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中国物理学会期刊

雷诺求似应力方法的推广和湍流的性质

CSTR: 32037.14.aps.4.1

On An Extension of Reynolds' Method of Finding Apparent Stress and the Nature of Turbulence

CSTR: 32037.14.aps.4.1
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  • 本論文的重要部份,除亂流的瑞諾氏平均運動方程式之導出外,為一組亂流漲落方程式之導出及其解法。若從原有奈非爾——斯托克氏微分方程式減去瑞諾氏之平均運動方程式,則必要的得到此組漲落方程式。解此組方程式之一法是從此求出速度與速度及速度與壓力的第二次與第三次的關連同它們所滿足的微分方程。要解這些關連的微分方程尚須引用兩個假定兩個之中的一個完全是一算學的近似律,其第二個則可物理的解作:亂流的漲落可以分作兩部份,一部份與流體中平均壓力梯度有關,而另一部份則與此梯度無關。論文中的普通理論會用來解释在壓力作用之下二平面間的亂流運動,其理論結果同實驗甚為相合。

     

    The important part of the present paper deals with the deriva tion of,besides Reynolds' equation of mean motion,a set of equations of tarbclent fluetuation and its solution. The latter set follows necessarily,if we subtract the former from the original Navier-Stokes differential equations.To solve these equations of turbulence we build velocity and velocity, velocity and pressure correlations of the second and third orders and the differential equations satisfied by themIt is shown that these equations containing correlations have no defite solution unless two new hypotheses are introduced:one of them is merely a mathematical approximation in nature and the aacond can be interpretel physically that turbulence is the sum of two parta:one depends upon the mean pressure gradient in the moving fluid while the other does not. The general theory is then applied to explain the pressure flow between two paralel planes. The restlt is in good agreement with observation.

     

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