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1.
赵宇蒙  温鸿杰  任冰  王超 《海洋工程》2021,39(4):134-143
基于光滑粒子流体动力学(SPH)方法,开发了能够准确描述水流作用下圆柱强迫振动特性的数学模型。通过引入适合于无网格粒子法的开边界算法,来模拟出入流边界条件,建立了具有造流功能的SPH数值水槽。圆柱及计算域的上下边界均采用修正的动力边界条件进行模拟。借助于粒子位移矫正和压力修正算法,避免了圆柱周围流体粒子压力大幅震荡以及结构下游区域出现空腔等非物理性现象。使用典型的圆柱绕流数据,验证了所建SPH模型的计算性能,研究了固定圆柱在低雷诺数情况下的尾涡脱落模式和升阻力变化规律。明确了低雷诺数下强迫振动圆柱在频率锁定以及非锁定区间内的升力变化规律,量化了升力与外界激励频率之间的关系。  相似文献   

2.
应用经CSPM法和黎曼解修正后的光滑粒子流体动力学(SPH)方法,建立了主动吸收无反射数值波浪水槽,研究波浪作用下多孔介质结构的水动力特性。流体运动控制方程采用N-S方程,多孔渗水结构内流体的运动控制方程考虑渗流力的影响。数值计算结果给出了水槽内不同位置测点的波面历时曲线和越浪量随时间变化曲线,并同试验结果和Philip Liu的数值计算结果进行了比较。并对一个波浪周期内斜坡堤多孔介质结构内外的速度场和压力分布进行了讨论分析。计算分析表明,数值计算波面较Philip Liu的计算结果与试验结果吻合更好。说明应用SPH方法建立的二维数学模型能够较好地模拟破碎波在多孔渗水斜坡上的爬坡和越浪。  相似文献   

3.
不规则波浪数值水槽的造波和阻尼消波   总被引:12,自引:1,他引:12  
高学平  曾广冬  张亚 《海洋学报》2002,24(2):127-132
利用MAC(marker and cell)法直接数值求解连续方程和N-S方程.为模拟不规则波长时段连续造波及消除波浪遇结构物后形成的二次反射,采用了源造波法.对开敞边界,采用了海绵阻尼消波和Sommerfeld条件相结合的处理方式.  相似文献   

4.
以Navier-Stokes方程为控制方程,使用VOF方法追踪自由液面,由连续性方程和动量方程推导出源函数。基于非线性波浪理论和UDF对FLUENT进行二次开发,在数值水槽的各个功能区将不同的源项添加到动量方程中,实现动量源造波和消波的功能。此法可以有效地消除波浪在水槽出流边界的反射及波浪遇到结构物后在入射边界形成的二次反射,从而得到稳定的波动场。本文将这种方法应用于直墙防波堤上波浪压力的数值模拟,分析了造波和消波的有效性,对直立式防波堤波浪力进行了数值研究。为了得到更精确的结果,采用结构化网格和非结构化网格相结合,在直墙防波堤附近使用三角形网格,在其他区域使用四边形结构化网格,为了较好地捕捉自由液面,在液面上下一个波高的范围内对网格进行加密。将计算结果与二阶stokes波理论解进行对比,该方法计算结果与理论解一致,表明该方法能够产生历时较长的稳定的非线性规则波浪,能够很好地吸收波浪遇到建筑物产生的反射波,可以有效消除建筑物反射波的影响,为实际工程方案的设计提供参考,有较高的实用价值。通过计算得到极端高水位,设计高水位,设计低水位时候的各个测点的最大正向波压力和最大负向波压力,并将计算结果与物理模型试验数据和经验公式结果进行对比,结果吻合较好。并且由于该数值方法可以考虑防波堤迎浪面不同倾角的工况,其适应范围比经验公式范围更广,因此可以为海岸结构设计提供依据。  相似文献   

5.
在RNGk-ε湍流模型下,基于Fluent平台中的DEFINE-SOURCE宏,结合KdV与eKdV理论编写相应程序,从粘性不可压缩流体的N-S方程出发,进行了基于质量源造波法的内孤立波数值模拟,并将所得模拟结果与物理实验结果、理论值及速度入口法与平板拍击法数值模拟结果进行了对比和分析。结果表明:质量源造波法所得波形与物理实验结果、理论值及速度入口法与平板拍击法数值模拟结果吻合较好,验证了本文所述质量源造波方法的可行性和有效性,且该方法对振幅水深比小于0.1和大于0.1的内孤立波均具有较好的适用性。此外,质量源造波法避免了动网格的使用、可用于研究速度边界未知的情况、耗时短、效率高、适应性强等优点为进一步研究内孤立波与海洋结构物的相互作用问题提供了一种新的实现方案。  相似文献   

