001     844676
005     20240712101013.0
020 _ _ |a 978-3-95806-305-1
024 7 _ |2 URN
|a urn:nbn:de:0001-2018032300
024 7 _ |2 Handle
|a 2128/18478
024 7 _ |2 ISSN
|a 1866-1793
037 _ _ |a FZJ-2018-02061
041 _ _ |a English
100 1 _ |0 P:(DE-Juel1)161557
|a Schmitt, Sebastian Harald
|b 0
|e Corresponding author
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245 _ _ |a Formation of Secondary Organic Aerosol from Photo-Oxidation of Benzene: a Chamber Study
|f - 2018-05-09
260 _ _ |a Jülich
|b Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag
|c 2018
300 _ _ |a III, 250 S.
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|s 1525872977_31953
336 7 _ |2 DRIVER
|a doctoralThesis
490 0 _ |a Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment
|v 412
502 _ _ |a Universität Bayreuth, Diss.,2017
|b Dissertation
|c Universität Bayreuth
|d 2017
520 _ _ |a 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). ...
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