Abstract:The phase states and glass transition temperatures (T g ) of secondary organic aerosol (SOA) particles are important to resolve for understanding the formation, growth, and fate of SOA as well as their cloud formation properties. Currently, there is a limited understanding of how T g changes with the composition of organic and inorganic components of atmospheric aerosol. Using broadband dielectric spectroscopy, we measured the T g of organic mixtures containing isoprene epoxydiol (IEPOX)-derived SOA components… Show more
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