Volume 102, Issue 3 pp. 518-526
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D. Proton transfer in complex systems, liquids and biological systems: Proton transfer reactions at the surface of Ice. Heterogeneous reactions involved in stratospheric ozone depletion

Roberto Bianco

Roberto Bianco

Department of Chemistry and Biochemistry

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Bradley J. Gertner

Bradley J. Gertner

Department of Chemistry and Biochemistry

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309-0215, USA

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James T. Hynes

James T. Hynes

Department of Chemistry and Biochemistry

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First published: 22 June 2010
Citations: 39

Abstract

Two heterogeneous reactions on an ice surface that are relevant in connection with stratospheric ozone depletion are discussed theoretically: the hydrolysis of chlorine nitrate, ClONO2, to produce HOC1 and HNO3, and the acid ionization of hydrochloric acid HC1. For the former, a recently proposed proton transfer mechanism actively involving the ice lattice is supported by examination of the ClONO2 hydrolysis energetics when proton transfer is prevented. For the latter, a previously proposed picture of facile HCl ionization at, but not on, the ice surface is supported by the results of a quantum treatment of the proton and of a model investigation of the free energetics of ionization atop the ice surface.

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