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  1. 極地研刊行誌
  2. 南極資料 (ISSN 2432-079X)
  3. No.12 (Mar. 1961)

南極海海底土の有機質含量

https://doi.org/10.15094/00007100
https://doi.org/10.15094/00007100
0bbf166e-d84b-47fb-8609-1b57b208de45
名前 / ファイル ライセンス アクション
KJ00002476022.pdf KJ00002476022 (551.5 kB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 1961-03-01
タイトル
タイトル
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 10.15094/00007100
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 ナンキョクカイ カイテイド ノ ユウキシツ ガンリョウ
著者名(日) 杉村, 行男

× 杉村, 行男

WEKO 11036

杉村, 行男

ja-Kana スギムラ, ユキオ

Search repository
野口, 喜三雄

× 野口, 喜三雄

WEKO 11037

野口, 喜三雄

ja-Kana ノグチ, キミオ

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著者名(英) SUGIMURA, Yukio

× SUGIMURA, Yukio

WEKO 11040

en SUGIMURA, Yukio

Search repository
NOGUCHI, Kimio

× NOGUCHI, Kimio

WEKO 11041

en NOGUCHI, Kimio

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著者所属(日)
気象研究所
著者所属(日)
東京都立大学理学部化学教室
著者所属(英)
en
Geochemical Laboratory, Meteorological Research Institute
著者所属(英)
en
Chemistry Department, Faculty of Science, Tokyo Metropolitan University
抄録(英)
内容記述タイプ Other
内容記述 The samples investigated were collected off Lutzow-Holm Bay in Antarctica by Dr. T. TORII aboard the "SOYA", research ship of the 2nd Japanese Antarctic Research Expedition (1957-58). The summary of the results is as follows (See the appendix). (1) Organic carbon in dry sediments ranges between 0.15 and 0.30% and organic nitrogen varies from 0.014 to 0.032%. However, the value of org. N/org.C, 0.05-0.17, does not differ from the corresponding values for bottom sediments from other ocean floors. (2) Chlorophyll derivatives which express an amount of pheophytin equivalent are 4-17 p.p.m. The values are less than the correspending values for the sediments off California, 18-46 p.p.m. (3) Marine humus, as calculated from the value of organic carbon and TRASK'S factor (1.72), varies from 0.3 to 0.5%. The values much differs from the corresponding values for the sediments of the northern Pacific, the southern Pacific and the Atlantic oceans, 1-1.5%, 0.4-1.0% and 0.3-1.5%. (4) Carbonate content shows that the value owes mostly to foraminiferal residues, as CaCO_3 varies from 2 to 11%. The number of the observations so far made is greatly limited. Therefore, the tendencies described above are only approaches to further investigation.
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 12, p. 1071-1073, 発行日 1961-03
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
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