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波浪与大孔隙多孔介质相互作用的耦合数学模型
引用本文:程永舟,王永学,陈智杰,蒋昌波.波浪与大孔隙多孔介质相互作用的耦合数学模型[J].海洋学报,2008,30(5):143-150.
作者姓名:程永舟  王永学  陈智杰  蒋昌波
作者单位:1.长沙理工大学水利学院, 湖南, 长沙, 410076;长沙理工大学水沙科学与水灾害防治湖南省重点实验室, 湖南, 长沙, 410076
基金项目:国家自然科学基金,教育部跨世纪优秀人才培养计划,长沙理工大学创新团队建设计划,湖南省重点学科建设项目 
摘    要:建立了波浪与大孔隙多孔介质相互作用的耦合数学模型,波浪域的控制方程为雷诺时均方程和k-ε紊流模型。对于计算域的入射波采用推板式造波,它可以是线性波、椭圆余弦波和孤立波。采用PLIC-VOF法追踪波浪自由表面。对于多孔介质内的孔隙流场采用非线性Forchheimer方程,两区域共享连续方程,最后导出的波浪域与孔隙流域的压力修正方程具有完全相同的形式,利用这个方程能够同时而不是分别求解波浪场和孔隙流场,避免了在内部边界上给定匹配条件,实现了波浪场与孔隙流场的同步耦合。波浪与粗颗粒海床、平底床面上抛石潜堤及斜坡上抛石潜堤相互作用的验证计算结果表明该模型可用于研究波浪与大孔隙多孔介质相互作用的问题。

关 键 词:波浪    大孔隙多孔介质    耦合模型    孔隙流
收稿时间:2008/4/10 0:00:00
修稿时间:2008/6/16 0:00:00

Coupling numerical model of interaction between wave and porous medium with large porosity
CHENG Yong-zhou,WANG Yong-xue,CHEN Zhi-jie and JIANG Chang-bo.Coupling numerical model of interaction between wave and porous medium with large porosity[J].Acta Oceanologica Sinica (in Chinese),2008,30(5):143-150.
Authors:CHENG Yong-zhou  WANG Yong-xue  CHEN Zhi-jie and JIANG Chang-bo
Institution:1.School of Hydraulic Engineering, Changsha University of Science & Technology, Changsha 410076, China;Key Laboratory of Hunan Province for Water & Sediment Science and Water Hazard Prevention, Changsha University of Science & Technology, Changsha 410076, China2.State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China
Abstract:A coupling model ofinteraction of wave with porous medium with large porosity is established. The wave field solveris based on the two-dimensional Reynolds averaged Navier-Stokes(RANS)equations with a k-ε closure.A piston-type wave makeris setup in the computational domain to produce incident waves and the free surface is traced through the piecewise linear interface construction-volume off luid.The incident waves can be the linear wave,the cnoidal waves and the solitary waves.For chheimer equations are adopted in porous flow within the porous media.By introducinga velocity-pressure correction equation for the waves and the porous flow,highly efficient coupling between the two flows is realized.The two flows can be solved simultaneously and no boundary condition is needed on the interface between them.It was found that the proposed model is effective for studying interaction of wave with scree seabed and is able to handle the water waves and the submerged porous breakwateron flat and slope beds.The verified numerical model can be used to study the interaction between waves and porous medium with large porosity.
Keywords:wave  porous medium with large porosity  coupling model  porous flow
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