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河川津波による塩水遡上現象に関する研究
https://kitami-it.repo.nii.ac.jp/records/8460
https://kitami-it.repo.nii.ac.jp/records/8460136cc0e5-cafc-437a-a9b1-783d8b3c3cde
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 | 2016-09-06 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 河川津波による塩水遡上現象に関する研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | A STUDY OF SALINITY INTRUSION BY TSUNAMI IN RIVER | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | river tsunami | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | salinity intrusion | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | vertical 2-dimensional model | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 1-dimensional 2-layer model | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | xperiment | |||||
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URI | open access | |||||
その他のタイトル | ||||||
その他のタイトル | A STUDY OF SALINITY INTRUSION BY TSUNAMI IN RIVER | |||||
著者 |
吉川, 泰弘
× 吉川, 泰弘× 阿部, 孝章× 中津川, 誠× 船木, 淳悟 |
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著者別名 | ||||||
姓名 | YOSHIKAWA, Yasuhiro | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | ABE, Takaaki | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | NAKATSUGAWA, Makoto | |||||
言語 | en | |||||
著者別名 | ||||||
姓名 | FUNAKI, Jungo | |||||
言語 | en | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This study aimed to clarify the phenomenon of salinity intrusion by tsunami in river. Influence of tsunami height and flow velocity given to salinity intrusion is examined by vertical 2-dimensional unsteady flow numerical calculation. The long term phenomenon of salinity intrusion by tsunami in real river is examined by 1-dimensional 2-layer unsteady flow numerical calculation. We conducted the validity of these numerical calculations by a hydraulic experiment. The following knowledge was acquired by this study. 1) When water level goes up by tsunami in river, This fluid, which is going up may not be salt water. 2) When the tsunami exceeding water surface of the river occurs, Tsunami flows quickly on the water surface of the river. 3) In the conditions that tsunami height is high and flow velocity is late, salt water ascends to the up-stream side. 4) When the tsunami which ascended to the river flows into the down-stream side, salt water tip position does not immediately flow into the down-stream side. | |||||
書誌情報 |
土木学会論文集B2(海岸工学) 巻 72, 号 2, p. I_403-I_408, 発行日 2015 |
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DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | http://doi.org/10.2208/kaigan.71.I_403 | |||||
権利 | ||||||
権利情報 | c 2015 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 |