The heterogeneous replacement of chloride by nitrate in individual sea
-salt particles was monitored continuously over time in the tropospher
e with the use of aerosol time-of-flight mass spectrometry. Modeling c
alculations show that the observed chloride displacement process is co
nsistent with a heterogeneous chemical reaction between sea-salt parti
cles and gas-phase nitric acid, leading to sodium nitrate production i
n the particle phase accompanied by liberation of gaseous HCl from the
particles. Such single-particle measurements, combined with a single-
particle model, make it possible to monitor and explain heterogeneous
gas/particle chemistry as it occurs in the atmosphere.