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 (1MB) doi: 10.31857/S0203-03062023321-33-4267672 (1MB) doi: 10.31857/S0203-03062023321-33-4267673 (4MB) doi: 10.31857/S0203-03062023321-33-4267674 (1MB) doi: 10.31857/S0203-03062023321-33-4267675 (964KB) doi: 10.31857/S0203-03062023321-33-4267676 (1MB) doi: 10.31857/S0203-03062023321-33-4267677 (2MB) doi: 10.31857/S0203-03062023321-33-4267678 (3MB) doi: 10.31857/S0203-03062023321-33-4267679 |
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 |