much less than would be expected for a dissociatively adsorbed state of HCl. The [alpha] state is therefore assigned to molecularly adsorbed HCl. 38 refs., 11 figs.

OSTI ID:
7267319
Journal Information:
Journal of Physical Chemistry; (United States), Journal Name: Journal of Physical Chemistry; (United States) Vol. 98:23; ISSN JPCHAX; ISSN 0022-3654
Country of Publication:
United States
Language:
English