RATE CONSTANTS FOR INTERACTION OF 1O21Δg) WITH AZIDE ION IN WATER

Abstract— The rate constant for quenching of ¹O₂ by azide ion in water was determined to be (5.0 ± 0.4) × 10⁸ M ⁻¹ s⁻¹ using a variety of sensitizers (including humic acids) and ¹O₂ acceptors. The apparent second-order rate constant decreases with pH below pH 5.5 in accordance with the protonation of azide ion to form hydrazoic acid (p K _a= 4.6). Quenching by hydrazoic acid is at least 2 orders of magnitude slower than by azide ion. Greater than 99% of all interactions between ¹O₂ and azide ion involve physical quenching rather than chemical reaction. Humic acid triplets are not significantly quenched by azide ion at concentrations less than 2 m M , allowing azide ion quenching to be used as a diagnostic test for the intermediacy of ¹O₂ in photosensitized oxidations in natural surface waters.