2002
DOI: 10.1021/es0113798
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Atmospheric Chemistry of HFE-7500 [n-C3F7CF(OC2H5)CF(CF3)2]:  Reaction with OH Radicals and Cl Atoms and Atmospheric Fate of n-C3F7CF(OCHO•)CF(CF3)2 and n-C3F7CF(OCH2CH2O•)CF(CF3)2 Radicals

Abstract: Relative rate techniques were used to measure k(OH + HFE-7500) = (2.6+/-0.6) x 10(-14), k(Cl + HFE-7500) = (2.3+/-0.7) x 10(-12), k[Cl + n-C3F7CF(OC(O)H)CF(CF3)2] = (9.7+/-1.4) x 10(-15), and k[Cl + n-C3F7CF(OC(O)CH3)CF(CF3)2] < 6 x 10(-17) cm3 molecule(-1) s(-1) at 295 K [HFE-7500 = n-C3F7-CF(OC2H5)CF(CF3)2]. From the value of k(OH + HFE-7500) an estimate of 2.2 years for the atmospheric lifetime of HFE-7500 is obtained. Two competing loss mechanisms for n-C3F7-CF(OCHO.CH3)CF(CF3)2 radicals were identified in… Show more

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Cited by 19 publications
(19 citation statements)
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“…Using this approaching we found a REs of 0.55 and 0.43 W m -2 ppbv -1 for the 0-2500 and 900-1900 cm -1 wavenumber intervals, respectively. The previous literature value measured for the 900-1900 cm -1 interval was reported by Goto et al (2002), and it is 16% lower than the predicted here, 0.37 vs 0.43. However, differences within 14-25% of existing experimental values provide a valuable data for the REs in order to calculate accurate GWPs values (Blowers et al, 2007;Bravo et al, 2010b).…”
Section: Strategies To Design Cfc Alternatives With Low Environmentalcontrasting
confidence: 78%
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“…Using this approaching we found a REs of 0.55 and 0.43 W m -2 ppbv -1 for the 0-2500 and 900-1900 cm -1 wavenumber intervals, respectively. The previous literature value measured for the 900-1900 cm -1 interval was reported by Goto et al (2002), and it is 16% lower than the predicted here, 0.37 vs 0.43. However, differences within 14-25% of existing experimental values provide a valuable data for the REs in order to calculate accurate GWPs values (Blowers et al, 2007;Bravo et al, 2010b).…”
Section: Strategies To Design Cfc Alternatives With Low Environmentalcontrasting
confidence: 78%
“…In units of W m -2 ppbv -1 f From Bravo et al (2010) g k(298K) = 7.3x10 -14 cm 3 molecule -1 s -1 (Bravo et al, 2010) h k(298K) = 1.5x10 -14 cm 3 molecule -1 s -1 (Bravo et al, 2010) i k(298K) = 1.5x10 -14 cm 3 molecule -1 s -1 (Bravo et al, 2010) j k(298K) = 2.6x10 -14 cm 3 molecule -1 s -1 (Goto et al, 2002) k From Goto et al (2002) …”
Section: Atmospheric Implicationsmentioning
confidence: 99%
“…To indicate that reactions competing for the OH radical make it difficult to consume significant amounts of a sample or reference in the older technique [8][9][10], (12) In mode 1, the OH radical concentration decreased rapidly from 2.78 × 10 11 to 3.47 × 10 10 radicals cm…”
Section: Simulation Of Oh Radical Formation Using a Chemical Modelmentioning
confidence: 99%
“…Photolytic sources include H 2 O 2 [3], HONO [4,5], CH 3 ONO-O 2 [6,7], and O 3 -H 2 O gas mixtures [8][9][10]. These sources typically produce OH radical concentrations of 10 7 -10 9 radicals cm −3 [11].…”
Section: Introductionmentioning
confidence: 99%
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