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首页> 外文期刊>Bulletin of the American Physical Society >APS -APS March Meeting 2017 - Event - Experiments in Environmental$~$Flows: Flow over Large-Scale Topography
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APS -APS March Meeting 2017 - Event - Experiments in Environmental$~$Flows: Flow over Large-Scale Topography

机译:APS -APS 3月会议2017年 - 事件 - 环境$〜$流程中的实验:流过大型地形

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In order to provide a better understanding of the flow over large-scale topography relevant to environmental applications, particle image velocimetry (PIV) was used in a refractive-index-matching (RIM) channel to study the flow over 2D and 3D walls defined by the same length scale and occupying roughly 10{%} of the boundary layer. A series of experiments were performed to investigate the impact of roughness three-dimensionality on the flow field in developed turbulent flow, developing turbulent flow, and the transition to turbulence regime. The results show that 3D topographies (in contrast to 2D ones) have characteristic spanwise flows within the topography that relatively reduce spanwise vorticity leading to reduced drag and turbulent activity. Furthermore, turbulent boundary layers exhibit a distinctive response to an abrupt large-scale topographic change depending on whether the topography is 2D or 3D. For example, the integral parameters (e.g., displacement and momentum thicknesses) are significantly more modulated by the topography in the 2D case due to large pressure variations in the streamwise direction. The three-dimensionality of the topography also impacts the nature by which the boundary layer transitions to turbulence. The transition over the 2D topography occurs due to an inflection point in the velocity profile resulting from flow separation within the roughness troughs. In the 3D case, the transition is significantly delayed due to the lack of such instability.
机译:为了提供对与环境应用相关的大规模地形的流量更好地了解,粒子图像速度(PIV)用于折射率匹配(RIM)通道中,以研究由2D和3D壁的流量进行研究相同的长度和占据边界层的大约10 {%}。进行了一系列实验,以研究粗糙度三维的影响在发育湍流,发育湍流和湍流状态的过渡中的流场上的影响。结果表明,3D地形(与2D膜形成对比)在地形内具有结构的特征,其相对减少翼展涡度,导致阻力和湍流活动减少。此外,湍流边界层对突然的大规模地形改变表现出独特的响应,这取决于地形是2D还是3D。例如,由于流动方向上的大的压力变化,由2D壳体中的形貌更明显地调节积分参数(例如,位移和动量厚度)。地形的三维性也影响了边界层转变为湍流的性质。由于粗糙度槽内的流动分离导致的速度曲线中的拐点,发生在2D地形上的过渡。在3D情况下,由于缺乏这种不稳定性,转变显着延迟。

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