Atmospheric chemistry of HFE-7200 (C4F9OC2H5): Reaction with OH radicals and fate of C4F9OCH2CH2O(•) and C4F9OCHO(•)CH3 radicals
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Atmospheric chemistry of HFE-7200 (C4F9OC2H5) : Reaction with OH radicals and fate of C4F9OCH2CH2O(•) and C4F9OCHO(•)CH3 radicals. / Christensen, L. K.; Sehested, J.; Nielsen, O. J.; Bilde, M.; Wallington, T. J.; Guschin, A.; Molina, L. T.; Molina, M. J.
I: Journal of Physical Chemistry A, Bind 102, Nr. 25, 18.06.1998, s. 4839-4845.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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TY - JOUR
T1 - Atmospheric chemistry of HFE-7200 (C4F9OC2H5)
T2 - Reaction with OH radicals and fate of C4F9OCH2CH2O(•) and C4F9OCHO(•)CH3 radicals
AU - Christensen, L. K.
AU - Sehested, J.
AU - Nielsen, O. J.
AU - Bilde, M.
AU - Wallington, T. J.
AU - Guschin, A.
AU - Molina, L. T.
AU - Molina, M. J.
PY - 1998/6/18
Y1 - 1998/6/18
N2 - Relative rate techniques were used to measure k(OH + n-C4F9OC2H5) = (6.4 ± 0.7) × 10-14 and k(OH + i-C4F9OC2H5) = (7.7 ± 0.8) × 10-14 cm3 molecule-1 s-1 at 295 K leading to estimates of ≈0.9 and 0.7 years for the atmospheric lifetimes of n-C4F9OC2H5 and i-C4F9OC2H5, respectively. A pulse radiolysis technique was used to measure k(F + HFE-7200) = (5.6 ± 2.1) × 10-11 cm3 molecule-1 s-1 (HFE-7200 = C4F9-OC2H5) at 296 K. Using FTIR-smog chamber relative rate techniques the following rate constants were determined at 296 K: k(F + HFE-7200) = (5.5 ± 1.1) × 10-11, k(Cl + HFE-7200) = (2.7 ± 0.6) times; 10-12, and k(Cl + C4F9OC(O)CH3) < 7 × 10-13 cm3 molecule-1 s-1. Two competing loss mechanisms for C4F9-OCHO(•)CH3 radicals were identified in 700 Torr of N2/O2 diluent at 296 K; reaction with O2 and decomposition via C-C bond scission with kO2/kdecomp = 0.026 ± 0.010 Torr-1. The Cl atom initiated oxidation of HFE-7200 in N2/O2 diluent gives two products: C4F9OC(O)CH3 and C4F9OC(O)H. C4F9OC(O)CH3 is the major atmospheric oxidation product of HFE-7200; C4F9OC(O)H is a minor product. The results are discussed with respect to the atmospheric chemistry of hydrofluoroethers.
AB - Relative rate techniques were used to measure k(OH + n-C4F9OC2H5) = (6.4 ± 0.7) × 10-14 and k(OH + i-C4F9OC2H5) = (7.7 ± 0.8) × 10-14 cm3 molecule-1 s-1 at 295 K leading to estimates of ≈0.9 and 0.7 years for the atmospheric lifetimes of n-C4F9OC2H5 and i-C4F9OC2H5, respectively. A pulse radiolysis technique was used to measure k(F + HFE-7200) = (5.6 ± 2.1) × 10-11 cm3 molecule-1 s-1 (HFE-7200 = C4F9-OC2H5) at 296 K. Using FTIR-smog chamber relative rate techniques the following rate constants were determined at 296 K: k(F + HFE-7200) = (5.5 ± 1.1) × 10-11, k(Cl + HFE-7200) = (2.7 ± 0.6) times; 10-12, and k(Cl + C4F9OC(O)CH3) < 7 × 10-13 cm3 molecule-1 s-1. Two competing loss mechanisms for C4F9-OCHO(•)CH3 radicals were identified in 700 Torr of N2/O2 diluent at 296 K; reaction with O2 and decomposition via C-C bond scission with kO2/kdecomp = 0.026 ± 0.010 Torr-1. The Cl atom initiated oxidation of HFE-7200 in N2/O2 diluent gives two products: C4F9OC(O)CH3 and C4F9OC(O)H. C4F9OC(O)CH3 is the major atmospheric oxidation product of HFE-7200; C4F9OC(O)H is a minor product. The results are discussed with respect to the atmospheric chemistry of hydrofluoroethers.
UR - http://www.scopus.com/inward/record.url?scp=0001545265&partnerID=8YFLogxK
M3 - Journal article
AN - SCOPUS:0001545265
VL - 102
SP - 4839
EP - 4845
JO - Journal of Physical Chemistry Part A: Molecules, Spectroscopy, Kinetics, Environment and General Theory
JF - Journal of Physical Chemistry Part A: Molecules, Spectroscopy, Kinetics, Environment and General Theory
SN - 1089-5639
IS - 25
ER -
ID: 225753691