Descripción
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Classical depth integrated SPH models for avalanches are extended in the present work to include a mu(I) rheological model enriched with a fragmentation law. With this improvement the basal friction becomes grain distribution dependent. Rock avalanches, where grain distribution tends to change with time while propagating, are the appropriate type of landslide to apply the new numerical proposal. The mu(I) rheological models considered in the present work are those of Hatano and Gray, combined with two different fragmentation laws, a hyperbolic and a fractal based law. As an application, Frank avalanche, which took place in Canada in 1903, is analyzed under the scope of the present approach, focusing in the influence of the rheological and fragmentation laws in the evolution of the avalanche. | |
Internacional
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Si |
JCR del ISI
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No |
Título de la revista
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INTERNATIONAL JOURNAL FOR NUMERICAL AND ANALYTICAL METHODS IN GEOMECHANICS |
ISSN
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0363-9061 |
Factor de impacto JCR
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2,481 |
Información de impacto
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Edited By: Félix Darve, René de Borst, Andrew J. Whittle, Ronaldo I. Borja, Gilles Pijaudier-Cabot Impact factor:2.481 ISI Journal Citation Reports © Ranking: 2018:16/38 (Engineering, Geological)137/293 (Materials Science, Multidisciplinary)39/134 (Mechanics) Online ISSN:1096-9853 |
Volumen
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43 |
DOI
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10.1002/nag.2912 |
Número de revista
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5 |
Desde la página
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833 |
Hasta la página
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857 |
Mes
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ABRIL |
Ranking
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SI Journal Citation Reports © Ranking: 2018:16/38 (Engineering, Geological)137/293 (Materials Science, Multidisciplinary)39/134 (Mechanics) |