The formation and decomposition of
peroxyacetyl nitrate (PAN),
an important atmospheric nitrogen oxide reservoir, can impact the
level and cycling of free radicals and nitrogen compounds in the atmosphere.
PAN sinks are poorly understood, highlighting the importance of elucidating
the heterogeneous reaction of PAN on aerosol surfaces. Here, we report
for the first time the uptake behavior, kinetics, and potential mechanism
of PAN uptake on real-world aerosol PM2.5 using a flow
tube system. The uptake coefficients (γ) of PAN increased non-linearly
from (1.5 ± 0.7) × 10–5 at 0% relative
humidity (RH) to (9.3 ± 2.0) × 10–5 at
80% RH. The γ decrease with increasing initial PAN concentration
is consistent with the Langmuir–Hinshelwood mechanism. Organic
components of aerosols may promote heterogeneous loss of PAN through
redox reactions. Higher γ occurs with higher water content,
lower pH, and lower ionic strength in the aqueous phase of aerosols.
The present study suggests that heterogeneous reaction of PAN on ambient
aerosols plays a non-negligible role in the atmospheric PAN budget
and provides new insights into the role of PAN in promoting atmospheric
oxidation capacity during hazy periods with cold and wet weather conditions.