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Three-Dimensional Numerical Modeling of Lava Dynamics Using the Smoothed Particle Hydrodynamics Method

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1. Title Title of document Three-Dimensional Numerical Modeling of Lava Dynamics Using the Smoothed Particle Hydrodynamics Method
2. Creator Author's name, affiliation, country I. S. Starodubtsev; Krasovsky Institute of Mathematics and Mechanics, Ural Branch of the Russian Academy of Sciences; Ural Federal University
2. Creator Author's name, affiliation, country Y. V. Starodubtseva; Krasovsky Institute of Mathematics and Mechanics, Ural Branch of the Russian Academy of Sciences
2. Creator Author's name, affiliation, country I. А. Tsepelev; Krasovsky Institute of Mathematics and Mechanics, Ural Branch of the Russian Academy of Sciences
2. Creator Author's name, affiliation, country A. T. Ismail-Zadeh; Karlsruhe Institute of Technology, Institute of Applied Geosciences
3. Subject Discipline(s)
3. Subject Keyword(s) lava dome; lava flow; viscosity; morphology; numerical analysis; scientific visualization
4. Description Abstract

Lava domes and lava flows are major manifestations of effusive volcanic eruptions. Less viscous lava tends to flow long distances, depending on the volcanic slope topography, the eruption rate, and the viscosity of the erupted magma. When magma is highly viscous, its eruption to the surface leads to the formation of lava domes and their growth. The meshless smoothed particle hydrodynamics (SPH) method is used in this paper to simulate lava dynamics. We describe the SPH method and present a numerical algorithm to compute lava dynamics models. The numerical method is verified by solving a model of cylindrical dam-break fluid flow, and the modelled results are compared to the analytical solution of the axisymmetric thin-layer viscous current problem. The SPH method is applied to study three models of lava advancement along the volcanic slope, when the lava viscosity is constant, depends on time and on the volume fraction of crystals in the lava. Simulation results show characteristic features of lava flows, such as lava channel and tube formation, and lava domes, such as the formation of a highly viscous carapace versus a less viscous dome core. Finally, the simulation results and their dependence on a particle size in the SPH method are discussed.

5. Publisher Organizing agency, location The Russian Academy of Sciences
6. Contributor Sponsor(s)
7. Date (DD-MM-YYYY) 01.05.2023
8. Type Status & genre Peer-reviewed Article
8. Type Type
9. Format File format
10. Identifier Uniform Resource Identifier https://journals.eco-vector.com/0203-0306/article/view/660087
10. Identifier Digital Object Identifier (DOI) 10.31857/S0203030623700165
10. Identifier eLIBRARY Document Number (EDN) TSOHRH
10. Identifier Digital Object Identifier (DOI) (PDF (Rus)) 10.31857/S0203-03062023321-33-175475
11. Source Title; vol., no. (year) Вулканология и сейсмология; No 3 (2023)
12. Language English=en
13. Relation Supp. Files (975KB) doi: 10.31857/S0203-03062023321-33-4267671
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14. Coverage Geo-spatial location, chronological period, research sample (gender, age, etc.)
15. Rights Copyright and permissions Copyright (c) 2023 И.С. Стародубцев, Ю.В. Стародубцева, И.А. Цепелев, А.Т. Исмаил-Заде