| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4439740 | Atmospheric Environment | 2011 | 10 Pages |
Abstract
⺠All the SOA from monoterpene ozonolysis evaporates after 16 s at temperatures less than 90 °C. ⺠The α- and β-pinene SOA formed at high NOx conditions is more volatile. ⺠The formation relative humidity has a small effect on volatility. ⺠The results are consistent with the volatility basis-set parameters. ⺠There are significant mass transfer limitations in the evaporation of biogenic SOA.
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Authors
Byong-Hyoek Lee, Jeffrey R. Pierce, Gabriella J. Engelhart, Spyros N. Pandis,