6.
波浪爬高是海岸工程中重要的水动力学问题之一,其数值模拟方法通常是通过离散Navier-Stokes方程或Boussinesq方程实现的,其中基于光滑粒子流体动力学方法是近年发展起来的。本文应用该方法模拟相同水深下,不同波高的孤立波在45(°)陡坡上的爬高,模拟结果与理论计算结果及已有物理模型试验结果进行了对比,并模拟出孤立波激散破碎过程及粒子分布和速度场的变化过程。结果表明,对密度近似方程进行重新初始化保持了流场内的质量守恒,同时整个计算域内的压力分布更加规则,说明光滑粒子流体动力学法在波浪爬高计算中的有效性。  相似文献   

7.
为研究以流体粒子描述波浪运动,以固体单元描述砾石运动的两相介质大变形运动,在港口、海岸工程科学研究中具有重要意义。本文提出砾石单元法(GEM),介绍了光滑粒子动力学方法(SPH)和GEM的基本原理,阐述了GEM与离散单元法(DEM)的异同之处,说明了采用SPH方法与GEM构建波浪砾石耦合运动数学模型的方法和过程。应用SPH方法建立数值波浪水槽,用GEM模拟波浪作用下堆积砾石的滚落、坍塌变形,构建了SPH方法与GEM耦合数学模型。模拟了水槽造波和波浪生成过程和波浪作用下砾石的滚落、坍塌变形,并与物理模型试验成果进行了比较,结果基本吻合。本文提出的GEM法具有模拟单相堆积砾石运动和堆积砾石与流体粒子耦合多相介质运动的功能,是对DEM法的补充和改善。本文提出的堆积力学球概念和拟序排列求解方法是砾石单元法的重要组成部分。  相似文献   

8.
基于FLUENT的海洋内孤立波数值水槽模拟   总被引:3,自引:0,他引:3  
基于FLUENT商业软件及其二次开发功能,在标准κ-ε湍流模型下,采用VOF方法追踪两层流体内界面,通过给定入口速度和水位的设置造波边界法,建立了可有效模拟弱非线性内孤立渡的分层流数值水槽,并与仿物理的双板造波方法进行了比较.采用设置边界法所造的波形与理论值符合较好,这为数值分析内孤立渡与海洋结构物相互作用问题提供了一条更加有效的途径.  相似文献   

9.
基于光滑粒子流体动力学-任意拉格朗日欧拉(SPH-ALE)方法建立二维数值波浪水槽,在控制方程中引入近似黎曼解替代人工黏性,采用排斥力边界条件防止流体粒子穿透固边界,采用指数型衰减函数设置海绵层以消除水槽末端的波浪反射。应用所建立的数值模型对规则波传播及其与浮力摆摆板的相互作用进行了水动力数值模拟,结果表明:文中SPH-ALE模型能够较精确地模拟波浪传播,合理地复现波浪与浮力摆摆板相互作用的物理过程。  相似文献   

10.
为评估不同内孤立波数值造波方法,本文基于Kd V、m Kd V和e Kd V三种理论模型,分别采用双推板、平板拍击和速度入射边界三种数值造波方法,对内孤立波进行了模拟,并将数值模拟结果与理论及实验结果进行对比和分析。结果表明:三种数值造波方法均能实现对内孤立波的模拟,但在造波效果及效率方面存在差异。速度入射边界法在造波效果及效率方面都比较好;平板拍击法的造波效果较好,效率略差;双推板法在造波效果及效率方面均略劣于以上两种方法。  相似文献   

11.
由于在前壁上设置了尺寸较小的孔,开孔沉箱受流体黏性力作用显著,依照弗劳德数相似准则设计模型存在比尺效应。为揭示比尺效应,建立了模拟波浪与开孔沉箱相互作用的光滑粒子流体动力学(SPH)模型。其中流体运动由连续性方程和Navier-Stokes方程控制,固壁边界由改进的动力边界粒子施加。模型收敛性通过分析不同粒子分辨率下的波浪反射系数得到,模型精度通过比较计算与理论波浪反射系数证明。使用经过验证的SPH模型,计算并比较了不同几何比尺和开孔率下开孔沉箱附近的涡量场、箱体外侧的波面时程曲线和波浪反射系数。结果表明,随着模型几何比尺的减小,开孔沉箱受到偏大的流体黏性力,致使更多波能在湍流运动中耗散,进而减小了波浪反射系数并降低了箱体外侧的波面高度。  相似文献   

12.
《Coastal Engineering》2006,53(9):723-735
The paper presents an incompressible Smoothed Particle Hydrodynamics (SPH) model to investigate the wave overtopping of coastal structures. The SPH method is a grid-less Lagrangian approach which is capable of tracking the large deformations of the free surface with good accuracy. The incompressible algorithm of the model is implemented by enforcing the constant particle density in the pressure projection. The SPH model is employed to reproduce a transient wave overtopping over a fixed horizontal deck and the regular/irregular waves overtopping of a sloping seawall. The computations are validated against the experimental and numerical data and a good agreement is observed. The SPH modelling is shown to provide a promising tool to predict the overtopping characteristics of different waves. The present model is expected to be of practical purpose if further improvement in the spatial resolution and CPU time can be adequately made.  相似文献   

