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Chemical characteristics of basal ice near Hamna Icefall, East Antarctica
https://doi.org/10.15094/00002908
https://doi.org/10.15094/000029084c6f19d9-c013-440b-9a43-043ba986ae84
名前 / ファイル | ライセンス | アクション |
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KJ00002364395 (1.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2000-11-01 | |||||
タイトル | ||||||
タイトル | Chemical characteristics of basal ice near Hamna Icefall, East Antarctica | |||||
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 | 10.15094/00002908 | |||||
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 | ||||||
Scientific Paper | ||||||
論文名よみ | ||||||
その他のタイトル | Chemical characteristics of basal ice near Hamna Icefall, East Antarctica | |||||
著者名よみ |
イイズカ, ヨシノリ
× イイズカ, ヨシノリ× イガラシ, マコト× シライワ, タカユキ× ナルセ, レンジ× ヤマダ, トモミ× ワタナベ, オキツグ |
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著者名(英) |
Iizuka, Yoshinori
× Iizuka, Yoshinori× Igarashi, Makoto× Shiraiwa, Takayuki× Naruse, Renji× Yamada, Tomomi× Watanabe, Okitsugu |
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著者所属(英) | ||||||
en | ||||||
Department of Polar Science, The Graduate University for Advanced Studies | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Low Temperature Science, Hokkaido University | ||||||
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 | Debris-laden basal ice is exposed along an ice cliff (about 30m high) near Hamna Icefall, Soya Coast, East Antarctica. The basal ice about 6.8m thick can be divided into an upper part (5.5m) and a lower part (1.3m) based on stratigraphic features. Major dissolved ions of the basal ice are probably composed of eight species (Na^+, K^+, Mg^<2+>, Ca^<2+>, Cl, SO_4^2,NO_3 and HCO_3). Almost all Na^+, K^+, Mg^<2+>, Ca^<2+>, SO_4^2 and HCO_3 in the basal ice are considered to have originated from chemical erosion of rock minerals at the base of the ice sheet. According to a calculation of ion composition, the primary rock mineral dissolved in the basal ice is considered to be carbonate. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1129795X | |||||
書誌情報 |
Polar meteorology and glaciology 巻 14, p. 8-15, 発行日 2000-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |