Haze events in China megacities involve the rapid oxidation of SO 2 to sulfate aerosol. Given the 9 weak photochemistry taking place in these optically thick hazes, it has been hypothesized that 10 SO 2 is mostly oxidized by NO 2 emissions in the bulk of pH > 5.5 aerosols. Since NO 2 (g) 11 dissolution in water is very slow and aerosols are more acidic, we decided to test such 12 hypothesis. Herein, we report that > 95% NO 2 (g) disproportionates: 2 NO 2 (g) + H 2 O(l) = H + + 13 NO 3 -(aq) + HONO (R1), upon hitting the surface of NaHSO 3 aqueous microjets exposed to 14 NO 2 (g) for < 50 µs, thereby giving rise to strong NO 3 -(m/z = 62) signals detected by online 15 electrospray mass spectrometry, rather than oxidizing HSO 3 -(m/z = 81) to HSO 4 -(m/z = 97) in 16 the relevant pH 3-6 range. Since NO 2 (g) will be consumed via R1 on the surface of typical 17 aerosols, the oxidation of S(IV) may in fact be driven by the HONO/NO 2 -generated therein. 18 S(IV) heterogeneous oxidation rates are expected to primarily depend on the surface density and 19 liquid water content of the aerosol, which are enhanced by fine aerosol and high humidity. 20Whether aerosol acidity affects the oxidation of S(IV) by HONO/NO 2 -remains to be elucidated. 21
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