Identification and Quantification of 4-Nitrocatechol Formed from OH and NO3 Radical-Initiated Reactions of Catechol in Air in the Presence of NOx: Implications for Secondary Organic Aerosol Formation from Biomass Burning

被引:137
作者
Finewax, Zachary [1 ,2 ]
de Gouw, Joost A. [2 ,3 ]
Ziemann, Paul J. [1 ,2 ]
机构
[1] Univ Colorado, Dept Chem & Biochem, Campus Box 215, Boulder, CO 80309 USA
[2] Univ Colorado, CIRES, Boulder, CO 80309 USA
[3] NOAA, Earth Syst Res Lab, Chem Sci Div, Boulder, CO 80305 USA
基金
美国国家科学基金会;
关键词
IONIZATION MASS-SPECTROMETRY; GAS-PHASE REACTIONS; RATE CONSTANTS; BROWN CARBON; ATMOSPHERIC CHEMISTRY; LIQUID-CHROMATOGRAPHY; RATE COEFFICIENTS; LIGHT-ABSORPTION; METHYL NITRITE; TRACE GASES;
D O I
10.1021/acs.est.7b05864
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Catechol (1,2-benzenediol) is emitted from biomass burning and produced from a reaction of phenol with OH radicals. It has been suggested as an important secondary organic aerosol (SOA) precursor, but the mechanisms of gas-phase oxidation and SOA formation have not been investigated in detail. In this study, catechol was reacted with OH and NO3 radicals in the presence of NOx in an environmental chamber to simulate daytime and nighttime chemistry. These reactions produced SOA with exceptionally high mass yields of 1.34 +/- 0.20 and 1.50 +/- 0.20, respectively, reflecting the low volatility and high density of reaction products. The dominant SOA product, 4-nitrocatechol, for which an authentic standard is available, was identified through thermal desorption particle beam mass spectrometry and Fourier transform infrared spectroscopy and was quantified in filter samples by liquid chromatography using UV detection. Molar yields of 4-nitrocatechol were 0.30 +/- 0.03 and 0.91 +/- 0.06 for reactions with OH and NO3 radicals, and thermal desorption measurements of volatility indicate that it is semivolatile at typical atmospheric aerosol loadings, consistent with field studies that have observed it in aerosol particles. Formation of 4-nitrocatechol is initiated by abstraction of a phenolic H atom by an OH or NO3 radical to form a beta-hydroxyphenoxy/o-semiquinone radical, which then reacts with NO2 to form the final product.
引用
收藏
页码:1981 / 1989
页数:9
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