The diffusivity of
molecules relevant to condensed-phase chemistry
within viscous secondary organic aerosol (SOA) remains highly uncertain.
Whereas there has been an effort to characterize water diffusivity
as well as the diffusivity of larger compounds, data are lacking almost
entirely for small molecules, such as carbon dioxide (CO2). Here we use photochemically generated CO2 in single
particles of aqueous citric acid as a SOA proxy, levitated in an electrodynamic
balance, to deduce CO2 diffusivity in the particle with
unprecedented accuracy. For medium viscosities at intermediate relative
humidities (∼25–40% RH), we find CO2 diffusivities D
CO2
≈ 10–14 m2 s–1, agreeing with the Stokes–Einstein
relationship based on current viscosity data but 10 times lower than
that for water. Conversely, under dry high-viscosity conditions, we
find that D
CO2
≈ 10–16 m2 s–1, which is 10
times higher than for water. We infer that the chemical degradation
of atmospheric SOA particles will likely not be limited by CO2 diffusivity.