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@ARTICLE{Zheng:17035,
author = {Zheng, J. and Hu, M. and Zhang, R. and Yue, D. and Wang, Z.
and Guo, S. and Li, X. and Bohn, B. and Shao, M. and He, L.
and Huang, X. and Wiedensohler, A. and Zhu, T.},
title = {{M}easurements of gaseous {H}2{SO}4 by {AP}-{ID}-{CIMS}
during {CAREB}eijing 2008 {C}ampaign},
journal = {Atmospheric chemistry and physics},
volume = {11},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-17035},
pages = {7755 - 7765},
year = {2011},
note = {This work was part of the Campaign of Atmospheric Research
in Beijing and surrounding areas supported by Beijing
Environment Protection Bureau (OITC-G08026056) and the
National Natural Science Foundation of China (20977001,
21025728). This work was also supported by the Robert A.
Welch Foundation (Grant A-1417). R. Z. acknowledged further
support from the National Natural Science Foundation of
China Grant (40728006).},
abstract = {As part of the 2008 Campaign of Air Quality Research in
Beijing and Surrounding Regions (CAREBeijing 2008),
measurements of gaseous sulfuric acid (H2SO4) have been
conducted at an urban site in Beijing, China from 7 July to
25 September 2008 using atmospheric pressure ion drift -
chemical ionization mass spectrometry (AP-ID-CIMS). This
represents the first gaseous H2SO4 measurements in China.
Diurnal profile of sulfuric acid is strongly dependent on
the actinic flux, reaching a daily maximum around noontime
and with an hourly average concentration of 5 x 10(6)
molecules cm(-3). Simulation of sulfuric acid on the basis
of the measured sulfur dioxide concentration, photolysis
rates of ozone and nitrogen dioxide, and aerosol surface
areas captures the trend of the measured H2SO4 diurnal
variation within the uncertainties, indicating that
photochemical production and condensation onto preexisting
particle surface dominate the observed diurnal H2SO4
profile. The frequency of the peak H2SO4 concentration
exceeding 5 x 10(6) molecules cm(-3) increases by $16\%$
during the period of the summer Olympic Games (8-24 August
2008), because of the implementation of air quality control
regulations. Using a multivariate statistical method, the
critical nucleus during nucleation events is inferred,
containing two H2SO4 molecules (R-2 = 0.85). The calculated
condensation rate of H2SO4 can only account for 10-25 $\%$
of PM1 sulfate formation, indicating that either much
stronger sulfate production exists at the SO2 source region
or other sulfate production mechanisms are responsible for
the sulfate production.},
keywords = {J (WoSType)},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000293826500022},
doi = {10.5194/acp-11-7755-2011},
url = {https://juser.fz-juelich.de/record/17035},
}