Fragmentation Under the Scaling Symmetry and Turbulent Cascade with Intermittency

Fragmentation plays an important role in a variety of physical, chemical, and geological processes. Examples include atomization in sprays, crushing of rocks, explosion and impact of solids, polymer degradation, etc. Although each individual action of fragmentation is a complex process, the number of these elementary actions is large. It is natural to abstract a simple effective scenario of fragmentation and to represent its essential features. One of the models is the fragmentation under the scaling symmetry each breakup action reduces the typical length of fragments, r double right arrow alpha r, by an independent random multiplier alpha 0 alpha 1, which is governed by the fragmentation intensity spectrum qalpha, integralexp 1sub 0 qalphad alpha 1. This scenario has been proposed by Kolmogorov 1941, when he considered the breakup of solid carbon particle. Describing the breakup as a random discrete process, Kolmogorov stated that at latest times, such a process leads to the log-normal distribution. In Gorokhovski Saveliev 2003, the fragmentation under the scaling symmetry has been reviewed as a continuous evolution process with new features established. The objective of this paper is twofold. First, the paper synthesizes and completes theoretical part of Gorokhovski Saveliev 2003. Second, the paper shows a new application of the fragmentation theory under the scale invariance. This application concerns the turbulent cascade with intermittency. We formulate here a model describing the evolution of the velocity increment distribution along the progressively decreasing length scale. The model shows that when the turbulent length scale gets smaller, the velocity increment distribution has central growing peak and develops stretched tails. The intermittency in turbulence is manifested in the same way large fluctuations of velocity provoke highest strain in narrow dissipative regions of flow.