There is now much evidence that OH radicals and HO are spontaneously generated at the air-water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl, Br, I), which are abundant in marine aerosols, on this HO production. Droplets were generated via nebulization of water solutions containing NaSO, NaCl, NaBr, and NaI containing solutions, and HO was monitored as a function of the salt concentration under atmospheric relevant conditions.
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