Atmospheric Chemistry and Physics Discussions www.atmos-chem-phys-discuss.net 1680-7367 1680-7375 2 3 2002 10.5194/acpd-2-739-2002 http://www.atmos-chem-phys-discuss.net/2/739/2002/ http://www.atmos-chem-phys-discuss.net/2/739/2002/acpd-2-739-2002.html http://www.atmos-chem-phys-discuss.net/2/739/2002/acpd-2-739-2002.pdf 739 763 2002-06-12 Uptake of HNO₃ to deliquescent sea-salt particles C. Guimbaud F. Arens L. Gutzwiller H. W. Gäggeler M. Ammann Paul Scherrer Institute, CH-5232 Villigen PSI, Switzerland Department of Chemistry and Biochemistry, University of Bern, CH-3012 Bern, Switzerland The uptake of HNO₃ to deliquescent airborne sea-salt particles (RH = 55%, P = 760 torr, T = 300 K) at concentrations from 2 to 575 ppbv is measured in an aerosol flow tube using ¹³N as a tracer. Small particles (~ 70 nm diameter) are used in order to minimize the effect of diffusion in the gas phase on the mass transfer. Below 100 ppbv, an uptake coefficient (<font face="Symbol" >g</font>_upt) of 0.50 ± 0.20 is derived. At higher concentrations, the uptake coefficient decreases along with the consumption of aerosol chloride. Data interpretation is further supported by using the North American Aerosol Inorganics Model (AIM), which predicts the aqueous phase activities of ions and the gas-phase partial pressures of H₂O, HNO₃, and HCl at equilibrium for the NaCl/HNO₃/H₂O system. These simulations show that the low concentration data are obtained far from equilibrium, which implies that the uptake coefficient derived is equal to the mass accommodation coefficient under these conditions. The observed uptake coefficient can serve as input to modeling studies of atmospheric sea-salt aerosol chemistry. The main sea-salt aerosol burden in the marine atmosphere is represented by coarse mode particles (&gt; 1 <font face="Symbol" >m</font>m diameter). This implies that diffusion in the gas-phase is the limiting step to HNO₃ uptake until the sea-salt has been completely processed.