Rate coefficients for reaction of OH with acetone between 202 and 395 K

被引:133
作者
Wollenhaupt, M
Carl, SA
Horowitz, A
Crowley, JN
机构
[1] Max Planck Inst Chem, Div Atmospher Chem, D-55020 Mainz, Germany
[2] Soreq Nucl Res Ctr, IL-81800 Yavne, Israel
关键词
D O I
10.1021/jp993738f
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 kinetics of the title reaction were investigated between 202 and 395 K and at 20, 50, and 100 Ton: of Ar or N-2 bath gas using pulsed laser photolysis (PLP) generation of OH combined with both resonance fluorescence (RF) and laser-induced fluorescence (LIF) detection. OH was generated either by the sequential 439 nm, two-photon dissociation of NO2 in the presence of H-2, or by HONO photolysis at 351 nm. The accuracy of the rate constants obtained was enhanced by optical absorption measurements of acetone concentrations both before and after the photolysis reactor. The temperature dependence is not described by a simple Arrhenius expression but by k(1) (202-395 K) = 8.8 x 10(-12) exp(-1320/T) + 1.7 x 10(-14) exp(423/T) cm(3) s(-1), indicating that a simple H atom abstraction may not be the only reaction mechanism. The estimated total error (95% confidence) associated with the rate coefficient derived from this expression is estimated as 5% and is independent of temperature. The curvature in the Arrhenius plot results in a significantly larger rate coefficient at low temperatures than obtained by extrapolation of the previous measurement and implies greater significance for the reaction with OH as a sink for acetone in the upper troposphere than presently assumed.
引用
收藏
页码:2695 / 2705
页数:11
相关论文
共 44 条
[1]   Observation of upper tropospheric sulfur dioxide- and acetone-pollution: Potential implications for hydroxyl radical and aerosol formation [J].
Arnold, F ;
Schneider, J ;
Gollinger, K ;
Schlager, H ;
Schulte, P ;
Hagen, DE ;
Whitefield, PD ;
vanVelthoven, P .
GEOPHYSICAL RESEARCH LETTERS, 1997, 24 (01) :57-60
[2]   Acetone in the upper troposphere and lower stratosphere: Impact on trace gases and aerosols [J].
Arnold, F ;
Burger, V ;
DrosteFanke, B ;
Grimm, F ;
Krieger, A ;
Schneider, J ;
Stilp, T .
GEOPHYSICAL RESEARCH LETTERS, 1997, 24 (23) :3017-3020
[3]   A SHOCK-TUBE STUDY OF THE REACTION OF METHYL RADICALS WITH HYDROXYL RADICALS [J].
BOTT, JF ;
COHEN, N .
INTERNATIONAL JOURNAL OF CHEMICAL KINETICS, 1991, 23 (11) :1017-1033
[4]   RATE COEFFICIENTS FOR THE REACTION OF OH WITH HONO BETWEEN 298-K AND 373-K [J].
BURKHOLDER, JB ;
MELLOUKI, A ;
TALUKDAR, R ;
RAVISHANKARA, AR .
INTERNATIONAL JOURNAL OF CHEMICAL KINETICS, 1992, 24 (08) :711-725
[5]  
Calvert J.G., 1966, Photochemistry
[6]   SOURCES AND SINKS OF ACETONE IN THE TROPOSPHERE - BEHAVIOR OF REACTIVE HYDROCARBONS AND A STABLE PRODUCT [J].
CHATFIELD, RB ;
GARDNER, EP ;
CALVERT, JG .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D4) :4208-4216
[7]   RATE CONSTANTS FOR THE GAS-PHASE REACTIONS OF OH RADICALS WITH BETA-DIMETHYLSTYRENE AND ACETONE - MECHANISM OF BETA-DIMETHYLSTYRENE NOX- AIR PHOTO-OXIDATION [J].
CHIORBOLI, C ;
BIGNOZZI, CA ;
MALDOTTI, A ;
GIARDINI, PF ;
ROSSI, A ;
CARASSITI, V .
INTERNATIONAL JOURNAL OF CHEMICAL KINETICS, 1983, 15 (06) :579-586
[8]   ATMOSPHERIC PHOTO-OXIDATION REACTIONS - RATES, REACTIVITY, AND MECHANISM FOR REACTION OF ORGANIC-COMPOUNDS WITH HYDROXYL RADICALS [J].
COX, RA ;
DERWENT, RG ;
WILLIAMS, MR .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1980, 14 (01) :57-61
[9]   OH formation in the photoexcitation of NO2 beyond the dissociation threshold in the presence of water vapor [J].
Crowley, JN ;
Carl, SA .
JOURNAL OF PHYSICAL CHEMISTRY A, 1997, 101 (23) :4178-4184
[10]   Temperature dependent rate constants for the gas-phase reaction between OH and CH3OCl [J].
Crowley, JN ;
CampuzanoJost, P ;
Moortgat, GK .
JOURNAL OF PHYSICAL CHEMISTRY, 1996, 100 (09) :3601-3606