2010
DOI: 10.1002/poc.1741
|View full text |Cite
|
Sign up to set email alerts
|

Product distribution in the Cl‐initiated photooxidation of CF3C(O)OCH2CF3

Abstract: The product distribution and the mechanism of the reaction of Cl atoms with 2,2,2‐trifluoroethyl 2,2,2‐trifluoroacetate (TFETFA; CF3C(O)OCH2CF3) were investigated using a 1080 L environmental chamber with in situ Fourier transform infrared (FTIR) spectroscopy detection. The experiments were performed at (296 ± 2) K and atmospheric pressure (760 ± 10) Torr of synthetic air free of NOx. A yield of (45 ± 3)% was obtained for the CF3C(O)OC(O)CF3 formation. CF2O and CO were produced with estimated yields of 35 and … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

2
21
0

Year Published

2013
2013
2015
2015

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 17 publications
(23 citation statements)
references
References 24 publications
2
21
0
Order By: Relevance
“…Therefore, it is necessary to understand the chemistry of fluorinated esters in the atmosphere in order to assess the environmental acceptability of HFEs as a plausible replacement for chlorofluorocarbons. The reaction mechanisms of FESs with atmospheric oxidants have been studied extensively both experimentally [20][21][22][23][24][25] and theoretically [26][27][28][29][30][31][32] and continue to receive considerable attention. FESs absorb strongly in the earthly infrared (IR) radiation region of 800-1,200 cm −1 .…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, it is necessary to understand the chemistry of fluorinated esters in the atmosphere in order to assess the environmental acceptability of HFEs as a plausible replacement for chlorofluorocarbons. The reaction mechanisms of FESs with atmospheric oxidants have been studied extensively both experimentally [20][21][22][23][24][25] and theoretically [26][27][28][29][30][31][32] and continue to receive considerable attention. FESs absorb strongly in the earthly infrared (IR) radiation region of 800-1,200 cm −1 .…”
Section: Introductionmentioning
confidence: 99%
“…At first, the reaction enthalpies ( H • r 298 ) of the isodesmic reactions (9-10) are determined using the total energy of the species obtained at the M06-2X/6-311++G(d,p) level, including thermal correction to enthalpy estimated at the M06-2X/6-31+G(d,p) level. Since the H • r 298 value corresponds to the difference in the enthalpies of formation ( H • f 298 ) of the reactants and products, the ( H • f 298 ) values of the reactant species can be easily evaluated by combining them with the known enthalpies of formation of the reference compounds involved in the isodesmic reaction schemes mentioned above (9)(10) 44 The H • f 298 values for radicals P1, P2, P3, and P4 determined from the energy data obtained at M06-2X/6-311++G(d,p) are found to be -227.6, -233.9,-228.2 and -225.5 kcal mol −1 , whereas the same for M06-2X/6-31+G(d,p) are found to be -227.7, -234.1, -228.3 and -225.6 kcal mol −1 , respectively. These data are not available in the literature and can therefore be useful for further thermochemical and kinetic modeling of reaction involving these species.…”
Section: Atmospheric Lifetimementioning
confidence: 99%
“…Geometries of all the species involved in the isodesmic reactions (9)(10) were first optimized at the M06-2X/6-31+G(d,p) level. Energies were further refined with an extended basis set (6-311++G(d,p)) using the same functional.…”
Section: Atmospheric Lifetimementioning
confidence: 99%
See 1 more Smart Citation
“…Recently, hydrofluoroethers (HFEs) [1,2] have been developed as the third generation alternatives for CFCs and used in various industrial applications for two reasons: one is these fluorine-containing compounds have zero ozone depletion [3][4][5][6], the other is they have little impact on climate change due to their relatively shorter atmospheric lifetimes in the troposphere than HFCs and HCFCs. The main degradation product of HFEs in the atmosphere is to form the corresponding hydrofluorinated esters (FESs) [7][8][9], which could be further photochemically oxidized in the troposphere by atmospheric oxidants, affording environmentally burdened products such as trifluoroacetic acid (TFA, CF 3 C(O)OH) and CO 2 et al [10,11]. Thus, to better assess the environmental impact of HFEs as candidates to replace CFCs, a complete understanding of the atmospheric chemistry of FESs is required.…”
Section: Introductionmentioning
confidence: 99%