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Effects of dynamic soil permeability on the wave-induced seabed response around a buried pipeline

机译:动态土壤渗透率对地下管线附近波浪诱导的海床响应的影响

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Soil permeability is one of key factors in the prediction of the wave-induced seabed response, which needs to be considered in the design of foundation around marine installations. Most previous studies in the field treated the soil permeability as a constant or varying in spacial domain, although it depends on numerous soil parameters. In this study, the soil permeability is considered as a function of pore-water pressures as reported in the literature. With this new feature, the governing equations will become non-linear differential equations. Numerical examples demonstrate the considerable influence of dynamic soil permeability on the wave-induced pore pressure and effective stresses. it is concluded that the conventional model with constant soil permeability under-estimates the liquefaction potential.
机译:土壤渗透性是预测波浪引起的海床响应的关键因素之一,在海洋设施周围的基础设计中需要考虑这一因素。尽管该领域取决于许多土壤参数,但大多数该领域的先前研究都将土壤渗透率视为恒定或变化的空间域。在这项研究中,土壤渗透率被认为是孔隙水压力的函数,正如文献报道的那样。有了这个新功能,控制方程将变成非线性微分方程。数值算例表明,动态土壤渗透率对波浪引起的孔隙压力和有效应力的影响很大。结论是,具有恒定土壤渗透率的常规模型低估了液化潜力。

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