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河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性
https://kitami-it.repo.nii.ac.jp/records/7767
ecd958bc-7029-41f2-9d76-04de26e09f28
名前 / ファイル | ライセンス | アクション | |
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2015-06-10 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | PRESSURE PROPAGATION VELOCITY AND PRESSURE ATTENUATION CHARACTERISTIC OF TSUNAMI IN ICE-COVERED RIVER | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Tsunami | |||||
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 | Pressure | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
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 | PRESSURE PROPAGATION VELOCITY AND PRESSURE ATTENUATION CHARACTERISTIC OF TSUNAMI IN ICE-COVERED RIVER | |||||
著者 |
吉川, 泰弘
× 吉川, 泰弘× 渡邊, 康玄× 阿部, 孝章× 大久保, 敦 |
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著者別名 | ||||||
姓名 | ||||||
姓名 | YOSHIKAWA, Yasuhiro | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | ||||||
姓名 | WATANABE, Yasuharu | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | ||||||
姓名 | ABE, Takaaki | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | ||||||
姓名 | OKUBO, Atsushi | |||||
言語 | en | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This study aimed to clarify the pressure propagation velocity and pressure attenuation characteristic of tsunami in ice-covered river. We carried out a hydraulics experiment for tsunami in ice-covered river. This research clari ed the following things. The pressure propagation velocity of a x-ice case is rapid as compared with an open-water case and free-ice case. This velocity of free-ice case becomes later than open-water case. In free-ice case, the pressure propagation velocity becomes late when ice-size becomes smaller. The pressure attenuation of a x-ice case is largest. If ice-size becomes small, pressure will not attenuate. When ice-size is small, the dispersion wave train of the same phenomenon as open-water case happens. On the other hand, When ice-size is big, It stops that dispersion wave train happens. |
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書誌情報 |
ja : 河川技術論文集 巻 19, p. 375-380, 発行日 2013-06 |
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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 |