Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry
<p>The effects of the chemical composition and size of sea-salt-containing particles on their cloud condensation nuclei (CCN) activity are incompletely understood. We used a ground-based counterflow virtual impactor (GCVI) coupled with a single-particle aerosol mass spectrometer (SPAMS) to cha...
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Copernicus Publications
2019-08-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/19/10469/2019/acp-19-10469-2019.pdf |
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record_format |
Article |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Q. Lin Y. Yang Y. Yang Y. Fu Y. Fu G. Zhang F. Jiang F. Jiang L. Peng L. Peng X. Lian X. Lian F. Liu F. Liu F. Liu X. Bi L. Li D. Chen M. Li J. Ou M. Tang X. Wang P. Peng G. Sheng |
spellingShingle |
Q. Lin Y. Yang Y. Yang Y. Fu Y. Fu G. Zhang F. Jiang F. Jiang L. Peng L. Peng X. Lian X. Lian F. Liu F. Liu F. Liu X. Bi L. Li D. Chen M. Li J. Ou M. Tang X. Wang P. Peng G. Sheng Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry Atmospheric Chemistry and Physics |
author_facet |
Q. Lin Y. Yang Y. Yang Y. Fu Y. Fu G. Zhang F. Jiang F. Jiang L. Peng L. Peng X. Lian X. Lian F. Liu F. Liu F. Liu X. Bi L. Li D. Chen M. Li J. Ou M. Tang X. Wang P. Peng G. Sheng |
author_sort |
Q. Lin |
title |
Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry |
title_short |
Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry |
title_full |
Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry |
title_fullStr |
Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry |
title_full_unstemmed |
Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry |
title_sort |
enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometry |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2019-08-01 |
description |
<p>The effects of the chemical composition and size of sea-salt-containing particles on their cloud condensation nuclei (CCN) activity
are incompletely understood. We used a ground-based counterflow virtual
impactor (GCVI) coupled with a single-particle aerosol mass spectrometer
(SPAMS) to characterize chemical composition of submicron (dry diameter of
0.2–1.0 <span class="inline-formula">µm</span>) and supermicron (1.0–2.0 <span class="inline-formula">µm</span>) sea-salt-containing cloud
residues (dried cloud droplets) at Mount Nanling, southern China. Seven cut
sizes (7.5–14 <span class="inline-formula">µm</span>) of cloud droplets were set in the GCVI system. The
highest number fraction of sea-salt-containing particles was observed at the
cut size of 7.5 <span class="inline-formula">µm</span> (26 %, by number), followed by 14 <span class="inline-formula">µm</span>
(17 %) and the other cut sizes (3 %–5 %). The submicron sea-salt-containing cloud residues contributed approximately 20 % (by number)
at the cut size of 7.5 <span class="inline-formula">µm</span>, which was significantly higher than the
percentages at the cut sizes of 8–14 <span class="inline-formula">µm</span> (below 2 %). This difference
was likely involved in the change in the chemical composition. At the
cut size of 7.5 <span class="inline-formula">µm</span>, nitrate was internally mixed with over 90 % of
the submicron sea-salt-containing cloud residues, which was higher than
sulfate (20 %), ammonium (below 1 %), amines (6 %), hydrocarbon
organic species (2 %), and organic acids (4 %). However, at the cut
sizes of 8–14 <span class="inline-formula">µm</span>, nitrate, sulfate, ammonium, amines, hydrocarbon
organic species, and organic acids were internally mixed with > 90 %, > 80 %, 39 %–84 %, 71 %–86 %, 52 %–90 %, and 32 %–77 %
of the submicron sea-salt-containing cloud residues. The proportion of sea-salt-containing particles in the supermicron cloud residues generally
increased as a function of cut size, and their CCN activity was less
influenced by chemical composition. This study provided a significant
contribution towards a comprehensive understanding of sea-salt CCN activity.</p> |
url |
https://www.atmos-chem-phys.net/19/10469/2019/acp-19-10469-2019.pdf |
work_keys_str_mv |
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spelling |
