A three-dimensional, size-resolved and chemically resolved aerosol mod
el is developed. Gas-to-particle conversion is represented by dynamic
mass transfer between the gas and aerosol phases. Particle-phase therm
odynamics is computed by a new thermodynamic model, Simulating Composi
tion of Atmospheric Particles at Equilibrium 2. The aerosol model is a
pplied to simulate gas and aerosol behavior in the August 27-29, 1987,
episode in the South Coast Air Basin of California. The assumption th
at volatile inorganic species such as NH4NO3 are at instantaneous, loc
al equilibrium is examined.