Unimolecular decomposition kinetics of the stabilised Criegee intermediates CH2OO and CD2OO

被引:47
作者
Stone, Daniel [1 ]
Au, Kendrew [2 ]
Sime, Samantha [1 ]
Medeiros, Diogo J. [1 ]
Blitz, Mark [1 ]
Seakins, Paul W. [1 ]
Decker, Zachary [2 ,3 ]
Sheps, Leonid [2 ]
机构
[1] Univ Leeds, Sch Chem, Leeds LS2 9JT, W Yorkshire, England
[2] Sandia Natl Labs, Combust Res Facil, Livermore, CA 94551 USA
[3] Univ Colorado, Boulder, CO 80302 USA
基金
英国自然环境研究理事会;
关键词
CORRELATED MOLECULAR CALCULATIONS; GAUSSIAN-BASIS SETS; ABSORPTION-SPECTRUM; RATE COEFFICIENTS; MASTER EQUATION; SO2; TEMPERATURE; OZONOLYSIS; CHEMISTRY; CH2I2;
D O I
10.1039/c8cp05332d
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
Decomposition kinetics of stabilised CH2OO and CD2OO Criegee intermediates have been investigated as a function of temperature (450-650 K) and pressure (2-350 Torr) using flash photolysis coupled with time-resolved cavity-enhanced broadband UV absorption spectroscopy. Decomposition of CD2OO was observed to be faster than CH2OO under equivalent conditions. Production of OH radicals following CH2OO decomposition was also monitored using flash photolysis with laser-induced fluorescence (LIF), with results indicating direct production of OH in the v = 0 and v = 1 states in low yields. Master equation calculations performed using the Master Equation Solver for Multi-Energy well Reactions (MESMER) enabled fitting of the barriers for the decomposition of CH2OO and CD2OO to the experimental data. Parameterisations of the decomposition rate coefficients, calculated by MESMER, are provided for use in atmospheric models and implications of the results are discussed. For CH2OO, the MESMER fits require an increase in the calculated barrier height from 78.2 kJ mol(-1) to 81.8 kJ mol(-1) using a temperature-dependent exponential down model for collisional energy transfer with <Delta E >(down) = 32.6(T/298 K)(1.7) cm(-1) in He. The low-and highpressure limit rate coefficients are k(1,0) = 3.2 x 10(-4)(T/298)(-5.81)exp(-12 770/T) cm(3) s(-1) and k(1, infinity) = 1.4 x 10(13)(T/298)(0.06)exp(-10 010/T) s(-1), with median uncertainty of B12% over the range of experimental conditions used here. Extrapolation to atmospheric conditions yields k(1)(298 K, 760 Torr) = 1.1(-1.1)(+1.5)x10(-3) s(-1). For CD2OO, MESMER calculations result in hDEidown = 39.6(T/298 K) 1.3 cm(-1) in He and a small decrease in the calculated barrier to decomposition from 81.0 kJ mol(-1) to 80.1 kJ mol(-1). The fitted rate coefficients for CD2OO are k(2,0) = 5.2 x 10(-5)(T/298)(-5.28)exp(-11 610/T) cm(3) s(-1) and k(2, infinity) = 1.2 x 10(13)(T/298)(0.06) exp(-9800/T) s(-1), with overall error of similar to 6% over the present range of temperature and pressure. The extrapolated k(2)(298 K, 760 Torr) = 5.5(-5.5)(+9.2) x 10(-3) s(-1). The master equation calculations for CH2OO indicate decomposition yields of 63.7% for H-2 + CO2, 36.0% for H2O + CO and 0.3% for OH + HCO with no significant dependence on temperature between 400 and 1200 K or pressure between 1 and 3000 Torr.
引用
收藏
页码:24940 / 24954
页数:15
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