The hydration of SO 3 plays an important role in atmospheric sulfuric acid formation. Some atmospheric species can involve in and facilitate the reaction. In this work, using quantum chemical calculations, we show that oxalic acid, the most common dicarboxylic acid in the atmosphere, can effectively catalyze the hydration of SO 3 . The energy barrier of SO 3 hydration reaction catalyzed by oxalic acid (cTt, tTt, tCt and cCt conformers) is about or below 1 kcal mol -1 , which is lower 15 than the energy barrier of 5.73 kcal mol -1 for water-catalyzed SO 3 hydration. By comparing the rate of SO 3 hydration reaction catalyzed by oxalic acid and water, it can be found that the oxalic acid-catalyzed SO 3 hydration can compete with water-catalyzed SO 3 hydration in the upper troposphere. This leads us to conclude that the involvement of oxalic acid in SO 3 hydration to form H 2 SO 4 is significant in the atmosphere.
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