Aromatic Carbonyl and Nitro Compounds as Photosensitizers and Their Photophysical Properties in the Tropospheric Aqueous PhaseClick to copy article linkArticle link copied!
- Tamara FelberTamara FelberLeibniz Institute for Tropospheric Research (TROPOS), Atmospheric Chemistry Department (ACD), Permoserstrasse 15, 04318 Leipzig, GermanyMore by Tamara Felber
- Thomas SchaeferThomas SchaeferLeibniz Institute for Tropospheric Research (TROPOS), Atmospheric Chemistry Department (ACD), Permoserstrasse 15, 04318 Leipzig, GermanyMore by Thomas Schaefer
- Lin HeLin HeLeibniz Institute for Tropospheric Research (TROPOS), Atmospheric Chemistry Department (ACD), Permoserstrasse 15, 04318 Leipzig, GermanyMore by Lin He
- Hartmut Herrmann*Hartmut Herrmann*Phone: +49 341 2717 7024; fax: +49 341 2717 99 7024; E-mail: [email protected]Leibniz Institute for Tropospheric Research (TROPOS), Atmospheric Chemistry Department (ACD), Permoserstrasse 15, 04318 Leipzig, GermanyMore by Hartmut Herrmann
Abstract

Secondary organic aerosol formation in the atmospheric aqueous/particulate phase by photosensitized reactions is currently subject to uncertainties. To understand the impact of photosensitized reactions, photophysical and -chemical properties of photosensitizers, kinetic data, and reaction mechanisms of these processes are required. The photophysical properties of acetophenones, benzaldehydes, benzophenones, and naphthalenes were investigated in aqueous solution using laser flash excitation. Quantum yields of excited photosensitizers were determined giving values between 0.06–0.80 at 298 K and pH = 5. Molar absorption coefficients (εmax(3PS*) = (0.8–13) × 104 L mol–1 cm–1), decay rate constants in water (k1st = (9.4 ± 0.5) × 102 to (2.2 ± 0.1) × 105 s–1), and quenching rate constants with oxygen (kq(O2) = (1.7 ± 0.1–4.4 ± 0.4) × 109 L mol–1 s–1) of the excited triplet states were determined at 298 K and pH = 5. Photosensitized reactions of carboxylic acids and alkenes show second-order rate constants in the range of (37 ± 7.0–0.55 ± 0.1) × 104 and (27 ± 5.0–0.04 ± 0.01) × 108 L mol–1 s–1. The results show that different compound classes act differently as a photosensitizer and can be a sink for certain organic compounds in the atmospheric aqueous phase.
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