The influences of mass loading and rapid dilution of secondary organic aerosol on particle volatility
The thermally induced evaporation of secondary organic aerosol (SOA) has been characterized for SOA formed from the dark ozonolysis of α-pinene at initial mass concentrations ranging from 1 to 800 μg m<sup>−3</sup>. Temperature-dependent particle size distributions were measu...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-08-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | http://www.atmos-chem-phys.net/15/9327/2015/acp-15-9327-2015.pdf |