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  1. 掲載誌一覧
  2. 鹿児島大学水産学部紀要
  3. vol.56
  1. 水産学部
  2. 水産学部・紀要論文

隆起楕円形島における海浜形成と底質の淘汰 : 鹿児島県新島(燃島)の例

http://hdl.handle.net/10232/4777
http://hdl.handle.net/10232/4777
9b1ea98f-c74c-4e9c-aa92-94ab8113b0bb
名前 / ファイル ライセンス アクション
01_NISHI.pdf 01_NISHI.pdf (12.9 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2015-01-13
タイトル
タイトル 隆起楕円形島における海浜形成と底質の淘汰 : 鹿児島県新島(燃島)の例
別言語のタイトル
その他のタイトル Formation of Beach and Sediment Sorting on Shinjima Island, Kagoshima, Japan
著者 西, 隆一郎

× 西, 隆一郎

WEKO 13848
NRID 1000030189253

西, 隆一郎

Search repository
宇多, 高明

× 宇多, 高明

WEKO 101714

宇多, 高明

Search repository
山本, 幸二

× 山本, 幸二

WEKO 101715

山本, 幸二

Search repository
別言語の著者
姓名 NISHI, Ryuichiro
別言語の著者
姓名 UDA, Takaaki
別言語の著者
姓名 YAMAMOTO, Koji
言語
言語 jpn
キーワード
主題Scheme Other
主題 Coastal processes
キーワード
主題Scheme Other
主題 Elliptic island
キーワード
主題Scheme Other
主題 Cliff erosion
キーワード
主題Scheme Other
主題 Spit formation
キーワード
主題Scheme Other
主題 Sediment sorting
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
要約(Abstract)
内容記述タイプ Other
内容記述 Shinjima Island is located in Kagoshima Bay, Japan. It was formed by raising of the soil from the sea bottom ofAira Caldera area due to the volcanic eruption of Mt. Sakurajima in the year 1778. Since then, cliff erosion has occurred at the west, north and east coasts of the island. On the other hand, sandy beach (spit) has been created at the south side of Shinjima Island by eroded materials from the cliff. The shape of the island becomes elliptic due to the predominant northern incident waves. This relatively new island is one of the ideal locations to study the formation process of natural beach and sediment sorting by waves in a natural manner, as well as to investigate the speed ofclifferosion. In Kagoshima Prefecture, a number of coasts are bounded by sea cliffs composed by Sirasu sand which is an unconsolidated volcanic debris and is a commonly found soil material in southern Kyushu in Japan. The study shows that a rate ofclifferosion at north coast of Shinjima Island is nearly 1.55m/yr and the cliff has been retreated over 289m since the rise. A sand spit created by the cliff material migrates to southeastward and southwestward directions depending on the seasonal change in predominant wave angle. A size of the spit recently tends to decrease due to the reduction of cliff erosion by revetments and breakwaters set in front of the cliff. Forty percent of the tarus sediment material is smaller than 0.5mm in front of the cliff, in contrast six percent of sediment material on the sandy spit is smaller than 0.5 mm. Most offiner portion of the supplied cliff material was dispersed into deep water while it was moving along the island to the southern tip. Coarse material which is larger than 5mm is left relatively close to the cliff(supply site) and a component of coarse material decreases to a down-drift direction. As a result, a sorting of transported sediment is increased in down-drift direction.
収録雑誌名 鹿児島大学水産学部紀要=Memoirs of Faculty of Fisheries Kagoshima University

巻 56, p. 1-9
作成日
日付 2007-12-25
ISSN
収録物識別子タイプ ISSN
ISSN 0453087X
NII書誌ID(雑誌)
収録物識別子タイプ NCID
NC ID AN00040498
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
NDC
主題Scheme NDC
主題 450
公開者・出版者
出版者 鹿児島大学
公開者よみ
公開者よみ カゴシマ ダイガク
公開者別名
公開者別名 Kagoshima University
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