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The measurement of liquefaction phenomena by resistivity and its evaluation

机译:电阻率法测量液化现象及其评价

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It is considering that the liquefaction occurs whenthe frame structure of particle in the loose sand layer is collapsedby over pore water pressure due to the earthquake motion. In otherwords, the shear resistance penetration test or the monitoring ofpore water pressure and becomes zero. The N value by the standardpenetration test or the monitoring of pore water pressure is usedfor understanding and evaluation of liquefaction so far. Thesetechniques, however, cannot directly observe the porosity of sandthat corresponds to the change of particle structure in the sandlayer. In this paper, the results of the resistivity monitoring forliquefaction was reported and the process of liquefaction fromthose results was considered by using Archie's law.As the result, it became clear that the liquefaction processconsidered from those results did not contradict the ordinarymodel, namely, the floating and sedimentation model of the sandparticles. Moreover, we referred to the possibility of the floatingof particle near the sand layer surface in the progress of liquefaction.Finally, we proposed the new evaluation method of theliquefaction layer which combine the resistivity of collected sandin a laboratory test with the resistivity obtained by resistivity logging.
机译:可以认为,由于地震运动引起的孔隙水压力使疏松砂层中的颗粒的框架结构塌陷时,就会发生液化。换句话说,抗剪切力渗透试验或孔隙水压力的监测为零。迄今为止,通过标准渗透试验或孔隙水压力监测得到的N值用于了解和评估液化。但是,这些技术不能直接观察与砂层中颗粒结构变化相对应的砂子孔隙率。本文报道了电阻率监测液化的结果,并使用阿奇定律考虑了液化的过程,结果清楚地表明从这些结果考虑的液化过程与普通模型不矛盾。沙粒的浮沉模型。此外,我们还提到了液化过程中颗粒可能在砂层表面附近漂浮的可能性。最后,提出了一种新的液化层评估方法,该方法结合了实验室测试中收集的砂岩的电阻率与通过电阻率测井获得的电阻率。

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