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Fractures, fractals and breakage energy of mineral particles

Identifieur interne : 00A845 ( Main/Curation ); précédent : 00A844; suivant : 00A846

Fractures, fractals and breakage energy of mineral particles

Auteurs : A. Thomas [France] ; L. O. Filippov [France]

Source :

RBID : ISTEX:4DA543DE80B62469FD00520539452DD3CCA79642

English descriptors

Abstract

Abstract: In this paper, we intend to test a classical and intuitive but not yet formalised idea expressed as: the fragmentation conditions of any mineral material first depend on its genuine structure especially of the architecture and of the shape of natural discontinuities. If such an assumption is reliable, relations must be found between the energy consumption during breakage and the structural properties. Of course, this requires an accurate description of the geometrical properties of the genuine and created discontinuity sets. The suggested model lies on two basic assumptions: the first is that initial fracture distribution is ruled by a fractal law already proposed by Turcotte and the second is that any fracture shape, on a size range to be specified, is accurately described by another scaling law. Some interesting properties result to the found relation between the Hukki's model of spent energy and the structural fractal model.

Url:
DOI: 10.1016/S0301-7516(99)00029-0

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ISTEX:4DA543DE80B62469FD00520539452DD3CCA79642

Le document en format XML

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<term>Crystal network</term>
<term>Discontinuity</term>
<term>Discontinuity network</term>
<term>Discontinuity surface element</term>
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<term>Energy balance</term>
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<term>Energy spending</term>
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<term>Little values</term>
<term>Logarithmic coordinates</term>
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<term>Particle bounds</term>
<term>Plastic zone</term>
<term>Potential energy</term>
<term>Quantitative analysis</term>
<term>Rupture</term>
<term>Separation paths</term>
<term>Size distribution</term>
<term>Size range</term>
<term>Strain energy</term>
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<term>Structural properties</term>
<term>Talc particles</term>
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