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駿河湾における窒素およびリンの季節変動
https://doi.org/10.14945/00000388
https://doi.org/10.14945/0000038805b5da04-a003-49b9-a75e-2fd5eddf6c2e
名前 / ファイル | ライセンス | アクション |
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KJ00000102488.pdf (868.7 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
タイトル | 駿河湾における窒素およびリンの季節変動 | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Nitrogen | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Phosphorus | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | N : P ratio | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Redfield ratio | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Suruga Bay | |||||||
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 | 10.14945/00000388 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | Seasonal variation of nitrogen and phosphorus pools in the Suruga Bay | |||||||
著者 |
名取, 雄太
× 名取, 雄太× 岩田, 樹哉× 篠村, 理子× 鈴木, 款
WEKO
334
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書誌情報 |
静岡大学地球科学研究報告 巻 29, p. 29-36, 発行日 2002-07 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 452 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | Elemental stoichiometry of inorganic and organic matter, especially for nitrogen (N) and phosphorus (P), is an important parameter for understanding of biogeochemical cycles within marine environments. We determined the pools of N and P for dissolved and particulate organic matter (DOM and POM, respectively) and inorganic matter in the Suruga Bay. Seawater samples were taken from 0 m to 1500 m in February. April, July, October, and December, 2001. Nitrate plus nitrite (NO_3 + NO_2), phosphate (PO_4), dissolved and particulate organic nitrogen (DON and PON, respectively) and those of phosphorus (DOP and POP) were measured, and then N : P ratios were calculated for each pool. N : P ratios showed seasonal variation and notable differences among the pools : N : P ratio was 0 - 15 for the inorganic pool [(NO_3 + NO_2) : PO_4], 20 - 30 for DOM (DON : DOP) and 10 - 16 for POM (PON : POP) . As a result, N : P ratio for inorganic and POM pools were lower than Redfield ratio (= 16 : 1), while that for DOM pool was higher. In other words, N was more deficient than P for inorganic and POM pools. In contrast to this result, P was more deficient than N for DOM. Based on these results, we propose that PON is preferentially remineralized over POP, while DOP is preferentially remineralized over DON in the Suruga Bay. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413412 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |