Authors
Mads P Sulbaek Andersen, Morten Frausig, Thomas Rosenoern, Casper Vindahl Jensen, Timothy J Wallington, Ole John Nielsen
Published in
Physical chemistry chemical physics : PCCP. Aug 25, 2026. Epub Aug 25, 2026.
Abstract
Smog chamber experiments were conducted to investigate the Cl atom and OH radical reactions with CF3CH(OH)CH(OH)CF3 and the photolysis of CF3C(O)C(O)CF3. The initial reaction of CF3CH(OH)CH(OH)CF3 leads to formation of α-hydroxyalkyl radicals which, in the presence of O2, are converted into CF3C(O)CH(OH)CF3, a suspected oxidation product of CF3CHCHCF3 (HFO-1336mzz). Rate constants of k(Cl + CF3CH(OH)CH(OH)CF3) = (5.2 ± 0.85) × 10-14 and k(OH + CF3CH(OH)CH(OH)CF3) = (1.1 ± 0.3) × 10-13 cm3 molecule-1 s-1 were measured using relative rate techniques in 700 Torr of air/N2 diluents at 296 ± 2 K. The rate constant for reaction of Cl atoms with CF3C(O)CH(OH)CF3 was established as k(Cl + CF3C(O)CH(OH)CF3) = (3.0 ± 0.6) × 10-14 cm3 molecule-1 s-1. Oxidation of CF3C(O)CH(OH)CF3 gives CF3C(O)C(O)CF3 in a yield of unity. IR spectra (cross sections) of CF3CH(OH)CH(OH)CF3, CF3C(O)CH(OH)CF3, and CF3C(O)C(O)CF3 are reported for the first time. The UV spectrum of CF3C(O)C(O)CF3 is reported and the photolysis rates were studied at 254 nm (UV-C) and 330 nm (broad band UV-B) radiation. Total quantum yields of (0.72 ± 0.10, 254 nm) and (0.010 ± 0.002, 330 nm) were established. Photolysis gives CF3C(O) as a significant photofragment. The dominant atmospheric fate of CF3C(O)C(O)CF3 is expected to be photolysis. This study provides a comprehensive description of the atmospheric chemistry and fate of CF3CH(OH)CH(OH)CF3, CF3C(O)CH(OH)CF3, and CF3C(O)C(O)CF3. The products and the oxidation mechanism are discussed in the context of the atmospheric degradation of 3rd generation CFC-replacement compounds.
PMID:
42639909
Bibliographic data and abstract were imported from PubMed on 25 Aug 2026.
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