Power-law distributions of particle concentration in free-surface flows

Abstract

Particles floating on the surface of a turbulent incompressible fluid accumulate along string-like structures, while leaving large regions of the flow domain empty. This is reflected experimentally by a very peaked probability distribution function of cr, the coarse-grained particle concentration at scale r, around cr = 0, with a power-law decay over two decades of cr, (cr) cr-βr. The positive exponent βr decreases with scale in the inertial range, and stays approximately constant in the dissipative range, thus indicating a qualitative difference between the dissipative and the inertial ranges of scales, also visible in the first moment of cr.

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