Abstract
Abstract. Rate coefficients, k, for the gas-phase reaction of CH3COCHO (methylglyoxal) with the OH and NO3 radicals and (CHO)2 (glyoxal) with the NO3 radical are reported. Rate coefficients for the OH + CH3COCHO (k1) reaction were measured under pseudo-first-order conditions in OH as a function of temperature (211–373 K) and pressure (100–220 Torr, He and N2 bath gases) using pulsed laser photolysis to produce OH radicals and laser induced fluorescence to measure its temporal profile. k1 was found to be independent of the bath gas pressure with k1(295 K) = (1.29 ± 0.13) × 10−11 cm3 molecule−1 s−1 and a temperature dependence that is well represented by the Arrhenius expression k1(T) = (1.74 ± 0.20) × 10−12 exp[(590 ± 40)/T] cm3 molecule−1 s−1 where the uncertainties are 2σ and include estimated systematic errors. Rate coefficients for the NO3 + (CHO)2 (k3) and NO3 + CH3COCHO (k4) reactions were measured using a relative rate technique to be k3(296 K) = (4.0 ± 1.0) × 10−16 cm3 molecule−1 s−1 and k4(296 K) = (5.1 ± 2.1) × 10−16 cm3 molecule−1 s−1. k3(T) was also measured using an absolute rate coefficient method under pseudo-first-order conditions at 296 and 353 K to be (4.2 ± 0.8) × 10−16 and (7.9 ± 3.6) × 10−16 cm3 molecule−1 s−1, respectively, in agreement with the relative rate result obtained at room temperature. The atmospheric implications of the OH and NO3 reaction rate coefficients measured in this work are discussed.
Highlights
Methylglyoxal, CH3COCHO, and glyoxal, (HCO)2, are dicarbonyls that play an important role in atmospheric chemistry as tracers of atmospheric biogenic and anthropogenic organic chemistry
Rate coefficients for the gas-phase reaction of OH with CH3COCHO were measured as a function of temperature (211–373 K) and pressure (100–200 Torr in He and N2) by producing OH via pulsed laser photolysis (PLP) and measuring its temporal profile using laser-induced fluorescence (LIF)
The key components of the apparatus were (1) a temperature controlled reactor where OH was produced by pulsed laser photolysis and its temporal profile measured by laser-induced fluorescence, (2) pulsed lasers used to generate and detect OH, (3) a gas handling manifold, and (4) UV and infrared absorption setups to determine the methylglyoxal concentration on-line using UV absorption at 184.9 nm and Fourier transform infrared (FTIR) spectroscopy
Summary
Methylglyoxal, CH3COCHO, and glyoxal, (HCO), are dicarbonyls that play an important role in atmospheric chemistry as tracers of atmospheric biogenic and anthropogenic organic chemistry. Several studies of the rate coefficient for Reaction (R1), k1, have been reported to date with room temperature values falling in the range (7–16) × 10−12 cm molecule−1 s−1 (Baeza-Romero et al, 2007; Kleindienst et al, 1982; Plum et al, 1983; Tyndall et al, 1995). Rate coefficients for the reaction of the NO3 radical with glyoxal and methylglyoxal are reported
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