Sunlight-driven chemical transformations
of secondary organic aerosol
(SOA) are important for understanding the climate- and health-relevant
properties of atmospheric particulate matter, but these photochemical
processes are not well understood. We measured the photodegradation
rates of SOA by observing condensed-phase photochemical processes
over many days of UV exposure. The experiments relied on a quartz
crystal microbalance to quantify the mass loss rate from SOA materials
prepared by ozonolysis of d-limonene and α-pinene and
photo-oxidation of toluene under either high or low NO
x
conditions. We observed that 254 nm irradiation
degraded SOA almost entirely after 24 h. The mass loss rates were
higher for toluene-derived SOA, which absorbs strongly at 254 nm.
Irradiation at 305 nm, which is more relevant for the troposphere,
resulted in larger mass loss rates from SOA generated from α-pinene
and d-limonene, even though toluene-derived SOA had a higher
absorption coefficient. In all 305 nm irradiation experiments, the
initial mass loss rate was high (corresponding to 1–5% fractional
mass loss per hour), but it slowed down after 24 h of irradiation,
with a photorecalcitrant fraction of SOA degrading much slower (<1%
fractional mass loss per hour). The mass loss rates were observed
to increase at a higher relative humidity because volatile photoproducts
could diffuse out of SOA faster. Long-term changes in the chemical
composition of limonene ozonolysis SOA were examined using high-resolution
electrospray ionization mass spectrometry and revealed a more complex
mixture of species after photodegradation compared to the initial
SOA. The compounds in the photodegraded sample had on average lower
molecular weights, lower H/C ratios, and higher O/C ratios compared
to the compounds in the un-photolyzed sample. These experiments confirm
that condensed-phase photochemistry is an important aging mechanism
for SOA during long-range transport.