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CHEMICAL CHARACTERISTICS OF POND WATERS IN THE LABYRINTH OF SOUTHERN VICTORIA LAND, ANTARCTICA
https://doi.org/10.15094/00002576
https://doi.org/10.15094/00002576161cdfc6-0b63-4543-918c-dcd83365c8c6
名前 / ファイル | ライセンス | アクション |
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KJ00002368166 (92.7 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1988-09-01 | |||||
タイトル | ||||||
タイトル | CHEMICAL CHARACTERISTICS OF POND WATERS IN THE LABYRINTH OF SOUTHERN VICTORIA LAND, 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 | 10.15094/00002576 | |||||
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 | CHEMICAL CHARACTERISTICS OF POND WATERS IN THE LABYRINTH OF SOUTHERN VICTORIA LAND, ANTARCTICA | |||||
著者名よみ |
トリイ, テツヤ
× トリイ, テツヤ× ナカヤ, シュウ× マツバヤ, オサム× マツモト, ゲンキ× タカマツ, ノブキ× マスダ, ノリヤス× カワノ, タミオ× ムラヤマ, ハルタ |
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著者名(英) |
TORII, Tetsuya
× TORII, Tetsuya× NAKAYA, Shyu× MATSUBAYA, Osamu× MATSUMOTO, Genki I.× TAKAMATSU, Nobuki× MASUDA, Noriyasu× KAWANO, Tamio× MURAYAMA, Haruta |
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著者所属(英) | ||||||
en | ||||||
Chiba Institute of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Hirosaki University | ||||||
著者所属(英) | ||||||
en | ||||||
Research Institute of Underground Resources, Mining College, Akita University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Chemistry, The College of Arts and Science, The University of Tokyo | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Chemistry, Toho University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Chemistry, Faculty of Fisheries, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Chemistry, Faculty of Education, Oita University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Chemistry, Faculty of Education, Yokohama National University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A large number of fresh and saline ponds are found in the Labyrinth (77°33'S, 160°50'E) of the upper Wright Valley in the Dry Valleys region of southern Victoria Land, Antarctica. They are located near the terminus of the Wright Upper Glacier between 800-1000m above sea level. From a limnological point of view, the most interesting problems concerning these saline ponds are the origin of their salts and their evolutional history. Chloride ion contents vary remarkably among the ponds ranging from 0.0049 to 52.4g kg^<-1>. Surprisingly, more than a half of the ponds are saline with the highest chloride ion content being 2.7 times greater than that of seawater. The δD and δ^<18>O values of the pond waters indicate a snow and/or glacier melt-water origin, and that the ponds underwent subsequent alteration due to evaporation or freezing. The composition of chemical components reveal no evidence of trapped seawater. Thus the salt concentrations in the Labyrinth pond waters must be explained principally by the accumulation of atmospheric salts and subsequent repeated cycles of evaporation and freezing of the pond waters over a considerable period of time. (This paper is submitted to the special issue of Hydrobiologia.) | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 2, p. 174, 発行日 1988-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |