2D simulation of granular flow over irregular steep slopes using global and local coordinates
In this work approximate augmented Riemann solvers are formulated providing appropriate numerical schemes for mathematical models of granular flow on irregular steep slopes. Fluxes and source terms are discretized to ensure steady state configurations including correct modeling of start/stop flow co...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2013 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/343842 |
| Acceso en línea: | http://hdl.handle.net/10261/343842 |
| Access Level: | acceso abierto |
| Palabra clave: | Weak solutions Well-balanced approach Roe methods Mud/Debris flow Stability region Wet/dry front Shallow water systems Coulomb stress Stopping conditions Gravity components Local coordinates Global coordinates |
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2D simulation of granular flow over irregular steep slopes using global and local coordinatesJuez, CarmeloMurillo, JavierGarcía-Navarro, PilarWeak solutionsWell-balanced approachRoe methodsMud/Debris flowStability regionWet/dry frontShallow water systemsCoulomb stressStopping conditionsGravity componentsLocal coordinatesGlobal coordinatesIn this work approximate augmented Riemann solvers are formulated providing appropriate numerical schemes for mathematical models of granular flow on irregular steep slopes. Fluxes and source terms are discretized to ensure steady state configurations including correct modeling of start/stop flow conditions, both in a global and a local system of coordinates. The weak solutions presented involve the effect of bed slope in pressure distribution and frictional effects by means of the adequate gravity acceleration components. The numerical solvers proposed are first tested against 1D cases with exact solution and then their results are compared with experimental data in order to check the suitability of the mathematical models described in this work. Comparisons between results provided when using global and local system of coordinates are presented. The obtained results point out that both the global and the local system of coordinates can be used to predict faithfully the overall behavior of the phenomena considered in this work.This work has been partially funded by the Spanish Ministry of Science and Technology under research project CGL2011-28590.Peer reviewedElsevierMinisterio de Ciencia y Tecnología (España)202420242013info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionapplication/pdfhttp://hdl.handle.net/10261/343842reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement///CGL2011-28590https://doi.org/10.1016/j.jcp.2013.08.002Noinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3438422026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| title |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| spellingShingle |
2D simulation of granular flow over irregular steep slopes using global and local coordinates Juez, Carmelo Weak solutions Well-balanced approach Roe methods Mud/Debris flow Stability region Wet/dry front Shallow water systems Coulomb stress Stopping conditions Gravity components Local coordinates Global coordinates |
| title_short |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| title_full |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| title_fullStr |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| title_full_unstemmed |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| title_sort |
2D simulation of granular flow over irregular steep slopes using global and local coordinates |
| dc.creator.none.fl_str_mv |
Juez, Carmelo Murillo, Javier García-Navarro, Pilar |
| author |
Juez, Carmelo |
| author_facet |
Juez, Carmelo Murillo, Javier García-Navarro, Pilar |
| author_role |
author |
| author2 |
Murillo, Javier García-Navarro, Pilar |
| author2_role |
author author |
| dc.contributor.none.fl_str_mv |
Ministerio de Ciencia y Tecnología (España) |
| dc.subject.none.fl_str_mv |
Weak solutions Well-balanced approach Roe methods Mud/Debris flow Stability region Wet/dry front Shallow water systems Coulomb stress Stopping conditions Gravity components Local coordinates Global coordinates |
| topic |
Weak solutions Well-balanced approach Roe methods Mud/Debris flow Stability region Wet/dry front Shallow water systems Coulomb stress Stopping conditions Gravity components Local coordinates Global coordinates |
| description |
In this work approximate augmented Riemann solvers are formulated providing appropriate numerical schemes for mathematical models of granular flow on irregular steep slopes. Fluxes and source terms are discretized to ensure steady state configurations including correct modeling of start/stop flow conditions, both in a global and a local system of coordinates. The weak solutions presented involve the effect of bed slope in pressure distribution and frictional effects by means of the adequate gravity acceleration components. The numerical solvers proposed are first tested against 1D cases with exact solution and then their results are compared with experimental data in order to check the suitability of the mathematical models described in this work. Comparisons between results provided when using global and local system of coordinates are presented. The obtained results point out that both the global and the local system of coordinates can be used to predict faithfully the overall behavior of the phenomena considered in this work. |
| publishDate |
2013 |
| dc.date.none.fl_str_mv |
2013 2024 2024 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/343842 |
| url |
http://hdl.handle.net/10261/343842 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement///CGL2011-28590 https://doi.org/10.1016/j.jcp.2013.08.002 No |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Elsevier |
| publisher.none.fl_str_mv |
Elsevier |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
| reponame_str |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869411879896481792 |
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15,811543 |