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dc.contributor.authorRomano, Alessandro
dc.contributor.authorLópez Lara, Javier 
dc.contributor.authorBarajas Ojeda, Gabriel
dc.contributor.authorLosada Rodríguez, Iñigo 
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2023-10-18T15:24:51Z
dc.date.available2023-10-18T15:24:51Z
dc.date.issued2023
dc.identifier.issn0378-3839
dc.identifier.issn1872-7379
dc.identifier.urihttps://hdl.handle.net/10902/30236
dc.description.abstractLandslide-generated tsunamis are a relevant hazard. Their low frequency/high consequences character and the complex phenomena related to their generation, propagation and interaction with the shore make the proper modeling of these phenomena a crucial activity to mitigate the related risk. In this article, a new numerical method for modeling tsunamis generated by granular landslides in OpenFOAM® is presented. The approach consists in modeling the granular material by using a Coulomb viscoplastic rheology (non-Newtonian rheology) implemented in the standard solver multiPhaseInterFoam. The proposed approach is simple as it only depends on few physics-based parameters, thus implying less uncertainties than dense fluid models and more flexibility and computational efficiency than Euler?Euler approaches. This numerical framework is applied to reproduce three literature benchmark landslide-tsunami cases: two-dimensional (2D) submerged as well as 2D and threedimensional (3D) subaerial. Comparing numerical and experimental results, a good agreement is found for granular material behavior, while an overall very good (excellent in some cases) agreement is found as far as fluid behavior and waves characteristics are concerned, testifying that the momentum transfer between granular and fluid phases is well reproduced by this simple rheological model. Qualitative descriptions of the numerical results, in terms of landslide behavior, wave generation characteristics, and velocity field during the generation/propagation process are provided. Moreover, quantitative comparisons between experimental and numerical results by comparing landslide evolution, free surface elevation time series, and runup time series are presented and discussed in the article.es_ES
dc.description.sponsorshipThe authors acknowledge the financial support from the Government of Cantabria through the Fénix Program. The kind help of Prof. Hermann Fritz, who provided further information on the 3D subaerial case, is warmly acknowledged. A special acknowledgment is due to Prof. Bellotti for the constant support and fruitful discussions.es_ES
dc.format.extent18 p.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsAttribution 4.0 Internationales_ES
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.sourceCoastal Engineering, 2023, 186, 104391es_ES
dc.subject.otherGranular landslideses_ES
dc.subject.otherNumerical modelinges_ES
dc.subject.otherTsunamises_ES
dc.subject.otherWater waveses_ES
dc.titleNumerical modeling of tsunamis generated by granular landslides in OpenFOAM®: A Coulomb viscoplastic rheologyes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1016/j.coastaleng.2023.104391es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1016/j.coastaleng.2023.104391
dc.type.versionpublishedVersiones_ES


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Attribution 4.0 InternationalExcepto si se señala otra cosa, la licencia del ítem se describe como Attribution 4.0 International