Temperature dependent rate coefficient for the reaction O(3P)+NO2→NO+O2

被引:52
作者
Gierczak, T
Burkholder, JB
Ravishankara, AR
机构
[1] NOAA, ERL, Aeron Lab, Boulder, CO 80303 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] Univ Warsaw, Dept Chem, PL-02089 Warsaw, Poland
[4] Univ Colorado, Dept Chem & Biochem, Boulder, CO 80309 USA
关键词
D O I
10.1021/jp983962p
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 rate coefficient (k(1)) for the reaction O(P-3) + NO2 --> O-2 + NO was measured under pseudo-first-order conditions in O(P-3) atom concentration over the temperature range 220-412 K. Measurements were made using pulsed laser photolysis of NO2 to produce oxygen atoms and time-resolved vacuum UV resonance fluorescence detection of O atoms. The NO2 concentration was measured using three techniques: flow rate, UV absorption, and chemical titration (NO + O-3 --> NO2 + O-2) The NO2 UV absorption cross section at 413.4 nm was determined as a function of temperature using the chemical titration and flow methods. Including the low-temperature data of Harder et al.(1), the temperature-dependent NO2 cross section is given by sigma(413.4)(T) (9.49 - 0.00549 T) x 10(-19) cm(2) molecule(-1). The measured rate coefficients for reaction 1 can be expressed as k(1)(T) = (5.26 +/- 0.60) x 10(-12) exp[(209 +/- 35)/T] cm(3) molecule(-1) s(-1), where the quoted uncertainties are 2 sigma and include estimated systematic errors. This result is compared with previously reported measurements of k(1).
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页码:877 / 883
页数:7
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