里耶卡湾三维VOF海岸流模型

L. Kranjčević, L. Grbčić, Matija Mrazović, Siniša Družeta
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引用次数: 0

摘要

对亚得里亚海里耶卡湾地区的三维多相流进行了分析。在海岸底区域的兴趣范围内收集必要的形态学数据,并创建空间表面。研究了三维模型在大范围的真实的海底和海岸随机结构中的功能。给出了模型中气象条件和风影响的概率。得到的结果给出了不同深度水平面上的速度场的详细视图。在开源程序OpenFOAM中采用欧拉方法,采用流体体积法(VOF)进行数值模拟。为了解决这一问题,使用了两种不可压缩、等温、不混相流体的interFOAM求解器。模拟结果显示,主要气流从克尔克岛西海岸流向伊斯特拉半岛东海岸。海水通过Srednja Vrata和Tihi Kanal进入海湾,并通过Vela Vrata离开海湾。该研究表明,利用VOF方法可以成功地描述海湾和海洋等大面积的流体运动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Rijeka Bay 3D VOF Costal Flow Model
3D multiphase flow was analyzed in the area of Rijeka bay in the Adriatic Sea. The necessary morphology data in the range of interest of the coastal bottom area were collected and the spatial surface was created. The functionality of the 3D model was studied in the large area of the realistic stochastic structure of the bottom and the shore. The probability of meteorological conditions and wind impact in the model has been shown. The obtained results give a detailed view of the velocity fields in the horizontal plane of different depths. Numerical simulation was performed in open source program OpenFOAM with Volume of Fluid (VOF) method using the Eulerian approach. For solving this problem interFOAM solver for two incompressible, isothermal, immiscible fluids was used. The resulting simulations showed dominant flow from the western coast of the Krk island to the eastern coast of the Istrian peninsula. Seawater enters the bay through the Srednja Vrata and Tihi Kanal and exits the bay through the Vela Vrata. This research has shown that using a VOF method can be successfully implemented for describing fluid motion in large areas such as bays and oceans.
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