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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Language: | English |
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National Institute of Polar Research
1992
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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 |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00003755 |
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 |