In the 2011 off the Pacific coast of Tohoku Earthquake, extensive liquefaction damages were observed over a wide range of reclaimed coastal land. It is reported that, in Chiba prefecture, the big aftershock occurred 29 minutes after the main shock and it caused expanding the liquefaction damage. In this paper, using a soil-water-air coupled finite deformation analysis code incorporating the elasto-plastic constitutive equation “SYS Cam-clay model”, it showed that groundwater level rise due to main shock expands liquefaction damage during aftershock.In the 2011 off the Pacific coast of Tohoku Earthquake, extensive liquefaction damages were observed over a wide range of reclaimed coastal land. It is reported that, in Chiba prefecture, the big aftershock occurred 29 minutes after the main shock and it caused expanding the liquefaction damage. In this paper, using a soil-water-air coupled finite deformation analysis code incorporating the elasto-plastic constitutive equation “SYS Cam-clay model”, it showed that groundwater level rise due to main shock expands liquefaction damage during aftershock.
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