Chapter
Apr 26, 2012
Projection of Topographic Change of an Estuary Terrace by Horizontal 2-D Simulation Model, Considering Grain Size
Authors: Toshimitsu Takagi [email protected], Go Asano [email protected], Takushi Inukai [email protected], and Masaya Fukuhama [email protected]Author Affiliations
Publication: Coastal Sediments '07
Abstract
A numerical model for estimating the terrace topography changes caused by floods is introduced, by considering grain size of sediment discharged from a river. Applying this model to Fuji river-mouth, the sediment discharged during floods can be estimated with an aspect of quantity and quality. As the result, it was obvious that the major part of sediment discharged from Fuji river-mouth at floods is flushed out offshore in deeper than 20m depth, which can not contribute as the longshore sediment transport that nourish the neighborhood of the river-mouth.
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Published In
Coastal Sediments '07
Pages: 1623 - 1634
Copyright
© 2007 American Society of Civil Engineers.
History
Published online: Apr 26, 2012
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INA Corporation, Sekiguchi 1-44-10, Bunkyo-ku 112-8668, Tokyo, Japan. E-mail: [email protected]
INA Corporation, Sekiguchi 1-44-10, Bunkyo-ku 112-8668, Tokyo, Japan. E-mail: [email protected]
INA Corporation, Sekiguchi 1-44-10, Bunkyo-ku 112-8668, Tokyo, Japan. E-mail: [email protected]
National Institute for Land and Infrastructure Management, Asahi 1, Tsukuba 305-0804, Japan. E-mail: [email protected]
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.