TY - JOUR
T1 - Atmospheric chemistry of cyc–CF2CF2CX=CX– (X=H, F)
T2 - Kinetics, products, and mechanism of gas–phase reactions with OH radicals, and atmospheric implication
AU - Zhang, Wenni
AU - Guo, Qin
AU - Quan, Hengdao
N1 - Publisher Copyright:
© 2025 Elsevier Ltd
PY - 2025/5/15
Y1 - 2025/5/15
N2 - Rate constants for gas-phase reactions of series of hydrofluorocyclobutene including 3,3,4,4-tetrafluorocyclobutene (HFO-c1334zz), 1,3,3,4,4-pentafluorocyclobutene (HFO-c1325yz), and hexafluorocyclobutene (PFO-c1316) with OH radicals were assessed by a relative rate method. The values were determined as (8.47 ± 1.96) × 10−13 exp[(–475 ± 68)/T], (5.37 ± 0.99) × 10−13 exp[(–643 ± 53)/T] and (8.41 ± 2.24) × 10−13 exp[(–905 ± 78)/T] between 253 and 328 K; and 1.77 × 10−13, 0.644 × 10−13, and 0.402 × 10−13 cm3 molecule−1 s−1 at 298K, respectively. The atmospheric lifetimes were 65, 180, and 288 days, while their radiative efficiency (RE) were evaluated to be 0.088, 0.174, and 0.228 W m−2 ppb−1, respectively. The 100-year time horizon global warming potentials (GWP100) were estimated to be 6, 31, and 65, respectively. The calculated POCPE values of HFO-c1334zz, HFO-c1325yz, and PFO-c1316 were then obtained as 1.719 and 0.688 for North-west European and USA urban conditions, 0.579 and 0.222 for North-west European and USA urban conditions, and 0.324 and 0.124 for North-west European and USA urban conditions, respectively. Furthermore, the products and mechanism for the OH radical-initiated oxidation reactions of HFO-c1334zz, HFO-c1325yz, and PFO-c1316 were studied for the first time. COF2, CO, and CO2 were identified as the main carbon-containing products of HFO-c1334zz, HFO-c1325yz. Additionally, COF2, CO2, CO, and FC(O)OH were observed as the main products of PFO-c1316.
AB - Rate constants for gas-phase reactions of series of hydrofluorocyclobutene including 3,3,4,4-tetrafluorocyclobutene (HFO-c1334zz), 1,3,3,4,4-pentafluorocyclobutene (HFO-c1325yz), and hexafluorocyclobutene (PFO-c1316) with OH radicals were assessed by a relative rate method. The values were determined as (8.47 ± 1.96) × 10−13 exp[(–475 ± 68)/T], (5.37 ± 0.99) × 10−13 exp[(–643 ± 53)/T] and (8.41 ± 2.24) × 10−13 exp[(–905 ± 78)/T] between 253 and 328 K; and 1.77 × 10−13, 0.644 × 10−13, and 0.402 × 10−13 cm3 molecule−1 s−1 at 298K, respectively. The atmospheric lifetimes were 65, 180, and 288 days, while their radiative efficiency (RE) were evaluated to be 0.088, 0.174, and 0.228 W m−2 ppb−1, respectively. The 100-year time horizon global warming potentials (GWP100) were estimated to be 6, 31, and 65, respectively. The calculated POCPE values of HFO-c1334zz, HFO-c1325yz, and PFO-c1316 were then obtained as 1.719 and 0.688 for North-west European and USA urban conditions, 0.579 and 0.222 for North-west European and USA urban conditions, and 0.324 and 0.124 for North-west European and USA urban conditions, respectively. Furthermore, the products and mechanism for the OH radical-initiated oxidation reactions of HFO-c1334zz, HFO-c1325yz, and PFO-c1316 were studied for the first time. COF2, CO, and CO2 were identified as the main carbon-containing products of HFO-c1334zz, HFO-c1325yz. Additionally, COF2, CO2, CO, and FC(O)OH were observed as the main products of PFO-c1316.
KW - Atmospheric chemistry
KW - Degradation mechanism
KW - Hydrofluorocycbutene
KW - Photochemical ozone creation potential
UR - http://www.scopus.com/inward/record.url?scp=85219054671&partnerID=8YFLogxK
U2 - 10.1016/j.atmosenv.2025.121125
DO - 10.1016/j.atmosenv.2025.121125
M3 - Article
AN - SCOPUS:85219054671
SN - 1352-2310
VL - 349
JO - Atmospheric Environment
JF - Atmospheric Environment
M1 - 121125
ER -