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dc.contributor.authorStarodubtsev, I.en
dc.contributor.authorVasev, P.en
dc.contributor.authorStarodubtseva, Y.en
dc.contributor.authorTsepelev, I.en
dc.date.accessioned2024-04-08T11:07:31Z-
dc.date.available2024-04-08T11:07:31Z-
dc.date.issued2022-
dc.identifier.citationStarodubtsev, 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.14.5.05harvard_pure
dc.identifier.citationStarodubtsev, 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.14.5.05apa_pure
dc.identifier.issn2079-3537-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access; Bronze Open Access3
dc.identifier.otherhttp://sv-journal.org/2022-5/05/en.pdf1
dc.identifier.otherhttp://sv-journal.org/2022-5/05/en.pdfpdf
dc.identifier.urihttp://elar.urfu.ru/handle/10995/131475-
dc.description.abstractThe 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.sponsorshipDeutsche Forschungsgemeinschaft, DFG, (20-51-12002)en
dc.description.sponsorshipRussian Foundation for Basic Research, РФФИen
dc.description.sponsorshipThe 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.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherNational Research Nuclear Universityen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceScientific Visualization2
dc.sourceScientific Visualizationen
dc.subjectLAVAen
dc.subjectNUMERICAL SIMULATIONen
dc.subjectSCIENTIFIC VISUALIZATIONen
dc.subjectSMOOTHED-PARTICLE HYDRODYNAMICSen
dc.subjectSPHen
dc.subjectDATA VISUALIZATIONen
dc.subjectHYDRODYNAMICSen
dc.subjectNUMERICAL METHODSen
dc.subjectNUMERICAL MODELSen
dc.subjectTHREE DIMENSIONAL COMPUTER GRAPHICSen
dc.subjectTOPOGRAPHYen
dc.subjectVISUALIZATIONen
dc.subjectVOLCANOESen
dc.subjectBUILDINGS MATERIALSen
dc.subjectFLOW PROCESSen
dc.subjectHUMAN ACTIVITIESen
dc.subjectINCOMPRESSIBLE FLUIDen
dc.subjectLAVAen
dc.subjectLAVA FLOWSen
dc.subjectSIMULATION AND VISUALIZATIONSen
dc.subjectSMOOTHED PARTICLE HYDRODYNAMICSen
dc.subjectSPHen
dc.subjectVOLCANIC ERUPTIONSen
dc.subjectNAVIER STOKES EQUATIONSen
dc.titleNumerical Simulation and Visualization of Lava Flowsen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.rsi50010689-
dc.identifier.doi10.26583/sv.14.5.05-
dc.identifier.scopus85145661213-
local.contributor.employeeStarodubtsev 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 Federationen
local.contributor.employeeVasev P., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federationen
local.contributor.employeeStarodubtseva Y., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federationen
local.contributor.employeeTsepelev I., A N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federationen
local.description.firstpage66-
local.description.lastpage76-
local.issue5-
local.volume14-
local.contributor.departmentA N.N. Krasovskii Institute of Mathematics and Mechanics, The Ural Branch, The Russian Academy of Sciences, Russian Federationen
local.contributor.departmentB Ural Federal University named after the first, Russia B.N.Yeltsin, Russian Federationen
local.identifier.pure33230435-
local.identifier.pureb07f55ca-57d9-4065-9cb8-830956616be7uuid
local.identifier.eid2-s2.0-85145661213-
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