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Kinetics of CF 3 CH 2 OCH 3 (HFE-263fb2), CHF 2 CF 2 CH 2 OCH 3 (HFE-374pcf), and CF 3 CF 2 CH 2 OCH 3 (HFE-365mcf3) with OH radicals, IR absorption cross sections, and global warming potentials.

Sergio BlázquezSara EspinosaMaría AntiñoloJosé AlbaladejoElena Jiménez
Published in: Physical chemistry chemical physics : PCCP (2022)
Hydrofluoroethers (HFEs), such as CF 3 CH 2 OCH 3 (HFE-263fb2), CHF 2 CF 2 CH 2 OCH 3 (HFE-374pcf), and CF 3 CF 2 CH 2 OCH 3 (HFE-365mcf3), have been proposed in the last few decades as the third-generation replacements for perfluorocarbons (PFCs) and hydrofluorocarbons (HFCs) because of their zero stratospheric ozone depletion potentials and relatively low global warming potentials (GWPs). These GWPs depend on the radiative efficiency (RE) and the atmospheric lifetime ( τ OH ) of HFEs due to the reaction with hydroxyl (OH) radicals. The temperature and pressure dependencies of the OH-rate coefficient ( k OH ( T )) for HFE-263fb2, HFE-374pcf, and HFE-365mcf3 are not known. Therefore, in this paper, we present the first study on the temperature (263-353 K) and pressure (50-500 torr of helium) dependence of k OH ( T ) for the titled HFEs. No pressure dependence of k OH ( T ) was observed in the investigated range. From k OH (298 K), estimated τ OH are 17 days (for HFE-263fb2), 12 days (for HFE-374pcf), and 13 days (for HFE-365mcf3). The observed T -dependencies of k OH ( T ) (in cm 3 molecule -1 s -1 ) are well described by (3.88 ± 0.89) × 10 -12 exp[-(508 ± 69)/ T ] for HFE-263fb2, (2.81 ± 0.33) × 10 -12 exp[-(312 ± 35)/ T ] for HFE-374pcf, and (2.60 ± 0.31) × 10 -12 exp[-(319 ± 35)/ T ] for HFE-365mcf3. A correlation between log  k OH (298 K) and the activation energy ( E a ) of the process is presented, allowing the prediction of E a for OH-reactions with other HFEs, exclusively investigated at room temperature. In addition to the kinetic measurements, the infrared absorption cross sections of HFE-263fb2, HFE-374pcf, and HFE-365mcf3 were determined between 520 and 3100 cm -1 . Lifetime corrected REs and GWPs relative to CO 2 at 100 years' time horizon were reexamined. The impact of the investigated HFEs on the radiative forcing of climate change would be negligible.
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