A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China

To obtain a thorough knowledge of PM<sub>2. 5</sub> chemical composition and its impact on aerosol optical properties across China, existing field studies conducted after the year 2000 are reviewed and summarized in terms of geographical, interannual and seasonal distributions. Annual...

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Main Authors: J. Tao, L. Zhang, J. Cao, R. Zhang
Format: Article
Language:English
Published: Copernicus Publications 2017-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/17/9485/2017/acp-17-9485-2017.pdf
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spelling doaj-f18fc19aa0b54ec289b8b87958d65fbf2020-11-24T23:06:40ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-08-01179485951810.5194/acp-17-9485-2017A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across ChinaJ. Tao0L. Zhang1J. Cao2R. Zhang3South China Institute of Environmental Sciences, Ministry of Environmental Protection, Guangzhou, ChinaAir Quality Research Division, Science and Technology Branch, Environment and Climate Change Canada, Toronto, CanadaKey Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, ChinaKey Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, ChinaTo obtain a thorough knowledge of PM<sub>2. 5</sub> chemical composition and its impact on aerosol optical properties across China, existing field studies conducted after the year 2000 are reviewed and summarized in terms of geographical, interannual and seasonal distributions. Annual PM<sub>2. 5</sub> was up to 6 times the National Ambient Air Quality Standards (NAAQS) in some megacities in northern China. Annual PM<sub>2. 5</sub> was higher in northern than southern cities, and higher in inland than coastal cities. In a few cities with data longer than a decade, PM<sub>2. 5</sub> showed a slight decrease only in the second half of the past decade, while carbonaceous aerosols decreased, sulfate (SO<sub>4</sub><sup>2−</sup>) and ammonium (NH<sub>4</sub><sup>+</sup>) remained at high levels, and nitrate (NO<sub>3</sub><sup>−</sup>) increased. The highest seasonal averages of PM<sub>2. 5</sub> and its major chemical components were typically observed in the cold seasons. Annual average contributions of secondary inorganic aerosols to PM<sub>2. 5</sub> ranged from 25 to 48 %, and those of carbonaceous aerosols ranged from 23 to 47 %, both with higher contributions in southern regions due to the frequent dust events in northern China. Source apportionment analysis identified secondary inorganic aerosols, coal combustion and traffic emission as the top three source factors contributing to PM<sub>2. 5</sub> mass in most Chinese cities, and the sum of these three source factors explained 44 to 82 % of PM<sub>2. 5</sub> mass on annual average across China. Biomass emission in most cities, industrial emission in industrial cities, dust emission in northern cities and ship emission in coastal cities are other major source factors, each of which contributed 7–27 % to PM<sub>2. 5</sub> mass in applicable cities.<br><br> The geographical pattern of scattering coefficient (<i>b</i><sub>sp</sub>) was similar to that of PM<sub>2. 5</sub>, and that of aerosol absorption coefficient (<i>b</i><sub>ap</sub>) was determined by elemental carbon (EC) mass concentration and its coating. <i>b</i><sub>sp</sub> in ambient condition of relative humidity (RH)  =  80 % can be amplified by about 1.8 times that under dry conditions. Secondary inorganic aerosols accounted for about 60 % of aerosol extinction coefficient (<i>b</i><sub>ext</sub>) at RH greater than 70 %. The mass scattering efficiency (MSE) of PM<sub>2. 5</sub> ranged from 3.0 to 5.0 m<sup>2</sup> g<sup>−1</sup> for aerosols produced from anthropogenic emissions and from 0.7 to 1.0 m<sup>2</sup> g<sup>−1</sup> for natural dust aerosols. The mass absorption efficiency (MAE) of EC ranged from 6.5 to 12.4 m<sup>2</sup> g<sup>−1</sup> in urban environments, but the MAE of water-soluble organic carbon was only 0.05 to 0.11 m<sup>2</sup> g<sup>−1</sup>. Historical emission control policies in China and their effectiveness were discussed based on available chemically resolved PM<sub>2. 5</sub> data, which provides the much needed knowledge for guiding future studies and emissions policies.https://www.atmos-chem-phys.net/17/9485/2017/acp-17-9485-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Tao
