首页> 外文会议>ASME International Conference on Ocean, Offshore and Arctic Engineering >MODELLING TURBULENT FLOW IN DEFORMABLE HIGHLY POROUS SEABED AND STRUCTURES
【24h】

MODELLING TURBULENT FLOW IN DEFORMABLE HIGHLY POROUS SEABED AND STRUCTURES

机译:可变形高度多孔海底和结构的涡轮涡流

获取原文

摘要

In this study, the fully-coupled and fully-dynamic Biot governing equations in the open-source geo tech Foam 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:在该研究中,开源地质技术泡沫求解器中的完全耦合和完全动态的BIOS控制方程被扩展到孔隙流体粘性应力。另外,通过传统的涡流粘度概念建模可变形多孔介质中的湍流孔隙流体流动,而无需解决所有湍流尺度。提出了一种新方法,以通过有效粘度来考虑多孔介质电阻(固体流体耦合),这涉及通过多孔介质流动引起的曲折性,晶粒形状和局部湍流。将新模型与Navier-Stokes方程中的实施扩展的达西前摩西师模型进行了比较,该模型考虑了层流,过渡,湍流和瞬态流动制度。此外,为了考虑骨架变形,关于地质材料的应变,更新孔隙率和其他模型参数。通过可用的单向和振荡流动的物理实验的可用结果校准所呈现的模型。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号