Kinetics of the reaction of CF3CHO with OH between 204 K and 361 K
Fabienne Baumann1, Christin Fernholz1, Jos Lelieveld1
1Max-Planck-Institute for Chemistry, Division of Atmospheric Chemistry, 55128 Mainz, Germany. fabienne.baumann@mpic.de.
Abstract:
Trifluoroacetaldehyde (CF3CHO) is formed in the atmosphere by the oxidation of a number of fluorinated, organic compounds of anthropogenic origin. The reaction of CF3CHO with the OH radical is a potential source of atmospheric trifluoroacetic acid (TFA) which is a highly persistent, water-soluble compound that may accumulate in aquatic ecosystems and for which uncertainty about its sources, fate, and potential ecological impact persists. In light of growing concerns about the impact of TFA, we present the first study of the temperature dependence of the rate coefficient for the title reaction over the atmospherically relevant temperature range of 204 K to 361 K. Rate coefficients were determined using pulsed laser photolysis-pulsed laser induced fluorescence (PLP-PLIF) and direct concentration measurements via Fourier Transform Infrared (FTIR) spectroscopy, as well as relative rate experiments in an atmospheric simulation chamber using ethane (C2H6) as a reference compound. The rate coefficient (k1) obtained with PLP-PLIF at room temperature is (5.8 ± 0.5) × 10-13 cm3 molecule-1 s-1. The temperature dependence is described by the expression k1(T) = (3.8 ± 0.2) × 10-13 × (T/300)2 × exp[(131 ± 16)/T]. The relative-rate experiments showed that the rate coefficient obtained can be significantly biased by reactions of the CF3O radical with CF3CHO and/or C2H6 and also reactions of CF3CHO with HO2. Based on the expression of k1 given above, the lifetime of CF3CHO with respect to reaction with the OH radical varies from 22 days at the surface (T ∼ 300 K) to 30 days in the upper troposphere (T ∼ 220 K).
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