Atmospheric chemistry of iodine anions: elementary reactions of I-, IO-, and IO2- with ozone studied in the gas-phase at 300 K using an ion trap

Phys Chem Chem Phys. 2018 Nov 21;20(45):28606-28615. doi: 10.1039/c8cp05721d.

Abstract

Using a radio-frequency ion trap to study ion-molecule reactions under isolated conditions, we report a direct experimental determination of reaction rate constants for the sequential oxidation of iodine anions by ozone at room temperature (300 K). The results are R1: I- + O3 → IO- + O2, k1 = (7 ± 2) × 10-12 cm3 s-1; R2: IO- + O3 → IO2- + O2, k2 = (10 ± 2) × 10-9 cm3 s-1; R3: IO2- + O3 → IO3- + O2, k3 = (16 ± 2) × 10-9 cm3 s-1. More oxidized forms such as IO4- and IO5- were not observed. Additionally, we performed quantum chemical calculations to elucidate the energetics of these oxidation reactions.