Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer

<p>Secondary organic aerosol (SOA) plays a significant role in atmospheric chemistry. However, little is known about the vertical profiles of SOA in the urban boundary layer (UBL). This knowledge gap constrains the SOA simulation in chemical transport models. Here, the aerosol samples were syn...

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Main Authors: H. Ren, W. Hu, L. Wei, S. Yue, J. Zhao, L. Li, L. Wu, W. Zhao, L. Ren, M. Kang, Q. Xie, S. Su, X. Pan, Z. Wang, Y. Sun, K. Kawamura, P. Fu
Format: Article
Language:English
Published: Copernicus Publications 2021-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/21/12949/2021/acp-21-12949-2021.pdf
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author H. Ren
H. Ren
W. Hu
L. Wei
S. Yue
S. Yue
J. Zhao
L. Li
L. Li
L. Wu
W. Zhao
L. Ren
M. Kang
Q. Xie
Q. Xie
S. Su
X. Pan
Z. Wang
Y. Sun
K. Kawamura
P. Fu
spellingShingle H. Ren
H. Ren
W. Hu
L. Wei
S. Yue
S. Yue
J. Zhao
L. Li
L. Li
L. Wu
W. Zhao
L. Ren
M. Kang
Q. Xie
Q. Xie
S. Su
X. Pan
Z. Wang
Y. Sun
K. Kawamura
P. Fu
Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer
Atmospheric Chemistry and Physics
author_facet H. Ren
H. Ren
W. Hu
L. Wei
S. Yue
S. Yue
J. Zhao
L. Li
L. Li
L. Wu
W. Zhao
L. Ren
M. Kang
Q. Xie
Q. Xie
S. Su
X. Pan
Z. Wang
Y. Sun
K. Kawamura
P. Fu
author_sort H. Ren
title Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer
title_short Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer
title_full Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer
title_fullStr Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer
title_full_unstemmed Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summer
title_sort measurement report: vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over beijing during late summer
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2021-09-01
description <p>Secondary organic aerosol (SOA) plays a significant role in atmospheric chemistry. However, little is known about the vertical profiles of SOA in the urban boundary layer (UBL). This knowledge gap constrains the SOA simulation in chemical transport models. Here, the aerosol samples were synchronously collected at 8, 120, and 260 <span class="inline-formula">m</span> based on a 325 <span class="inline-formula">m</span> meteorological tower in Beijing from 15 August to 10 September 2015. Strict emission controls were implemented during this period for the 2015 China Victory Day parade. Here, we observed that the total concentration of biogenic SOA tracers increased with height. The fraction of SOA from isoprene oxidation increased with height, whereas the fractions of SOA from monoterpenes and sesquiterpenes decreased, and 2,3-dihydroxy-4-oxopentanoic acid (DHOPA), a tracer of anthropogenic SOA from toluene oxidation, also increased with height. The complicated vertical profiles of SOA tracers highlighted the need to characterize SOA within the UBL. The mass concentration of estimated secondary organic carbon (SOC) ranged from 341 to 673 <span class="inline-formula">ng C m<sup>−3</sup></span>. The increase in the estimated SOC fractions from isoprene and toluene with height was found to be more related to regional transport, whereas the decrease in the estimated SOC from monoterpenes and sesquiterpene with height was more subject to local emissions. Emission controls during the parade reduced SOC by 4 %–35 %, with toluene SOC decreasing more than the other SOC. This study demonstrates that vertical distributions of SOA within the UBL are complex, and the vertical profiles of SOA concentrations and sources should be considered in field and modeling studies in the future.</p>
url https://acp.copernicus.org/articles/21/12949/2021/acp-21-12949-2021.pdf
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spelling doaj-36618e494fba449a909102eadfddbdcd2021-09-01T07:30:11ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242021-09-0121129491296310.5194/acp-21-12949-2021Measurement report: Vertical distribution of biogenic and anthropogenic secondary organic aerosols in the urban boundary layer over Beijing during late summerH. Ren0H. Ren1W. Hu2L. Wei3S. Yue4S. Yue5J. Zhao6L. Li7L. Li8L. Wu9W. Zhao10L. Ren11M. Kang12Q. Xie13Q. Xie14S. Su15X. Pan16Z. Wang17Y. Sun18K. Kawamura19P. Fu20Institute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaInstitute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, Chinanow at: Minerva Research Group, Max Planck Institute for Chemistry, 55128 Mainz, GermanyState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, Chinanow at: Department of Chemistry and Molecular Biology, University of Gothenburg, 412 96 Gothenburg, SwedenInstitute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaInstitute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaInstitute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaInstitute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaChubu Institute for Advanced Studies, Chubu University, Kasugai 487-8501, JapanInstitute of Surface-Earth System Science, School of Earth-System Science, Tianjin University, Tianjin 300072, China<p>Secondary organic aerosol (SOA) plays a significant role in atmospheric chemistry. However, little is known about the vertical profiles of SOA in the urban boundary layer (UBL). This knowledge gap constrains the SOA simulation in chemical transport models. Here, the aerosol samples were synchronously collected at 8, 120, and 260 <span class="inline-formula">m</span> based on a 325 <span class="inline-formula">m</span> meteorological tower in Beijing from 15 August to 10 September 2015. Strict emission controls were implemented during this period for the 2015 China Victory Day parade. Here, we observed that the total concentration of biogenic SOA tracers increased with height. The fraction of SOA from isoprene oxidation increased with height, whereas the fractions of SOA from monoterpenes and sesquiterpenes decreased, and 2,3-dihydroxy-4-oxopentanoic acid (DHOPA), a tracer of anthropogenic SOA from toluene oxidation, also increased with height. The complicated vertical profiles of SOA tracers highlighted the need to characterize SOA within the UBL. The mass concentration of estimated secondary organic carbon (SOC) ranged from 341 to 673 <span class="inline-formula">ng C m<sup>−3</sup></span>. The increase in the estimated SOC fractions from isoprene and toluene with height was found to be more related to regional transport, whereas the decrease in the estimated SOC from monoterpenes and sesquiterpene with height was more subject to local emissions. Emission controls during the parade reduced SOC by 4 %–35 %, with toluene SOC decreasing more than the other SOC. This study demonstrates that vertical distributions of SOA within the UBL are complex, and the vertical profiles of SOA concentrations and sources should be considered in field and modeling studies in the future.</p>https://acp.copernicus.org/articles/21/12949/2021/acp-21-12949-2021.pdf