Atmos. Chem. Phys., 16, 12703–12713, 2016 www.atmos-chem-phys.net/16/12703/2016/ doi:10.5194/acp-16-12703-2016 © Author(s) 2016. CC Attribution 3.0 License. Photolysis of frozen iodate salts as a source of active iodine in the polar environment Óscar Gálvez1,a, M. Teresa Baeza-Romero2, Mikel Sanz2,b, and Alfonso Saiz-Lopez3 1Departamento de Física Molecular, Instituto de Estructura de la Materia, IEM-CSIC, 28006 Madrid, Spain 2Escuela de Ingeniería Industrial, Universidad de Castilla-La Mancha, 45071 Toledo, Spain 3Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, 28006 Madrid, Spain anow at: Departamento de Física Interdisciplinar, Facultad de Ciencias, Universidad Nacional de Educación a Distancia, 28040 Madrid, Spain bnow at: Institute of Physical Chemistry Rocasolano, CSIC, 28006 Madrid, Spain Correspondence to: Óscar Gálvez (
[email protected],
[email protected]) Received: 15 September 2015 – Published in Atmos. Chem. Phys. Discuss.: 15 October 2015 Revised: 22 September 2016 – Accepted: 26 September 2016 – Published: 12 October 2016 Abstract. Reactive halogens play a key role in the oxida- 1 Introduction tion capacity of the polar troposphere. However, sources and mechanisms, particularly those involving active iodine, are still poorly understood. In this paper, the photolysis of an Atmospheric iodine compounds are present in the marine atmospherically relevant frozen iodate salt has been experi- and polar boundary layers (Saiz-Lopez et al., 2012), where mentally studied using infrared (IR) spectroscopy. The sam- they play a relevant role in catalytic ozone destruction (Saiz- ples were generated at low temperatures in the presence of Lopez et al., 2007b; Read et al., 2008), and they could also different amounts of water.