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- W2317953502 abstract "A significant development of sandbars can be seen at the entrance of Lake Tofutsu, one of the lagoons located along the Okhotsk Sea in Hokkaido, Japan. The purpose of this study is to investigate the sequential sedimentation history of these sandbars. We examined the shear-wave velocity and stiffness structures of these sandbars using a surface wave method called the multichannel analysis of surface waves (MASW) in order to identify and describe the stratigraphy of the sediments at the entrance of Lake Tofutsu. We discovered that even though the sandbars appear to be composed of the same sandy material, the subsoil under the sandbars has a very varied sedimentation stratigraphy, consisting of muddy soil derived from the upstream of the lake and sandy soil derived from the coastal sand of the Okhotsk Sea. On the basis of the shear-wave velocity structure obtained in this study, we successfully determined the sequential sedimentation process." @default.
- W2317953502 created "2016-06-24" @default.
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- W2317953502 date "2010-10-29" @default.
- W2317953502 modified "2023-09-25" @default.
- W2317953502 title "Evaluation of Sedimentation History of Sandbars at Entrance of Lake Tofutsu, Hokkaido, Japan, by MASW Technology" @default.
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- W2317953502 doi "https://doi.org/10.1061/41147(392)102" @default.
- W2317953502 hasPublicationYear "2010" @default.
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