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Atmospheric homogeneous nucleation of H<sub>2</sub>SO<sub>4</sub> and H<sub>2</sub>O

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Fig. 1. A flow reactor used in KSU aerosol nucleation setup. This new design allows for significantly less wall loss of H 2 SO 4 in the nucleation reactor (see Fig
Fig. 2a. [H 2 SO 4 ] measured by two CIMSs at the beginning of the nucleation reactor
Fig. 2b. The measured WLF with two CIMSs located at the beginning (initial [H 2 SO 4 ]) and end of the nucleation reactor (residual [H 2 SO 4 ]) as a function of initial [H 2 SO 4 ]
Fig. 3. The measured nucleation rates and [H 2 SO 4 ] when SO 2 and UV were introduced to the reactor
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