書誌事項
- タイトル別名
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- Relative Importance of Tide and River Discharge on Sediment Transport on Intertidal Flat
- 津波により形成される岸沖断面地形の時空間変動と波数スペクトル特性
- カコウ チョウカンタイ ヒガタ ノ ドシャ ドウタイ ニ オヨボス チョウセキ ト カセン シュッスイ ノ ソウタイテキ ジュウヨウド
- Time-Space Variations and Spectral Evolutions of Sandy Beach Profiles under Tsunami
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抄録
Relative importance of tidal motions and river discharges for the sediment transport was evaluated using field measurements and data analysis on an intertidal flat adjacent to the Shirakawa River mouth. Monthly-averaged sediment budgets during flood periods indicated the different pattern at the closest point to the river mouth. Sediment is transported to north during non-flood period while transported to south during flood period at this point. The basinscale tidal motions are found to be important for the sediment transport during non-flood period. The phase relationships between the peak river discharge and tide level during the flood are most important for the sediment transport on the intertidal flat adjacent to the river mouth in the fetch-limited closed bay.
収録刊行物
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- 土木学会論文集B2(海岸工学)
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土木学会論文集B2(海岸工学) 66 (1), 531-535, 2010
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
- 1390001205320973440
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- NII論文ID
- 130004956620
- 130003808108
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- NII書誌ID
- AA12508551
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- ISSN
- 18838944
- 18848222
- 18842399
- 09167897
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- NDL書誌ID
- 11236098
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
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- 抄録ライセンスフラグ
- 使用不可