Effects of the sample matrix on the photobleaching and photodegradation of toluene-derived secondary organic aerosol compounds
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Published:2022-08-09
Issue:15
Volume:22
Page:10155-10171
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Klodt Alexandra L., Adamek Marley, Dibley Monica, Nizkorodov Sergey A.ORCID, O'Brien Rachel E.
Abstract
Abstract. Secondary organic aerosol (SOA) generated from the photooxidation
of aromatic compounds in the presence of oxides of nitrogen (NOx) is
known to efficiently absorb ultraviolet and visible radiation. With exposure
to sunlight, the photodegradation of chromophoric compounds in the SOA
causes this type of SOA to slowly photobleach. These photodegradation
reactions may occur in cloud droplets, which are characterized by low
concentrations of solutes, or in aerosol particles, which can have highly
viscous organic phases and aqueous phases with high concentrations of
inorganic salts. To investigate the effects of the surrounding matrix on the
rates and mechanisms of photodegradation of SOA compounds, SOA was prepared
in a smog chamber by photooxidation of toluene in the presence of NOx.
The collected SOA was photolyzed for up to 24 h using near-UV radiation
(300–400 nm) from a xenon arc lamp under different conditions: directly on
the filter, dissolved in pure water, and dissolved in 1 M ammonium sulfate.
The SOA mass absorption coefficient was measured as a function of
irradiation time to determine photobleaching rates. Electrospray ionization
high-resolution mass spectrometry coupled to liquid chromatography
separation was used to observe changes in SOA composition resulting from the
irradiation. The rate of decrease in SOA mass absorption coefficient due to
photobleaching was the fastest in water, with the presence of 1 M ammonium
sulfate modestly slowing down the photobleaching. By contrast,
photobleaching directly on the filter was slower. The high-resolution
mass spectrometry analysis revealed an efficient photodegradation of
nitrophenol compounds on the filter but not in the aqueous phases, with
relatively little change observed in the composition of the SOA irradiated
in water or 1 M ammonium sulfate despite faster photobleaching than in the
on-filter samples. This suggests that photodegradation of nitrophenols
contributes much more significantly to photobleaching in the organic phase
than in the aqueous phase. We conclude that the SOA absorption coefficient
lifetime with respect to photobleaching and lifetimes of individual
chromophores in SOA with respect to photodegradation will depend strongly on
the sample matrix in which SOA compounds are exposed to sunlight.
Funder
Directorate for Geosciences
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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