Abstract
We investigate systems of nature where the common physical processes diffusion and fragmentation compete.We derive a rate equation for the size distribution of fragments. The equation leads to a third order differential equation which we solve exactly in terms of Bessel functions. The stationary state is a universal Bessel distribution described by one parameter, which fits perfectly experimental data from two very different systems of nature, namely, the distribution of ice-crystal sizes from the Greenland ice sheet and the length distribution of helices in proteins.
Original language | English |
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Journal | Physical Review Letters |
Volume | 91 |
Pages (from-to) | 266103-266106 |
ISSN | 0031-9007 |
Publication status | Published - 2003 |
Externally published | Yes |