Secondary Organic Aerosol Formation from Nitrophenols Photolysis under Atmospheric Conditions

Secondary organic aerosol formation

Introduction Conclusions References

Secondary organic aerosol formation from isoprene photooxidation under high-NOx conditions

[1] The oxidation of isoprene (2-methyl-1,3-butadiene) is known to play a central role in the photochemistry of the troposphere, but is generally not considered to lead to the formation of secondary organic aerosol (SOA), due to the relatively high volatility of known reaction products. However, in the chamber studies described here, we measure SOA production from isoprene photooxidation under ...

Nonequilibrium atmospheric secondary organic aerosol formation and growth.

Airborne particles play critical roles in air quality, health effects, visibility, and climate. Secondary organic aerosols (SOA) formed from oxidation of organic gases such as α-pinene account for a significant portion of total airborne particle mass. Current atmospheric models typically incorporate the assumption that SOA mass is a liquid into which semivolatile organic compounds undergo insta...

Secondary organic aerosol formation from biomass burning

Secondary organic aerosol formation from aromatics

Secondary organic aerosol formation from m-xylene, toluene, and benzene N. L. Ng, J. H. Kroll, A. W. H. Chan, P. S. Chhabra, R. C. Flagan, and J. H. Seinfeld Departments of Chemical Engineering and Environmental Science and Engineering, California Institute of Technology, Pasadena, CA 91125, USA current address: Aerodyne Research, Inc. 45 Manning Road, Billerica, MA 01821, USA Received: 1 March...