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@PHDTHESIS{Schmitt:844676,
      author       = {Schmitt, Sebastian Harald},
      title        = {{F}ormation of {S}econdary {O}rganic {A}erosol from
                      {P}hoto-{O}xidation of {B}enzene: a {C}hamber {S}tudy},
      volume       = {412},
      school       = {Universität Bayreuth},
      type         = {Dissertation},
      address      = {Jülich},
      publisher    = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
      reportid     = {FZJ-2018-02061},
      isbn         = {978-3-95806-305-1},
      series       = {Schriften des Forschungszentrums Jülich Reihe Energie $\&$
                      Umwelt / Energy $\&$ Environment},
      pages        = {III, 250 S.},
      year         = {2018},
      note         = {Universität Bayreuth, Diss.,2017},
      abstract     = {Atmospheric aerosol plays a key role in the Earth's climate
                      system. Aerosol particles influence the Earth's radiation
                      budget because of their light scattering and absorbing
                      properties (direct effect) and their ability to form cloud
                      condensation nuclei (indirect effect). A large fraction of
                      atmospheric aerosol is of organic origin, either directly
                      emitted as solid or liquid particles (Primary Organic
                      Aerosol; POA) or formed from volatile organic compounds
                      (VOCs) by photooxidation(Secondary Organic Aerosol; SOA).
                      SOA contributes up to 90 $\%$ to the total organic aerosol
                      mass and participates in new particle formation
                      (nucleation). Understanding the formation of SOA is crucial
                      for estimating its impact on the climate as wellas on human
                      health and the development of future mitigation and
                      adaptation strategies. Therefore, SOA is typically
                      classiffied into anthropogenic SOA (ASOA) originating from
                      anthropogenic precursors (e.g. aromatic hydrocarbons) and
                      biogenic SOA (BSOA) formed by (photo-)oxidation of plant
                      emissions (e.g. monoterpenes). ...},
      cin          = {IEK-8},
      cid          = {I:(DE-Juel1)IEK-8-20101013},
      pnm          = {899 - ohne Topic (POF3-899)},
      pid          = {G:(DE-HGF)POF3-899},
      typ          = {PUB:(DE-HGF)3 / PUB:(DE-HGF)11},
      urn          = {urn:nbn:de:0001-2018032300},
      url          = {https://juser.fz-juelich.de/record/844676},
}