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Large-eddy simulation of pyroclastic density currents

Author(s)
Esposti Ongaro, T.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Barsotti, S.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Neri, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Salvetti, M. V.  
Aerospace Engineering Department, University of Pisa, Pisa, Italy  
Editor(s)
Salvetti, M. V.  
Aerospace Engineering Department, University of Pisa, Pisa, Italy  
Geurts, B.  
Multiscale Modeling and Simulation, Faculty EEMCS, University of Twente, Enschede, The Netherlands; Anisotropic Turbulence, Faculty Applied Physics, Eindhoven University of Technology, Eindhoven, The Netherlands  
Meyers, J.  
Katholieke Universiteit Leuven, Div. Appl. Mechanics & Energy Conversion, Leuven, Belgium  
Sagaut, P.  
Université Pierre et Marie Curie 6, Institut Jean le Rond d'Alembert, Paris Cedex, France  
Language
English
Obiettivo Specifico
3.6. Fisica del vulcanismo
Status
Published
Pages Number
161-170
Refereed
Yes
Journal
Quality and Reliability of Large-Eddy Simulations II (in ERCOFTAC Book Series)  
Date Issued
2010
ISBN
978-94-007-02.30-1
Link to last version
http://hdl.handle.net/2122/5833
URI
https://www.earth-prints.org/handle/2122/6844
Subjects
04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous  
05. General::05.01. Computational geophysics::05.01.99. General or miscellaneous  
Subjects

Large-Eddy Simulation...

pyroclastic density c...

numerical simulation

multiphase flows

Abstract
We 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.
Type
book chapter
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