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arXiv 2505.10285physics.flu-dyn
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压力梯度湍流边界层中携带雷诺应力结构的空间特征

Spatial Features of Reynolds-Stress Carrying Structures in Turbulent Boundary Layers with Pressure Gradient

M. Ali Yesildag, Taygun R. Gungor, Ayse G. Gungor, Yvan Maciel

AI总结:

本文基于四个DNS数据库比较非平衡压力梯度边界层与均匀剪切湍流中的下扫、上抛结构,揭示1–10个Corrsin尺度内形状一致性及局部平均剪切的主导作用。

摘要:

我们利用四个直接数值模拟数据库研究了非平衡压力梯度湍流边界层外层中携带雷诺剪切应力的结构,其中包括两个非平衡压力梯度边界层工况和两个均匀剪切湍流工况。我们考察并比较了所有工况中雷诺剪切应力结构(特别是下扫和上抛)的空间组织与形状。分析涵盖边界层中的五个流向位置,这些位置在压力梯度的符号、强度和上游历史方面各不相同。对于边界层,考虑了两类三维速度场:完全空间场,以及采用 Taylor 冻结湍流假设的时空场。结果比较表明,下扫和上抛形状的统计量对 Taylor 假设中对流速度的选择很敏感。当下扫和上抛的尺寸处于1至10个 Corrsin 长度尺度范围内时,其形状在所有流动中保持一致,这表明平均剪切在所有工况中发挥相似作用,驱动携带雷诺剪切应力结构的形成并促进湍流产生。不同类型的下扫和上抛形成并排配对,而相同类型的结构则以上游—下游构型排列。无论压力梯度变化或上游历史如何,这种行为都持续存在,突显了局部平均剪切的主导影响。

英文摘要:

We investigate the Reynolds-shear-stress carrying structures in the outer layer of non-equilibrium pressure-gradient turbulent boundary layers using four direct numerical simulation databases, two cases of non-equilibrium pressure-gradient boundary layers and two of homogeneous shear turbulence. We examine and compare the spatial organization and shapes of the Reynolds-shear-stress structures, specifically sweeps and ejections, across all cases. The analysis includes five streamwise locations in the boundary layers, varying in pressure-gradient sign, intensity, and upstream history. For the boundary layers, two types of three-dimensional velocity fields are considered: fully spatial fields and spatio-temporal fields using Taylor's frozen turbulence hypothesis. Comparisons of the results indicate that the statistics of sweep and ejection shapes are sensitive to the choice of convection velocity in Taylor's hypothesis. The sweep and ejection shapes are consistent across all flows when their sizes range from 1 to 10 Corrsin length scales, suggesting that mean shear plays a similar role in all cases, driving the formation of Reynolds-shear-stress carrying structures and contributing to turbulence production. Sweeps and ejections of different types form side-by-side pairs, while structures of the same type align in an upstream-downstream configuration. This behavior persists regardless of pressure gradient variations or upstream history, emphasizing the dominant influence of local mean shear.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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