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MECHANISM OF LIQUEFACTION IN REPEATED EARTHQUAKE VIBRATION

机译:重复地震振动中的液化机理

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摘要

During Great East Japan Earthquake happened in March 11 2011,reclaimed ground in Urayasu city,Chiba prefecture,Japan,experienced severn liquefaction not only in the main shock but also in an aftershock with a maximum acceleration of 25gal.In some areas,liquefaction happened in the aftershock is even morn serious than that happened in the major shock.Based on the observed data,a series of dynamic-static analyses,not only considering the earthquake loading but also static loading during the consolidation after the earthquake shock,are conducted in sequential way just the same as the scenario happened in the earthquake.The calculation is conducted with soil-water coupling finite elementfinite difference (FE-FD)analyses based on Cyclic Mobility Model.From the analysis,it is known that some small sequential earthquakes,which cannot cause liquefaction of a ground in an independent earthquake vibration,cannot be neglected when the ground has already experienced liquefaction after a major vibration.It is also known from the analyses that the influence of the aftershock to the long-term settlement of clayed ground is not negligible.
机译:在2011年3月11日发生的东日本大地震期间,日本千叶县浦安市的填海场不仅在主震中经历了液化,而且在最大加速度为25加仑的余震中也经历了严重的液化。在某些地区,液化发生在根据观测数据,依次进行一系列动静分析,不仅考虑地震荷载,还考虑地震震后固结过程中的静荷载,进行了一系列动静分析。这种计算方法与地震中发生的情况相同。基于循环运动模型,通过水-水耦合有限元有限差分(FE-FD)分析进行了计算。在独立的地震振动中不会引起地面的液化,在大振动后地面已经经历液化的情况下不能忽略从分析中还可以知道,余震对黏土长期沉降的影响是不可忽略的。

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