Rapid and long runout landslides triggered by earthquake: motion mechanism and countermeasure

Abstract: In 2018, because of earthquakes, lot of landslides occurred in Japan. Most of them moved in high speed and for long runout distance. It is very important and urgent to study the seismic performance of the natural slope, and consider the reasonable countermeasures.
In this presentation, we will take some landslides triggered by earthquake in Japan, to examine the motion mechanism and consider the countermeasures.
The 2018 Hokkaido Eastern Iburi Earthquake triggered massive landslides in pyroclastic fall deposits. Fig. 1 shows one example occurred in Atsuma-cho. Most of the landslides are shallow debris slides. Based on the field reconnaissance and long term monitoring, the shallow landslides were investigated in depth through longitudinal sections, vertical stratigraphic sections, in-situ hardness tests, and long term moisture monitoring in trench. All of the shallow landslides were found to initiate from the liquefied failure of the weak Ta-d pumice layer and further evolve to the overall mobilization of the superimposed pyroclastic fall deposits along the liquefied sliding zone. To testify the controlling role and to study the shear behavior as well as the anti-liquefaction strength of the weak Ta-d pumice layer, a series of laboratory tests were conducted on the soils around the sliding zone. The test results indicate that the medium sandy Ta-d pumice MS can be easily liquefied under intense ground motion. After the slope failure and during the landslide motion, the weathered pumice showed high susceptibility for grain crushing, which resulted in high pore-water pressure generation during the motion. The liquefied sliding zone soil was left behind the sliding mass, because of the viscosity and low shear resistance. Fig. 2 shows a concept model of the motion mechanism for rapid and long runout landslide.
Another landslide triggered by 2018.4 earthquake in Shimane will also be presented for comparison. Moreover, for landslide motion prediction, a software was developed, and it can be used as a soft countermeasure to reduce the landslide disasters.

Biography

Prof Fawu Wang is full professor at the Department of Geoscience, Shimane University, Japan. He is also the director of Research Center on Geo-disaster Reduction in the university.

He obtained a doctorate degree in science on landslide from Kyoto University in 1999.

Prior to joining Shimane University in 2010, he worked at the Disaster Prevention Research Institute of Kyoto University in Japan for 6 years, in Department of Civil Engineering, Kanazawa University in Japan for 4 years, and Changchun College of Geology in China for 5 years.

He has been working on challenging problems in landslides, such as the mechanism of rapid and long runout landslides, the transformation mechanism from landsliding to flow-sliding, motion prediction of landslides, motion behavior of submarine landslides, and landslides triggered by earthquakes, heavy rainfall, and water impoundment.

His primary research interests are to clarify the common mechanisms of landslides initiated by different triggers, and to find a way to predict the occurrence and motion of landslides, for the purpose of landslide disaster mitigation.

In his career on landslide study for more than 30 years, he co-authored 2 books, co-edited 7 books, and published more than 70 peer-reviewed scientific papers related to landslides. He also attended lots of international conference, and made more than 30 oral presentations.

From 2001, he obtained more than 15 competitive research funds, including Fundamental research grant (Kiban Kenkyu A) from Japan Society for Promotion of Science (JSPS). With those funds, he build his own laboratory on landslide study in Shimane University.

Currently, the on-going projects in his laboratory include:

  1. Time prediction of shallow landslides triggered by heavy rainfall
  2. The impact force evaluation of submarine landslides on pipelines
  3. Influence of water level variation on reactivated landslide in water reservoir

Besides the teaching and research activities, he is also working as the Director-General of the International Consortium on Geo-disaster Reduction, the chair holder of UNESCO Chair on Geoenvironmental Disaster Reduction, the Editor-in-Chief of a Springer open access journal: Geoenvironmental Disasters, the deputy-director of Department of International Affairs of Japan Landslide Society.

Further Information

Prof. Fawu Wang

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