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Полная запись метаданных
Поле DC | Значение | Язык |
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dc.contributor.author | Starodubtsev, I. | en |
dc.contributor.author | Vasev, P. | en |
dc.contributor.author | Starodubtseva, Y. | en |
dc.contributor.author | Tsepelev, I. | en |
dc.date.accessioned | 2024-04-08T11:07:31Z | - |
dc.date.available | 2024-04-08T11:07:31Z | - |
dc.date.issued | 2022 | - |
dc.identifier.citation | Starodubtsev, I, Vasev, P, Starodubtseva, Y & Tsepelev, I 2022, 'Numerical Simulation and Visualization of Lava Flows', Scientific Visualization, Том. 14, № 5, стр. 66 - 76. https://doi.org/10.26583/sv.14.5.05 | harvard_pure |
dc.identifier.citation | Starodubtsev, I., Vasev, P., Starodubtseva, Y., & Tsepelev, I. (2022). Numerical Simulation and Visualization of Lava Flows. Scientific Visualization, 14(5), 66 - 76. https://doi.org/10.26583/sv.14.5.05 | apa_pure |
dc.identifier.issn | 2079-3537 | - |
dc.identifier.other | Final | 2 |
dc.identifier.other | All Open Access; Bronze Open Access | 3 |
dc.identifier.other | http://sv-journal.org/2022-5/05/en.pdf | 1 |
dc.identifier.other | http://sv-journal.org/2022-5/05/en.pdf | |
dc.identifier.uri | http://elar.urfu.ru/handle/10995/131475 | - |
dc.description.abstract | The study of the behavior of lava flows plays an important role in predicting, preventing and reducing the consequences of volcanic eruptions. Lava has been used as a building material for centuries and has been a source of nutrients for agriculture, but lava flows remain a threat to human activities. Lava flow process is modelled as a spread of a viscous inhomogeneous incompressible fluid under the influence of gravitational forces. The mathematical model is described by the Navier-Stokes equation and the continuity equation with the corresponding initial and boundary conditions. The model takes into account the variable viscosity of the lava, which depends on the volume fraction of crystals. As a spreading surface, we use the generated topography, which is a realistic slope of a mountainous area, formed taking into account natural geological processes. Numerical simulation is carried out using the meshless SPH method. The results of various cases of modeling of lava flows over the surface are presented. Simulation results are visualized using our custom-developed Cinema Science 3D approach. It allows generating a custom 3D visualization with a simple CSV file configuration. We used it for presenting our results in a natural view, showing underlying terrain as mesh and lava as points, moving and changing according to time and other computation parameters. This view was enough for achieving visualization aims of our research. © 2022 National Research Nuclear University. All rights reserved. | en |
dc.description.sponsorship | Deutsche Forschungsgemeinschaft, DFG, (20-51-12002) | en |
dc.description.sponsorship | Russian Foundation for Basic Research, РФФИ | en |
dc.description.sponsorship | The research described here was supported by the Russian Foundation for Basic Research and DFG (grant no. 20-51-12002). During the work, the supercomputer “Uranus” IMM URO was used RAS. | en |
dc.format.mimetype | application/pdf | en |
dc.language.iso | en | en |
dc.publisher | National Research Nuclear University | en |
dc.rights | info:eu-repo/semantics/openAccess | en |
dc.source | Scientific Visualization | 2 |
dc.source | Scientific Visualization | en |
dc.subject | LAVA | en |
dc.subject | NUMERICAL SIMULATION | en |
dc.subject | SCIENTIFIC VISUALIZATION | en |
dc.subject | SMOOTHED-PARTICLE HYDRODYNAMICS | en |
dc.subject | SPH | en |
dc.subject | DATA VISUALIZATION | en |
dc.subject | HYDRODYNAMICS | en |
dc.subject | NUMERICAL METHODS | en |
dc.subject | NUMERICAL MODELS | en |
dc.subject | THREE DIMENSIONAL COMPUTER GRAPHICS | en |
dc.subject | TOPOGRAPHY | en |
dc.subject | VISUALIZATION | en |
dc.subject | VOLCANOES | en |
dc.subject | BUILDINGS MATERIALS | en |
dc.subject | FLOW PROCESS | en |
dc.subject | HUMAN ACTIVITIES | en |
dc.subject | INCOMPRESSIBLE FLUID | en |
dc.subject | LAVA | en |
dc.subject | LAVA FLOWS | en |
dc.subject | SIMULATION AND VISUALIZATIONS | en |
dc.subject | SMOOTHED PARTICLE HYDRODYNAMICS | en |
dc.subject | SPH | en |
dc.subject | VOLCANIC ERUPTIONS | en |
dc.subject | NAVIER STOKES EQUATIONS | en |
dc.title | Numerical Simulation and Visualization of Lava Flows | en |
dc.type | Article | en |
dc.type | info:eu-repo/semantics/article | en |
dc.type | info:eu-repo/semantics/publishedVersion | en |
dc.identifier.rsi | 50010689 | - |
dc.identifier.doi | 10.26583/sv.14.5.05 | - |
dc.identifier.scopus | 85145661213 | - |
local.contributor.employee | Starodubtsev I., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federation, B Ural Federal University named after the first, Russia B.N.Yeltsin, Russian Federation | en |
local.contributor.employee | Vasev P., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federation | en |
local.contributor.employee | Starodubtseva Y., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federation | en |
local.contributor.employee | Tsepelev I., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federation | en |
local.description.firstpage | 66 | - |
local.description.lastpage | 76 | - |
local.issue | 5 | - |
local.volume | 14 | - |
local.contributor.department | A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federation | en |
local.contributor.department | B Ural Federal University named after the first, Russia B.N.Yeltsin, Russian Federation | en |
local.identifier.pure | 33230435 | - |
local.identifier.pure | b07f55ca-57d9-4065-9cb8-830956616be7 | uuid |
local.identifier.eid | 2-s2.0-85145661213 | - |
Располагается в коллекциях: | Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC |
Файлы этого ресурса:
Файл | Описание | Размер | Формат | |
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2-s2.0-85145661213.pdf | 1,01 MB | Adobe PDF | Просмотреть/Открыть |
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