CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS

P(論文) Inland atmospheric aerosols were sampled by members of JARE-29 (1988-1989) using a modified Andersen type cascade impacter, which consists of 12 impacter stages and a back-up filter and can fractionate aerosol particles down to 0.04 micron. MSA (methane sulfonic acid) and nssSO_4 showed their...

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Main Authors: カナモリ, サトル, カナモリ, ノブコ, ニシカワ, マサタカ, ワタナベ, オキツグ, アオキ, シュンジ, KANAMORI, Satoru, KANAMORI, Nobuko, NISHIKAWA, Masataka, WATANABE, Okitsugu, AOKI, Shuhji
Language:English
Published: National Institute of Polar Research 1992
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3755/files/KJ00000767909.pdf
https://doi.org/10.15094/00003755
https://nipr.repo.nii.ac.jp/records/3755
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author カナモリ, サトル
カナモリ, ノブコ
ニシカワ, マサタカ
ワタナベ, オキツグ
アオキ, シュンジ
KANAMORI, Satoru
KANAMORI, Nobuko
NISHIKAWA, Masataka
WATANABE, Okitsugu
AOKI, Shuhji
author_facet カナモリ, サトル
カナモリ, ノブコ
ニシカワ, マサタカ
ワタナベ, オキツグ
アオキ, シュンジ
KANAMORI, Satoru
KANAMORI, Nobuko
NISHIKAWA, Masataka
WATANABE, Okitsugu
AOKI, Shuhji
author_sort カナモリ, サトル
collection National Institute of Polar Research Repository, Japan
description P(論文) Inland atmospheric aerosols were sampled by members of JARE-29 (1988-1989) using a modified Andersen type cascade impacter, which consists of 12 impacter stages and a back-up filter and can fractionate aerosol particles down to 0.04 micron. MSA (methane sulfonic acid) and nssSO_4 showed their maximum in size distribution at 0.2-0.3 micron. Their distribution curves run parallel with similar trend and strongly suggest their same or closely related origin. Na has its maximum at 0.6-0.7 micron; its marine origin is indicated by the similar trend of Mg and also by the Mg/Na ratio close to that in seawater. Therefore, MSA and nssSO_4 ratio at the peak of size distribution was at nearly 0.1,which is higher than 0.2 over the Antarctic sea and at Syowa Station, and suggests their supply from a warmer low-latitude sea area. departmental bulletin paper
genre Antarc*
Antarctic
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Antarc*
Antarctic
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
geographic Antarctic
Syowa Station
The Antarctic
geographic_facet Antarctic
Syowa Station
The Antarctic
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institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003755
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
6
151
AA10756213
https://nipr.repo.nii.ac.jp/record/3755/files/KJ00000767909.pdf
https://doi.org/10.15094/00003755
https://nipr.repo.nii.ac.jp/records/3755
publishDate 1992
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003755 2025-04-13T14:08:11+00:00 CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS カナモリ, サトル カナモリ, ノブコ ニシカワ, マサタカ ワタナベ, オキツグ アオキ, シュンジ KANAMORI, Satoru KANAMORI, Nobuko NISHIKAWA, Masataka WATANABE, Okitsugu AOKI, Shuhji 1992-12 application/pdf https://nipr.repo.nii.ac.jp/record/3755/files/KJ00000767909.pdf https://doi.org/10.15094/00003755 https://nipr.repo.nii.ac.jp/records/3755 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 6 151 AA10756213 https://nipr.repo.nii.ac.jp/record/3755/files/KJ00000767909.pdf https://doi.org/10.15094/00003755 https://nipr.repo.nii.ac.jp/records/3755 1992 ftnipr https://doi.org/10.15094/00003755 2025-03-19T10:19:57Z P(論文) Inland atmospheric aerosols were sampled by members of JARE-29 (1988-1989) using a modified Andersen type cascade impacter, which consists of 12 impacter stages and a back-up filter and can fractionate aerosol particles down to 0.04 micron. MSA (methane sulfonic acid) and nssSO_4 showed their maximum in size distribution at 0.2-0.3 micron. Their distribution curves run parallel with similar trend and strongly suggest their same or closely related origin. Na has its maximum at 0.6-0.7 micron; its marine origin is indicated by the similar trend of Mg and also by the Mg/Na ratio close to that in seawater. Therefore, MSA and nssSO_4 ratio at the peak of size distribution was at nearly 0.1,which is higher than 0.2 over the Antarctic sea and at Syowa Station, and suggests their supply from a warmer low-latitude sea area. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Antarctic Syowa Station The Antarctic
spellingShingle カナモリ, サトル
カナモリ, ノブコ
ニシカワ, マサタカ
ワタナベ, オキツグ
アオキ, シュンジ
KANAMORI, Satoru
KANAMORI, Nobuko
NISHIKAWA, Masataka
WATANABE, Okitsugu
AOKI, Shuhji
CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
title CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
title_full CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
title_fullStr CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
title_full_unstemmed CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
title_short CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
title_sort chemistry of antarctic atmospheric aerosols
url https://nipr.repo.nii.ac.jp/record/3755/files/KJ00000767909.pdf
https://doi.org/10.15094/00003755
https://nipr.repo.nii.ac.jp/records/3755