Journal
JOURNAL OF PHYSICAL CHEMISTRY A
Volume 120, Issue 16, Pages 2561-2568Publisher
AMER CHEMICAL SOC
DOI: 10.1021/acs.jpca.6b01402
Keywords
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Funding
- National Science Foundation [AGS-1219508, AGS-1420007]
- Div Atmospheric & Geospace Sciences
- Directorate For Geosciences [1420007] Funding Source: National Science Foundation
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Previous studies have shown that 1,4-hydroxycarbonyls, which are often major products of the atmospheric oxidation of hydrocarbons, can undergo acid-catalyzed cyclization and dehydration in aerosol particles to form highly reactive unsaturated dihydrofurans. In this study the kinetics of dehydration of cyclic hemiacetals, the rate-limiting step in this process, was investigated in a series of environmental chamber experiments in which secondary organic aerosol (SOA) containing cyclic hemiacetals was formed from the reaction of n-pentadecane with OH radicals in dry air in the presence of HNO3. A particle beam mass spectrometer was used to monitor the formation and dehydration of cyclic hemiacetals in real time, and SOA and HNO3 were quantified in filter samples by gravimetric analysis and ion chromatography. Measured dehydration rate constants increased linearly with increasing concentration of HNO3 in the gas phase and in SOA, corresponding to catalytic rate constants of 0.27 h(-1) ppmv(-1) and 7.0 h(-1) M-1, respectively. The measured Henry's law constant for partitioning of HNO3 into SOA was 3.7 x 10(4) M atm(-1), similar to 25% of the value for dissolution into water, and the acid dissociation constant was estimated to be <8 x 10(-4), at least a factor of 10(4) less than that for HNO3 in water. The results indicate that HNO3 was only weakly dissociated in the SOA and that dehydration of cyclic hemiacetals was catalyzed by molecular HNO3 rather than by H+. The Henry's law constant and kinetics relationships measured here can be used to improve mechanisms and models of SOA formation from the oxidation of hydrocarbons in dry air in the presence of NOx, which are conditions commonly used in laboratory studies. The fate of cyclic hemiacetals in the atmosphere, where the effects of higher relative humidity, organic/aqueous phase separation, and acid catalysis by molecular H2SO4 and/or H+ are likely to be important, is discussed.
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