Identification of Polymers as Major Components of Atmospheric Organic Aerosols
By M. Kalberer, D. Paulsen, M. Sax, M. Steinbacher, J. Dommen, A. Prévôt, R. Fisseha, E. Weingartner, V. Frankevich, R. Zenobi and 1 more. Science, 2004
972 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Engineering
View Paper: https://www.semanticscholar.org/paper/589846315c3986d23c9f6cdad1f181c8b63f2fdb
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In Atmospheric Science
- Markku Kulmala
- V. Kerminen
- K. Lehtinen
- M. Shiraiwa
- I. Riipinen
- T. Anttila
- Lauri Laakso
- Miikka Dal Maso
In Environmental Engineering
Citations in the corpus
- Competition between water uptake and ice nucleation by glassy organic aerosol particles (2014, positive): “Oligomerization is however also expected for aromatic SOA, shown e.g. by Kalberer et al. (2004), which would lead to higherTg,org (Koop et al., 2011).”
- Initial steps of aerosol growth (2004, positive): “An increasing piece of evidence has emerged on the important role of various multi-phase reactions in secondary organic aerosol formation (Jang et al., 2002; Inuma et al., 2004; Kalberer et al., 2004; Limbeck et al., 2003; Tolocka et al., 2004).”
- Gas uptake and chemical aging of semisolid organic aerosol particles (2011, neutral): “On the other hand, slow trans- 11006 ∣ www.pnas.org/cgi/doi/10.1073/pnas.1103045108 Shiraiwa et al. port from the bulk to the surface may play an important role in the suppression of SOA evaporation (65).”
- Towards closing the gap between hygroscopic growth and activation for secondary organic aerosol - Part 2: Theoretical approaches (2008, background): “Phys., 9, 3999–4009, 2009 www.atmos-chem-phys.net/9/3999/2009/ (Kalberer et al., 2004; Baltensperger et al., 2005) occurred in the condensed phase.”
- A simplified description of the evolution of organic aerosol composition in the atmosphere (2010, background): “Development of a generalized scheme requires further investigation of the time scales for this aging in different environments.”