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arXiv physics/0206034physics.flu-dyn
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用精确结构-功能方程研究局部齐次渐近线的Turbulence方法

The Approach of Turbulence to the Locally Homogeneous Asymptote as Studied using Exact Structure-Function Equations

Reginald J. Hill

摘要:

从纳维-斯托克斯方程和不可压缩性出发,但没有其他近似的方程在这里被称为“精确”方程。得到了关于二阶和三阶结构函数的精确方程,以及关于二阶速度结构函数的精确不可压缩条件。所有的时间和空间平均值都被考虑,因为它们产生不同的统计方程。精确方程有特别简单的形式的情况下,平均在一个球在r-空间以及DNS具有周期性的边界条件。该迹线减轻了方程中各向异性的影响,从而揭示了三阶结构函数的迹线预计对于量化渐近标度律是优越的。获得水动力量的两点的中点和差为X和r; t为时间。在X和方向上的r和t褪色的渐近统计状态的局部均匀性,局部各向同性,和局部平稳性,分别接近的方向上的渐近性。因此,精确方程适用于研究接近这些渐近状态的方法。一个新的定义的局部齐性与以前的定义进行了对比。局部均匀性的渐近状态的方法进行了研究,通过使用尺度分析,以确定所需的近似和近似方程有关的实验和模拟的小尺度结构的高雷诺数湍流,但没有调用局部各向同性。这些方程不同于均匀湍流方程。

英文摘要:

Equations that follow from the Navier-Stokes equation and incompressibility but with no other approximations are called "exact" here. Exact equations relating 2nd and 3rd-order structure functions are obtained, as is an exact incompressibility condition on the 2nd-order velocity structure function. Ensemble, temporal, and spatial averages are all considered because they produce different statistical equations. Exact equations have particularly simple forms for the cases of an average over a sphere in r-space as well as DNS that has periodic boundary conditions. The trace mitigates the effect of anisotropy in the equations, thereby revealing that the trace of the third-order structure function is expected to be superior for quantifying asymptotic scaling laws. The midpoint and the difference of the two points at which the hydrodynamic quantities are obtained are X and r; t is time. Dependencies on X and on the orientation of r and on t fade as the asymptotic statistical states of local homogeneity, local isotropy, and local stationarity, respectively, are approached. The exact equations are thus applicable to study of the approach toward those asymptotic states. A new definition of local homogeneity is contrasted with previous definitions. The approach toward the asymptotic state of local homogeneity is studied by using scale analysis to determine the required approximations and the approximate equations pertaining to experiments and simulations of the small-scale structure of high-Reynolds-number turbulence, but without invoking local isotropy. Those equations differ from equations for homogeneous turbulence.

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