4.7 Article

A new high-stress undrained ring-shear apparatus and its application to the 1792 Unzen-Mayuyama megaslide in Japan

期刊

LANDSLIDES
卷 11, 期 5, 页码 827-842

出版社

SPRINGER HEIDELBERG
DOI: 10.1007/s10346-014-0501-1

关键词

Landslide; Undrained ring-shear apparatus; Unzen; Mayuyama

资金

  1. Japan Science and Technology Agency (JST)
  2. Japan International Cooperation Agency (JICA)

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Sassa and others in the Disaster Prevention Research Institute (DPRI), Kyoto University, developed a series of undrained ring-shear apparatus to physically simulate landslide initiation and motion, from DPRI-3 (Sassa 1992) to DPRI-7 (Sassa et al., Landslides 1(1): 7-19, 2004). The maximum undrained capacities in the DPRI series ranged from 300 to 650 kPa. Sassa and others in the International Consortium on Landslides (ICL) have developed a new series of undrained ring-shear apparatus (ICL-1 and ICL-2) for two projects of the International Programme on Landslides (IPL-161 and IPL-175). Both projects are supported by the Science and Technology Research Partnership for Sustainable Development Program (SATREPS) of Japan. ICL-1 was developed to create a compact and transportable apparatus for practical use in Croatia; one set was donated to Croatia in 2012. ICL-2 was developed in 2012-2013 to simulate the initiation and motion of megaslides of more than 100m in thickness. The successful undrained capacity of ICL-2 is 3MPa. This apparatus was applied to simulate possible conditions for the initiation and motion of the 1792 Unzen-Mayuyama megaslide (volume, 3.4x10(8)m(3); maximum depth, 400m) triggered by an earthquake. The megaslide and resulting tsunami killed about 15,000 people. The Unzen Restoration Office of the Ministry of Land, Infrastructure and Transport (MLIT) of Japan systematically collected various papers and reports and published two summary leaflets: one in English in 2002 and an extended version in Japanese in 2003. Samples were taken from the source area (for initiation) and the moving area (for motion). The hazard area was estimated by the integrated landslide simulation model LS-RAPID, using parameters obtained with the ICL-2 undrained ring-shear apparatus. The estimated hazard area agrees reasonably with the landslide moving area reported in the Ministry leaflets.

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