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A coupled fluid layer-rigid disk-poroelastic half-space vibration problem

机译:耦合流体层-刚性盘-多孔弹性半空间振动问题

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This paper proposes a coupled fluid layer-foundation-poroelastic half-space vibration model to study how still water affects foundations operating underwater. As an example, we consider the problem of the vertical vibration of a rigid disk on a poroelastic half-space covered by a fluid layer having a finite depth. The solution of the disk vibration problem is obtained using the boundary conditions at the free surface of the fluid layer and the boundary conditions at the fluid layer-poroelastic medium interface. The solution is expressed in terms of dual integral equations that are converted into Fredholm integral equations of the second kind and solved numerically. Selected numerical results for the vertical dynamic impedance coefficient are examined based on different water depths, poroelastic materials, disk permeabilities and frequencies of excitation. Based on the numerical results, it is proposed that the hydrodynamic pressure caused by the foundation vibration is the intrinsic reason that the existence of a fluid layer has such a great effect on the dynamic characteristics of the foundation. In many cases, the hydrodynamic pressure caused by the foundation vibration cannot be ignored when designing dynamic underwater foundations. These results are helpful in understanding the dynamic response of foundations under still water without water waves, such as foundations in pools, lakes and reservoirs.
机译:本文提出了一个耦合的流体层-基础-多孔弹性半空间振动模型,以研究静水如何影响水下作业的地基。例如,我们考虑在具有有限深度的流体层覆盖的多孔弹性半空间上,刚性磁盘的垂直振动问题。使用流体层自由表面的边界条件和流体层-多孔弹性介质界面的边界条件,可以解决磁盘振动问题。该解用对偶积分方程表示,该对偶积分方程被转换为第二种Fredholm积分方程,并用数值方法求解。根据不同的水深,多孔弹性材料,磁盘磁导率和激励频率,检查了垂直动态阻抗系数的选定数值结果。根据数值结果,提出由地基振动引起的水动力压力是流体层的存在对地基动力特性产生如此大影响的内在原因。在许多情况下,设计动态水下基础时,不能忽略由基础振动引起的水动力压力。这些结果有助于理解没有水波的静水下地基的动态响应,例如水池,湖泊和水库中的地基。

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