An investigation was made of the influence of atmospheric concentrations (15 or 130 ppbv) of NO 2 on the aqueous-phase oxidation rate of S(IV) in the presence and absence of Fe(III), Mn(II) and Cr(VI) metal ions under controlled experimental conditions (pH, T, concentration of reactants, etc.). The reaction rate in the presence of the NO 2 flow was slower than the reaction rate using only clean air with an initial S(IV) concentration of 10 −4 mol/L. NO 2 appears to react with S(IV), producing a kind of inhibitor that slows down the reaction. Conversely, tenfold lower concentrations of S(IV) ([S(IV)] • = 10 −5 mol/L) caused a faster reaction in the presence of NO 2 than the reaction using purified air. Under these conditions, therefore, the equilibrium shifts to sulfate formation. With the addition of Fe(III), Mn(II) or Cr(VI) in the presence of a NO 2 flow, the reaction occurred faster under all the conditions in which S(IV) oxidation was investigated.