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Is Secondary Organic Aerosol Yield Governed by Kinetic Factors Rather Than Equilibrium Partitioning?

The numerical description of the formation of secondary organic aerosol (SOA) in the atmosphere relies on the use of particle yields, which are often determined in chamber experiments. What is sometimes not appreciated is that such yields (i) can be defined in different ways and (ii) depend on atmospheric co Modeling in Environmental Chemistry

Authors:   Chen Wang; Frank Wania; Kai-Uwe Goss
Journal:   Journal of Environmental Monitoring
DOI:   10.1039/C7EM00451F
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