海底近傍に形成される高濁度水の物理化学特性
書誌事項
- タイトル別名
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- Physical and Chemical Property of High Turbidity Layer Formed near the Sea Bottom
抄録
An unstable density field is formed near the bottom of Kaita Bay. It is predicted that the unstable density field is kept by density increment from suspended organic mud. In order to understand the property and behavior of suspended organic mud, relationship among of settling time, diameter and composition was investigated. Furthermore, density increment from suspended organic mud is confirmed. As a result, it is cleared that property of slowly suspended organic mud is small diameter and low C/N ratio. Additionally, density increment of suspended organic mud is bigger than that of soil particle.
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） 67 (2), I_861-I_865, 2011
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
- 1390001205321463040
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- NII論文ID
- 130004550607
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- ISSN
- 18838944
- 18842399
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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
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- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可