% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Tan:902384,
author = {Tan, Zhaofeng and Ma, Xuefei and Lu, Keding and Jiang,
Meiqing and Zou, Qi and Wang, Haichao and Zeng, Limin and
Zhang, Yuanhang},
title = {{D}irect evidence of local photochemical production driven
ozone episode in {B}eijing: {A} case study},
journal = {The science of the total environment},
volume = {800},
issn = {0048-9697},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2021-04218},
pages = {148868 -},
year = {2021},
abstract = {We present a comprehensive field campaign conducted in
Beijing, September 2016, to elucidate the photochemical smog
pollution, i.e. Ozone (O3). The observed daily maximum
hydroxyl radical (OH) and hydroperoxy radical (HO2)
concentrations were up to 1 × 107 cm-3 and
6 × 108 cm-3, respectively, indicating the active
photochemistry in autumn Beijing. Photolysis of nitrous acid
(HONO) and O3 contributed 1-2 ppbv h-1 to OH primary
production during daytime. OH termination were dominated by
the reaction with nitric oxide (NO) and nitrogen dioxide
(NO2), which were in general larger than primary production
rates, indicating other primary radical sources maybe
important. The measurement of radicals facilitates the
direct determination of local ozone production rate P (Ox)
(Ox = O3 + NO2). The integrated P(Ox) reached 75
ppbv in afternoon (for 4 h) when planetary boundary layer
was well developed. At the same time period, the observed
total oxidant concentrations Ox, increased significantly by
70 ppbv. In addition, the Ox measurement showed compact
increase in 12 stations both temporally and spatially in
Beijing, indicating that active photochemical production
happened homogenously throughout the city. The
back-trajectory analysis showed that Beijing was isolated
from the other cities during the episode, which further
proved that the fast ozone pollution was contributed by
local photochemical production rather than regional
advection.},
cin = {IEK-8},
ddc = {610},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {2111 - Air Quality (POF4-211)},
pid = {G:(DE-HGF)POF4-2111},
typ = {PUB:(DE-HGF)16},
pubmed = {34384967},
UT = {WOS:000702510000005},
doi = {10.1016/j.scitotenv.2021.148868},
url = {https://juser.fz-juelich.de/record/902384},
}