Atmospheric Chemistry of (E)- and (Z)-CF3CF2CH═CHCF2CF3 (HFO-153-10mczz): Kinetics and Mechanisms of the Reactions with Cl Atoms, OH Radicals, and O3

被引:0
|
作者
Andersen, Mads P. Sulbaek [1 ,2 ]
Borcher, Josefine Ellerup [2 ]
Blair, Connor [1 ]
Robin, Mark L. [3 ]
Nielsen, Ole John [2 ]
机构
[1] Calif State Univ Northridge, Dept Chem & Biochem, Northridge, CA 91330 USA
[2] Univ Copenhagen, Copenhagen Ctr Atmospher Res, Dept Chem, DK-2100 Frederiksberg O, Copenhagen, Denmark
[3] Chemours Co, Wilmington, DE 19899 USA
来源
JOURNAL OF PHYSICAL CHEMISTRY A | 2024年 / 128卷 / 47期
关键词
GAS-PHASE REACTIONS; PEROXY-RADICALS; CHLORINE; FATE; DECOMPOSITION; SERIES;
D O I
10.1021/acs.jpca.4c05302
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Smog chamber experiments were conducted to establish the atmospheric chemistry of (E)- and (Z)-CF3CF2CH & boxH;CHCF2CF3. Kinetics of the reactions of the two compounds with Cl atoms and OH radicals were measured using relative rate techniques, giving k(Cl + (E)-CF3CF2CH & boxH;CHCF2CF3) = (5.63 +/- 0.84) x 10(-12), k(Cl + (Z)-CF3CF2CH & boxH;CHCF2CF3) = (1.17 +/- 0.20) x 10(-11), k(OH + (E)-CF3CF2CH & boxH;CHCF2CF3) = (1.64 +/- 0.21) x 10(-13), and k(OH + (Z)-CF3CF2CH & boxH;CHCF2CF3) = (3.13 +/- 0.38) x 10(-13) cm(3) molecule(-1) s(-1) in 680 Torr air/N-2/O-2 diluents at 296 +/- 2 K. Rate coefficients for the reactions with O-3, k(O-3 + (E)-CF3CF2CH & boxH;CHCF2CF3) similar to 1 x 10(-22) and k(O-3 + (Z)-CF3CF2CH & boxH;CHCF2CF3) <= 5x 10(-24) cm(3) molecule(-1) s(-1), were established using absolute techniques in a 680 Torr air diluent and 296 +/- 2 K. The Cl reaction with (E)-CF3CF2CH & boxH;CHCF2CF3 gives CF3CF2CHClC(O)CF2CF3 as the sole oxidation product, whereas the reaction with (Z)-CF3CF2CH & boxH;CHCF2CF3 also gives rise to the formation of the (E)-isomer in minor yields. The reaction of OH radicals with CF3CF2CH & boxH;CHCF2CF3 gives CF3CF2CHO in a yield of 177 +/- 17%. The main atmospheric fate of (E)- and (Z)-CF3CF2CH & boxH;CHCF2CF3 is the reaction with OH radicals, resulting in overall atmospheric lifetime estimates of 71 and 37 days, for (E)- and (Z)-CF3CF2CH & boxH;CHCF2CF3, respectively. The IR absorption cross sections are reported, and the global warming potentials of (E)- and (Z)-CF3CF2CH & boxH;CHCF2CF3 for the 20-, 100-, and 500-year time horizons are calculated to be 36, 10, and 3 for the (E)-isomer and 11, 3, and 1 for the (Z)-isomer, respectively. Atmospheric processing of (E)- and (Z)-CF3CF2CH & boxH;CHCF2CF3 is expected to yield CF3CF2COOH and CF3COOH in yields of <10%. This study provides a comprehensive description of the atmospheric chemistry and fate of (E)- and (Z)-CF3CF2CH & boxH;CHCF2CF3.
引用
收藏
页码:10167 / 10180
页数:14
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