Kinetics of CH2OO reactions with SO2, NO2, NO, H2O and CH3CHO as a function of pressure

被引:181
作者
Stone, Daniel [1 ]
Blitz, Mark [1 ,2 ]
Daubney, Laura [1 ]
Howes, Neil U. M. [1 ]
Seakins, Paul [1 ,2 ]
机构
[1] Univ Leeds, Sch Chem, Leeds LS2 9JT, W Yorkshire, England
[2] Univ Leeds, Natl Ctr Atmospher Sci, Leeds, W Yorkshire, England
基金
英国工程与自然科学研究理事会;
关键词
CRIEGEE INTERMEDIATE CH2OO; GAS-PHASE OZONOLYSIS; ABSORPTION CROSS-SECTIONS; ATMOSPHERIC CHEMISTRY; RADICALS; YIELDS; OXIDATION; CH2((X)OVER-TILDE(3)B(1)); REACTIVITY; SPECTRUM;
D O I
10.1039/c3cp54391a
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
Kinetics of CH2OO Criegee intermediate reactions with SO2, NO2, NO, H2O and CH3CHO and CH2I radical reactions with NO2 are reported as a function of pressure at 295 K. Measurements were made under pseudo-first-order conditions using flash photolysis of CH2I2-O-2-N-2 gas mixtures in the presence of excess co-reagent combined with monitoring of HCHO reaction products by laser-induced fluorescence (LIF) spectroscopy and, for the reaction with SO2, direct detection of CH2OO by photoionisation mass spectrometry (PIMS). Rate coefficients for CH2OO + SO2 and CH2OO + NO2 are independent of pressure in the ranges studied and are (3.42 +/- 0.42) x 10(-11) cm(3) s(-1) (measured between 1.5 and 450 Torr) and (1.5 +/- 0.5) x 10(-12) cm(3) s(-1) (measured between 25 and 300 Torr), respectively. The rate coefficient for CH2OO + CH3CHO is pressure dependent, with the yield of HCHO decreasing with increasing pressure. Upper limits of 2 x 10(-13) cm(3) s(-1) and 9 x 10(-17) cm(3) s(-1) are placed on the rate coefficients for CH2OO + NO and CH2OO + H2O, respectively. The upper limit for the rate coefficient for CH2OO + H2O is significantly lower than has been reported previously, with consequences for modelling of atmospheric impacts of CH2OO chemistry.
引用
收藏
页码:1139 / 1149
页数:11
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