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Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a)

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Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a). / RATTIGAN, OV; ROWLEY, DM; WILD, O et al.
In: Journal of the Chemical Society, Faraday Transactions, Vol. 90, No. 13, 07.07.1994, p. 1819-1829.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

RATTIGAN, OV, ROWLEY, DM, WILD, O, JONES, RL & COX, RA 1994, 'Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a)', Journal of the Chemical Society, Faraday Transactions, vol. 90, no. 13, pp. 1819-1829. https://doi.org/10.1039/FT9949001819

APA

RATTIGAN, OV., ROWLEY, DM., WILD, O., JONES, RL., & COX, RA. (1994). Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a). Journal of the Chemical Society, Faraday Transactions, 90(13), 1819-1829. https://doi.org/10.1039/FT9949001819

Vancouver

RATTIGAN OV, ROWLEY DM, WILD O, JONES RL, COX RA. Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a). Journal of the Chemical Society, Faraday Transactions. 1994 Jul 7;90(13):1819-1829. doi: 10.1039/FT9949001819

Author

RATTIGAN, OV ; ROWLEY, DM ; WILD, O et al. / Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a). In: Journal of the Chemical Society, Faraday Transactions. 1994 ; Vol. 90, No. 13. pp. 1819-1829.

Bibtex

@article{15029ddf1e0947f8a9e654c4cbc1c201,
title = "Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a)",
abstract = "The chlorine-initiated photooxidation of hydrofluorocarbon 134a (CF3CH2F) has been studied in the temperature range 235-318 K and at 1 atm total pressure using UV absorption. Trifluoroacetyl fluoride [CF3C(O)F] and formyl fluoride [HC(O)F] were observed as the major products. IR analysis of the reaction mixture also showed carbonyl fluoride [C(O)F2] as a product. By measurement of the yields of HC(O)F from the photooxidation as a function of [O2] and temperature, the rate of the unimolecular decomposition of the oxy radical, CF3CHFO, reaction (5), was determined relative to its reaction with O2, reaction (4): CF3CHFO + O2 --> CF3C(O)F + HO2 (4) CF3CHFO --> CF3 + HO(O))F (5).The results were treated using both an arithmetic derivation and numerical integration with a detailed reaction scheme. Inclusion of other recently published kinetic data leads to the following recommended rate expression for reaction (5) at 1 atm k5 = 7.4 x 10(11) exp[(-4720 +/- 220)/T] s-1.The errors are 1sigma.The observation of enhanced product yields in the present work is attributed to the reaction of the CF3O radical with HFC 134a leading to further peroxy radical formation. The results have been incorporated into a 2D atmospheric model to assess the environmental implications of HFC 134a release in the troposphere.",
keywords = "CHLORINE ATOMS, HYDROFLUOROCARBON 134A, UV ABSORPTION, ABSORPTION CROSS-SECTIONS, RADICALS, SELF-REACTION, CHEMISTRY, FLASH-PHOTOLYSIS, GAS-PHASE, CF3O",
author = "OV RATTIGAN and DM ROWLEY and O WILD and RL JONES and RA COX",
year = "1994",
month = jul,
day = "7",
doi = "10.1039/FT9949001819",
language = "English",
volume = "90",
pages = "1819--1829",
journal = "Journal of the Chemical Society, Faraday Transactions",
issn = "0956-5000",
publisher = "Royal Society of Chemistry",
number = "13",

}

RIS

TY - JOUR

T1 - Mechanism of atmospheric oxidation of 1,1,1,2-tetrafluoroethane (HFC 134a)

AU - RATTIGAN, OV

AU - ROWLEY, DM

AU - WILD, O

AU - JONES, RL

AU - COX, RA

PY - 1994/7/7

Y1 - 1994/7/7

N2 - The chlorine-initiated photooxidation of hydrofluorocarbon 134a (CF3CH2F) has been studied in the temperature range 235-318 K and at 1 atm total pressure using UV absorption. Trifluoroacetyl fluoride [CF3C(O)F] and formyl fluoride [HC(O)F] were observed as the major products. IR analysis of the reaction mixture also showed carbonyl fluoride [C(O)F2] as a product. By measurement of the yields of HC(O)F from the photooxidation as a function of [O2] and temperature, the rate of the unimolecular decomposition of the oxy radical, CF3CHFO, reaction (5), was determined relative to its reaction with O2, reaction (4): CF3CHFO + O2 --> CF3C(O)F + HO2 (4) CF3CHFO --> CF3 + HO(O))F (5).The results were treated using both an arithmetic derivation and numerical integration with a detailed reaction scheme. Inclusion of other recently published kinetic data leads to the following recommended rate expression for reaction (5) at 1 atm k5 = 7.4 x 10(11) exp[(-4720 +/- 220)/T] s-1.The errors are 1sigma.The observation of enhanced product yields in the present work is attributed to the reaction of the CF3O radical with HFC 134a leading to further peroxy radical formation. The results have been incorporated into a 2D atmospheric model to assess the environmental implications of HFC 134a release in the troposphere.

AB - The chlorine-initiated photooxidation of hydrofluorocarbon 134a (CF3CH2F) has been studied in the temperature range 235-318 K and at 1 atm total pressure using UV absorption. Trifluoroacetyl fluoride [CF3C(O)F] and formyl fluoride [HC(O)F] were observed as the major products. IR analysis of the reaction mixture also showed carbonyl fluoride [C(O)F2] as a product. By measurement of the yields of HC(O)F from the photooxidation as a function of [O2] and temperature, the rate of the unimolecular decomposition of the oxy radical, CF3CHFO, reaction (5), was determined relative to its reaction with O2, reaction (4): CF3CHFO + O2 --> CF3C(O)F + HO2 (4) CF3CHFO --> CF3 + HO(O))F (5).The results were treated using both an arithmetic derivation and numerical integration with a detailed reaction scheme. Inclusion of other recently published kinetic data leads to the following recommended rate expression for reaction (5) at 1 atm k5 = 7.4 x 10(11) exp[(-4720 +/- 220)/T] s-1.The errors are 1sigma.The observation of enhanced product yields in the present work is attributed to the reaction of the CF3O radical with HFC 134a leading to further peroxy radical formation. The results have been incorporated into a 2D atmospheric model to assess the environmental implications of HFC 134a release in the troposphere.

KW - CHLORINE ATOMS

KW - HYDROFLUOROCARBON 134A

KW - UV ABSORPTION

KW - ABSORPTION CROSS-SECTIONS

KW - RADICALS

KW - SELF-REACTION

KW - CHEMISTRY

KW - FLASH-PHOTOLYSIS

KW - GAS-PHASE

KW - CF3O

U2 - 10.1039/FT9949001819

DO - 10.1039/FT9949001819

M3 - Journal article

VL - 90

SP - 1819

EP - 1829

JO - Journal of the Chemical Society, Faraday Transactions

JF - Journal of the Chemical Society, Faraday Transactions

SN - 0956-5000

IS - 13

ER -