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arXiv 2602.04564physics.flu-dyn

纳维-斯托克斯驱动分析湍流通道流中平均和脉动壁面剪应力

Navier-Stokes-driven analysis of mean and fluctuating wall shear stress in turbulent channel flow

Le Yin, Yongyun Hwang, John Christos Vassilicos

AI总结:

本文提出基于纳维-斯托克斯方程分析湍流通道流中平均和脉动壁面剪应力的方法,揭示了湍流生产与扫过现象对剪切加速度协方差的影响。

摘要:

我们提出了一种纳维-斯托克斯驱动分析,用于研究湍流通道流数据中的平均和脉动壁面剪应力(WSS),这些数据来自直接数值模拟,摩擦雷诺数高达$Re_τ≈2000$。从流体方向动量方程出发,我们推导出精确的积分方程,将平方平面平均值和平方脉动WSS与壁面法向积分项结合起来,这些项包括剪切与加速度、剪切与压力梯度以及剪切与粘性扩散的组合。平方平面平均WSS可以很好地近似为平面平均剪切与平面平均加速度的乘积,积分范围为缓冲层,并通过平均压力梯度进行修正,修正幅度随雷诺数的倒数减小。平方脉动WSS同样可以近似为缓冲层中剪切加速度和剪切压力梯度的协方差积分,但后者在雷诺数增加时幅度增大,因此不可忽略。围绕平面平均加速度的加速度波动包括局部欧拉波动加速度、对流加速度以及一个产生剪切加速度协方差湍流生产贡献的项。根据泰勒的冻结湍流假设,欧拉加速度和流体方向平均对流部分的对流加速度相互抵消。剪切加速度协方差由近壁峰值特征,其源于湍流生产,更具体地说是扫过现象。

英文摘要:

We propose a Navier-Stokes-driven analysis of the mean and fluctuating wall shear stress (WSS) applied to turbulent channel flow data from direct numerical simulations at friction Reynolds numbers up to $Re_τ\approx 2000$. Starting from the streamwise momentum equation, we derive exact integral equations that relate the square plane-average and the square fluctuating WSS to wall-normal integrals of terms combining shear with acceleration, shear with pressure-radient, and shear with viscous diffusion. The square plane-average WSS can be well approximated by the product of plane-average shear and plane-average acceleration integrated over the buffer layer with corrections from the mean pressure gradient which diminish as the reciprocal of the Reynolds number. The square fluctuating WSS is similarly well approximated by the shear-acceleration and shear-pressure-gradient covariances integrated over the buffer layer, but the latter increases in magnitude with Reynolds number and is therefore not negligible. The acceleration fluctuations around the plane-average acceleration consist of a local Eulerian fluctuating acceleration, an advective acceleration and a term which gives rise a turbulence production contribution to the shear-acceleration covariance. By Taylor's frozen turbulence hypothesis the Eulerian acceleration and the streamwise mean advection part of the advective acceleration cancel each other. The shear-acceleration covariance is characterised by a near-wall peak which results from turbulence production and, more specifically, sweeps.

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