Observation of viscosity transition in α-pinene secondary organic aerosol

Under certain conditions, secondary organic aerosol (SOA) particles can exist in the atmosphere in an amorphous solid or semi-solid state. To determine their relevance to processes such as ice nucleation or chemistry occurring within particles requires knowledge of the temperature and relative humid...

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Detalles Bibliográficos
Autores principales: Järvinen, Emma, Ignatius, Karoliina, Nichman, Leonid, Kristensen, Thomas B, Fuchs, Claudia, Hoyle, Christopher R, Höppel, Niko, Corbin, Joel C, Craven, Jill, Duplissy, Jonathan, Ehrhart, Sebastian, El Haddad, Imad, Frege, Carla, Gordon, Hamish, Jokinen, Tuija, Kallinger, Peter, Kirkby, Jasper, Kiselev, Alexei, Naumann, Karl-Heinz, Petäjä, Tuukka, Pinterich, Tamara, Prevot, Andre S H, Saathoff, Harald, Schiebel, Thea, Sengupta, Kamalika, Simon, Mario, Slowik, Jay G, Tröstl, Jasmin, Virtanen, Annele, Vochezer, Paul, Vogt, Steffen, Wagner, Andrea C, Wagner, Robert, Williamson, Christina, Winkler, Paul M, Yan, Chao, Baltensperger, Urs, Donahue, Neil M, Flagan, Rick C, Gallagher, Martin, Hansel, Armin, Kulmala, Markku, Stratmann, Frank, Worsnop, Douglas R, Möhler, Ottmar, Leisner, Thomas, Schnaiter, Martin
Lenguaje:eng
Publicado: 2016
Materias:
Physics in General
Acceso en línea:https://dx.doi.org/10.5194/acp-16-4423-2016
http://cds.cern.ch/record/2268407

Internet

https://dx.doi.org/10.5194/acp-16-4423-2016
http://cds.cern.ch/record/2268407

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