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Experimental and numerical modeling on the liquefaction potential and ground settlement of silt-interlayered stratified sands

机译:淤泥层间分层砂液化电位和地面沉降的实验和数值模型

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Recent seismic events indicate that the simplified liquefaction-evaluation procedures are incapable of depicting general trends in liquefaction damage for stratified sands interlayered with silts. The conditions and mechanisms affecting the liquefaction potential of stratified sands exist in the field and ground settlement after liquefaction remain poorly understood. This work aims to investigate the seismic response of nonhomogeneous soil deposits by large-scale model tests and numerical simulations using an advanced constitutive model. A comprehensive experimental program was undertaken in which a total of three shake-table tests were performed on uniform sand and two stratified-sand deposits interlayered with different thicknesses of silt to investigate the ground settlement and distribution and dissipation of excess pore pressure during and after shaking. The shake-table test results and the numerical simulations of the silt-interlayered stratified sands, first indicate that the thickness of the silt seam has a significant influence on the liquefaction resistance of stratified-sand deposits beneath the silt layer. The second conclusion of this study reveals that the thickness and coefficient of consolidation of the silt and the liquefied sand below the silt layer significantly alter the degree of dissipation after the shake, and this causes different deformation/settlement at the ground surface. Therefore, there will be probably inaccuracies in applying simplified liquefaction evaluation procedures to the actual soil profile characterized by various patterns of layering in the field.
机译:最近的地震事件表明,简化的液化评估程序无法描绘与淤泥的分层砂的液化损伤的一般趋势。影响分层砂液液化电位的条件和机制存在于液化后的田间和地面沉降中,仍然不知难以理解。这项工作旨在通过使用先进的本构模型来研究大规模模型试验和数值模拟的非均匀土壤沉积的地震反应。进行了一个综合的实验计划,其中在均匀的沙子和两个分层砂沉积上进行了三种摇型表试验,其具有不同厚度的淤泥,以研究摇动期间和后的过度孔隙压力的地面沉降和分布和耗散。摇动表测试结果和淤泥层间分层砂的数值模拟,首先表明淤泥接缝的厚度对淤泥层下面的分层砂沉积物的液化抗性有显着影响。该研究的第二个结论揭示了淤泥层和下方的液化砂的厚度和系数显着改变摇动后的耗散程度,这导致地面的不同变形/沉降。因此,将简化的液化评估程序应用于实际土壤曲线,其特征在于该领域中的各种图案的实际土壤曲线将存在不准确。

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