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Effect of vertical seismic motion on the dynamic response and instantaneous liquefaction in a two-layer porous seabed

机译:垂直地震运动对两层多孔海床动力响应和瞬时液化的影响

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The evaluation of seismic-induced responses in a porous seabed is a fundamental problem in geotechnical and coastal engineering. Although ground motions generally include both horizontal and vertical components, a majority of previous theoretical investigations assumed vertically propagating shear waves in a horizontally layered soil-rock system and simply ignored the effect of site response to vertical earthquake motion. In this paper, the dynamic response and instantaneous liquefaction of a porous seabed that is induced by vertical earthquake loading is studied using an analytical method. The seabed is treated as a two-layer poroelastic medium and characterized by the dynamic formulation of Biot theory. The analytical solutions for the response variables, such as induced displacement, pore pressure and vertical effective stress, are derived individually, and the mechanism of instantaneous liquefaction in liquefiable sediment is investigated based on the excess pore pressure criterion. A set of parametric analysis is performed to discuss the effects of seawater, the seabed and earthquake parameters on the seismic response and maximum liquefaction depth. It is worth noting that the properties of the surface seabed layer have a significant influence on the seismic response and, consequently, the potential stability of the seabed, which is important in the analysis of offshore structure foundations.
机译:评估多孔海底地震引起的响应是岩土和海岸工程中的一个基本问题。尽管地面运动通常包括水平分量和垂直分量,但大多数先前的理论研究都假设在水平分层的土石系统中垂直传播剪切波,而忽略了场地对垂直地震运动的影响。本文采用解析方法研究了垂直地震荷载作用引起的多孔海床的动力响应和瞬时液化。该海床被视为两层多孔弹性介质,其特征在于动态描述了毕奥特理论。分别推导了诱发位移,孔隙压力和垂直有效应力等响应变量的解析解,并根据孔隙压力超额准则研究了液化沉积物瞬时液化的机理。进行了一组参数分析,以讨论海水,海床和地震参数对地震响应和最大液化深度的影响。值得注意的是,表层海床的性质对地震反应有很大影响,因此,对海床的潜在稳定性也有重要影响,这在分析海上结构基础中很重要。

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