Towards the Numerical Modelling of Residual Seabed Liquefaction Using OpenFOAM

Ranjith khumar Shanmugasundaram, H. Rusche, C. Windt, Özgür Kirca, Mutlu Sumer, N. Goseberg
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引用次数: 2

Abstract

Knowledge of the interaction between free surface waves and the seabed is required for the reliable design of marine structures, preventing severe structural failures. To that end, this paper presents the numerical modelling of wave-induced residual liquefaction of seabed soil. An OpenFOAM® finite volume solver is developed to simulate the behaviour of pore pressure and shear stress in the soil and is validated against analytical reference data. The soil is considered as a poro-elastic solid and an additional equation is solved for the pore pressure buildup. The governing equations are valid only up to the onset of liquefaction. A criterion based on the accumulated pore pressure is applied in order to predict the onset of residual liquefaction. The results show that the pore pressure and shear stresses are in good agreement with the analytical results and the relative errors are less than three percent. Also, the numerical results indicate that the wave induced residual liquefaction originates from the mudline and progresses slowly down the soil which is consistent with the analytical results. The pore pressure buildup for a seabed with stone columns shows that the liquefaction potential is very low near the stone column.
基于OpenFOAM的海底残余液化数值模拟研究
海洋结构的可靠设计需要了解自由表面波与海床之间的相互作用,以防止严重的结构破坏。为此,本文提出了海底土壤波浪残余液化的数值模拟方法。开发了OpenFOAM®有限体积求解器来模拟土壤中的孔隙压力和剪切应力的行为,并根据分析参考数据进行了验证。将土视为多孔弹性固体,并求解了孔隙压力累积的附加方程。控制方程只在液化开始前有效。为了预测残余液化的发生,采用了基于累积孔隙压力的判据。结果表明,孔隙压力和剪应力与分析结果吻合较好,相对误差小于3%。数值计算结果表明,波浪引起的残余液化起源于泥线,并在土壤中缓慢发展,这与分析结果一致。有石柱海床的孔隙压力累积表明,石柱附近的液化潜力很低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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