A local scour model for single pile on silty seabed considering soil cohesion (SedCohFOAM): Model and validation

Chenxi Qin, L. Duan, Duoyin Wang, Bingchuang Duan, Wei Liu
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Abstract

In this study, the sediment transport two-phase flow model named SedFOAM is expanded to include soil cohesion, creating a new model named SedCohFOAM within OpenFOAM. The local scouring flume experiment involving a pile on silty seabed and sandy seabed is conducted in a curved flume. Due to the influence of cohesion, the scouring depth at different locations on sandy seabed is 15%–18% greater than that on silty seabed. Observations from this experiment informed the analysis of force balance, wherein the agglomerated silt particles are modeled as large singular entities and the cohesive force is treated as a downward influence that keeps the aggregated particles stationary. Meanwhile, the experimental outcomes are utilized to validate the accuracy of the SedCohFOAM model. The numerical findings demonstrated that SedCohFOAM can simulate the flow field distribution around the pile, variations in seabed shear stress, and alterations in seabed surface morphology. Compared with the SedFOAM model, the SedCohFOAM model has a significantly reduced simulation error in simulating scour on silty seabed. When comparing the cross-sectional profiles of the scour holes derived from the flume experiments with those simulated by SedCohFOAM, it was observed that the ultimate-equilibrium scour depth predicted by the model is consistently lower, but the scour radius in the numerical simulations is larger. The deviation from the experimental results is nearly within 8%, while when the flow velocity is high, the simulation error of the simulated scouring depth behind the pile and the scouring radius in front of pile is amplified.
考虑土壤内聚力的淤泥质海床单桩局部冲刷模型(SedCohFOAM):模型与验证
本研究将名为 SedFOAM 的沉积物输运两相流模型扩展到土壤内聚力,在 OpenFOAM 中创建了名为 SedCohFOAM 的新模型。在弧形水槽中进行了涉及淤泥质海床和砂质海床上桩的局部冲刷水槽实验。由于内聚力的影响,沙质海床不同位置的冲刷深度比淤泥质海床大 15%-18%。该实验的观察结果为力平衡分析提供了依据,其中聚结的淤泥颗粒被模拟为大型奇异实体,而内聚力则被视为使聚结颗粒保持静止的向下影响。同时,利用实验结果验证了 SedCohFOAM 模型的准确性。数值结果表明,SedCohFOAM 可以模拟桩周围的流场分布、海底剪应力的变化以及海底表面形态的改变。与 SedFOAM 模型相比,SedCohFOAM 模型在模拟淤泥质海床冲刷时的模拟误差明显减小。将水槽实验得出的冲刷孔横截面剖面与 SedCohFOAM 模拟的冲刷孔横截面剖面进行比较,发现模型预测的极限平衡冲刷深度一直较低,但数值模拟的冲刷半径较大。与实验结果的偏差几乎在 8%以内,而当流速较高时,桩后冲刷深度和桩前冲刷半径的模拟误差会扩大。
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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