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A generalized class of Cantor-set models are introduced in a deductive way to explain the intermittent and multifractal structure in the inertial range of isotropic turbulence. All such Cantor-set models are produced by taking the probability density of the stochastic ratio of averaged disspations in the basic breakdown process with scale ratio A^-1, εᵣ/εAr, as a polynomial {δ} function, and it is proved that only some can guarantee the f-{α} spectra with a non-negative f. The whole statistics of the dissipation density, its square root, and the scaling index {α} which these models should imply are revealed, and typical models are compared with a recent direct numerical simulation to indicate promising applications.
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Iwao Hosokawa (1991) studied this question.
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