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CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS
https://doi.org/10.15094/00003755
https://doi.org/10.15094/000037559c818cde-b845-4394-b36b-530585604174
名前 / ファイル | ライセンス | アクション |
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KJ00000767909 (65.4 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1992-12-01 | |||||
タイトル | ||||||
タイトル | CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003755 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | CHEMISTRY OF ANTARCTIC ATMOSPHERIC AEROSOLS | |||||
著者名よみ |
カナモリ, サトル
× 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 |
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著者名(英) |
KANAMORI, Satoru
× KANAMORI, Satoru× KANAMORI, Nobuko× NISHIKAWA, Masataka× WATANABE, Okitsugu× AOKI, Shuhji |
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著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute for Environmental Studies | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 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. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 6, p. 151, 発行日 1992-12 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |