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arXiv 2108.12940physics.flu-dyn
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边界层turbulence中惯性尺度子区间内的自相似几何

Self-similar geometries within the inertial subrange of scales in boundary layer turbulence

Michael Heisel, Charitha M. de Silva, Gabriel G. Katul, Marcelo Chamecki

摘要:

湍流尺度的惯性子区通常由集合统计中的幂律特征反映,例如能谱和结构函数-无论是在理论上还是从观测中。尽管在湍流中的分形几何的主题有希望的发现,有没有被接受的图像的物理流的功能对应于这个统计签名的惯性子范围。本研究使用边界层湍流测量来评估速度等值面的自相似几何特性,并调查它们对速度信号统计的影响。流向速度等值面的分形维数,表示沿每个等值面的“皱纹”的大小的统计自相似性,被证明是恒定的尺度的惯性子范围内。对于惯性子范围和生产范围之间的过渡,据推断,最大的皱纹变得越来越局限于大规模的相干速度区域,如均匀动量区的整体尺寸。等值面的自相似性在随后的一维统计中产生幂律趋势。例如,结构函数的理论2/3幂律指数可以通过考虑大量等值面水平集的集体行为来恢复。结果表明,惯性子区涡的物理存在表现在等值面的自相似皱纹。

英文摘要:

The inertial subrange of turbulent scales is commonly reflected by a power law signature in ensemble statistics such as the energy spectrum and structure functions - both in theory and from observations. Despite promising findings on the topic of fractal geometries in turbulence, there is no accepted image for the physical flow features corresponding to this statistical signature in the inertial subrange. The present study uses boundary layer turbulence measurements to evaluate the self-similar geometric properties of velocity isosurfaces and investigate their influence on statistics for the velocity signal. The fractal dimension of streamwise velocity isosurfaces, indicating statistical self-similarity in the size of "wrinkles" along each isosurface, is shown to be constant only within the inertial subrange of scales. For the transition between the inertial subrange and production range, it is inferred that the largest wrinkles become increasingly confined by the overall size of large-scale coherent velocity regions such as uniform momentum zones. The self-similarity of isosurfaces yields power law trends in subsequent one-dimensional statistics. For instance, the theoretical 2/3 power law exponent for the structure function can be recovered by considering the collective behavior of numerous isosurface level sets. The results suggest that the physical presence of inertial subrange eddies is manifested in the self-similar wrinkles of isosurfaces.

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