Rethinking Organic Aerosols: Semivolatile Emissions and Photochemical Aging

By A. Robinson, N. Donahue, M. Shrivastava, E. A. Weitkamp, A. Sage, A. Grieshop, T. Lane, J. Pierce, Spyros N. Pandis. Science, 2007

1,870 citations recorded by the source corpus.

Subfields: Atmospheric Science, Automotive Engineering, Health, Toxicology and Mutagenesis

View Paper: https://www.semanticscholar.org/paper/1eedb96b3f00c9ecc24845107909cd74dee9e39b

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. C. Cappa
2. D. Worsnop
3. T. Onasch
4. M. Canagaratna
5. J. Jayne
6. J. Jimenez
7. P. DeCarlo
8. C. Heald

In Automotive Engineering

1. C. Cappa
2. J. Jimenez
3. P. DeCarlo
4. Yutaka Kondo
5. D. Worsnop
6. F. Drewnick
7. S. Borrmann

In Health, Toxicology and Mutagenesis

1. C. Cappa
2. D. Worsnop
3. T. Onasch
4. J. Jimenez
5. P. DeCarlo
6. P. Adams
7. Spyros N. Pandis
8. Yutaka Kondo

Citations in the corpus

• Understanding atmospheric organic aerosols via factor analysis of aerosol mass spectrometry: a review (2011, background): “[119]) treats primary emissions as semi-volatile species (SVOCs) that can evaporate from the particle phase after emissions and then react to form less volatile SOA.”
• Evolution of organic aerosol mass spectra upon heating: implications for OA phase and partitioning behavior (2010, methodology): “Atmospheric models of OA formation generally follow from absorptive partitioning theory (Pankow, 1994), using either a two-product (Odum et al., 1996) or volatility basis-set (Donahue et al., 2006;Robinson et al., 2007) framework.”
• Modeling global secondary organic aerosol formation and processing with the volatility basis set: Implications for anthropogenic secondary organic aerosol (2010, background): “Recently, this assumption has been challenged [Shrivastava et al., 2006; Robinson et al., 2007].”
• A simplified description of the evolution of organic aerosol composition in the atmosphere (2010, background): “These results suggest that the chemical evolution of OA in the atmosphere may be simply represented in models.”
• Ubiquity and dominance of oxygenated species in organic aerosols in anthropogenically‐influenced Northern Hemisphere midlatitudes (2007, result): “…is indicative of an extended SOA source (either from urban emissions or from regional biogenic emissions), consistent with recent studies [Goldstein and Galbally, 2007; Robinson et al., 2007], although large amounts of OOA can also be produced in the urban environment [Volkamer et al., 2006].”