The reaction of gaseous N 2 O 5 with sea salt and its components is a potential source of halogen atoms in the marine boundary layer. There are two possible reaction paths when water is present on the salt surface. Reaction with the chloride ion forms nitryl chloride (ClNO 2 ), a photolyzable compound: N 2 O 5 + NaCl ! ClNO 2 + NaNO 3 , while hydrolysis of N 2 O 5 generates HNO 3 that can react further with NaCl to form gaseous HCl: N 2 O 5 + H 2 O (on NaCl) ! 2 HNO 3 , HNO 3 + NaCl ! HCl + NaNO 3 . We report here Knudsen cell studies at 23 C of the reaction of N 2 O 5 with NaCl, using less than one layer of salt particles. A model, which takes into account the effective salt surface area exposed to the gas, was applied, allowing for the determination of uptake coefficients without introducing uncertainties associated with diffusion into multiple layers of salt particles. The net uptake coefficient for the sum of both channels for the N 2 O 5 reaction was measured to be g N 2 O 5 ¼ (2.9 AE 1.7) Â 10
À3, where the error cited is the 2s statistical error. The cumulative error is estimated to be better than a factor of three. Both ClNO 2 and HCl were observed as gaseous products from the N 2 O 5 -salt reaction and the branching ratio for ClNO 2 was 0.73 AE 0.28 (2s). A limited number of experiments were carried out for the reaction with synthetic sea salt, resulting in an uptake coefficient of about an order of magnitude larger than for NaCl, and a ClNO 2 yield of 100%. We propose a mechanism for this reaction in which surfaceadsorbed water plays a key role in the competition between hydrolysis of N 2 O 5 to generate HNO 3 and the reaction with NaCl to generate ClNO 2 . Reaction with NaCl is shown to be a potentially important source of ClNO 2 , and thus, of highly reactive chlorine atoms in urban marine regions at dawn. Application of our model to previous data from this laboratory for the reaction of chlorine nitrate (ClONO 2 ) with fractional layers of NaCl gives a corrected uptake coefficient of g ClONO 2 ¼ (2.4 AE 1.2) Â 10 À2 (2s), which suggests that the ClONO 2 -NaCl reaction may contribute significantly to the observed concentrations of Cl 2 in the marine boundary layer.