Rate constants of the reactions of CF2ClC(O)OCH3 and CF2ClC(O)OCH2CH3 with OH radicals and Cl atoms at atmospheric pressure

被引:14
作者
Blanco, Maria B. [1 ]
Teruel, Mariano A. [1 ]
机构
[1] Univ Nacl Cordoba, Fac Ciencias Quim, Dept Fisicoquim, INFIQC,Inst Invest Fisicoquim, RA-5000 Cordoba, Argentina
关键词
D O I
10.1016/j.cplett.2007.04.071
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Rate coefficients for the reactions of hydroxyl radicals and chlorine atoms with methyl chlorodifluoroacetate and ethyl chlorodifluoroacetate have been determined at 298 K and atmospheric pressure. The decay of the organics was followed using a gas chromatograph with a flame ionization detector (GC-FID), and the rate constants were determined using a relative rate method with different references. Room temperature rate constants are found to be (in cm(3) molecule(-1) s(-1)): k(1)(OH + CF2ClC(O)OCH3) = (1.1 +/- 0.3) x 10(--13), k(2) (Cl + CF2ClC(O)OCH3) = (1.0 +/- 0.2) x 10(-13), k(3)(OH + CF2ClC(O)OCH2CH3) = (5.4 +/- 1 1.5) x 10(-13) and k(4)(Cl + CF2CIC(O)OCH2 CH3) = (1.5 +/- 0.3) x 10(-12) with uncertainties representing +/- 2 sigma. This is the first kinetic study of the studied reactions under atmospheric pressure. Free-energy relationships are presented, and halogen substitution in the ester is discussed in terms of reactivity with OH radicals and Cl atoms. On the basis of our kinetic measurements, the tropospheric lifetimes of CF2ClC(O)OCH3, and CF2ClC(O)OCH2CH3 are estimated to be around 53 and 11 days, respectively, primarily due to their reaction with hydroxyl radicals in the troposphere. (C) 2007 Elsevier B.V.. All rights reserved.
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页码:1 / 6
页数:6
相关论文
共 21 条
[1]   Atmospheric chemistry of CF3OCF2CF2H and CF3OC(CF3)2H:: Reaction with Cl atoms and OH radicals, degradation mechanism, global warming potentials, and empirical relationship between k(OH) and k(Cl) for organic compounds [J].
Andersen, MPS ;
Nielsen, OJ ;
Wallington, TJ ;
Hurley, MD .
JOURNAL OF PHYSICAL CHEMISTRY A, 2005, 109 (17) :3926-3934
[3]  
Atkinson R., 2001, IUPAC SUBCOMMITTEE G, P1
[4]   Determination of chloroacetates in atmospheric particulate matter [J].
Bakeas, EB ;
Economou, AG ;
Siskos, PA .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2003, 37 (11) :2336-2339
[5]   On the OH-initiated degradation of methacrylates in the troposphere: Gas-phase kinetics and formation of pyruvates [J].
Blanco, Maria B. ;
Taccone, Raul A. ;
Lane, Silvia I. ;
Teruel, Mariano A. .
CHEMICAL PHYSICS LETTERS, 2006, 429 (4-6) :389-394
[6]  
BLANCO MB, UNPUB ATMOS ENV
[7]   Testing frontier orbital control: Kinetics of OH with ethane, propane, and cyclopropane from 180 to 360K [J].
Clarke, JS ;
Kroll, JH ;
Donahue, NM ;
Anderson, JG .
JOURNAL OF PHYSICAL CHEMISTRY A, 1998, 102 (48) :9847-9857
[8]   Formation of chloroacetic acids from soil, humic acid and phenolic moieties [J].
Fahimi, IJ ;
Keppler, F ;
Schöler, HF .
CHEMOSPHERE, 2003, 52 (02) :513-520
[9]   CHLORINE ATOMS AS A POTENTIAL TROPOSPHERIC OXIDANT IN THE MARINE BOUNDARY-LAYER [J].
FINLAYSONPITTS, BJ .
RESEARCH ON CHEMICAL INTERMEDIATES, 1993, 19 (03) :235-249
[10]   TROPOSPHERIC BUDGET OF REACTIVE CHLORINE [J].
GRAEDEL, TE ;
KEENE, WC .
GLOBAL BIOGEOCHEMICAL CYCLES, 1995, 9 (01) :47-77