Oxidation of aqueous bromide into reactive, gas-phase bromine species has been of interest since the 1980’s, when the presence of bromine in the Arctic boundary layer was linked to ozone depletion events. We have investigated two different mechanisms for Br2 release from sea ice. We have shown that nitrate in sea ice can photolyze to produce OH, which can go on to form gas-phase Br2. This reaction is analogous to a known reaction that occurs in the aqueous phase. We have also investigated Br2 production from a heterogeneous reaction between gas-phase ozone and sea ice/seawater. We have determined ozone’s reactive uptake coefficient, and have shown how it varies with temperature, bromide concentration, ozone concentration and acidity. We have been able to decouple the bulk aqueous chemistry that occurs from the Langmuir-Hinshelwood surface chemistry, and quantify the relative contribution of each.
| Identifer | oai:union.ndltd.org:TORONTO/oai:tspace.library.utoronto.ca:1807/18970 |
| Date | 16 February 2010 |
| Creators | Oldridge, T. Nathan William |
| Contributors | Abbatt, Jonathan P. D. |
| Source Sets | University of Toronto |
| Language | en_ca |
| Detected Language | English |
| Type | Thesis |
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