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Streamwise Vortices in Plane Mixing Layers Originating from Laminar or Turbulent Initial Conditions

机译:层流或湍流初始条件引起的平面混合层中的沿流涡流

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Large Eddy Simulations of the plane mixing layer have been performed, for the purpose of educing the streamwise vortex structure that may exist in these flows. Both an initially-laminar and initially-turbulent mixing layer are considered in this study. The initially-laminar flow originates from Blasius profiles with a white noise fluctuation environment, whilst the initially turbulent flow has an inflow condition obtained from an inflow turbulence generation method. Both simulations produce good mean flow statistics when compared with reference experimental data. The simulations capture the change in growth rate when the initial conditions are either laminar or turbulent. Flow visualisation images demonstrate that both mixing layers contain organised turbulent coherent structures, and that the structures contain rows of streamwise vortices distributed across the span of the mixing layer. Ensemble averaging of the cross-plane data, however, shows no evidence for statistically stationary streamwise vortices in either simulation.
机译:为了产生可能存在于这些流动中的流向涡旋结构,已经进行了平面混合层的大涡模拟。这项研究考虑了初始层状和初始湍流混合层。最初的层流来自具有白噪声波动环境的Blasius轮廓,而最初的湍流具有通过流入湍流生成方法获得的流入条件。与参考实验数据相比,这两种模拟均产生了良好的平均流量统计数据。当初始条件为层流或湍流时,模拟捕获了增长率的变化。流动可视化图像表明,两个混合层均包含有组织的湍流相干结构,并且该结构中包含成行的,沿整个混合层跨度分布的涡流。但是,横断面数据的集合平均显示在任何一种模拟中都没有证据表明统计涡流在统计上是静止的。

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