Sedimentation History of the Sand Bars in the Entrance of Tofutsu Lake Evaluated by Means of MASW

Bibliographic Information

Other Title
  • 濤沸湖における湖口周辺砂州の表面波探査を活用した堆積形成史の復元

Abstract

At the entrance of the Tofutsu Lake, which is one of the lagoons located along the Okhotsk Sea in Hokkaido, sand bars have been significantly developed. The objective of this study is to evaluate the sequential sedimentation history of the sand bars by means of MASW (Multi-channel Analysis of Surface Waves) technology. We found out that the sedimentation stratigraphy under the sand bars were significantly different from muddy to sandy, even though the sand bars apparently consisted of the same sandy material. From the shear wave velocity structure obtained in this study, we successfully restored the sequential sedimentation process. Also, the sedimentation history was consistent with an old aerial photograph and memories of local inhabitants.

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Details 詳細情報について

  • CRID
    1390001205317040512
  • NII Article ID
    130004956365
  • DOI
    10.2208/kaigan.65.661
  • ISSN
    18838944
    18842399
  • Text Lang
    en
  • Data Source
    • JaLC
    • Crossref
    • CiNii Articles
  • Abstract License Flag
    Disallowed

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