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MODELLING TURBULENT FLOW IN DEFORMABLE HIGHLY POROUS SEABED AND STRUCTURES

机译:在可变形的高孔隙海和结构中模拟湍流

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In this study, the fully-coupled and fully-dynamic Biot governing equations in the open-source geotechFoam solver are extended to account for pore fluid viscous stresses. Additionally, turbulent pore fluid flow in deformable porous media is modeled by means of the conventional eddy viscosity concept without the need to resolve all turbulence scales. A new approach is presented to account for porous media resistance to flow (solid-to-fluid coupling) by means of an effective viscosity, which accounts for tortuosity, grain shape and local turbulences induced by flow through porous media. The new model is compared to an implemented extended Darcy-Forchheimer model in the Navier-Stokes equations, which accounts for laminar, transitional, turbulent and transient flow regimes. Further, to account for skeleton deformation, the porosity and other model parameters are updated with regard to strain of geomaterials. The presented model is calibrated by means of available results of physical experiments of unidirectional and oscillatory flows.
机译:在这项研究中,开源的geotechFoam解算器中的完全耦合和完全动态的Biot控制方程得以扩展,以解决孔隙流体的粘性应力问题。另外,可变形多孔介质中的湍流流体流动是通过常规涡流粘度概念建模的,无需解决所有湍流尺度。提出了一种新方法来通过有效粘度解决多孔介质的流动阻力(固-液耦合),这解决了通过多孔介质流动引起的曲折度,晶粒形状和局部湍流。将该新模型与Navier-Stokes方程中已实现的扩展Darcy-Forchheimer模型进行了比较,该模型考虑了层流,过渡,湍流和瞬态流动状态。此外,考虑到骨架变形,关于土工材料的应变,更新了孔隙率和其他模型参数。通过单向流动和振荡流动的物理实验的可用结果,对提出的模型进行了校准。

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