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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},
}