Mechanism of Earthquake-induced Landslides on almost Flat Slopes Studied with a Ring Shear Apparatus
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概要
- 論文の詳細を見る
A series of undrained ring shear tests were made on coarse grain sandy soil to simulate stress conditions in a landslide on an almost flat slope during an earthquake. Test results indicated that pore pressure was generated in the shear zone and that the soil was likely to liquefy. The mechanism in this process, however, is speculated to differ from that of conventional liquefaction, because liquefaction phenomena still was present in the dense state. In addition, frequency of loading influenced the total dissipated energy required for liquefaction. The possible mechanism for a landslide on a flat slope is proposed. The reliability and suitability of the ring shear apparatus for reproducing stress conditions on a potential sliding surface was proved.
- 日本自然災害学会の論文
著者
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Sassa Kyoji
Professor Landslide Section Dpri Kyoto University
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Sassa Kyoji
Professor Disaster Prevention Research Institute Kyoto University
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Vankov Dmitri
Graduate student, Landslide section, DPRI, Kyoto University
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Vankov Dmitri
Graduate Student Landslide Section Dpri Kyoto University
関連論文
- SHEAR DISPLACEMENT BEHAVIOR OF SANDY SOILS IN DIFFERENT STATES OF SATURATION AND THE SEISMIC COEFFICIENT IN CYCLIC-LOADING RING-SHEAR TESTS
- Mechanism of Earthquake-induced Landslides on almost Flat Slopes Studied with a Ring Shear Apparatus