posted on 2016-03-08, 00:00authored byNicole
K. Richards-Henderson, Allen H. Goldstein, Kevin R. Wilson
There
remains considerable uncertainty in how anthropogenic gas
phase emissions alter the oxidative aging of organic aerosols in the
troposphere. Here we observe a 10–20 fold acceleration in the
effective heterogeneous OH oxidation rate of organic aerosol in the
presence of SO2. This acceleration originates from the
radical chain reactions propagated by alkoxy radicals, which are formed
efficiently inside the particle by the reaction of peroxy radicals
with SO2. As the OH approaches atmospheric concentrations,
the radical chain length increases, transforming the aerosol at rates
predicted to be up to 10 times the OH-aerosol collision frequency.
Model predictions, constrained by experiments over orders of magnitude
changes in [OH] and [SO2], suggest that in polluted regions
the heterogeneous processing of organic aerosols by OH ([SO2] ≥ 40 ppb) occur on similar time scales as analogous gas-phase
oxidation reactions. These results provide evidence for a previously
unidentified mechanism by which organic aerosol oxidation is enhanced
by anthropogenic gas phase emissions.