Organic
nitrate ester compounds (RONO2) are an important
sink for nitrogen oxides (NO
x
≡
NO + NO2) that impact ozone and organic aerosol formation
in the lower atmosphere. While RONO2 formation from gas
phase oxidation chemistry and heterogeneous reactions involving reactive
uptake of NO3 into organic aerosols is well documented, in situ bulk-aqueous-phase production of RONO2 within organic aerosols has not been explored as extensively. Here,
we provide evidence that RONO2 species are produced during
aqueous phase reactions of nitronium (NO2
+)
with humic and fulvic acids, which are used as surrogates for aerosol
organic matter. X-ray photoelectron spectroscopy (XPS) and high-resolution
mass spectrometry were used to characterize nitrogen functional groups
and changes in bulk chemical composition during nitration reactions.
Correlations between the organic N abundance in reacted humic and
fulvic acids and functional group abundance measured by solid-state 13C NMR indicate that NO2
+ targets the
lipid fraction of the organic matter. Fourier transform infrared spectroscopy
(FTIR) analysis of model lipid compounds shows that the reaction of
NO2
+ with terminal alcohols (ROH) and alkenes
is a source of stable RONO2 compounds. Further, the low-pH
environment of most nitrate aerosols is expected to enhance the total
terminal ROH pool through acid-catalyzed ester hydrolysis within the
lipid-like fraction of natural organic matter. Our findings demonstrate
that multiphase oxidation of organic matter by NO2
+, along with air-particle partitioning of products from gas-phase
chemistry, may be an important source of particle-phase organic nitrates.