Rate constants for the reactions of chlorine atoms with deuterated methanes: Experiment and theory

被引:34
作者
Boone, GD [1 ]
Agyin, F [1 ]
Robichaud, DJ [1 ]
Tao, FM [1 ]
Hewitt, SA [1 ]
机构
[1] Calif State Univ Fullerton, Dept Chem & Biochem, Fullerton, CA 92834 USA
关键词
D O I
10.1021/jp0027290
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
Long-path FTIR spectroscopy and ab initio calculations combined with conventional transition state theory were used to study the kinetics of the reactions of Cl atoms with deuterated methanes. The following experimental relative rate constants for the reaction of Cl atoms at 298 +/- 5 K and 760 +/- 5 Torr were determined: CH3D, (6.5 +/- 0.5) x 10(-14); CH2D2, (4.2 +/- 0.5) x 10(-14); CHD3, (1.9 +/- 0.3) x 10(-14); CD4, (5.4 +/- 0.4) x 10(-15). All experimental and theoretical rate constants are in units of cm(3) molecule(-1) s(-1) and are relative to the 1.0 x 10(-13) cm(3) molecule(-1) s(-1) rate constant for the reaction of Cl with CH4. All experimental uncertainty limits are 2 sigma. The geometries, energies, and frequencies of the reactants, products, and transition states were calculated at the level of the second-order Moller-Plesset approximation using a 6-311++G-(2d,2p) basis set. The following theoretical relative rate constants were calculated at 298 K using conventional transition state theory combined with an Eckart one-dimensional tunneling correction: CH3D, 6.8 x 10(-14); CH2D2, 4.2 x 10(-14); CHD3, 2.1 x 10(-14); CD4, 4.4 x 10(-15). The theoretical rate constants agree well with the experimental results. The curvature in both the experimental and theoretical rate constants as a function of deuteration is due to a secondary kinetic isotope effect, involving mainly the rate constant preexponential factors. The large decrease in Cl atom rate constant in going from CH4 to CH3D (i.e., the increase in curvature at CH3D) is due to the reduced symmetry in the transition state and a mass-dependent effect. The implications for previous studies, atmospheric chemistry, and chemical reactivity are discussed.
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页码:1456 / 1464
页数:9
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[1]   Isotope analysis based source identification for atmospheric CH4 and CO sampled across Russia using the Trans-Siberian railroad [J].
Bergamaschi, P ;
Brenninkmeijer, CAM ;
Hahn, M ;
Rockmann, T ;
Scharffe, DH ;
Crutzen, PJ ;
Elansky, NF ;
Belikov, IB ;
Trivett, NBA ;
Worthy, DEJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D7) :8227-8235
[2]   Implications of the large carbon kinetic isotope effect in the reaction CH4+Cl for the C-13/C-12 ratio of stratospheric CH4 [J].
Bergamaschi, P ;
Bruhl, C ;
Brenninkmeijer, CAM ;
Saueressig, G ;
Crowley, JN ;
Grooss, JU ;
Fischer, H ;
Crutzen, PJ .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (17) :2227-2230
[3]  
Brahan KM, 1996, INT J CHEM KINET, V28, P397, DOI 10.1002/(SICI)1097-4601(1996)28:6<397::AID-KIN1>3.0.CO
[4]  
2-Q
[5]   ACUCHEM - A COMPUTER-PROGRAM FOR MODELING COMPLEX CHEMICAL-REACTION SYSTEMS [J].
BRAUN, W ;
HERRON, JT ;
KAHANER, DK .
INTERNATIONAL JOURNAL OF CHEMICAL KINETICS, 1988, 20 (01) :51-62
[6]   A large (CO)-C-13 deficit in the lower Antarctic stratosphere due to ''ozone hole'' chemistry .1. Observations [J].
Brenninkmeijer, CAM ;
Muller, R ;
Crutzen, PJ ;
Lowe, DC ;
Manning, MR ;
Sparks, RJ ;
vanVelthoven, PFJ .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (16) :2125-2128
[7]   CARBON KINETIC ISOTOPE EFFECT IN THE OXIDATION OF METHANE BY THE HYDROXYL RADICAL [J].
CANTRELL, CA ;
SHETTER, RE ;
MCDANIEL, AH ;
CALVERT, JG ;
DAVIDSON, JA ;
LOWE, DC ;
TYLER, SC ;
CICERONE, RJ ;
GREENBERG, JP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D13) :22455-22462
[8]  
Chase M. e. a., 1985, JANAF THERMOCHEMICAL, V14
[9]   KINETIC ISOTOPE EFFECT IN PHOTOCHLORINATION OF H2, CH4, CHCL3, AND C2H6 [J].
CHILTZ, G ;
JOHNSTON, HS ;
HUYBRECHTS, G ;
GOLDFINGER, P ;
MEYERS, L ;
VERBEKE, G ;
ECKLING, R .
JOURNAL OF CHEMICAL PHYSICS, 1963, 38 (05) :1053-&
[10]  
Clyne M. A. A., 1973, J. Chem. Soc., V69, P1547, DOI [10.1039/f19736901547, DOI 10.1039/F19736901547]