Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise

Abstract. Halogenated dicarboxylic acids, such as bromomalonic (Br-C3), chlorosuccinic (Cl-C4) and bromosuccinic (Br-C4) acids, have been measured, for the first time, in the arctic aerosols dur-ing the polar sunrise experiment ALERT2000 (February to May). They were detected in the light spring, but...

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Main Authors: M. Narukawa, K. Kawamura, H. Hatsushika, K. Yamazaki, S. -m. Li, J. W. Bottenheim, K. G. Anlauf
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2002
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.981
http://environ.lowtem.hokudai.ac.jp/saishin.pdf/narukawa2003jac.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.511.981 2023-05-15T14:54:51+02:00 Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise M. Narukawa K. Kawamura H. Hatsushika K. Yamazaki S. -m. Li J. W. Bottenheim K. G. Anlauf The Pennsylvania State University CiteSeerX Archives 2002 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.981 http://environ.lowtem.hokudai.ac.jp/saishin.pdf/narukawa2003jac.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.981 http://environ.lowtem.hokudai.ac.jp/saishin.pdf/narukawa2003jac.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://environ.lowtem.hokudai.ac.jp/saishin.pdf/narukawa2003jac.pdf text 2002 ftciteseerx 2016-01-08T09:41:30Z Abstract. Halogenated dicarboxylic acids, such as bromomalonic (Br-C3), chlorosuccinic (Cl-C4) and bromosuccinic (Br-C4) acids, have been measured, for the first time, in the arctic aerosols dur-ing the polar sunrise experiment ALERT2000 (February to May). They were detected in the light spring, but not in the dark winter. Concentration ranges of halogenated diacids in the spring were 0.11–0.68 ng m−3 for Br-C3 diacid, 0.04–0.10 ng m−3 for Cl-C4 diacid and 0.12–0.20 ng m−3 for Br-C4 diacid. Those of Br-C3 diacid increased from late April to early May, whereas Cl-C4 diacid decreased. In contrast, Br-C4 diacid showed maximum concentrations in the middle of the experiment. A strong negative correlation (R = −0.98) was obtained between Br-C3 and Cl-C4 diacids. Concentrations of methanesulfonic acid (MSA) also increased from late April to early May whereas those of Cl − ion decreased. A strong positive correlation was found between Cl-C4 diacid and Cl − ion (R = 0.99) and between Br-C3 diacid and MSA (R = 0.96). These results suggest that Br-C3 diacid is primarily derived from marine biogenic source, whereas Cl-C4 diacid is secondarily formed by heterogeneous reaction involving halogen chemistry on sea salt. Satellite images of sea ice concentrations and backward air mass trajectories suggest that the aerosols containing halogenated diacids were transported over the sampling sites from the Arctic Ocean covered with sea ice. Key words: polar sunrise, bromomalonic acid, chlorosuccinic acid, bromosuccinic acid, sea salt. 1. Text Arctic Arctic Ocean Sea ice Unknown Arctic Arctic Ocean
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Abstract. Halogenated dicarboxylic acids, such as bromomalonic (Br-C3), chlorosuccinic (Cl-C4) and bromosuccinic (Br-C4) acids, have been measured, for the first time, in the arctic aerosols dur-ing the polar sunrise experiment ALERT2000 (February to May). They were detected in the light spring, but not in the dark winter. Concentration ranges of halogenated diacids in the spring were 0.11–0.68 ng m−3 for Br-C3 diacid, 0.04–0.10 ng m−3 for Cl-C4 diacid and 0.12–0.20 ng m−3 for Br-C4 diacid. Those of Br-C3 diacid increased from late April to early May, whereas Cl-C4 diacid decreased. In contrast, Br-C4 diacid showed maximum concentrations in the middle of the experiment. A strong negative correlation (R = −0.98) was obtained between Br-C3 and Cl-C4 diacids. Concentrations of methanesulfonic acid (MSA) also increased from late April to early May whereas those of Cl − ion decreased. A strong positive correlation was found between Cl-C4 diacid and Cl − ion (R = 0.99) and between Br-C3 diacid and MSA (R = 0.96). These results suggest that Br-C3 diacid is primarily derived from marine biogenic source, whereas Cl-C4 diacid is secondarily formed by heterogeneous reaction involving halogen chemistry on sea salt. Satellite images of sea ice concentrations and backward air mass trajectories suggest that the aerosols containing halogenated diacids were transported over the sampling sites from the Arctic Ocean covered with sea ice. Key words: polar sunrise, bromomalonic acid, chlorosuccinic acid, bromosuccinic acid, sea salt. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author M. Narukawa
K. Kawamura
H. Hatsushika
K. Yamazaki
S. -m. Li
J. W. Bottenheim
K. G. Anlauf
spellingShingle M. Narukawa
K. Kawamura
H. Hatsushika
K. Yamazaki
S. -m. Li
J. W. Bottenheim
K. G. Anlauf
Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise
author_facet M. Narukawa
K. Kawamura
H. Hatsushika
K. Yamazaki
S. -m. Li
J. W. Bottenheim
K. G. Anlauf
author_sort M. Narukawa
title Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise
title_short Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise
title_full Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise
title_fullStr Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise
title_full_unstemmed Measurement of Halogenated Dicarboxylic Acids in the Arctic Aerosols at Polar Sunrise
title_sort measurement of halogenated dicarboxylic acids in the arctic aerosols at polar sunrise
publishDate 2002
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.511.981
http://environ.lowtem.hokudai.ac.jp/saishin.pdf/narukawa2003jac.pdf
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
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http://environ.lowtem.hokudai.ac.jp/saishin.pdf/narukawa2003jac.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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