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タイトル: 大潟海岸・上下浜の海底地形と海底底質の粒度組成 --主に弧状沿岸砂州において--
その他のタイトル: The Profile of the Sea Bottom and the Grain Size Composition of the Sediment on the Sea Bottom in Jogehama, Ogata Coast --As for the Crescent-Shaped Bar, Principally--
著者: 内山, 清  KAKEN_name
著者名の別形: UCHIYAMA, Kiyoshi
キーワード: 弧状沿岸砂州接合部
弧状沿岸砂州中心部
極深部
極浅部
トラフ
バー
jointed measuring line of a crescent-shaped bar
central measuring line of a crescent-shaped bar
extremely deep region
extremely shallow region
trough
bar
発行日: Jun-2016
出版者: 京都大学防災研究所
誌名: 京都大学防災研究所年報. B
巻: 59
号: B
開始ページ: 447
終了ページ: 474
抄録: Ogata Wave Observatory, Kyoto University is located in Yotsuyahama coast, Niigata Pref., Japan. Yotsuyahama coast is in the center of Joetsu-Ogata Coast. In this region, Katamachi sand dune develops very much, and the sediment in Joetsu-Ogata Coast is composed of both sand and gravel. Jogehama coast is another coast in Joetsu-Ogata Coast and is in a natural state. The distance between Yotsuyahama and Jogehama coast is about 3.0km long. The seashore between Yotsuyahama and Jogehama coast has been suffered from severe beach erosion. Both sounding and sediment sampling on the sea bottom have been carried out in Jogehama coast on Nov.7 2010, July.27 2011, July.24 2012. The longshore measurement section is about 200m offshore from shoreline, and the cross-shore measurement sections are at the joint region and the central region of a crescent-shaped bar. The sediment sampling has been conducted in the cross-shore measurement sections at intervals of 1.0m deep. The results of data analyses on both the bottom profile and the grain size composition of the sediment on the sea bottom provide some ideas to understand the reasons for the coastal erosion.
URI: http://hdl.handle.net/2433/217279
関連リンク: http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html
出現コレクション:Vol.59 B

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