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南極塩湖の化学的特徴
https://doi.org/10.15094/00007900
https://doi.org/10.15094/00007900d1e72acb-3b0c-4cfe-8b28-e1e39c1e0667
名前 / ファイル | ライセンス | アクション |
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KJ00002477003 (3.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1977-03-01 | |||||
タイトル | ||||||
タイトル | 南極塩湖の化学的特徴 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Chemical Characteristics of Antarctic Saline Lakes | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.15094/00007900 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | ナンキョク エンコ ノ カガクテキ トクチョウ | |||||
著者名(日) |
鳥居, 鉄也
× 鳥居, 鉄也× 山県, 登× 中谷, 周× 村田, 貞雄 |
|||||
著者名(英) |
TORII, Tetsuya
× TORII, Tetsuya× YAMAGATA, Noboru× NAKAYA, Shyu× MURATA, Sadao |
|||||
著者所属(日) | ||||||
千葉工業大学 | ||||||
著者所属(日) | ||||||
国立公衆衛生院 | ||||||
著者所属(日) | ||||||
北海道大学水産学部 | ||||||
著者所属(日) | ||||||
千葉工業大学 | ||||||
著者所属(英) | ||||||
en | ||||||
Chiba Institute of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Public Health | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Fisheries, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Chiba Institute of Technology | ||||||
抄録(日) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 南極大陸の露岩地域には多くの湖沼が存在するが,その塩分濃度あるいは化学組成にはさまざまな特徴がみられる.この報告は,昭和,マクマード,ベストフォールドの各オアシスの湖沼調査から,とくに塩湖の化学的特徴を中心として述べたものである.南極の塩湖は,沿岸地域と山岳地域のものとに大別されるが,前者は一般に湖面高度が海面下にあって,地形上からも,また水質や湖岸堆積物などの化学的特徴からみても海跡湖とみられるものが多い.一方,山岳地域のものは,旧湖岸線も存在し湖水面が過去に大きく変動し,湖水がくりかえし濃縮されたことを示唆するが,水質が海水と異なって単純に塩分の起因を説明しえない.しかし,最近実施されたDVDP調査の結果から,これら山岳地域の塩湖も塩類の大部分は海水に由来し,その後変質したと考えられるに至った.そして水質の考察から,沿岸地域のものより一般に古い歴史をもつものと推定される. | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Chemical characteristics of main Antarctic saline lakes found in the oases of McMurdo. Vestfold and Syowa are reviewed. Lakes are primarily classified into the fresh and saline ones and then the latter into coastal lakes and those located in the glacial trough such as the Dry Valleys, Victoria Land. The coastal saline lakes are characterized by that the elevation of lake surface is below sea level and the chemical composition, such as M/C1 ratio, isotopic ratio of oxygen and hydrogen, and also the nutrient elements resemble those of sea water, while the saline lakes in the Dry Valleys have a complex origin. From the geochemical point of view, it is suggested that the formation of the coastal lakes is much younger than that of the lakes in the Dry Valleys. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00181831 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00857289 | |||||
書誌情報 |
南極資料 巻 58, p. 9-19, 発行日 1977-03 |
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出版者 | ||||||
出版者 | 国立極地研究所 |