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@ARTICLE{Anttila:42749,
      author       = {Anttila, T. and Kerminen, V.-M. and Kulmala, M. and
                      Laaksonen, A. and O'Dowd, C.},
      title        = {{M}odelling the formation of organic particles in the
                      atmosphere},
      journal      = {Atmospheric chemistry and physics},
      volume       = {4},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-42749},
      pages        = {1071 - 1083},
      year         = {2004},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Particle formation resulting from activation of inorganic
                      stable clusters by a supersaturated organic vapour was
                      investigated using a numerical model. The applied aerosol
                      dynamic model included a detailed description of the
                      activation process along with a treatment of the appropriate
                      aerosol and gas-phase processes. The obtained results
                      suggest that both gaseous sulphuric acid and organic vapours
                      contribute to organic particle formation in continental
                      background areas. The initial growth of freshly-nucleated
                      clusters is driven mainly by condensation of gaseous
                      sulphuric acid and by a lesser extent self-coagulation.
                      After the clusters have reached sizes of around 2 nm in
                      diameter, low-volatile organic vapours start to condense
                      spontaneously into the clusters, thereby accelerating their
                      growth to detectable sizes. A shortage of gaseous sulphuric
                      acid or organic vapours limit, or suppress altogether, the
                      particle formation, since freshly-nucleated clusters are
                      rapidly coagulated away by pre-existing particles. The
                      obtained modelling results were applied to explaining the
                      observed seasonal cycle in the number of aerosol formation
                      events in a continental forest site.},
      keywords     = {J (WoSType)},
      cin          = {ICG-II},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB48},
      pnm          = {Chemie und Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK257},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000222473800003},
      url          = {https://juser.fz-juelich.de/record/42749},
}