A simple yet physically based and highly accurate parameterization of the nucleation rate is obtained. In essence, the log nucleation rate is expanded in special coordinates suggested by the first and second nucleation theorems and only linear terms are required. The results support an Arrhenius model of the temperature dependence and are highly accurate over the range of a typical set of measurements – about 3–5 orders of magnitude in nucleation rate. This range is likely sufficient for most applications to atmospheric particle formation, which now seem feasible without the need for bulk properties estimation, as would be required using classical nucleation theory, and without significant higher-order corrections to the linear result.
Keywords Heterogeneous nucleation, nucleation theorem, Arrhenius temperature dependence
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McGraw, R. (2007). Arrhenius Temperature Dependence of Homogeneous Nucleation Rates. In: O'Dowd, C.D., Wagner, P.E. (eds) Nucleation and Atmospheric Aerosols. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-6475-3_29
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