Fine sediment deposition in a curved channel with an intake weir

Yoshiyuki Shirotori, Kozo Watanabe, Keiko Udo, Akira Mano

    Research output: Chapter in Book/Report/Conference proceedingChapter


    On the upstream of Atago weir, Hirose River, Japan, the sedimentation phenomenon is complex due to the coexistence of the weir and channel bend. Moreover, fine sediment accumulates on the river bed notably. From the observed results, it is found that silt is the major component in the flood water and accumulates significantly in the discharge increasing stage by the backwater of the weir. From the theoretical computation considering the settling and resuspension of the suspended sediment, the cohesion of fine sediment is an important factor of the net deposition process.

    Original languageEnglish
    Title of host publicationAdvances in Geosciences
    Subtitle of host publicationVolume 11: Hydrological Science (HS)
    PublisherWorld Scientific Publishing Co.
    Number of pages13
    ISBN (Electronic)9789812836144
    ISBN (Print)9812836136, 9789812836137
    Publication statusPublished - 2009 Jan 1

    ASJC Scopus subject areas

    • Earth and Planetary Sciences(all)
    • Environmental Science(all)


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