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結氷時の塩水遡上に関する現地観測
https://kitami-it.repo.nii.ac.jp/records/7745
https://kitami-it.repo.nii.ac.jp/records/7745c6126295-4866-4064-8d19-db59d7a1da76
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
2006-06_結氷時の塩水遡上に関する現地観測.pdf (900.6 kB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2015-06-02 | |||||
| タイトル | ||||||
| タイトル | 結氷時の塩水遡上に関する現地観測 | |||||
| 言語 | ja | |||||
| タイトル | ||||||
| タイトル | FIELD OBSERVATIONS ON SALINITY INTRUSION AT ICE-COVERED RIVERS | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Ice-Covered River | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Tidal Zone | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Field Observation | |||||
| 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 | journal article | |||||
| アクセス権 | ||||||
| アクセス権 | open access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
| その他のタイトル | ||||||
| その他のタイトル | FIELD OBSERVATIONS ON SALINITY INTRUSION AT ICE-COVERED RIVERS | |||||
| 著者 |
吉川, 泰弘
× 吉川, 泰弘× 渡邊, 康玄 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 39767 | |||||
| 姓名 | YOSHIKAWA, Yasuhiro | |||||
| 言語 | en | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 39768 | |||||
| 姓名 | WATANABE, Yasuharu | |||||
| 言語 | en | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The purpose of this study is to clarify hydraulic phenomena in the estuarine basins of ice-covered rivers. Field observations were therefore conducted. As a result, it was found that reducing the time for each measurement was important when conducting flow observations in estuarine basins. Similarities and differences of phenomena in rivers when they were covered or not covered with ice were also clarified. Similar phenomena indicate a correlation between the water-level fluctuation velocity and the total discharge, and the two different relationships between the tidal and water levels that result from increases and decreases in the former. Different phenomena indicate a great variety in flow direction depending on the tides when the rivers were covered with ice, and the reduction of the freshwater flow velocity due to the friction resistance of ice sheets during salinity intrusion. |
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| 書誌情報 |
河川技術論文集 巻 12, p. 157-162, 発行日 2006-06 |
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| 権利 | ||||||
| 権利情報 | c 2006 公益社団法人 土木学会 | |||||
| 出版者 | ||||||
| 出版者 | 公益社団法人 土木学会 | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
