Cyclic characterization of wave-induced oscillatory and residual response of liquefiable seabed
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Cyclic characterization of wave-induced oscillatory and residual response of liquefiable seabed

机译:液化海床的波致振荡和残余反应的循环表征

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Abstract The paper presents a robust modeling method for a fully coupled effective stress analysis of the wave-induced liquefaction scenarios, based on the Biot consolidation theory. In this context, emphasis is placed on the implementation of a well-calibrated cyclic soil model and an empirical shear-volume coupling equation, which links the increment of volumetric strain per cycle of wave with the shear strain occurring during that particular cycle. Unlike most of the previous investigations using the amplitude of shear stress over the wave period (or the phase-resolved oscillatory shear stresses) as the source term for calculating the residual pore pressure, in this study, the source term is related to the rate of plastic volumetric deformation and implemented into the Biot consolidation equation to consider both generation and partial dissipation of excess pore pressure during wave propagation. Then, the proposed modeling method is incorporated into a dynamic finite difference analysis procedure. Model calibrations are carried out in terms of individual soil element behavior and seabed response under progressive waves, respectively. Overall good agreement demonstrates the reliability of the modeling method for the prediction of wave-induced seabed response. Finally, the paper highlights the potentials of proposed modeling framework to simulate the basic features of wave-induced seabed response (i.e., the coupling of progressive buildup of pore pressure and cyclic softening of soil skeleton), by means of numerical examples. The obtained results show that the cyclic behavior of liquefiable seabed under wave actions can be well captured by the proposed model. Highlights ? A cyclic characterization method of wave-induced response of liquefiable seabed is presented. ? The source term related to the rate of volumetric compaction is defined within the Biot equation. ? Model calibrations are carried out in terms of single element behavior and seabed response. ? Typical results on the cyclic behavior of liquefiable seabed under wave actions are shown. ]]>
机译:<![cdata [ 抽象 纸张提出了一种鲁棒建模方法,用于基于波诱导的液化方案的全耦合有效应力分析论生物合并理论。在这种情况下,重点放置在校准良好的循环土模型和经验剪切体积耦合方程的实施方面,这与在该特定循环期间发生的剪切应变的剪切应变相连。与使用波浪周期(或相位分辨振荡剪切应力)的剪切应力幅度的大多数研究是不同的,因为用于计算残留孔隙压力的源术语,在本研究中,源期限与速率有关塑料体积变形并实施到Biot Consolidation方程中,以考虑波传播期间过量孔隙压力的一代和部分耗散。然后,将所提出的建模方法结合到动态有限差分分析过程中。在渐进波下的各个土壤元素行为和海底反应方面,分别进行模型校准。整体良好的一致性展示了对波引起的海底反应预测的建模方法的可靠性。最后,通过数值例子,突出了建模框架模拟波引起的海底响应的基本特征的潜力(即,土壤骨架的孔隙压力和循环软化的循环软化的耦合)。所得结果表明,在提出的模型中可以很好地捕获波动下液化海床的循环行为。 亮点 呈现了液化海底的波引起的波引起的循环响应的循环表征方法。 源代码与体积压缩速率相关的有关在Biot方程中定义。 在单个元素行为和海底响应方面进行型号校准。 显示了在波动动作下液化海底循环行为的典型结果。 ]]>

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