O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1)
Non sea-salt sulfate (NSS) of 2.2-2.3 nmol m(-3) total magnitude in aerosols observed during the First Aerosol Characterization Experiment (ACE-1) at Cape Grim, Tasmania, was trimodally distributed with similar to 1 nmol NSS m(-3) in > 0.7 mu m ambient diameter (diam) coarse seasalt mode aerosols...
Published in: | Journal of Geophysical Research: Atmospheres |
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American Geophysical Union (AGU)
1999
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Online Access: | https://real.mtak.hu/3418/ https://real.mtak.hu/3418/1/1039010.pdf https://doi.org/10.1029/1998JD100086 |
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ftmtak:oai:real.mtak.hu:3418 2024-06-09T07:49:46+00:00 O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) Sievering, H. Lerner, B. Slavich, J. Anderson, J. Pósfai, Mihály Cainey, J. 1999-09-20 application/pdf https://real.mtak.hu/3418/ https://real.mtak.hu/3418/1/1039010.pdf https://doi.org/10.1029/1998JD100086 en eng American Geophysical Union (AGU) https://real.mtak.hu/3418/1/1039010.pdf Sievering, H. and Lerner, B. and Slavich, J. and Anderson, J. and Pósfai, Mihály and Cainey, J. (1999) O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1). Journal of Geophysical Research, 104 (D17). pp. 21707-21717. ISSN 2169-897X QD06 Mineralogy / ásványtan QE Geology / földtudományok Article PeerReviewed 1999 ftmtak https://doi.org/10.1029/1998JD100086 2024-05-15T13:44:04Z Non sea-salt sulfate (NSS) of 2.2-2.3 nmol m(-3) total magnitude in aerosols observed during the First Aerosol Characterization Experiment (ACE-1) at Cape Grim, Tasmania, was trimodally distributed with similar to 1 nmol NSS m(-3) in > 0.7 mu m ambient diameter (diam) coarse seasalt mode aerosols; despite this low NSS concentration, [H2SO4(g)] was so low that < 1% of this NSS could have been due to H2SO4 scavenging. Ammonium was not associated with these coarse seasalt aerosols, suggesting that cloud processing was a minor contributor to the NSS found in > 0.7 mu m diam aerosols. The mechanism of O-3 oxidation of SO2 in sea-salt aerosol water (SSAW) is assessed for its capability to explain this coarse aerosol NSS. Limitation of this mechanism's NSS contribution is largely due to SSAW's buffering capacity since its reaction rate is reduced by 2 orders of magnitude at pH 6 versus the pH greater than or equal to 8 of unreacted SSAW. However, the buffering capacity of sea-salt aerosols may have been significantly enhanced over that of bulk seawater alkalinity. This appears to be due to carbonate resulting from small fragments of biogenic CaCO3 in the ocean's surface microlayer. Given the observed nonsoil calcium excess over that in bulk seawater, the estimated actual buffering capacity of sea-salt aerosols observed during ACE 1 was 50%, or more, enhanced over that due to bulk seawater alkalinity. Considering this enhanced buffering capacity, O-3 oxidation of SO2 in SSAW can produce sufficient NSS to explain 70-90% of the similar to 1 nmol m(-3) found in > 0.7 mu m diam coarse sea-salt aerosols with cloud processing and further oxidation of SO2 in SSAW (i.e., pH < 6) by other sea-salt conversion mechanisms contributing the remainder. The amount of NSS produced by sea-salt conversion mechanisms during the ACE 1 remote Southern Ocean experiment vied with homogeneous and cloud processing in their contribution to the total observed NSS of 2.2-2.3 nmol m(-3). Article in Journal/Newspaper Southern Ocean MTAK: REAL (Library and Information Centre of the Hungarian Academy of Sciences Grim ENVELOPE(-64.486,-64.486,-65.379,-65.379) Southern Ocean Journal of Geophysical Research: Atmospheres 104 D17 21707 21717 |
institution |
Open Polar |
collection |
MTAK: REAL (Library and Information Centre of the Hungarian Academy of Sciences |
op_collection_id |
ftmtak |
language |
English |
topic |
QD06 Mineralogy / ásványtan QE Geology / földtudományok |
spellingShingle |
