Kinetic Studies of Imidazoles in Tropospheric Aqueous-Phase Chemistry: Photochemistry of Imidazole-2-carboxaldehyde and Oxidation Reaction with Hydroxyl Radicals
Abstract
The formation of imidazoles via the reaction of dicarbonyls with nitrogen containing compounds in the atmosphere and their potential to act as photosensitizers possibly initiating secondary organic aerosol (SOA) growth is a field of increasing activity. A recent field study quantified and qualified imidazoles in ambient aerosol samples from Europe and China. However, kinetic data and mechanisms of particle-phase reactions involving imidazoles are still scarce. In this study, kinetic measurements were investigated using laser flash photolysis-laser long path absorption (LFP-LLPA). Quenching rate constants for the reactions of the excited triplet state of imidazole-2-carboxaldehyde (IC) with bromide anion (kq = (1.6 ± 0.3) × 107 L mol-1 s-1), oxygen (kq = (2.5 ± 0.07) × 109 L mol-1 s-1), and formic acid (kq = (8.8 ± 0.5) × 109 L mol-1 s-1) are determined. IC is efficiently quenched by oxygen and formic acid. Furthermore, the quenching reaction of IC with isopropanol is investigated and compared to the reaction with formic acid to propose a preliminary mechanism of photosensitized reactions of IC with organic compounds. It is suggested that an electron transfer occurs, as it is the case for inorganics. Furthermore, rate constants of hydroxyl (OH) radical oxidation reactions with different imidazoles were determined. Following rate constants are obtained at a temperature of 298 K: k(imidazole-2-carboxaldehyde) = (3.3 ± 1.3) × 109 L mol-1 s-1, k(1-methylimidazolium hydrogen sulfate) = (2.7 ± 0.2) × 109 L mol-1 s-1, k(2-methylimidazole) = (5.4 ± 0.2) × 109 L mol-1 s-1, k(4(5)-methylimidazole) = (5.1 ± 0.3) × 109 L mol-1 s-1, k(1-ethylimidazole) = (3.0 ± 0.3) × 109 L mol-1 s-1, k(2-ethylimidazole) = (5.0 ± 0.2) × 109 L mol-1 s-1. The OH radical reaction rate constants of imidazoles are in the same range as for non-heteroaromatic compounds. Therefore, imidazoles can be expected to exist just for a limited time in the atmosphere (τ = 16 - 29 hours) after their formation. The received kinetic data will be added into model studies to evaluate the importance of aqueous-phase chemistry of imidazoles for atmospheric processes as well as the impact of photosensitized reactions on atmospheric particles possibly contributing to SOA formation.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2017
- Bibcode:
- 2017AGUFM.A43G2545F
- Keywords:
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- 0317 Chemical kinetic and photochemical properties;
- ATMOSPHERIC COMPOSITION AND STRUCTURE;
- 0320 Cloud physics and chemistry;
- ATMOSPHERIC COMPOSITION AND STRUCTURE;
- 0365 Troposphere: composition and chemistry;
- ATMOSPHERIC COMPOSITION AND STRUCTURE;
- 3311 Clouds and aerosols;
- ATMOSPHERIC PROCESSES