doaj-394d69f7923446a49bc17880af7a52d72020-11-25T00:48:34ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242019-08-0119104691047910.5194/acp-19-10469-2019Enrichment of submicron sea-salt-containing particles in small cloud droplets based on single-particle mass spectrometryQ. Lin0Y. Yang1Y. Yang2Y. Fu3Y. Fu4G. Zhang5F. Jiang6F. Jiang7L. Peng8L. Peng9X. Lian10X. Lian11F. Liu12F. Liu13F. Liu14X. Bi15L. Li16D. Chen17M. Li18J. Ou19M. Tang20X. Wang21P. Peng22G. Sheng23State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaUniversity of Chinese Academy of Sciences, Beijing 100039, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaUniversity of Chinese Academy of Sciences, Beijing 100039, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaUniversity of Chinese Academy of Sciences, Beijing 100039, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaUniversity of Chinese Academy of Sciences, Beijing 100039, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaUniversity of Chinese Academy of Sciences, Beijing 100039, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaUniversity of Chinese Academy of Sciences, Beijing 100039, PR Chinacurrently at: College of Economics and Management, Taiyuan University of Technology, Taiyuan 030024, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaInstitute of Mass Spectrometer and Atmospheric Environment, Jinan University, Guangzhou 510632, PR ChinaState Environmental Protection Key Laboratory of Regional Air Quality Monitoring, Guangdong Environmental Monitoring Center, Guangzhou 510308, PR ChinaInstitute of Mass Spectrometer and Atmospheric Environment, Jinan University, Guangzhou 510632, PR ChinaShaoguan Environmental Monitoring Center, Shaoguan 512026, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR ChinaState Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Resources Utilization and Protection, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PR China<p>The effects of the chemical composition and size of sea-salt-containing particles on their cloud condensation nuclei (CCN) activity are incompletely understood. We used a ground-based counterflow virtual impactor (GCVI) coupled with a single-particle aerosol mass spectrometer (SPAMS) to characterize chemical composition of submicron (dry diameter of 0.2–1.0 <span class="inline-formula">µm</span>) and supermicron (1.0–2.0 <span class="inline-formula">µm</span>) sea-salt-containing cloud residues (dried cloud droplets) at Mount Nanling, southern China. Seven cut sizes (7.5–14 <span class="inline-formula">µm</span>) of cloud droplets were set in the GCVI system. The highest number fraction of sea-salt-containing particles was observed at the cut size of 7.5 <span class="inline-formula">µm</span> (26 %, by number), followed by 14 <span class="inline-formula">µm</span> (17 %) and the other cut sizes (3 %–5 %). The submicron sea-salt-containing cloud residues contributed approximately 20 % (by number) at the cut size of 7.5 <span class="inline-formula">µm</span>, which was significantly higher than the percentages at the cut sizes of 8–14 <span class="inline-formula">µm</span> (below 2 %). This difference was likely involved in the change in the chemical composition. At the cut size of 7.5 <span class="inline-formula">µm</span>, nitrate was internally mixed with over 90 % of the submicron sea-salt-containing cloud residues, which was higher than sulfate (20 %), ammonium (below 1 %), amines (6 %), hydrocarbon organic species (2 %), and organic acids (4 %). However, at the cut sizes of 8–14 <span class="inline-formula">µm</span>, nitrate, sulfate, ammonium, amines, hydrocarbon organic species, and organic acids were internally mixed with > 90 %, > 80 %, 39 %–84 %, 71 %–86 %, 52 %–90 %, and 32 %–77 % of the submicron sea-salt-containing cloud residues. The proportion of sea-salt-containing particles in the supermicron cloud residues generally increased as a function of cut size, and their CCN activity was less influenced by chemical composition. This study provided a significant contribution towards a comprehensive understanding of sea-salt CCN activity.</p>https://www.atmos-chem-phys.net/19/10469/2019/acp-19-10469-2019.pdf |