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dc.contributor.authorAravena, A.
dc.contributor.authorChupin, L.
dc.contributor.authorDubois, T.
dc.contributor.authorRoche, O.
dc.date.accessioned2023-03-14T18:20:34Z
dc.date.available2023-03-14T18:20:34Z
dc.date.issued2022
dc.identifier.urihttp://repositorio.ucm.cl/handle/ucm/4502
dc.description.abstractA model accounting for fluidisation by pore gas pressure in dense granular flows is presented. A viscoplastic rheology, based on the Drucker-Prager criterium, is used to describe the granular medium which is a mixture of air and glass beads. The pore gas pressure, which satisfies an advection-diffusion equation, reduces the friction between the particles and thus the value of the apparent viscosity. As a consequence, dense fluidised granular flows can travel longer distances. In laboratory experiments, the run-out distance reached by dense granular columns when collapsing is almost doubled when fluidisation is applied. This fundamental result, in the context of pyroclastic density currents, is reproduced by numerical simulations performed with the fluidised model.es_CL
dc.language.isoenes_CL
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/*
dc.source8th European Congress on Computational Methods in Applied Sciences and Engineering, ECCOMAS Congress, Oslo, Norway, 1-12es_CL
dc.subjectDense granular flowes_CL
dc.subjectViscoplastic rheologyes_CL
dc.subjectMultiphase flow,es_CL
dc.subjectLevel Set Methodes_CL
dc.titleFluidisation by pore pressure of dense granular flows: numerical simulations versus experimentses_CL
dc.typeArticlees_CL
dc.ucm.facultadFacultad de Ciencias Básicases_CL
dc.ucm.indexacionScopuses_CL
dc.ucm.urihorizon.documentation.ird.fr/exl-doc/pleins_textes/2022-11/010085789.pdfes_CL
dc.ucm.doidoi.org/10.23967/eccomas.2022.123es_CL


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