Kinetics of the reaction of CF<sub>3</sub>CHO with OH between 204 K and 361 K

Trifluoroacetaldehyde (CF<sub>3</sub>CHO) is formed in the atmosphere by the oxidation of a number of fluorinated, organic compounds of anthropogenic origin. The reaction of CF<sub>3</sub>CHO 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 <i>via</i> Fourier Transform Infrared (FTIR) spectroscopy, as well as relative rate experiments in an atmospheric simulation chamber using ethane (C<sub>2</sub>H<sub>6</sub>) as a reference compound. The rate coefficient (<i>k</i><sub>1</sub>) obtained with PLP-PLIF at room temperature is (5.8 ± 0.5) × 10<sup>-13</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup>. The temperature dependence is described by the expression <i>k</i><sub>1</sub>(<i>T</i>) = (3.8 ± 0.2) × 10<sup>-13</sup> × (<i>T</i>/300)<sup>2</sup> × exp[(131 ± 16)/<i>T</i>]. The relative-rate experiments showed that the rate coefficient obtained can be significantly biased by reactions of the CF<sub>3</sub>O radical with CF<sub>3</sub>CHO and/or C<sub>2</sub>H<sub>6</sub> and also reactions of CF<sub>3</sub>CHO with HO<sub>2</sub>. Based on the expression of <i>k</i><sub>1</sub> given above, the lifetime of CF<sub>3</sub>CHO with respect to reaction with the OH radical varies from 22 days at the surface (<i>T</i> ∼ 300 K) to 30 days in the upper troposphere (<i>T</i> ∼ 220 K).

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Publication Details

Journal
Physical Chemistry Chemical Physics
Published
2025-01-01
DOI
https://doi.org/10.1039/d5cp02871j
Citations
2
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
2.60

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article

Kinetics of the reaction of CF3CHO with OH between 204 K and 361 K

Jos Lelieveld, Christin Fernholz, John N. Crowley, Fabienne Baumann
2 citations
Physical Chemistry Chemical Physics
Atmospheric chemistry and aerosols
2.60
article

Kinetics of the reaction of CF3CHO with OH between 204 K and 361 K

Jos Lelieveld, Christin Fernholz, John N. Crowley, Fabienne Baumann
article en
2 citations

Abstract

Trifluoroacetaldehyde (CF<sub>3</sub>CHO) is formed in the atmosphere by the oxidation of a number of fluorinated, organic compounds of anthropogenic origin. The reaction of CF<sub>3</sub>CHO 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 <i>via</i> Fourier Transform Infrared (FTIR) spectroscopy, as well as relative rate experiments in an atmospheric simulation chamber using ethane (C<sub>2</sub>H<sub>6</sub>) as a reference compound. The rate coefficient (<i>k</i><sub>1</sub>) obtained with PLP-PLIF at room temperature is (5.8 ± 0.5) × 10<sup>-13</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup>. The temperature dependence is described by the expression <i>k</i><sub>1</sub>(<i>T</i>) = (3.8 ± 0.2) × 10<sup>-13</sup> × (<i>T</i>/300)<sup>2</sup> × exp[(131 ± 16)/<i>T</i>]. The relative-rate experiments showed that the rate coefficient obtained can be significantly biased by reactions of the CF<sub>3</sub>O radical with CF<sub>3</sub>CHO and/or C<sub>2</sub>H<sub>6</sub> and also reactions of CF<sub>3</sub>CHO with HO<sub>2</sub>. Based on the expression of <i>k</i><sub>1</sub> given above, the lifetime of CF<sub>3</sub>CHO with respect to reaction with the OH radical varies from 22 days at the surface (<i>T</i> ∼ 300 K) to 30 days in the upper troposphere (<i>T</i> ∼ 220 K).

Physical Chemistry Chemical PhysicsVol. 27(36)
Max Planck Institute for Chemistry (DE)
AstraZeneca, Max-Planck-Gesellschaft
Openalex Percentile: Top 10%
Atmospheric chemistry and aerosols
2.60
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