Abstract
We report on an experimental characterization of the isolated reaction of hydrated iodide I(H 2O) - with ozone O 3 at room temperature performed using a radio-frequency ion trap combined with a quadrupole mass spectrometer. Contrary to the oxidation reaction of the bare I - ion, the hydrated iodide I(H 2O) - primarily reacts to form I - and IO 2 - with significant absolute reaction rate constants of 2.0 ± 0.3 × 10 -10 cm 3 molecule -1 s -1 and 2.5 ± 0.3 × 10 -10 cm 3 molecule -1 s -1 while direct pathways to IO - and IO 3 - are much weaker. Quantum chemical calculations indicate that in aqueous phase and for atmospherically relevant temperatures, the presence of hydrated iodides are favored over bare I - ions, thus suggesting that the chemistry of the hydrated ions is relevant for understanding and modeling atmospheric processes at the air-water interface.
Originalsprog | Engelsk |
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Tidsskrift | Physical Chemistry Chemical Physics |
Vol/bind | 21 |
Nummer | 32 |
Sider (fra-til) | 17546-17554 |
Antal sider | 9 |
ISSN | 1463-9076 |
DOI | |
Status | Udgivet - aug. 2019 |