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

水槽 海床 凝聚力(化学) 岩土工程 地质学 淤泥 流量(数学) 泥沙输移 沉积物 机械 地貌学 物理 海洋学 量子力学
作者
Chenxi Qin,Lunliang Duan,Duoyin Wang,Bingchuan Duan,Wei Zheng Liu
出处
期刊:Physics of Fluids [American Institute of Physics]
卷期号:36 (5) 被引量:4
标识
DOI:10.1063/5.0207743
摘要

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.
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