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@ARTICLE{Nehr:155681,
author = {Nehr, Sascha and Bohn, Birger and Dorn, Hans-Peter and
Fuchs, Hendrik and Häseler, Rolf and Hofzumahaus, Andreas
and Li, Xin and Rohrer, Franz and Tillmann, Ralf and Wahner,
Andreas},
title = {{A}tmospheric photochemistry of aromatic hydrocarbons: {OH}
budgets during {SAPHIR} chamber experiments},
journal = {Atmospheric chemistry and physics},
volume = {14},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2014-04734},
pages = {6941 - 6952},
year = {2014},
abstract = {Current photochemical models developed to simulate the
atmospheric degradation of aromatic hydrocarbons tend to
underestimate OH radical concentrations. In order to analyse
OH budgets, we performed experiments with benzene, toluene,
p-xylene and 1,3,5-trimethylbenzene in the atmosphere
simulation chamber SAPHIR. Experiments were conducted under
low-NO conditions (typically 0.1–0.2 ppb) and high-NO
conditions (typically 7–8 ppb), and starting
concentrations of 6–250 ppb of aromatics, dependent on OH
rate constants. For the OH budget analysis a steady-state
approach was applied in which OH production and destruction
rates (POH and DOH) have to be equal. The POH were
determined from measurements of HO2, NO, HONO, and O3
concentrations, considering OH formation by photolysis and
recycling from HO2. The DOH were calculated from
measurements of the OH concentrations and total OH
reactivities. The OH budgets were determined from DOH/POH
ratios. The accuracy and reproducibility of the approach
were assessed in several experiments using CO as a reference
compound where an average ratio DOH/POH = 1.13 ± 0.19 was
obtained. In experiments with aromatics, these ratios ranged
within 1.1–1.6 under low-NO conditions and 0.9–1.2 under
high-NO conditions. The results indicate that OH budgets
during photo-oxidation experiments with aromatics are
balanced within experimental accuracies. Inclusion of a
further, recently proposed OH production via HO2 + RO2
reactions led to improvements under low-NO conditions but
the differences were small and insignificant within the
experimental errors.},
cin = {IEK-8},
ddc = {550},
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:000339244600028},
doi = {10.5194/acp-14-6941-2014},
url = {https://juser.fz-juelich.de/record/155681},
}