QD06 Mineralogy / ásványtan QE Geology / földtudományok Sievering, H. Lerner, B. Slavich, J. Anderson, J. Pósfai, Mihály Cainey, J. O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) |
topic_facet |
QD06 Mineralogy / ásványtan QE Geology / földtudományok |
description |
Non sea-salt sulfate (NSS) of 2.2-2.3 nmol m(-3) total magnitude in aerosols observed during the First Aerosol Characterization Experiment (ACE-1) at Cape Grim, Tasmania, was trimodally distributed with similar to 1 nmol NSS m(-3) in > 0.7 mu m ambient diameter (diam) coarse seasalt mode aerosols; despite this low NSS concentration, [H2SO4(g)] was so low that < 1% of this NSS could have been due to H2SO4 scavenging. Ammonium was not associated with these coarse seasalt aerosols, suggesting that cloud processing was a minor contributor to the NSS found in > 0.7 mu m diam aerosols. The mechanism of O-3 oxidation of SO2 in sea-salt aerosol water (SSAW) is assessed for its capability to explain this coarse aerosol NSS. Limitation of this mechanism's NSS contribution is largely due to SSAW's buffering capacity since its reaction rate is reduced by 2 orders of magnitude at pH 6 versus the pH greater than or equal to 8 of unreacted SSAW. However, the buffering capacity of sea-salt aerosols may have been significantly enhanced over that of bulk seawater alkalinity. This appears to be due to carbonate resulting from small fragments of biogenic CaCO3 in the ocean's surface microlayer. Given the observed nonsoil calcium excess over that in bulk seawater, the estimated actual buffering capacity of sea-salt aerosols observed during ACE 1 was 50%, or more, enhanced over that due to bulk seawater alkalinity. Considering this enhanced buffering capacity, O-3 oxidation of SO2 in SSAW can produce sufficient NSS to explain 70-90% of the similar to 1 nmol m(-3) found in > 0.7 mu m diam coarse sea-salt aerosols with cloud processing and further oxidation of SO2 in SSAW (i.e., pH < 6) by other sea-salt conversion mechanisms contributing the remainder. The amount of NSS produced by sea-salt conversion mechanisms during the ACE 1 remote Southern Ocean experiment vied with homogeneous and cloud processing in their contribution to the total observed NSS of 2.2-2.3 nmol m(-3). |
format |
Article in Journal/Newspaper |
author |
Sievering, H. Lerner, B. Slavich, J. Anderson, J. Pósfai, Mihály Cainey, J. |
author_facet |
Sievering, H. Lerner, B. Slavich, J. Anderson, J. Pósfai, Mihály Cainey, J. |
author_sort |
Sievering, H. |
title |
O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) |
title_short |
O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) |
title_full |
O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) |
title_fullStr |
O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) |
title_full_unstemmed |
O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1) |
title_sort |
o3oxidation of so2in sea-salt aerosol water: size distribution of non-sea-salt sulfate during the first aerosol characterization experiment (ace 1) |
publisher |
American Geophysical Union (AGU) |
publishDate |
1999 |
url |
https://real.mtak.hu/3418/ https://real.mtak.hu/3418/1/1039010.pdf https://doi.org/10.1029/1998JD100086 |
long_lat |
ENVELOPE(-64.486,-64.486,-65.379,-65.379) |
geographic |
Grim Southern Ocean |
geographic_facet |
Grim Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
https://real.mtak.hu/3418/1/1039010.pdf Sievering, H. and Lerner, B. and Slavich, J. and Anderson, J. and Pósfai, Mihály and Cainey, J. (1999) O3oxidation of SO2in sea-salt aerosol water: Size distribution of non-sea-salt sulfate during the First Aerosol Characterization Experiment (ACE 1). Journal of Geophysical Research, 104 (D17). pp. 21707-21717. ISSN 2169-897X |
op_doi |
https://doi.org/10.1029/1998JD100086 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
104 |
container_issue |
D17 |
container_start_page |
21707 |
op_container_end_page |
21717 |
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1801382570629267456 |