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VolcFlow capabilities and potential development for the simulation of lava flows

By
Karim Kelfoun
Karim Kelfoun
Laboratoire Magmas et Volcans, Université Blaise Pascal–CNRS–IRD, OPGC, 5 rue Kessler, 63038 Clermont-Ferrand, France
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Silvia Vallejo Vargas
Silvia Vallejo Vargas
Instituto Geofisico, Escuela Politécnica Nacional, Ladrón de Guevara E11-253 y Andalucía, Apartado 2759, Quito, Ecuador
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Published:
January 01, 2016

Abstract

VolcFlow is a finite-difference Eulerian code based on the depth-averaged approach and developed for the simulation of isothermal geophysical flows. Its capability for reproducing lava flows is tested here for the first time. The field example chosen is the 2010 lava flow of Tungurahua volcano (Ecuador), the emplacement of which is tracked by projecting thermal images onto a georeferenced digital topography. Results show that, at least for this case study, the isothermal approach of VolcFlow is able to simulate the velocity of the lava through time, as well as the extent of the solidified lava. However, the good fit between the modelled and the natural flow may be explained by the short emplacement time (c. 20 h) of a thick lava (c. 5 m), which could limit the influence of cooling on the flow dynamics, thus favouring the use of an isothermal rheology.

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Geological Society, London, Special Publications

Detecting, Modelling and Responding to Effusive Eruptions

A. J. L. Harris
A. J. L. Harris
Université Blaise Pascal, France
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T. De Groeve
T. De Groeve
Joint Research Centre of the European Commission, Italy
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F. Garel
F. Garel
Université de Montpellier, France
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S. A. Carn
S. A. Carn
Michigan Technological University, USA
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Geological Society of London
Volume
426
ISBN electronic:
9781862399587
Publication date:
January 01, 2016

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