書誌事項
- タイトル別名
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- DEVELOPMENT OF A MEANDERING CHANNEL CAUSED BY A SHAPE OF THE ALTERNATE BARS
- サス チケイ ニ ユウハツ サレタ ダコウ ハッタツ
- DEVELOPMENT OF A MEANDERING CHANNEL CAUSED BY A SHAPE OF THE ALTERNATE BARS
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抄録
In September 2011, the largest discharge in recorded history was observed in Otofuke River, causing riverbank erosion in various parts of the basin. Damage was especially serious in the middle reaches, where part of a dike was completely washed out. The results of a survey suggested that the cause of the dike breakage was bank erosion associated with the development of a meandering channel. As the related development mechanism and predominant factors have not yet been clarified, this remains a priority for disaster prevention. In this study, the meandering-channel development process was reproduced using a slope failure model that linked bank erosion with bed fluctuations. The study attempted to clarify the meander development mechanism and predominant related factors based on this model.
収録刊行物
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- 土木学会論文集B1(水工学)
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土木学会論文集B1(水工学) 69 (4), I_1099-I_1104, 2013
公益社団法人 土木学会
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詳細情報 詳細情報について
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- CRID
- 1050282813784919040
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- NII論文ID
- 40019820026
- 120005983955
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- NII書誌ID
- AN10426673
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- ISSN
- 18808751
- 09167374
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- NDL書誌ID
- 024918286
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- 本文言語コード
- ja
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- 資料種別
- journal article
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- データソース種別
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- IRDB
- NDL
- CiNii Articles
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