Research Project
Grant-in-Aid for Challenging Exploratory Research
Skeletal structure in soil from a sliding surface of Aratozawa Landslide was investigated to reveal the sliding mechanisms using Cryo-SEM. Many cylindrical and latticed grains were found in silt stone that formed the sliding surface of the landslide, while those were not found in the tufa that overlay the silt. Crushing of cylindrical and latticed grains was likely leading to pore-fluid pressure build-up resulting in the long travelling distance (300m) on the gentle slope (< 4 degrees) of the Aratozawa Landslide.
All 2012 Other
All Journal Article (2 results) (of which Peer Reviewed: 1 results) Presentation (1 results)
森林総合研究所研究報告
Volume: 11巻2号 Pages: 71-75
40019465704
Proceedings of International Symposium on Earthquake-induced Landslides
Volume: 1巻 Pages: 431-435