The first steps of iodine gas-to-particle conversion as seen in the lab: constraints on the role of iodine oxides and oxyacids
Authors: Gomez Martin Juan Carlos , Lewis Tom , Kumar Manoj , Plane John , Francisco Joseph , Saiz-Lopez Alfonso 
Published: March 2020

&lt;p&gt;The photooxidation of gas phase iodine-bearing molecules emitted by marine biota leads to intense particle nucleation events in the coastal and polar marine boundary layer&lt;sup&gt;1-3&lt;/sup&gt;. The ubiquity of iodine in the marine atmospheric environment&lt;sup&gt;4-7&lt;/sup&gt; has suggested that this may be a previously unrecognized global source of new aerosol particles&lt;sup&gt;8&lt;/sup&gt;. Atmospheric modeling is required in order to evaluate the importance of this process, but a substantial lack of understanding of the gas-to-particle conversion mechanism is hindering this effort, especially regarding the gas phase chemistry of the nucleating molecules (iodine oxides&lt;sup&gt;9&lt;/sup&gt;&lt;sup&gt;,&lt;/sup&gt;&lt;sup&gt;10&lt;/sup&gt; and/or oxyacids&lt;sup&gt;7&lt;/sup&gt;) and the formation kinetics of molecular clusters. To address this problem, we have conducted new flow tube laboratory experiments where pulsed laser photolysis or continuous broad-band photolysis of I&lt;sub&gt;2&lt;/sub&gt;/O&lt;sub&gt;3&lt;/sub&gt; mixtures&amp;#160; in air are used to generate iodine radicals in the presence of atmospherically representative mixing ratios of water vapor. The molecular reactants and the resulting molecular products are detected by time-resolved VUV laser photo-ionization time-of-flight mass spectrometry. High-level quantum chemistry and master equation calculations and gas kinetics modelling are used to analyse the experimental data. In this presentation we discuss our results and their implications for the interpretation of field meassurements and for the implementatiion of an iodine oxide particle formation mechanism in atmospheric models.&lt;/p&gt;&lt;p&gt;References:&lt;/p&gt;&lt;p&gt;1. Hoffmann, T., O'Dowd, C. D. &amp; Seinfeld, J. H. Iodine oxide homogeneous nucleation: An explanation for coastal new particle production. Geophys. Res. Lett. &lt;strong&gt;28&lt;/strong&gt;, 1949-1952 (2001).&lt;/p&gt;&lt;p&gt;2. McFiggans, G. et al. Direct evidence for coastal iodine particles from Laminaria macroalgae - linkage to emissions of molecular iodine. Atmos. Chem. Phys. &lt;strong&gt;4&lt;/strong&gt;, 701-713 (2004).&lt;/p&gt;&lt;p&gt;3. O'Dowd, C. D. et al. Marine aerosol formation from biogenic iodine emissions. Nature &lt;strong&gt;417&lt;/strong&gt;, 632-636 (2002).&lt;/p&gt;&lt;p&gt;4. Prados-Roman, C. et al. Iodine oxide in the global marine boundary layer. Atmos. Chem. Phys. &lt;strong&gt;15&lt;/strong&gt;, 583-593, doi:10.5194/acp-15-583-2015 (2015).&lt;/p&gt;&lt;p&gt;5. Sch&amp;#246;nhardt, A. et al. Simultaneous satellite observations of IO and BrO over Antarctica. Atmos. Chem. Phys. &lt;strong&gt;12&lt;/strong&gt;, 6565-6580, doi:10.5194/acp-12-6565-2012 (2012).&lt;/p&gt;&lt;p&gt;6. Mahajan, A. S. et al. Concurrent observations of atomic iodine, molecular iodine and ultrafine particles in a coastal environment. Atmos. Chem. Phys. &lt;strong&gt;10&lt;/strong&gt;, 27227-27253 (2010).&lt;/p&gt;&lt;p&gt;7. Sipil&amp;#228;, M. et al. Molecular-scale evidence of aerosol particle formation via sequential addition of HIO3. Nature &lt;strong&gt;537&lt;/strong&gt;, 532-534, doi:10.1038/nature19314 (2016).&lt;/p&gt;&lt;p&gt;8. Saiz-Lopez, A. et al. Atmospheric Chemistry of Iodine. Chem. Rev. &lt;strong&gt;112&lt;/strong&gt;, 1773&amp;#8211;1804, doi:DOI: 10.1021/cr200029u (2012).&lt;/p&gt;&lt;p&gt;9. G&amp;#243;mez Mart&amp;#237;n, J. C. et al. On the mechanism of iodine oxide particle formation. Phys. Chem. Chem. Phys. &lt;strong&gt;15&lt;/strong&gt;, 15612-15622, doi:10.1039/c3cp51217g (2013).&lt;/p&gt;&lt;p&gt;10. Saunders, R. W., Mahajan, A. S., G&amp;#243;mez Mart&amp;#237;n, J. C., Kumar, R. &amp; Plane, J. M. C. Studies of the Formation and Growth of Aerosol from Molecular Iodine Precursor. Z. Phys. Chem. &lt;strong&gt;224&lt;/strong&gt;, 1095-1117 (2010).&lt;/p&gt;