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アイテム
嶮淵川における背水の影響を考慮したアイスジャムの検討
https://kitami-it.repo.nii.ac.jp/records/2000051
https://kitami-it.repo.nii.ac.jp/records/200005180210b94-dda4-48bb-9541-71faf150f0df
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
河川技術論文集, 26, pp.175-180.pdf (1.7 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||||||
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| 公開日 | 2021-05-26 | |||||||||
| タイトル | ||||||||||
| タイトル | 嶮淵川における背水の影響を考慮したアイスジャムの検討 | |||||||||
| 言語 | ja | |||||||||
| タイトル | ||||||||||
| タイトル | EXAMINATION OF ICE JAM CONSIDERING THE EFFECT OF BACK WATER IN THE KENUFUCHI RIVER | |||||||||
| 言語 | en | |||||||||
| 言語 | ||||||||||
| 言語 | jpn | |||||||||
| キーワード | ||||||||||
| 言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | ice jam | |||||||||
| キーワード | ||||||||||
| 言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | ice-covered river | |||||||||
| キーワード | ||||||||||
| 言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | numerical simulation | |||||||||
| キーワード | ||||||||||
| 言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | back water | |||||||||
| 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 | |||||||||
| 著者 |
伊波, 友生
× 伊波, 友生
× 吉川, 泰弘× 横山, 洋× 矢部, 浩規 |
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| 抄録 | ||||||||||
| 内容記述タイプ | Abstract | |||||||||
| 内容記述 | On March 9, 2018, an ice jam occurred on the Kenefuchi River a tributary of Chitose river, due to rainfall and rising temperatures. The Kenefuchi River is narrow and has several bridges, etc., making it more vulnerable to ice jam. These ice jams can cause collision of floating ice and floods. In river management, it is important to understand how the formation of ice jam is controlled by different hydraulic conditions. In this study, we performed numerical calculations on the Kenefuchi River to quantitatively understand how the ice jam formation condition changes with boundary conditions. Considering that the boundary conditions of Kenefuchi river are affected by the water level of the main river, i.e. Chitose River, we focused on the water level at the downstream end of the kenefuchi river. We examined how it affects the formation, melting and flow of river ice. The numerical calculations suggest that a rise in the water level in the main river increased the range of area in which ice jams occurred. It also increased the time required for resolving the ice jams. Increased water level in the main river affects the backwater in the Kenefuchi River, contributing to an increase in the number of ice jam Also, a phenomenon was observed in which multiple ice jams united to form one large ice jam. From this, it was found that it is necessary to consider the influence of backwater to correctly determine the location and scale of the ice jam. |
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| 言語 | en | |||||||||
| 書誌情報 |
ja : 河川技術論文集 巻 26, p. 175-180, 発行日 2020-06 |
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| 権利 | ||||||||||
| 権利情報 | c 2020 公益社団法人 土木学会 | |||||||||
| 出版者 | ||||||||||
| 出版者 | 土木学会 | |||||||||
| 言語 | ja | |||||||||
| 著者版フラグ | ||||||||||
| 言語 | en | |||||||||
| 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 | |||||||||
