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EXPERIMENTAL AND NUMERICAL STUDIES ON THE CHANGE INGROUND STIFFNESS BEFORE AND AFTER LIQUEFACTION

机译:液化前后周围刚度变化的实验和数值研究

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It is possible, at present, to simulate liquefaction of ground due to earthquake with reasonable accuracyusing an effective stress analysis. One of the key issues in liquefaction analyses is how to make a modelthat can take into consideration ground stiffness reduction before liquefaction. Yet, the process of groundstiffness recovery after liquefaction is also important issue. The change of soil stiffness has been studiedwith undrained cyclic triaxial tests or shaking table tests [1]. Based on the experimental results, a numberof well-performed constitutive models have been proposed. Among those constitutive models, someelastoplastic models based on a nonlinear kinematical hardening rule have been well used in liquefactionanalyses, mainly for clean sands. Unfortunately, those models cannot predict the change in groundstiffness well for soils of fine grains and gravels. In this study, in order to clarify the ground stiffnesschange during liquefaction, shaking table tests, undrained cyclic triaxial tests and effective stress analysesare conducted for three kinds of geomaterials. Decomposed granite, clean sand called Kasumigaura-sandand crushed stone called gravel are used in the series of tests and simulations. The experimental resultsare compared with the results of effective stress analyses. It is found that the change in pore waterpressure during liquefaction is well simulated for Kasumigaura-sand and gravel. On the other hand, fordecomposed granite, simulation results of the change in excessive pore water pressure in liquefactionprocess cannot express the experimental results well. It is also found that from laboratory tests, the changein ground stiffness in the process of primary liquefaction is largely affected from the performance of theexcessive pore water pressure.
机译:目前,可以使用有效的应力分析以合理的精度模拟地震引起的地面液化。液化分析的关键问题之一是如何建立一个可以考虑液化前地面刚度降低的模型。然而,液化后地基刚度恢复的过程也是重要的问题。用不排水的循环三轴试验或振动台试验研究了土壤刚度的变化[1]。根据实验结果,提出了许多性能良好的本构模型。在这些本构模型中,基于非线性运动学硬化规则的弹塑性模型已广泛用于液化分析中,主要用于清洁砂土。不幸的是,这些模型无法很好地预测细粒和砾石土壤的地基刚度变化。在这项研究中,为弄清液化过程中的地面刚度变化,对三种土工材料进行了振动台试验,不排水循环三轴试验和有效应力分析。在一系列的测试和模拟中,使用了分解的花岗岩,称为Kasumigaura沙的干净沙子和称为砾石的碎石。将实验结果与有效应力分析的结果进行比较。发现Kasumigaura砂和砾石在液化过程中孔隙水压力的变化得到了很好的模拟。另一方面,对于分解后的花岗岩,液化过程中孔隙水压力过大变化的模拟结果不能很好地表达实验结果。从实验室测试还发现,初级液化过程中地面刚度的变化很大程度上受孔隙水压力过大的影响。

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