垂直板周围分层流动的可视化:实验室实验和数值模拟

Y. Chashechkin, Ya. V. Zagumennyi
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引用次数: 4

摘要

在包括连续性方程、动量方程和线性化状态方程的物质传递方程的基本系统的基础上,发展了实验和数值研究的方法来可视化在分层介质中垂直板均匀水平运动所产生的流动扰动场。在独特的研究设施“hPC IPMech raS”的“实验室移动槽”展台上,通过高灵敏度和高分辨率的纹影仪lab -458在实验室槽中可视化分层流动,并在开源CfD实用程序OpenfOaM框架内使用集群系统和超级计算机的计算资源进行数值计算。计算结果和实验室可视化数据均表明,垂直板在分层流体中均匀运动产生的流型包含复杂的内波系统,包括上游、附着和短内波系统,以及由于分层和耗散效应的共同影响而形成的薄界面,如韧带。板块运动速度的增加导致经过板块的尾流发生本质上的重构,其中典型的涡旋元素,如涡旋偶极子和“涡旋气泡”,在内波相面发散区形成。所有流的结构成分都在不断演化,并与自由流相互作用。观测结果与计算结果在定性和定量上有很好的一致性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Visualization of stratified flows aro und a vertical plate: laboratory experiment and numerical simulation
On the basis of the fundamental system, which includes equations of continuity, momentum, and substance transfer with a linearized equation of state, methods of experimental and numerical study are developed for visualizing the flow perturbation fields generated by uniform horizontal movement of a vertical plate in a stratified medium. The stratified flows were visualized in the laboratory tank by the high-sensitive and high-resolution Schlieren instrument Iab-458 at the stand ‘laboratory Mobile Tank’ of the unique research facility ‘hPC IPMech raS’ and numerically calculated within the frame of the open source CfD utility OpenfOaM using computing resources of cluster systems and supercomputers. both the computation results and the laboratory visualization data show that a vertical plate uniformly moving in a stratified fluid generates flow patterns which contain complex systems of internal waves, including upstream, attached and short ones, and thin interfaces, such as ligaments, formed due to the combined influence of the stratification and dissipation effects. Increase in the velocity of the plate movement leads to an essential restructuring of the wake flow past the plate, where typical vortex elements, such as vortex dipoles and ‘vortex bubbles’, are formed in the divergence zones of the phase surfaces of internal waves. all the flow structural components evolve and actively interact with each other and with the free stream. The observation and calculation results are in a good qualitative and quantitative agreement with each other.
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