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  • 1980-1984  (3)
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Year
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Applied mathematics and mechanics 3 (1982), S. 845-851 
    ISSN: 1573-2754
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Mathematics , Physics
    Notes: Abstract The whole paper consists of two parts (Part I and Part II). In part I, we shall analyze the relation between the two theories of turbulence involving large Reynolds number: the Markov process theory from the Lagrangian point of view and Kolmogoroff's theory from the Eulerian point of view. It will be pointed out that the Reynolds number needed for the Markovian description of turbulence should be as large as that needed for Kolmogoroff's second hypothesis, that the eddies of the period of order T1 (the self-correlation time scale of the random velocity u) and the eddies of the period of order T1 (the self-correlation time scale of the random force f) correspond to the energy-containing eddies and the eddies in the dissipation range respectively, and that T*⩽t≪β−1, the time interval for the applicability of Richardson's law during twoparticle's dispersion, corresponds to the inertial subrange in Kolmogoroff's theory. Thus, these two theories reflect the property of the turbulence involving very large Reynolds number arguing from different aspects. In Part II, by using physical analysis in Part I, we shall establish in a certain way the quantitative relation between these two theories. In terms of this relation and the results of the study of two-particle's dispersion motion, we shall obtain the structure functions, the correlation functions and the energy spectrum, which are appliciable not only to the inertial subrange, but also to the whole range with the wave number less than that in the inertial subrange. Kolmogoroff's “2/3 law” and ”−5/3 law” are the asymptotic solutions with respect to the present result in the inertial subrange. Thus, the present result is an extension of Kolmogoroff's laws.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Applied mathematics and mechanics 4 (1983), S. 191-204 
    ISSN: 1573-2754
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Mathematics , Physics
    Notes: Abstract By using the physical analysis described in Paper I (Part I of this paper), we shall establish, in a certain way, the quantitative relation between the Markov process theory of two particle dispersion in a turbulence of very large Reynolds number and the Kolmogoroff's theory. In terms of this relation and the results of two-particle dispersion, we shall obtain the structure functions, the correlation functions and the energy spectrum, which are applicable not only to the inertial subrange, but also to the whole range of the wave number less than that in the inertial subrange. The Kolmogoroff's “2/3 law” and “−5/3 Law” are the asymptotic cases of the present result for large k. Thus, the present resuit is an extension of Kolmogoroff's laws.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Applied mathematics and mechanics 5 (1984), S. 1163-1172 
    ISSN: 1573-2754
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics , Mathematics , Physics
    Notes: Abstract Based on the geographic approximation the two-dimensional dynamical structure of the wind fields of Jupiter's Great Red Spot and White Oval BC is obtained. The results of calculation are in good agreement with the observations. Thus, an explanation of the observed dispersion of the velocities along the horizontal streamline is given. The major physical mechanism of this dispersion is as follwos: The distance between two adjacent elliptical streamlines varies along the elliptical streamline, leading to the variance of the normal pressure gradient. Thus, the horizontal velocity Vt has to vary correspondingly so that the Coriolis force can approximately balance the normal pressure gradient Another less important factor, i. e., the change of the Coriolis force parameter with the latitude, is also taken into account. The distributions of the vorticities of GRS and White Oval BC are also calculated.
    Type of Medium: Electronic Resource
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