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Intermittency in the Outer Region of Turbulent Boundary Layers

机译:湍流边界层外部区域的间歇性

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Characteristics of external intermittency in the outer region ofturbulent boundary layers are presented based on single-pointhotwire measurements. The distinction between the turbulentand non-turbulent state of the flow is marked by applying athreshold on instantaneous kinetic-energy, and this criteria isfound to be adequate for this study. Mean intermittency profilesare in consistent agreement with previous observations. Further,conditionally averaged profiles of the streamwise velocityand its standard deviation show good agreement with scalingproposed by Chauhan et al. [3]. Probability density functionsof the lengths of turbulenton-turbulent zones show a range ofintermediate scales over which power-law scaling is observed.The observed power-law scaling provides further evidence for afractal geometry of the turbulenton-turbulent interface (TNTI)over a wide range of Reynolds number and scale separation[8]. Finally, longer lengths (streamwise extent greater than δ=4,where δ is the layer thickness) exhibit exponential probabilitydistribution, indicating that a long turbulenton-turbulent stateoccurs in the flow independent of the length of the alternate statepreceding it.
机译:外部区域的外部间歇性特征 基于单点的湍流边界层 热线测量。湍流之间的区别 并通过应用 瞬时动能的阈值,此标准为 被发现足以进行这项研究。平均间歇性 与以前的观察一致。进一步, 流向速度的条件平均轮廓 其标准偏差与缩放比例显示出良好的一致性 Chauhan等人提出。 [3]。概率密度函数 湍流区/非湍流区的长度范围为 可以观察到幂律定标的中间标度。 观察到的幂律定标为 湍流/非湍流界面的分形几何(TNTI) 广泛的雷诺数和尺度分离 [8]。最后,更长的长度(沿河段的距离大于δ= 4, 其中δ是层的厚度)呈指数机率 分布,表明处于长期湍流/非湍流状态 发生在流中而与交替状态的长度无关 在它之前。

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