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首页> 外文期刊>European Journal of Mechanics, B. Fluids >Scaling of the near-wall layer beneath turbulent separated flow
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Scaling of the near-wall layer beneath turbulent separated flow

机译:湍流分离流下近壁层的缩放

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This paper is a continuation of an earlier paper [P. E. Hancock, Velocity scales in the near-wall layer beneath reattaching turbulent separated and boundary layer flows, Eur. J. Mech. B Fluids 24 (2005) 425-438] in which it is proposed that each Reynolds stress has its own velocity scale. Two of these, u'{sub}τ and w'{sub}τ, are directly related by definition to the r.m.s. of the wall-shear-stress fluctuations (τ{sub}x and τ{sub}z) in the streamwise and transverse directions. They are also velocity scales for the true dissipation of the turbulent kinetic energy and the Kolmogorov velocity and length scales at the surface. From asymptotic considerations it is shown that the other two scales are related to averages involving instantaneous gradients of wall-shear-stress fluctuations. The measurements, made using pulsed-wire anemometry into the viscous sublayer, show that u'{sub}τ and w'{sub}τ are also the velocity scales for the respective streamwise and transverse fourth-order velocity moments, together with the viscous velocity scale (v/y). Normalised, the fourth-order moments show an inner-layer-like behaviour independent of both position and direction, like that seen in the second-order moments [P. E. Hancock, Velocity scales in the near-wall layer beneath reattaching turbulent separated and boundary layer flows, Eur. J. Mech. B Fluids 24 (2005) 425-438]. However, not surprisingly, the third order moments exhibit an effect of mean shear, seen in the skewing of the probability distributions. Though not measured directly, the measurements imply the behaviour of the averaged products of fluctuations in wall-shear-stress and wall-pressure-gradient (τ{sub}x {partial deriv}p/{partial deriv}x and τ{sub}x {partial deriv}p/{partial deriv}z). Normalised, they also are independent of position and direction. Some of the results presented apply more generally to the near-wall region beneath turbulent flow.
机译:本文是先前论文的延续[P. E. Hancock,速度在重新附着的湍流分离边界层流下面的近壁层中扩展,Eur。 J.机甲[B Fluids 24(2005)425-438]中提出,每个雷诺应力具有其自己的速度标度。根据定义,u'{sub}τ和w'{sub}τ其中两个与r.m.s直接相关。流向和横向的壁剪应力波动(τ{sub} x和τ{sub} z)的变化。它们还是真实消散动能的速度标度,以及表面的Kolmogorov速度和长度标度。从渐近考虑,可以看出其他两个比例与均值有关,均值涉及壁剪应力波动的瞬时梯度。使用脉冲线风速计对粘性子层进行的测量表明,u'{sub}τ和w'{sub}τ也是相应的沿流和横向四阶速度矩的速度尺度以及粘性速度刻度(v / y)。归一化,四阶矩显示出与位置和方向无关的内层状行为,就像在二阶矩中看到的一样。 E. Hancock,速度在重新附着的湍流分离边界层流下面的近壁层中扩展,Eur。 J.机甲B Fluids 24(2005)425-438]。然而,毫不奇怪,从概率分布的偏斜中可以看出,三阶矩表现出平均剪切效应。尽管未直接测量,但测量结果暗示了壁切应力和壁压梯度波动的平均乘积行为(τ{sub} x {偏导} p / {偏导} x和τ{sub} x {偏导数p / {偏导数z})。归一化,它们也与位置和方向无关。提出的某些结果更普遍地适用于湍流下方的近壁区域。

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