Statistical mechanics of fragmentation processes of ice and rock bodies

被引:19
|
作者
Bashkirov, AG
Vityazev, AV
机构
[1] Institute of Planetary Geophysics, United Institute of Earth Physics, Russian Acad. Sci., Moscow 123810
关键词
D O I
10.1016/0032-0633(96)00025-6
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
It is a well-known experimental fact that impact fragmentation, specifically of ice and rock bodies, causes a two-step (''knee''-shaped) power distribution of fragment masses with exponent values within the limits -4 and -1.5 (here and henceforth the differential distribution is borne in mind). A new theoretical approach is proposed to determine the exponent values, a minimal fracture mass, and properities of the knee. As a basis for construction of nonequilibrium statistical mechanics of condensed matter fragmentation the maximum-entropy variational principle is used. In contrast to the usual approach founded on the Boltzmann entropy the more general Tsallis entropy allowing stationary solutions not only in the exponential Boltzmann-Gibbs form but in the form of the power (fractal) law distribution as well is invoked. Relying on the analysis of a lot of published experiments a parameter beta is introduced to describe an inhomogeneous distribution of the impact energy over the target. It varies from 0 (for an utterly inhomogeneous distribution of the impact energy) to 1 (for a homogeneous distribution). The lower limit of fragment masses is defined as a characteristic fragment mass for which the energy of fragment formation is minimal. This mass value depends crucially on the value of beta. It is shown that for beta much less than 1 only small fragment can be formed, and the maximal permitted fragment (of mass m(1)) is the upper boundary of the first stage of the fracture process and the point where the knee takes place. The second stage may be realized after a homogeneous redistribution of the remainder of the impact energy over the remainder of the target (when beta --> 1). Here, the formation of great fragments is permitted only and the smallest of them (of mass m(2)) determines a lower boundary of the second stage. Different forms of the knee can be observed depending on relations between m(1) and m(2). Copyright (C) 1996 Elsevier Science Ltd
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页码:909 / 915
页数:7
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