Determination and interpretation of fractal properties of the sandstone pore system

A knowledge of fractal properties of the pore system is extremely useful with regard to the interrelationships between moisture transport and pore structure. The fractal dimension characterises the egree of resolutiondependence of a property. Given a completely interlaced pore system such as that of sandstone, the fractal dimension of the pore volume, or the porosity, quantifies the cross-sectional variability of the pore channels and is thus of great relevance with regard to transport processes. The fractal dimension of the pore surface describes the surface roughness. A newly-developed measuing technique is presented for the simultaneous determination of fractal dimensions of porosity and pore surface and for establishing fraction radii distributions in order to derive relevant parameters for moisture transport.RésuméL'intérêt de connaître les propriétés fractales des systèmes poreux des grès est d'une grande utilité quant à l'interaction entre processus de transfert d'humidité et structures poreuses. La dimension fractale caractérise le degré de dépendance de la résolution d'une propriété. Étant donné un système poreux en complète interconnexion comme celui des grès, la dimension fractale du volume des pores ou de la porosité quantifie la variabilité sectionnelle du système poreux et est ainsi d'une grande importance en ce qui conceme les processus de transfert. La dimension fractale de la surface poreuse décrit la rugosité de la surface. On présente un nouveau procédé qui permet de déterminer simultanément les dimensions fractales de la porosité et de la surface poreuse ainsi que d'établir une répartition des fractions des rayons pour en déduire des paramètres essentiels pour les processus de transfert.

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