Secondary organic aerosol (SOA) formation due to limonene ozonolysis indoors is parameterized.
SOA formation is quantified with the aerosol mass fraction, AMF = Δ(SOA)/Δ(limonene).
Limonene is doubly unsaturated, so its AMF varies by a factor of 4 if one or both bonds are ozonated.
The ‘resultant AMF’ depends on ozone and limonene concentrations and air exchange rate (AER).
Framework predicts ‘resultant AMF’ based on reactants and AER using volatility basis set (VBS).