2016
DOI: 10.1021/acs.jpca.6b05305
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Relative Rate and Product Studies of the Reactions of Atomic Chlorine with Tetrafluoroethylene, 1,2-Dichloro-1,2-difluoroethylene, 1,1-Dichloro-2,2-difluoroethylene, and Hexafluoro-1,3-butadiene in the Presence of Oxygen

Abstract: Rate coefficients k 1–k 3 have been measured for Cl atom reactions with CF2CF2, CFClCFCl, and CCl2CF2 relative to k 4 for CF2CF–CFCF2 at 293 ± 2 K. k 4 was remeasured relative to Cl + ethane. Cl was generated by UV photolysis of Cl2, and other species were monitored by FT-IR spectroscopy. The measurements yield k 1 = (6.6 ± 1.0) × 10–11, k 2 = (6.5 ± 1.0) × 10–11, and k 3 = (7.1 ± 1.1) × 10–11 cm3 molecule–1 s–1, respectively, and k 4 = (8.0 ± 1.2) × 10–11 cm3 molecule–1 s–1 is proposed. These results are… Show more

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Cited by 5 publications
(5 citation statements)
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“… τ = 1 k 0.25em false( overall false) × false[ OH false] where k (overall) is the overall rate coefficient of the reaction studied with OH radicals, and [OH] is the global average concentration of OH radicals. The concentration of OH radicals is considered to be 1.0 × 10 6 molecules cm –3 . , …”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“… τ = 1 k 0.25em false( overall false) × false[ OH false] where k (overall) is the overall rate coefficient of the reaction studied with OH radicals, and [OH] is the global average concentration of OH radicals. The concentration of OH radicals is considered to be 1.0 × 10 6 molecules cm –3 . , …”
Section: Resultsmentioning
confidence: 99%
“…The concentration of OH radicals is considered to be 1.0 × 10 6 molecules cm −3 . 57,58 The atmospheric lifetimes (τ) of A, B, and C at 298.15 K are 36.75, 35.11, and 17.45 days, respectively. This indicates that A and B have more chance than C to interact directly with human beings and the environment when emitted in the atmosphere as it will remain in the atmosphere for a longer period.…”
Section: Atmospheric Implications 341 Atmospheric Lifetimes (τ)mentioning
confidence: 99%
“…We use IR spectroscopy to probe the chemistry initiated by photolytically generated chlorine atoms, evaluate reaction kinetics, identify products and quantify product yields. Our apparatus has been described in detail elsewhere [12]. In overview, mixtures of HFB and molecular chlorine diluted in a large excess of argon bath gas at 1 bar pressure and room temperature were exposed to steady UV illumination at 365 nm from a mercury lamp over time scales of 10-50 min.…”
Section: Experimental Methodsmentioning
confidence: 99%
“…Commercial samples were purified by repeated freeze–pump–thaw cycles with liquid nitrogen. The general principles of relative rate measurements are well established , and we have described our apparatus and procedures in detail elsewhere . Briefly, molecular chlorine is photolyzed by steady UV illumination from a mercury pen lamp in the presence of the reactant ketone and a reference compound in a 100‐cm 3 Pyrex multipass IR cell, with a path length of 2.4 m. The Pyrex walls are expected to block lamp emission at 184 and 254 nm but not at 365 nm.…”
Section: Methodsmentioning
confidence: 99%