13.
A numerical investigation of the bottom pressure and wave elevation generated by a planing hull in finite-depth water is presented. While the existing literature addresses the free-surface deformation and pressure field at the seafloor independently, this work proposes a direct comparison between the two hydrodynamic quantities. The dependence of the pressure disturbances at the ocean floor from the waves generated at the free-surface by a planing hull is studied for several values of both the depth and hull Froude numbers. The methodology employed is Smoothed Particle Hydrodynamics (SPH), a numerical technique based on the discretization of the continuum fields of hydrodynamics through mesh-less particles. The SPH code herein chosen is initially validated against experimental data for transom-stern flow. Subsequently, numerical simulations are presented for a planing hull in high-speed regimes. The results show a direct correlation between surface wave dynamics and hydrodynamic pressure disturbances at the seafloor as the value of the Froude number is varied. This is assessed by studying the inverse dependence of the low-pressure wake angle with the Froude number and by comparison of SPH results with similar works in the cited literature.  相似文献   

14.
A smoothed particle hydrodynamic (SPH) model is developed to simulate wave interaction with porous structures. The mean flow outside the porous structures is obtained by solving Reynolds Averaged Navier–Stokes (RANS) equations and the turbulence field is calculated by a large eddy simulation (LES) model. The porous flow is described by the spatially averaged Navier–Stokes type equations with the resistance effect of the porous media being represented by an empirical frictional source term. The interface boundaries between the porous flow and the outside flow are modeled by means of specifying a transition zone along the interface. The model is validated against other available numerical results and experimental data for wave damping over porous seabed with different levels of permeability. The validated model is then employed to investigate wave breaking over a submerged porous breakwater and good agreements between the SPH model results and the experimental data are obtained in terms of free surface displacement. In addition the predicted velocity, vorticity and pressure fields near the porous breakwater and in the breaking wave zone are also analyzed.  相似文献   

15.
The wave runup caused by a vertical cylinder surging in regular waves is studied both experimentally and numerically. The so-called DualSPHysics Smoothed Particle Hydrodynamics (SPH) code is used for the 3-D numerical modelling. A wide range of cylinder sizes and wave conditions is investigated with results comparing favourably between the experimental and SPH model under both fixed and forced-surge conditions. The experimental and SPH results are further used to predict the maximum runup amplification, in particular the ratio of the runup caused by the surging cylinder to that of the fixed, over the phase difference between the incident wave and surge motion. This maximum runup ratio has been analysed for its dependence on factors such as wave steepness, wave scattering and surge amplitude. An empirical equation is proposed for predicting the maximum runup ratio from known incident wave and surge conditions. Comparison with results from linear solvers suggests that the linear solvers under-predict the full nonlinear runup by a factor of 1.3–1.5.  相似文献   

16.
When the shock wave of underwater explosion propagates to the surfaces of different boundaries, it gets reflected. Then, a negative pressure area is formed by the superposition of the incident wave and reflected wave. Cavitation occurs when the value of the negative pressure falls below the vapor pressure of water. An improved numerical model based on the spectral element method is applied to investigate the cavitation effect of underwater shock near different boundaries, mainly including the feature of cavitation effect near different boundaries and the influence of different parameters on cavitation effect. In the implementation of the improved numerical model, the bilinear equation of state is used to deal with the fluid field subjected to cavitation, and the field separation technique is employed to avoid the distortion of incident wave propagating through the mesh and the second-order doubly asymptotic approximation is applied to simulate the non-reflecting boundary. The main results are as follows. As the peak pressure and decay constant of shock wave increases, the range of cavitation domain increases, and the duration of cavitation increases. As the depth of water increases, the influence of cavitation on the dynamic response of spherical shell decreases.  相似文献   

17.
《Coastal Engineering》2006,53(2-3):141-147
Smoothed Particle Hydrodynamics (SPH) is a relatively new method for examining the propagation of highly nonlinear and breaking waves. At Johns Hopkins University, we have been working since 2000 to develop an engineering tool using this technique. However, there have been some difficulties in taking the model from examples using a small number of particles to more elaborate and better resolved cases.Several improvements that we have implemented are presented here to handle turbulence, the fluid viscosity and density, and a different time-stepping algorithm is used. The final model is shown to be able to model breaking waves on beaches in two and three dimensions, green water overtopping of decks, and wave–structure interaction.  相似文献   

18.
A method of incorporating pressure forcing into a nonlinear potential flow wave model is presented. A semi-analytical pseudo-spectral method is used to calculate dynamic response of a water body exposed to evolving local pressure distribution. Surface slope coherent and slope proportional pressure functions are directly applied through a pressure term appearing in the dynamic free-surface boundary condition of a formulated initial boundary-value problem. First, a monochromatic pressure distribution is used to generate steady regular waves of permanent form. The pressure-induced wave motion exhibits stable harmonic structure for deepwater, transitional water and shallow water waves. In the next step, a more complex pressure system is used to initiate multi-component wave propagation. It is demonstrated that the proposed method provides well-posed initial conditions for studying various water wave scenarios within a framework of nonlinear potential flow solutions.  相似文献   

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