Measurements of Radical Reactivity with an Imine, (CF3)2CNH: Rate Constants for Chlorine Atoms and Hydroxyl Radicals and the Global Warming Potential

The rate constant <i>k</i><sub>OH</sub> for the reaction of 1,1,1,3,3,3-hexafluoroprop-2-imine with OH radicals was measured relative to two reference compounds, CH<sub>3</sub>F and CH<sub>3</sub>CHF<sub>2</sub>, to be <i>k</i><sub>OH</sub> = (4.2 ± 1.1) × 10<sup>-14</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup> at 295 K. This implies an atmospheric lifetime with respect to consumption by OH of 0.75 years. Reaction with Cl atoms yielded <i>k</i><sub>Cl</sub> = (7.9 ± 1.7) × 10<sup>-16</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup> at 295 K, and reaction with O<sub>3</sub> has an upper limit of <i>k</i><sub>O3</sub> < 4 × 10<sup>-23</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup>, so that the atmospheric consumption by Cl and O<sub>3</sub> is negligibly slow. Absolute infrared cross sections of the imine yield a radiative efficiency of 0.34 W m<sup>-2</sup> ppb<sup>-1</sup>, which is corrected to 0.23 W m<sup>-2</sup> ppb<sup>-1</sup> for the effects of atmospheric lifetime. The imine's corresponding 100-year global warming potential is 64 ± 19. This value is an upper limit, given that heterogenous atmospheric removal paths, such as hydrolysis in water droplets, are not included.

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Journal
Molecules
Published
2026-01-26
DOI
https://doi.org/10.3390/molecules31030424
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

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article

Measurements of Radical Reactivity with an Imine, (CF3)2CNH: Rate Constants for Chlorine Atoms and Hydroxyl Radicals and the Global Warming Potential

Paul Marshall, Savi Savi
Molecules
Atmospheric chemistry and aerosols
article

Measurements of Radical Reactivity with an Imine, (CF3)2CNH: Rate Constants for Chlorine Atoms and Hydroxyl Radicals and the Global Warming Potential

Paul Marshall, Savi Savi
article en

Abstract

The rate constant <i>k</i><sub>OH</sub> for the reaction of 1,1,1,3,3,3-hexafluoroprop-2-imine with OH radicals was measured relative to two reference compounds, CH<sub>3</sub>F and CH<sub>3</sub>CHF<sub>2</sub>, to be <i>k</i><sub>OH</sub> = (4.2 ± 1.1) × 10<sup>-14</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup> at 295 K. This implies an atmospheric lifetime with respect to consumption by OH of 0.75 years. Reaction with Cl atoms yielded <i>k</i><sub>Cl</sub> = (7.9 ± 1.7) × 10<sup>-16</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup> at 295 K, and reaction with O<sub>3</sub> has an upper limit of <i>k</i><sub>O3</sub> < 4 × 10<sup>-23</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup>, so that the atmospheric consumption by Cl and O<sub>3</sub> is negligibly slow. Absolute infrared cross sections of the imine yield a radiative efficiency of 0.34 W m<sup>-2</sup> ppb<sup>-1</sup>, which is corrected to 0.23 W m<sup>-2</sup> ppb<sup>-1</sup> for the effects of atmospheric lifetime. The imine's corresponding 100-year global warming potential is 64 ± 19. This value is an upper limit, given that heterogenous atmospheric removal paths, such as hydrolysis in water droplets, are not included.

MoleculesVol. 31(3)
University of North Texas (US)
National Science Foundation, U.S. Department of Energy, Office of Science, Basic Energy Sciences
Clean water and sanitation
Openalex Percentile: Top 83%
Atmospheric chemistry and aerosols
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Measurements of Radical Reactivity with an Imine, (CF3)2CNH: Rate Constants for Chlorine Atoms and Hydroxyl Radicals and the Global Warming Potential — Paul Marshall, Savi Savi · Molecules (2026) | TGRS Research Map | TGRS