Soil and rock strength parameters of the Shiraidake Landslide, Japan

Authors

  • Robert Jelinek Laboratory of Forest Conservation, Department of Forest and Forest Products, Faculty of Agriculture, Kyushu University, Higashi-ku, Hakozaki 6-10-1, Fukuoka 812-8581
  • Prem Prasad Paudel Laboratory of Forest Conservation, Department of Forest and Forest Products, Faculty of Agriculture, Kyushu University, Higashi-ku, Hakozaki 6-10-1, Fukuoka 812-8581
  • Hiroshi Omura Laboratory of Forest Conservation, Department of Forest and Forest Products, Faculty of Agriculture, Kyushu University, Higashi-ku, Hakozaki 6-10-1, Fukuoka 812-8581

DOI:

https://doi.org/10.3126/jngs.v23i0.32030

Keywords:

Shiriadake landslide, , Rock and soil strength, Japan

Abstract

The Shiraidake area of northwest Kyushu has an extensive distribution of landslides. A series of undrained triaxial tests and unconfined compression tests were carried out to investigate the variation of strength properties in a selected borehole from the Shiraidake Landslide. It is a translational landslide (called the Hokusho-type in Japan) and is composed of the Early Tertiary and Quaternary sedimentary rocks that are prone to rapid weathering. Core rock samples and recompacted soil samples were used for the study. The results provided the fundamental characteristics of soil and rock under the triaxial and uniaxial tests, and indicated that the undrained behaviour of tested soils generally depends on the pre-shear consolidation pressure and dry density. In addition, the type of material used and the tests performed are important factors that influence the soil and rock strength.

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Published

2001-12-01

How to Cite

Jelinek, R., Paudel, P. P., & Omura, H. (2001). Soil and rock strength parameters of the Shiraidake Landslide, Japan. Journal of Nepal Geological Society, 23, 91–98. https://doi.org/10.3126/jngs.v23i0.32030

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