High time-resolved measurement of stable carbon isotope composition in water-soluble organic aerosols: method optimization and a case study during winter haze in eastern China
-
Published:2019-09-02
Issue:17
Volume:19
Page:11071-11087
-
ISSN:1680-7324
-
Container-title:Atmospheric Chemistry and Physics
-
language:en
-
Short-container-title:Atmos. Chem. Phys.
Author:
Zhang WenqiORCID, Zhang Yan-LinORCID, Cao Fang, Xiang Yankun, Zhang Yuanyuan, Bao Mengying, Liu Xiaoyan, Lin Yu-Chi
Abstract
Abstract. Water-soluble organic carbon (WSOC) is a significant fraction of
organic carbon (OC) in atmospheric aerosols. WSOC is of great interest due
to its significant effects on atmospheric chemistry, the Earth's climate and
human health. The stable carbon isotope (δ13C) can be used to track
the potential sources and investigate atmospheric processes of organic
aerosols. However, the previous methods measuring the δ13C
values of WSOC in ambient aerosols require a large amount of carbon content, are time-consuming and require labor-intensive preprocessing. In this study,
a method of simultaneously measuring the mass concentration and the δ13C values of WSOC from aerosol samples is established by coupling the
GasBench II preparation device with isotopic ratio mass spectrometry. The
precision and accuracy of isotope determination is better than 0.17 ‰ and 0.5 ‰, respectively, for
samples containing WSOC amounts larger than 5 µg. This method is then applied
for the aerosol samples collected every 3 h during a severe wintertime
haze period in Nanjing, eastern China. The WSOC values vary between 3 and 32 µg m−3, whereas δ13C−WSOC ranges from −26.24 ‰ to −23.35 ‰. Three different
episodes (Episode 1, Episode 2 and Episode 3) are
identified in the sampling period, showing a different tendency of δ13C−WSOC with the accumulation process of WSOC aerosols. The
increases in both the WSOC mass concentrations and the δ13C−WSOC values in Episode 1 indicate that WSOC is subject to
a substantial photochemical aging during the air mass transport. In Episode 2, the decline of the δ13C−WSOC is accompanied
by the increase in the WSOC mass concentrations, which is associated with
regional-transported biomass burning emissions. In Episode 3, heavier
isotope (13C) is exclusively enriched in total carbon (TC) in comparison to WSOC aerosols. This suggests that the non-WSOC fraction in total carbon may
contain 13C-enriched components such as dust carbonate, which is
supported by the enhanced Ca2+ concentrations and air mass
trajectory analysis. The present study provides a novel method to
determine the stable carbon isotope composition of WSOC, and it offers
a great potential to better understand the source emission, the atmospheric
aging and the secondary production of water-soluble organic aerosols.
Funder
National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference70 articles.
1. Agarwal, S., Aggarwal, S. G., Okuzawa, K., and Kawamura, K.: Size distributions of dicarboxylic acids, ketoacids, α-dicarbonyls, sugars, WSOC, OC, EC and inorganic ions in atmospheric particles over Northern Japan: implication for long-range transport of Siberian biomass burning and East Asian polluted aerosols, Atmos. Chem. Phys., 10, 5839–5858, https://doi.org/10.5194/acp-10-5839-2010, 2010. 2. Aggarwal, S. G. and Kawamura, K.: Molecular distributions and stable carbon
isotopic compositions of dicarboxylic acids and related compounds in
aerosols from Sapporo, Japan: Implications for photochemical aging during
long-range atmospheric transport, J. Geophys. Res.-Atmos., 113, 1–13, https://doi.org/10.1029/2007JD009365, 2008. 3. Anderson, R. S., Iannone, R., Thompson, A. E., Rudolph, J., and Huang, L.: Carbon kinetic isotope effects in the gas-phase reactions of aromatic hydrocarbons with the OH radical at 296±4 K, Geophys. Res. Lett., 31, L15108, https://doi.org/10.1029/2004GL020089, 2004. 4. Anderson, C., Dibb, J. E., Griffin, R. J., and Bergin, M. H.: Simultaneous
measurements of particulate and gas-phase water-soluble organic carbon
concentrations at remote and urban-influenced locations, Geophys.
Res. Lett., 35, 2–5, https://doi.org/10.1029/2008GL033966, 2008. 5. Asa-Awuku, A., Moore, R. H., Nenes, A., Bahreini, R., Holloway, J. S., Brock, C. A., Middlebrook, A. M., Ryerson, T. B., Jimenez, J. L., DeCarlo, P. F., Hecobian, A., Weber R. J., Stickel, R., Tanner D. J., and Huey, L. G.: Airborne Cloud Condensation Nuclei Measurements during the 2006 Texas Air Quality Study, J. Geophys. Res.-Atmos., 116, 1–18. https://doi.org/10.1029/2010JD014874, 2011.
Cited by
24 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|