A possible unaccounted source of atmospheric sulfate formation: amine-promoted hydrolysis and non-radical oxidation of sulfur dioxide.

Numerous field and laboratory studies have shown that amines, especially dimethylamine (DMA), are crucial to atmospheric particulate nucleation. However, the molecular mechanism by which amines lead to atmospheric particulate formation is still not fully understood. Herein, we show that DMA molecules can also promote the conversion of atmospheric SO to sulfate. Based on simulations, we find that in the presence of DMA, the originally endothermic and kinetically unfavourable hydrolysis reaction between gaseous SO and water vapour can become both exothermic and kinetically favourable. The resulting product, bisulfite NH(CH) ·HSO , can be readily oxidized by ozone under ambient conditions. Kinetic analysis suggests that the hydrolysis rate of SO and DMA with water vapour becomes highly competitive with and comparable to the rate of the reaction between SO and OH·, especially under the conditions of heavily polluted air and high humidity. We also find that the oxidants NO and NO (whose role in sulfate formation is still under debate) appear to play a much less significant role than ozone in the aqueous oxidation reaction of SO. The newly identified oxidation mechanism of SO promoted by both DMA and O provides another important new source of sulfate formation in the atmosphere.