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dc.contributor.authorVivas Miranda, J.G.
dc.contributor.authorGarcía Chomiczak, S.
dc.contributor.authorPaz González, Antonio
dc.date.accessioned2010-01-25T09:34:20Z
dc.date.available2010-01-25T09:34:20Z
dc.date.issued1999
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1999, 24: 99-119 ISSN: 00213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6389
dc.description.abstract[Abstract] In this article the fractal theory and its application to soil structure and porosity is rewieved.Fractal geometry may provide a reliable description of soil structure, particularly in the case of heterogeneous soil. The rewiev illustrates how the geometry of complex porous media may be represented with simple fractal scaling models. Furthermore, three main clases of models proposed in the literature for soil porous space representation are discussed. A case study was presented based on quantitative evaluation of pore size distributions carried on nine pairs of cultivated and uncultivated neighbour located soils. The fractal approach appears to be a useful tool for understanding domains of organization as found in soil aggregates.
dc.language.isospaes_ES
dc.publisherUniversidade da Coruñaes_ES
dc.titleTeoría fractal y efecto de cambio de escala: aplicación al estudio de la porosidad del sueloes_ES
dc.title.alternativeFractal theory and scale change effect: application for studying soil porosity
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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