Project Details
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Data-driven thermomechanical modelling of lava flows

Subject Area Mineralogy, Petrology and Geochemistry
Geophysics
Term from 2020 to 2023
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 429622451
 
Final Report Year 2024

Final Report Abstract

Volcanic eruptions belong to the extreme events that change the Earth’s landscape and affect global climate and environment. Although a main attention is given to explosive eruptions, non-explosive eruptions leading to large lava flows or dome growth, with their subsequent collapse and pyroclastic flows, are equally important. This project has addressed the main scientific question: how quantitative modelling and observations can improve the understanding of the lava dynamics? Although no mathematical/numerical model is likely to represent the exact magma extrusion and lava dynamics, the thermomechanical models developed in this project account for the main dynamic processes and characteristics associated with lava flows or dome growth. Namely, the models include the mass and heat transfer, the degassing-induced crystallization kinetics, the latent heat of crystallization, the convective and radiative heat flux at the air-lava interface, conductive heat flux at the crater surface and the shallow conduit wall, and the lava viscosity depending on the volume fraction of crystals and temperature. To solve the models, a few numerical approaches have been developed and applied to study the lava dynamics in different geological areas: an andesitic lava dome growth at Volcán de Colima, Mexico during 2007-2009; an ancient rhyolitic lava flow at Summit Lake, Yellowstone, USA; and a basaltic lava flow at Mt. Etna, Italy in 2015. Three-dimensional numerical models of lava flow have clarified the influence of the surface topography and lava flow viscosity on the advancement and duration of the flow. A sensitivity analysis of the model results with respect to model parameters, performed for the case of lava flows at Mt. Etna, showed a range of the parameters, where the model results fit well the observations. The modelled lava advancement at the Summit Lake agrees with the observations assuming that the pressure change in the magma chamber during the eruption changed the volcanic topography. With the increase of the magma viscosity, the lava flow on the surface slows down and its thickness increases leading to changes in the lava flow morphology. It was shown that the combined effects of the thermal evolution and crystallization in the dome interior and the cooling at the air-lava interface shape the lava dome during long episodes of its building at Volcán de Colima. The developed thermomechanical models of the lava dynamics can be used at other volcanoes during effusive eruptions, lava flows, and lava dome building.

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