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アイテム
"深見池の成層期における溶存態鉄,懸濁態鉄の存在状態 : 特に溶存有機態鉄について"
https://nagoya-wu.repo.nii.ac.jp/records/2217
https://nagoya-wu.repo.nii.ac.jp/records/221705a88f48-b798-4e59-8164-a47a3a0efeab
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00000179512.pdf (617.7 kB)
|
BY-NC-ND
|
| アイテムタイプ | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 1995-03-05 | |||||
| タイトル | ||||||
| タイトル | "深見池の成層期における溶存態鉄,懸濁態鉄の存在状態 : 特に溶存有機態鉄について" | |||||
| タイトル | ||||||
| タイトル | "Dissolved and Particulate Irons during the Stagnation Period in the Seasonally Anoxic Lake, Lake Fukami-ike : Dissolved Organic Iron" | |||||
| 言語 | en | |||||
| 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 | |||||
| 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 | 〓 | |||||
| 著者名(日) |
八木, 明彦
× 八木, 明彦× 長谷, 成子× 山田, 久美子 |
|||||
| 著者名よみ |
ヤギ, アキヒコ
× ヤギ, アキヒコ× ハセ, シゲコ× ヤマダ, クミコ |
|||||
| 著者名(英) |
YAGI, Akihiko
× YAGI, Akihiko× HASE, Shigeko× YAMADA, Kumiko |
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| 著者所属(日) | ||||||
| 値 | 名古屋女子大学 | |||||
| 著者所属(日) | ||||||
| 値 | 名古屋女子大学 | |||||
| 著者所属(日) | ||||||
| 値 | 名古屋女子大学 | |||||
| 著者所属(英) | ||||||
| 言語 | en | |||||
| 値 | NAGOYA WOMEN'S UNIVERSITY | |||||
| 著者所属(英) | ||||||
| 言語 | en | |||||
| 値 | NAGOYA WOMEN'S UNIVERSITY | |||||
| 著者所属(英) | ||||||
| 言語 | en | |||||
| 値 | NAGOYA WOMEN'S UNIVERSITY | |||||
| 抄録(英) | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | "Lake Fukami-ike is a small lake having a maximum depth of 8.0m, and is well protected from the wind. Lake water stratified from March to October and circulated from November to March. Anoxic condition prevailed below 4-5m depth from April to October. This study was undertaken to clarify in detail the distributions of iron chemical forms in Lake Fukami-ike. The concentration of dissolved iron seemed to be controlled by the balance among the supply of Allochtonous iron, the deposition or dissolution of particulate iron (P-Fe) in the hypolimnion and the FeS fixation at the bottom. The dissolved iron (D-Fe) in the hypolimnion water was specified by ultrafiltration. Percentages of dissolved iron in two molecular weight fractions in depth of 7.0m were 20-30% (M. W. < 5,000), 45-10% (5,000 < M. W. < 100,000) and 5-70% (M. W. > 100,000), respectively. These results indicate that about 50-80% of total dissolved iron was present as the organic form, mainly having a molecular weight of 5,000-100,000, in the hypolimnion of Lake Fukami-ike." | |||||
| 雑誌書誌ID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN10088581 | |||||
| 書誌情報 |
名古屋女子大学紀要. 家政・自然編 en : Journal of Nagoya Women's University. Home economics・natural science 巻 41, p. 147-154, 発行日 1995-03-05 |
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