dc.creatorAravena, A.
dc.creatorChupin, L.
dc.creatorDubois, T.
dc.creatorRoche, O.
dc.date2023-03-14T18:20:34Z
dc.date2023-03-14T18:20:34Z
dc.date2022
dc.date.accessioned2024-05-02T20:30:40Z
dc.date.available2024-05-02T20:30:40Z
dc.identifierhttp://repositorio.ucm.cl/handle/ucm/4502
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/9274747
dc.descriptionA 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.
dc.languageen
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://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, 1-12
dc.subjectDense granular flow
dc.subjectViscoplastic rheology
dc.subjectMultiphase flow,
dc.subjectLevel Set Method
dc.titleFluidisation by pore pressure of dense granular flows: numerical simulations versus experiments
dc.typeArticle


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