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南極オングル島付近のパドルの水質(海洋部門)(<特集>南極シンポジウム)
https://doi.org/10.15094/00007032
https://doi.org/10.15094/00007032664b421a-cf1a-48e9-8334-c9f15b5882ff
名前 / ファイル | ライセンス | アクション |
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KJ00002406696 (2.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1961-01-01 | |||||
タイトル | ||||||
タイトル | 南極オングル島付近のパドルの水質(海洋部門)(<特集>南極シンポジウム) | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | On the Puddle Waters in the Vicinity of Ongul Island, Antarctica (OCEANOGRAPHY) (<Special Publication>Antarctic Symposium in Tokyo, 1960) | |||||
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 | 10.15094/00007032 | |||||
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 オングルトウ フキン ノ パドル ノ スイシツ | |||||
著者名(日) |
南, 英一
× 南, 英一× 松本, 利松× 小坂, 丈予 |
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著者名(英) |
MINAMI, Eiiti
× MINAMI, Eiiti× MATUMOTO, Tosimatu× OSSAKA, Joyo |
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著者所属(英) | ||||||
en | ||||||
The Earthquake Research Institute, Tokyo University:(Present address)Sophia University | ||||||
著者所属(英) | ||||||
en | ||||||
The Earthquake Research Institute, Tokyo University:The Japanese Antarctic Research Expedition, 1956-57 | ||||||
著者所属(英) | ||||||
en | ||||||
The Earthquake Research Institute, Tokyo University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Chemical analyses on the water collected in January-February 1957 from 8 puddles on the fast ice near Ongul Island showed the results as seen in Table 2 and led us to the following considerations. The remarkable lower value of the salinity in comparison with sea water means naturally that the puddles were formed by remelting of ice bed, and the remarkable local variation in the salt contents denies the consideration if these puddles should be in reciprocal communication under the surface ice sheet. Of course, the fact, that the relative proportions of the elements contained in puddle waters are quite similar to these of the sea water, tells that the former has got the influence from the latter. But, in details, the equivalent ratios calculated show sufficient differences from that of mean sea waters. This comes from the fractionation in the path of transportation of sea water into puddles, and the stability of the contents through the transportation is in an ascending order as SO_4<Cl≦Na<K, Mg<Ca. This order presents the similarity rather to that of the pond water on East Ongul Island investigated by Ken SUGAWARA than to that of the waters in Japan. The results of investigation on deutrium content indicate that the puddle waters lies between the pond water in East Ongul Island and the nearby sea water in its value. | |||||
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 11, p. 841-847, 発行日 1961-01 |
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国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.46 | |||||
出版者 | ||||||
出版者 | 国立極地研究所 |