Production of HCl in the OH plus ClO reaction: Laboratory measurements and statistical rate theory calculations

被引:24
作者
Lipson, JB
Beiderhase, TW
Molina, LT
Molina, MJ [1 ]
Olzmann, M
机构
[1] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
[2] MIT, Dept Chem, Cambridge, MA 02139 USA
[3] Univ Halle Wittenberg, Inst Phys Chem, D-06099 Halle, Germany
关键词
D O I
10.1021/jp9847787
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
The branching ratio for the OH + ClO reaction has been measured using the turbulent flow technique with high-pressure chemical ionization mass spectrometry for the detection of reactants and products. In our earlier study, OD was used instead of OH due to the large HCl background produced by the ClO source (J. Chem. Sec., Faraday Trans. 1997, 93, 2665). Improvements to our experimental technique have significantly reduced this HCl background, thus making it possible to observe directly the production of very small concentrations of HCl (similar to 10(9) molecule cm(-3)) from the minor channel of the OH + ClO reaction. At room temperature and similar to 100 Ton pressure, the rate constant for this minor channel was determined to be (9.5 +/- 1.6) x 10(-13) cm(3) molecule(-1) s(-1) with a two standard deviation error limit, which remained unchanged when the pressure was increased to 200 Torr. The temperature dependence of the rate constant for this minor channel was also investigated between 207 and 298 K;, and the data were fit to the following Arrhenius expression: (3.2 +/- 0.8) x 10(-13) exp[(325 +/- 60)/T] cm(3) molecule(-1) s(-1). The branching ratio for the HCl channel was determined to be 0.07 +/- 0.03 at all pressures and temperatures investigated in this study. Statistical rate theory calculations were also performed on the OH + ClO reaction system and are in good agreement with the experimental results.
引用
收藏
页码:6540 / 6551
页数:12
相关论文
共 79 条
[1]   INFERRING THE ABUNDANCES OF CLO AND HO2 FROM SPACELAB-3 ATMOSPHERIC TRACE MOLECULE SPECTROSCOPY OBSERVATIONS [J].
ALLEN, M ;
DELITSKY, ML .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D2) :2913-2919
[2]   UNIMOLECULAR PROCESSES IN VIBRATIONALLY HIGHLY EXCITED CYCLOHEPTATRIENES .1. THERMAL-ISOMERIZATION IN SHOCK-WAVES [J].
ASTHOLZ, DC ;
TROE, J ;
WIETERS, W .
JOURNAL OF CHEMICAL PHYSICS, 1979, 70 (11) :5107-5116
[3]   EVALUATED KINETIC AND PHOTOCHEMICAL DATA FOR ATMOSPHERIC CHEMISTRY SUPPLEMENT-IV - IUPAC SUBCOMMITTEE ON GAS KINETIC DATA EVALUATION FOR ATMOSPHERIC CHEMISTRY [J].
ATKINSON, R ;
BAULCH, DL ;
COX, RA ;
HAMPSON, RF ;
KERR, JA ;
TROE, J .
JOURNAL OF PHYSICAL AND CHEMICAL REFERENCE DATA, 1992, 21 (06) :1125-1568
[4]   NUMBER OF MULTIPLY-RESTRICTED PARTITIONS [J].
BEYER, T ;
SWINEHART, DF .
COMMUNICATIONS OF THE ACM, 1973, 16 (06) :379-379
[5]   STRATOSPHERIC RESPONSE TO CHEMICAL PERTURBATIONS [J].
BRASSEUR, G ;
DERUDDER, A ;
TRICOT, C .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1985, 3 (02) :261-288
[6]   SPECIFIC RATE CONSTANTS K(E,J) AND PRODUCT STATE DISTRIBUTIONS IN SIMPLE BOND FISSION REACTIONS .2. APPLICATION TO HOOH-]OH+OH [J].
BROUWER, L ;
COBOS, CJ ;
TROE, J ;
DUBAL, HR ;
CRIM, FF .
JOURNAL OF CHEMICAL PHYSICS, 1987, 86 (11) :6171-6182
[7]   KINETICS OF THE REACTION OF OH WITH CLO [J].
BURROWS, JP ;
WALLINGTON, TJ ;
WAYNE, RP .
JOURNAL OF THE CHEMICAL SOCIETY-FARADAY TRANSACTIONS II, 1984, 80 :957-971
[8]   PRESSURE-DEPENDENCE OF THE REACTIONS OF HO2 WITH CL AND CLO [J].
CATTELL, FC ;
COX, RA .
JOURNAL OF THE CHEMICAL SOCIETY-FARADAY TRANSACTIONS II, 1986, 82 :1413-1426
[9]   Simultaneous measurements of stratospheric HOx, NOx, and Cl-x: Comparison with a photochemical model [J].
Chance, K ;
Traub, WA ;
Johnson, DG ;
Jucks, KW ;
Ciarpallini, P ;
Stachnik, RA ;
Salawitch, RJ ;
Michelsen, HA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D4) :9031-9043
[10]   CHLORINE CATALYZED DESTRUCTION OF OZONE - IMPLICATIONS FOR OZONE VARIABILITY IN THE UPPER-STRATOSPHERE [J].
CHANDRA, S ;
JACKMAN, CH ;
DOUGLASS, AR ;
FLEMING, EL ;
CONSIDINE, DB .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (05) :351-354