Issue 15, 2011

HCl adsorption on ice at low temperature: a combined X-ray absorption, photoemission and infrared study

Abstract

The reaction of HCl on water ice provides a simple case for understanding dissociation and proton transfer in this non-optimal, incomplete solvation environment, playing a central role in atmospheric chemistry. This reaction has been repeatedly reported as thermally dependent, whereas the theoretical models predict a spontaneous dissociation. We examine the adsorption of HCl on ice at low temperature (50 K and 90 K) via a combination of near-edge X-ray absorption spectroscopy (NEXAFS) at the chlorine L-edge, photoemission (XPS and UPS), and reflection-adsorption infrared spectroscopy (FT-RAIRS). We show the complete dissociation of HCl into Cl and H+ through 3 hydrogen bonds, predominantly by direct reaction with water (80%) and by self-solvation (20%), in full agreement with the prediction of a barrierless process.

Graphical abstract: HCl adsorption on ice at low temperature: a combined X-ray absorption, photoemission and infrared study

Supplementary files

Article information

Article type
Paper
Submitted
13 Dec 2010
Accepted
17 Feb 2011
First published
15 Mar 2011

Phys. Chem. Chem. Phys., 2011,13, 7142-7148

HCl adsorption on ice at low temperature: a combined X-ray absorption, photoemission and infrared study

P. Parent, J. Lasne, G. Marcotte and C. Laffon, Phys. Chem. Chem. Phys., 2011, 13, 7142 DOI: 10.1039/C0CP02864A

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