Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6844
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dc.contributor.authorallEsposti Ongaro, T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallBarsotti, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallNeri, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallSalvetti, M. V.; Aerospace Engineering Department, University of Pisa, Pisa, Italyen
dc.contributor.editorallSalvetti, M. V.; Aerospace Engineering Department, University of Pisa, Pisa, Italyen
dc.contributor.editorallGeurts, B.; Multiscale Modeling and Simulation, Faculty EEMCS, University of Twente, Enschede, The Netherlands; Anisotropic Turbulence, Faculty Applied Physics, Eindhoven University of Technology, Eindhoven, The Netherlandsen
dc.contributor.editorallMeyers, J.; Katholieke Universiteit Leuven, Div. Appl. Mechanics & Energy Conversion, Leuven, Belgiumen
dc.contributor.editorallSagaut, P.; Université Pierre et Marie Curie 6, Institut Jean le Rond d'Alembert, Paris Cedex, Franceen
dc.date.accessioned2011-01-24T06:55:09Zen
dc.date.available2011-01-24T06:55:09Zen
dc.date.issued2010en
dc.identifier.isbn978-94-007-02.30-1en
dc.identifier.urihttp://hdl.handle.net/2122/6844en
dc.description.abstractWe investigate the dynamics of turbulent pyroclastic density currents (PDCs) by adopting a 3D, Eulerian-Eulerian multiphase flow model, in which solid particles are treated as a continuum and the grain-size distribution is simplified by assuming two particulate phases. The turbulent sub-grid stress of the gas phase is modelled within the framework of Large-Eddy Simulation (LES) by means of a eddy-viscosity model together with a wall closure. Despite the significant numerical diffusion associated to the upwind method adopted for the Finite-Volume discretization, numerical simulations demonstrate the need of adopting a Sub-Grid Scale (SGS) model, while revealing the complex interplay between the grid and the SGS filter sizes. We also analyse the relationship between the averaged flow dynamic pressure and the action exerted by the PDC on a cubic obstacle, to evaluate the impact of a PDC on a building. Numerical results suggest that the average flow dynamic pressure can be used as a proxy for the force per unit surface acting on the building envelope (Fig. 5), even for such steeply stratified flows. However, it is not possible to express such proportionality as a constant coefficient such as the drag coefficient in a steady-state current. The present results indeed indicate that the large epistemic and aleatory uncertainty on initial and boundary conditions has an impact on the numerical predictions which is comparable to that of grid resolution.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofQuality and Reliability of Large-Eddy Simulations II (in ERCOFTAC Book Series)en
dc.relation.isversionofhttp://hdl.handle.net/2122/5833en
dc.subjectLarge-Eddy Simulationen
dc.subjectpyroclastic density currentsen
dc.subjectnumerical simulationen
dc.subjectmultiphase flowsen
dc.titleLarge-eddy simulation of pyroclastic density currentsen
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber161-170en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneousen
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.99. General or miscellaneousen
dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.fulltextopenen
dc.contributor.authorEsposti Ongaro, T.en
dc.contributor.authorBarsotti, S.en
dc.contributor.authorNeri, A.en
dc.contributor.authorSalvetti, M. V.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentAerospace Engineering Department, University of Pisa, Pisa, Italyen
dc.contributor.editorSalvetti, M. V.en
dc.contributor.editorGeurts, B.en
dc.contributor.editorMeyers, J.en
dc.contributor.editorSagaut, P.en
dc.contributor.editordepartmentAerospace Engineering Department, University of Pisa, Pisa, Italyen
dc.contributor.editordepartmentMultiscale Modeling and Simulation, Faculty EEMCS, University of Twente, Enschede, The Netherlands; Anisotropic Turbulence, Faculty Applied Physics, Eindhoven University of Technology, Eindhoven, The Netherlandsen
dc.contributor.editordepartmentKatholieke Universiteit Leuven, Div. Appl. Mechanics & Energy Conversion, Leuven, Belgiumen
dc.contributor.editordepartmentUniversité Pierre et Marie Curie 6, Institut Jean le Rond d'Alembert, Paris Cedex, Franceen
item.openairetypebook chapter-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptUniversità di Pisa-
crisitem.author.orcid0000-0002-6663-5311-
crisitem.author.orcid0000-0002-3536-3624-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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