Abstract
Long path length FTIR-smog chamber techniques were used to study the title reactions in 650 Torr of N2, oxygen, or air diluent at 296 ± 3 K. Values of k(Cl + (Z)-CF2HCF = CHCl)═(6.6 ± 0.7) × 10−11 and k(OH + (Z)-CF2HCF═CHCl)═(4.1 ± 0.7) × 10−12 cm3 molecule−1 s−1 were measured. The IR spectrum of (Z)-CF2HCF═CHCl is reported. The atmospheric lifetime of (Z)-CF2HCF═CHCl is determined by the reaction with OH and is approximately 2.8 days. Reaction of (Z)-CF2HCF═CHCl with Cl atoms gives HC(O)Cl and CF2HC(O)F as major primary products. Under environmental conditions, the OH radical initiated oxidation gives CF2HC(O)F and HC(O)Cl in yields of (98 ± 8)% and (100 ± 4)%, respectively. Accounting for non-uniform horizontal and vertical mixing leads to a 100-year time-horizon global warming potential value for (Z)-CF2HCF═CHCl of essentially zero.
Original language | English |
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Journal | International Journal of Chemical Kinetics |
ISSN | 0538-8066 |
DOIs | |
Publication status | E-pub ahead of print - 2024 |
Bibliographical note
Publisher Copyright:© 2024 The Author(s). International Journal of Chemical Kinetics published by Wiley Periodicals LLC.
Keywords
- HFO
- hydrofluoroolefin
- kinetics
- ozone
- smog chamber
- stratosphere