L. Zhang
J. Cao
R. Zhang
spellingShingle J. Tao
L. Zhang
J. Cao
R. Zhang
A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China
Atmospheric Chemistry and Physics
author_facet J. Tao
L. Zhang
J. Cao
R. Zhang
author_sort J. Tao
title A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China
title_short A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China
title_full A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China
title_fullStr A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China
title_full_unstemmed A review of current knowledge concerning PM<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across China
title_sort review of current knowledge concerning pm<sub>2. 5</sub> chemical composition, aerosol optical properties and their relationships across china
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2017-08-01
description To obtain a thorough knowledge of PM<sub>2. 5</sub> chemical composition and its impact on aerosol optical properties across China, existing field studies conducted after the year 2000 are reviewed and summarized in terms of geographical, interannual and seasonal distributions. Annual PM<sub>2. 5</sub> was up to 6 times the National Ambient Air Quality Standards (NAAQS) in some megacities in northern China. Annual PM<sub>2. 5</sub> was higher in northern than southern cities, and higher in inland than coastal cities. In a few cities with data longer than a decade, PM<sub>2. 5</sub> showed a slight decrease only in the second half of the past decade, while carbonaceous aerosols decreased, sulfate (SO<sub>4</sub><sup>2−</sup>) and ammonium (NH<sub>4</sub><sup>+</sup>) remained at high levels, and nitrate (NO<sub>3</sub><sup>−</sup>) increased. The highest seasonal averages of PM<sub>2. 5</sub> and its major chemical components were typically observed in the cold seasons. Annual average contributions of secondary inorganic aerosols to PM<sub>2. 5</sub> ranged from 25 to 48 %, and those of carbonaceous aerosols ranged from 23 to 47 %, both with higher contributions in southern regions due to the frequent dust events in northern China. Source apportionment analysis identified secondary inorganic aerosols, coal combustion and traffic emission as the top three source factors contributing to PM<sub>2. 5</sub> mass in most Chinese cities, and the sum of these three source factors explained 44 to 82 % of PM<sub>2. 5</sub> mass on annual average across China. Biomass emission in most cities, industrial emission in industrial cities, dust emission in northern cities and ship emission in coastal cities are other major source factors, each of which contributed 7–27 % to PM<sub>2. 5</sub> mass in applicable cities.<br><br> The geographical pattern of scattering coefficient (<i>b</i><sub>sp</sub>) was similar to that of PM<sub>2. 5</sub>, and that of aerosol absorption coefficient (<i>b</i><sub>ap</sub>) was determined by elemental carbon (EC) mass concentration and its coating. <i>b</i><sub>sp</sub> in ambient condition of relative humidity (RH)  =  80 % can be amplified by about 1.8 times that under dry conditions. Secondary inorganic aerosols accounted for about 60 % of aerosol extinction coefficient (<i>b</i><sub>ext</sub>) at RH greater than 70 %. The mass scattering efficiency (MSE) of PM<sub>2. 5</sub> ranged from 3.0 to 5.0 m<sup>2</sup> g<sup>−1</sup> for aerosols produced from anthropogenic emissions and from 0.7 to 1.0 m<sup>2</sup> g<sup>−1</sup> for natural dust aerosols. The mass absorption efficiency (MAE) of EC ranged from 6.5 to 12.4 m<sup>2</sup> g<sup>−1</sup> in urban environments, but the MAE of water-soluble organic carbon was only 0.05 to 0.11 m<sup>2</sup> g<sup>−1</sup>. Historical emission control policies in China and their effectiveness were discussed based on available chemically resolved PM<sub>2. 5</sub> data, which provides the much needed knowledge for guiding future studies and emissions policies.
url https://www.atmos-chem-phys.net/17/9485/2017/acp-17-9485-2017.pdf
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