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Numerical Experiments of Seabed Liquefaction during Ocean Wave Loading

机译:海波加载过程中海底液化的数值实验

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Seabed soil behavior under ocean wave loading is important to understand for the safety of coastal infrastructure, e.g., breakwaters, wind turbines, coastal armoring. A two-dimensional finite element model is generated in OpenSees to simulate nearshore seabed soil reaction to progressive wave loading by coupling pore water pressure and soil particle displacement. Wave loading is applied at the surface of a two-dimensional rectangular seabed domain as vertical pressure as well as pore water pressure. The numerical model is justified by comparing with analytical solution using different material parameters. A parametric study on model boundary effects shows that for the same wavelength wave, effective finite element domain size is not related to the full domain size as long as the lateral domain size is at least one wavelength. Soil liquefaction potential at different locations is studied with changing wave frequencies. A standing wave situation is also examined to simulate an ideally fully reflected wave in front of a coastal structure. The node and anti-node location of the standing wave greatly affect the liquefaction potential prediction. The results show that the wave properties are important for predicting soil liquefaction depth as well as liquefaction initiation time. Soil parameters like hydraulic conductivity and the elasto-plastic material behavior would also have the impact to the liquefaction region size and magnitude. This study provides a reasonable reference for further soil-fluid-structure interaction studies.
机译:海波载荷下的海底土壤行为对于沿海基础设施的安全性非常重要,例如,防波堤,风力涡轮机,沿海装甲。在Opensees中产生二维有限元模型,以通过耦合孔隙水压和土壤颗粒位移来模拟近山地层土壤反应。波浪加载在二维矩形海底域的表面上作为垂直压力以及孔隙水压力。通过使用不同材料参数的分析解决方案比较了数值模型。关于模型边界效果的参数研究表明,对于相同的波长波,有效的有限元域大小与横向域大小为至少一个波长,有效的有限元域尺寸与全域大小无关。利用变化波频率研究了不同地点的土壤液化电位。还检查了站立的波浪情况,以模拟沿海结构前面的理想完全反射波。驻波的节点和反节点位置大大影响液化电位预测。结果表明,波属性对于预测土壤液化深度以及液化启动时间很重要。液压导电性等土壤参数也将对液化区域尺寸和幅度产生影响。本研究为进一步的土壤流体结构相互作用研究提供了合理的参考。

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