Photolysis of CF3CHO at 254 nm and potential contribution to the atmospheric abundance of HFC-23
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Photolysis of CF3CHO at 254 nm and potential contribution to the atmospheric abundance of HFC-23. / Sulbaek Andersen, Mads Peter; Madronich, Sasha; Ohide, Joanna May; Frausig, Morten; Nielsen, Ole John.
I: Atmospheric Environment, Bind 314, 120087, 2023.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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TY - JOUR
T1 - Photolysis of CF3CHO at 254 nm and potential contribution to the atmospheric abundance of HFC-23
AU - Sulbaek Andersen, Mads Peter
AU - Madronich, Sasha
AU - Ohide, Joanna May
AU - Frausig, Morten
AU - Nielsen, Ole John
N1 - Publisher Copyright: © 2023
PY - 2023
Y1 - 2023
N2 - In this work, the 254 nm photolysis of CF3CHO was investigated using a 101 L quartz chamber coupled with FTIR detection. The overall quantum yield was determined as (0.52 ± 0.07) at 700 Torr, independent of diluent gas. Photolysis in 700 Torr N2 and in the presence of NO yields (26 ± 3) % CF3H and (73 ± 6) % CF3NO. In 700 Torr of air or oxygen, products identified include CF3H, COF2, CF3OH, CF3O2CF3 and CF3O3CF3. In the presence of NO in 700 Torr of air or O2, alkoxy- and peroxy-nitrates were also quantified. A full carbon balance for the fluorine-bearing carbon was achieved. The photolytic channel quantum yields were established: Φ(CF3H + CO) = (0.16 ± 0.02) and Φ(CF3 + HCO) = (0.36 ± 0.07) at 700 Torr total pressure. This is the first large chamber study of the stratospheric photolysis of CF3CHO. The quantum yields measured here are lower than those reported previously and show a different relative importance associated with the photolysis channels. Atmospheric photolysis coefficients of CF3CHO were modeled giving an estimate for the average atmospheric lifetime for CF3CHO of 13 ± 4 days (at 5 km altitude, tropics). Based on the present work, photolytic production of CF3H, which is a strong greenhouse gas, can occur at stratospheric altitudes above 30–40 km. This has implications for the environmental impact of CF3CHO generated as an oxidation product in the higher atmosphere from long-lived chlorofluorocarbon-replacement compounds. However, the majority of CF3CHO will undergo photochemical degradation in the lower troposphere. Hence, photochemical degradation of CF3CHO will make a negligible contribution to the atmospheric burden of CF3H.
AB - In this work, the 254 nm photolysis of CF3CHO was investigated using a 101 L quartz chamber coupled with FTIR detection. The overall quantum yield was determined as (0.52 ± 0.07) at 700 Torr, independent of diluent gas. Photolysis in 700 Torr N2 and in the presence of NO yields (26 ± 3) % CF3H and (73 ± 6) % CF3NO. In 700 Torr of air or oxygen, products identified include CF3H, COF2, CF3OH, CF3O2CF3 and CF3O3CF3. In the presence of NO in 700 Torr of air or O2, alkoxy- and peroxy-nitrates were also quantified. A full carbon balance for the fluorine-bearing carbon was achieved. The photolytic channel quantum yields were established: Φ(CF3H + CO) = (0.16 ± 0.02) and Φ(CF3 + HCO) = (0.36 ± 0.07) at 700 Torr total pressure. This is the first large chamber study of the stratospheric photolysis of CF3CHO. The quantum yields measured here are lower than those reported previously and show a different relative importance associated with the photolysis channels. Atmospheric photolysis coefficients of CF3CHO were modeled giving an estimate for the average atmospheric lifetime for CF3CHO of 13 ± 4 days (at 5 km altitude, tropics). Based on the present work, photolytic production of CF3H, which is a strong greenhouse gas, can occur at stratospheric altitudes above 30–40 km. This has implications for the environmental impact of CF3CHO generated as an oxidation product in the higher atmosphere from long-lived chlorofluorocarbon-replacement compounds. However, the majority of CF3CHO will undergo photochemical degradation in the lower troposphere. Hence, photochemical degradation of CF3CHO will make a negligible contribution to the atmospheric burden of CF3H.
KW - Atmospheric chemistry
KW - Climate
KW - HFC-23
KW - Lifetimes
KW - Quantum yield
KW - Stratosphere
U2 - 10.1016/j.atmosenv.2023.120087
DO - 10.1016/j.atmosenv.2023.120087
M3 - Journal article
AN - SCOPUS:85172082711
VL - 314
JO - Atmospheric Environment
JF - Atmospheric Environment
SN - 1352-2310
M1 - 120087
ER -
ID: 368805564