Rate Coefficients for the Gas-Phase Reaction of ( E)- and ( Z)-CFCF═CFCF with the OH Radical and Cl-Atom.

J Phys Chem A

Earth System Research Laboratory, Chemical Sciences Division , National Oceanic and Atmospheric Administration , 325 Broadway , Boulder , Colorado 80305-3328 , United States.

Published: June 2019

The rate coefficients, k, for the gas-phase reaction of the OH radical and Cl-atom with ( E)- and ( Z)-CFCF═CFCF were measured using a relative rate technique over a range of temperature (240-375 K) and bath gas pressure (50-630 Torr, He). The obtained rate coefficients were found to be independent of pressure under these conditions. The obtained rate coefficients for the reaction of Cl-atom with ( E)- and ( Z)-CFCF═CFCF at 296 K were k(296 K) = (7.23 ± 0.3) × 10 cm molecule s and k(296 K) = (6.70 ± 0.3) × 10 cm molecule s, respectively, with the temperature dependence described by the Arrhenius expressions: k( T) = (3.47 ± 0.35) × 10 exp[(210 ± 25)/ T] cm molecule s and k( T) = (3.37 ± 0.35) × 10 exp[(199 ± 25)/ T] cm molecule s. The rate coefficients for the OH radical reaction with ( E)- and ( Z)-CFCF═CFCF were found to be k(296-375 K) = (4.34 ± 0.45) × 10 cm molecule s and k(296-375 K) = (3.30 ± 0.35) × 10 cm molecule s, respectively. The quoted rate coefficient uncertainties are 2σ (95% confidence level) and include estimated systematic errors. The rate coefficients for the reaction of OH with a mixture of the two stereoisomers were determined using a pulsed laser photolysis-laser-induced fluorescence (PLP-LIF) technique for comparison with previous kinetic measurements using stereoisomer mixtures. The effective rate coefficient for the 0.7/0.3 ( E)/( Z) stereoisomer sample was found to be nearly independent of temperature over the range 222-375 K with a value of (4.47 ± 0.36) × 10 cm molecule s. The atmospheric lifetimes for ( E)- and ( Z)-CFCF═CFCF due to OH-reactive loss are estimated to be 25 and 35 days, respectively. The lifetime-corrected radiative efficiencies (W m ppb) and 100 year time horizon global warming potentials derived in this work are 0.05 and 1.2 for ( E)-CFCF═CFCF and 0.13 and 4.1 for ( Z)-CFCF═CFCF. The photochemical ozone creation potentials for ( E)- and ( Z)-CFCF═CFCF are estimated to be 2.5 and 2.1, respectively.

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http://dx.doi.org/10.1021/acs.jpca.9b03095DOI Listing

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