A three-dimensional model of the atmospheric chemistry of E and Z-CF3CH = CHCl (HCFO-1233(zd) (E/Z))

被引:27
作者
Andersen, Mads P. Sulbaek [1 ,2 ]
Schmidt, Johan A. [2 ,3 ]
Volkova, Aleksandra [1 ]
Wuebbles, Donald J. [4 ]
机构
[1] Calif State Univ Northridge, Dept Chem & Biochem, 18111 Nordhoff St, Northridge, CA 91330 USA
[2] Univ Copenhagen, Dept Chem, Copenhagen Ctr Atmospher Res, Univ Pk 5, DK-2100 Copenhagen, Denmark
[3] Harvard Univ, Sch Engn & Appl Sci, 29 Oxford St, Cambridge, MA 02138 USA
[4] Univ Illinois, Dept Atmospher Sci, 105 S Gregory Ave, Urbana, IL 61801 USA
关键词
Halogenated olefin; Trifluoroacetic acid; Global warming potentials; Atmospheric lifetimes; Ozone depletion potentials; Photochemical ozone creation potentials; OZONE DEPLETION POTENTIALS; GAS-PHASE REACTIONS; OH RADICALS; CL ATOMS; CREATION POTENTIALS; TRIFLUOROACETATE; KINETICS; DEGRADATION; MECHANISM; SPECTRA;
D O I
10.1016/j.atmosenv.2018.02.018
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Using a 3-dimensional global atmospheric chemistry and transport model we investigated the atmospheric degradation of HCFO-1233zd(E), E-CF3CH = CHCI, a commercially important, new hydrofluorocarbon replacement compound. Atmospheric degradation of E-CF3CH = CHCl is initiated by reaction with OH radicals, which leads to several chemical oxidation products. Dissemination of these oxidation products to the environment is of concern due to the possible formation of trifluoroacetic acid (TFA) as a degradation product. The model indicates that the average global yield of TFA from atmospheric processing of E-CF3CH = CHCI is approximately 2%. The annually averaged atmospheric lifetime of E-CF3CH = CHCl was found to be approximately 36 days (12 days for Z-CF3CH = CHCl). As E-CF3CH = CHCl is short lived, by far the majority of its Cl atoms will be released and deposited in the lower atmosphere, and the impact on stratospheric ozone is insignificant. An Ozone Depletion Potential of 0.00030 was determined. The Photochemical Ozone Creation Potential was evaluated and a value of 3.6 determined. Finally, we derive a Global Warming Potential for E-CF3CH = CHCl for a 100 year time horizon of < 5. For comparison, data for the stereoismeric analogue, Z-CF3CH = CHCl, was also obtained from the model.
引用
收藏
页码:250 / 259
页数:10
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