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Investigation on the dynamic liquefaction responses of saturated granular soils due to dynamic compaction in coastal area

机译:沿海地区动力压实因饱和颗粒土的动态液化反应研究

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Dynamic compaction (DC) has been widely used for a variety of soil types and conditions in coastal area. However, as the ground water table is near the ground surface, a significant increase of pore water pressure is noticed after each impact, which results in local liquefaction and limits further drop effect. Consequently, to obtain effective compaction effects on saturated soils, it is essential for the evaluation of the liquefaction responses of soil medium caused by DC to determine the time delay between the drops and prevent 'rubbery soil'. In this study, a numerical investigation on the liquefaction responses of saturated granular soils during DC is carried out using a coupled hydro-mechanical model. The developed model considers all the stages of DC involved in impact stage and consolidation stage. A new cap model for simulations of high strain rate behaviors of soils under DC is incorporated in the coupled hydro-mechanical model. Verification of the proposed model is performed against the previous test data and analytical result. Then, a series of parametric studies have been performed to examine the effects of the tamping energy level, hammer radius and permeability on liquefaction responses of saturated granular soils at several stages of DC. The numerical results demonstrate that the dimension of liquefaction zone is driven by the tamping energy level rather than the permeability, and strain rate has a significant effect on soil responses in DC.
机译:动态压实(DC)已广泛用于沿海地区的各种土壤类型和条件。然而,当接地水位靠近地面时,每次冲击后都会注意到孔隙水压力的显着增加,这导致局部液化并限制进一步下降效果。因此,为了获得对饱和土壤的有效压实作用,对于DC引起的土壤培养基的液化反应至关重要,以确定下降和防止“橡胶状土”之间的时间延迟。在该研究中,使用耦合的水力机械模型进行DC期间饱和粒状土壤液化响应的数值研究。开发的模型考虑了涉及影响阶段和整合阶段的所有DC的阶段。 DC下土壤高应变率行为模拟的新帽模型掺入了耦合的水力机械模型中。针对先前的测试数据和分析结果进行提出的模型的验证。然后,已经进行了一系列的参数研究以检查夯实能级,锤子半径和渗透性在DC的几个阶段的饱和颗粒土壤的液化反应上的效应。数值结果表明,液化区的尺寸由夯实能级而不是渗透性驱动,并且应变速率对DC的土壤反应具有显着影响。

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