Nighttime measurements of particle number distribution and mass compos
ition, and concentrations of NO2, O-3, NH3, and HNO3, were made at nig
ht at a rural site in Ontario in August of 1992. A simple model of par
ticle growth was constructed to simulate the observed rapid growth of
aerosol mass in the 0.2 to 0.5 mu m diameter range. Both measurements
and model results indicate that the growth of accumulation mode aeroso
l mass was due to condensation of the nitrate radical, HNO3, and NH(3
)onto particles, with the formation of particle ammonium nitrate. The
results show that the reaction of O(3 )with NO2 in the isolated noctur
nal boundary layer can lead to the production of gas-phase nitric acid
. When this occurs in the presence of local ammonia emissions and pree
xisting particles, rapid growth of particle ammonium nitrate takes pla
ce. The model results show that most of the observed variations can be
accounted for by a coupled system of equations including dynamical an
d thermodynamic effects. The dynamical approach to equilibrium is suff
iciently fast that the gas-phase nitric acid concentrations are more s
ensitive to the magnitude of the thermodynamic equilibrium concentrati
on than the dynamical time constant. A simple parameterization for the
effects of sulphate on particle nitrate formation was developed and s
hown to provide a good estimate of the equilibrium concentration of ga
s-phase nitric acid.