Abstract

Coherent fine scale eddies (CFSEs) play an important role in generating streak structures and Reynolds shear stress not only in the near-wall region but also in the logarithmic region. The diameter and maximum azimuthal velocity of the CFSEs in the near-wall, logarithmic and wake regions can be scaled by Kolmogorov length η and velocity uk. The most expected diameter and maximum azimuthal velocity of the CFSEs are about 10 η and 2.0 uk in the near-wall region (y + < 40). In the logarithmic region (40 <y + < 200 ∼ 300), they become about 8.5 η and 1.7uk, respectively. These features are independent of Reynolds number up to Reτ = 1270. Large-scale structure in turbulent channel flows is organized by the CFSEs in the logarithmic region, which contribute to the streamwise velocity deficit (i.e. low-momentum region). By visualizing spatial distributions of the CFSE axes, it is made clear that the probability that the CFSEs exist in low- momentum regions is higher than that existing in high-momentum regions. The low-momentum regions of the logarithmic layer are composed of the CFSEs which have narrower diameter and stronger azimuthal velocity.

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