Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning

Transmission electron microscopy (TEM) was employed to obtain morphology, size, composition, and mixing state of background aerosols with diameter less than 1 μm in the northern Qinghai–Tibet Plateau (QTP) during 15 September to 15 October 2013. Individual aerosol particles mainly contained secondar...

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Main Authors: W. J. Li, S. R. Chen, Y. S. Xu, X. C. Guo, Y. L. Sun, X. Y. Yang, Z. F. Wang, X. D. Zhao, J. M. Chen, W. X. Wang
Format: Article
Language:English
Published: Copernicus Publications 2015-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/13365/2015/acp-15-13365-2015.pdf
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spelling doaj-9f219da0b612486aac79506d536bc2632020-11-25T00:03:46ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-12-011523133651337610.5194/acp-15-13365-2015Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burningW. J. Li0S. R. Chen1Y. S. Xu2X. C. Guo3Y. L. Sun4X. Y. Yang5Z. F. Wang6X. D. Zhao7J. M. Chen8W. X. Wang9Environment Research Institute, Shandong University, 250100, Jinan, ChinaEnvironment Research Institute, Shandong University, 250100, Jinan, ChinaChinese Research Academy of Environmental Sciences, Beijing 100012, ChinaEnvironment Research Institute, Shandong University, 250100, Jinan, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaChinese Research Academy of Environmental Sciences, Beijing 100012, ChinaState Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaQinghai Environmental Monitoring Center, Qinghai 810007, ChinaEnvironment Research Institute, Shandong University, 250100, Jinan, ChinaEnvironment Research Institute, Shandong University, 250100, Jinan, ChinaTransmission electron microscopy (TEM) was employed to obtain morphology, size, composition, and mixing state of background aerosols with diameter less than 1 μm in the northern Qinghai–Tibet Plateau (QTP) during 15 September to 15 October 2013. Individual aerosol particles mainly contained secondary inorganic aerosols (SIA – sulfate and nitrate) and organics during clean periods (PM<sub>2.5</sub> mass concentration less than 2.5 μg m<sup>&minus;3</sup>). The presence of K–Na–Cl associated with organics and an increase in soot particles suggest that an intense biomass burning event caused the highest PM<sub>2.5</sub> concentrations (> 30 μg m<sup>&minus;3</sup>) during the study. A large number fraction of the fly-ash-containing particles (21.73 %) suggests that coal combustion emissions in the QTP significantly contributed to air pollutants at the medium pollution level (PM<sub>2.5</sub>: 10–30 μg m<sup>&minus;3</sup>). We concluded that emissions from biomass burning and from coal combustion both constantly contribute to anthropogenic particles in the QTP atmosphere. Based on size distributions of individual particles at different pollution levels, we found that gas condensation on existing particles is an important chemical process for the formation of SIA with organic coating. TEM observations show that refractory aerosols (e.g., soot, fly ash, and visible organic particles) likely adhere to the surface of SIA particles larger than 200 nm due to coagulation. Organic coating and soot on surface of the aged particles likely influence their hygroscopic and optical properties, respectively, in the QTP. To our knowledge, this study reports the first microscopic analysis of fine particles in the background QTP air.http://www.atmos-chem-phys.net/15/13365/2015/acp-15-13365-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author W. J. Li
S. R. Chen
Y. S. Xu
X. C. Guo
Y. L. Sun
X. Y. Yang
Z. F. Wang
X. D. Zhao
J. M. Chen
W. X. Wang
spellingShingle W. J. Li
S. R. Chen
Y. S. Xu
X. C. Guo
Y. L. Sun
X. Y. Yang
Z. F. Wang
X. D. Zhao
J. M. Chen
W. X. Wang
Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning
Atmospheric Chemistry and Physics
author_facet W. J. Li
S. R. Chen
Y. S. Xu
X. C. Guo
Y. L. Sun
X. Y. Yang
Z. F. Wang
X. D. Zhao
J. M. Chen
W. X. Wang
author_sort W. J. Li
title Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning
title_short Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning
title_full Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning
title_fullStr Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning
title_full_unstemmed Mixing state and sources of submicron regional background aerosols in the northern Qinghai–Tibet Plateau and the influence of biomass burning
title_sort mixing state and sources of submicron regional background aerosols in the northern qinghai–tibet plateau and the influence of biomass burning
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2015-12-01
description Transmission electron microscopy (TEM) was employed to obtain morphology, size, composition, and mixing state of background aerosols with diameter less than 1 μm in the northern Qinghai–Tibet Plateau (QTP) during 15 September to 15 October 2013. Individual aerosol particles mainly contained secondary inorganic aerosols (SIA – sulfate and nitrate) and organics during clean periods (PM<sub>2.5</sub> mass concentration less than 2.5 μg m<sup>&minus;3</sup>). The presence of K–Na–Cl associated with organics and an increase in soot particles suggest that an intense biomass burning event caused the highest PM<sub>2.5</sub> concentrations (> 30 μg m<sup>&minus;3</sup>) during the study. A large number fraction of the fly-ash-containing particles (21.73 %) suggests that coal combustion emissions in the QTP significantly contributed to air pollutants at the medium pollution level (PM<sub>2.5</sub>: 10–30 μg m<sup>&minus;3</sup>). We concluded that emissions from biomass burning and from coal combustion both constantly contribute to anthropogenic particles in the QTP atmosphere. Based on size distributions of individual particles at different pollution levels, we found that gas condensation on existing particles is an important chemical process for the formation of SIA with organic coating. TEM observations show that refractory aerosols (e.g., soot, fly ash, and visible organic particles) likely adhere to the surface of SIA particles larger than 200 nm due to coagulation. Organic coating and soot on surface of the aged particles likely influence their hygroscopic and optical properties, respectively, in the QTP. To our knowledge, this study reports the first microscopic analysis of fine particles in the background QTP air.
url http://www.atmos-chem-phys.net/15/13365/2015/acp-15-13365-2015.pdf
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