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@ARTICLE{Emanuelsson:186565,
author = {Emanuelsson, Eva U. and Mentel, Thomas F. and Watne, Ågot
K. and Spindler, Christian and Bohn, Birger and Brauers,
Theo and Dorn, Hans-Peter and Hallquist, Åsa M. and
Häseler, Rolf and Kiendler-Scharr, Astrid and Müller,
Klaus Peter and Pleijel, Håkan and Rohrer, Franz and
Rubach, Florian and Schlosser, Eric and Tillmann, Ralf and
Hallquist, Mattias},
title = {{P}arameterization of {T}hermal {P}roperties of {A}ging
{S}econdary {O}rganic {A}erosol {P}roduced by
{P}hoto-{O}xidation of {S}elected {T}erpene {M}ixtures},
journal = {Environmental science $\&$ technology},
volume = {48},
number = {11},
issn = {0013-936X},
address = {Columbus, Ohio},
publisher = {American Chemical Society},
reportid = {FZJ-2015-00638},
pages = {6168 - 6176},
year = {2014},
abstract = {Formation and evolution of secondary organic aerosols (SOA)
from biogenic VOCs influences the Earth’s radiative
balance. We have examined the photo-oxidation and aging of
boreal terpene mixtures in the SAPHIR simulation chamber.
Changes in thermal properties and chemical composition,
deduced from mass spectrometric measurements, were providing
information on the aging of biogenic SOA produced under
ambient solar conditions. Effects of precursor mixture,
concentration, and photochemical oxidation levels (OH
exposure) were evaluated. OH exposure was found to be the
major driver in the long term photochemical transformations,
i.e., reaction times of several hours up to days, of SOA and
its thermal properties, whereas the initial concentrations
and terpenoid mixtures had only minor influence. The
volatility distributions were parametrized using a sigmoidal
function to determine TVFR0.5 (the temperature yielding a
$50\%$ particle volume fraction remaining) and the steepness
of the volatility distribution. TVFR0.5 increased by 0.3 ±
$0.1\%$ (ca. 1 K), while the steepness increased by 0.9 ±
$0.3\%$ per hour of 1 × 106 cm–3 OH exposure. Thus, aging
reduces volatility and increases homogeneity of the vapor
pressure distribution, presumably because highly volatile
fractions become increasingly susceptible to gas phase
oxidation, while less volatile fractions are less reactive
with gas phase OH.},
cin = {IEK-8},
ddc = {050},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {233 - Trace gas and aerosol processes in the troposphere
(POF2-233)},
pid = {G:(DE-HGF)POF2-233},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000336952000015},
doi = {10.1021/es405412p},
url = {https://juser.fz-juelich.de/record/186565},
}