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Explorando la respuesta hidrodinámica de un río altamente perturbado por erupciones volcánicas: el Río Blanco, Chaitén (Chile)

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Explorando la respuesta hidrodinámica de un río altamente perturbado por erupciones volcánicas: el Río Blanco, Chaitén (Chile)

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dc.contributor.author Mazzorana, Bruno es_ES
dc.contributor.author Bahamondes Rosas, Diego es_ES
dc.contributor.author Montecinos, Liz es_ES
dc.contributor.author Ruiz-Villanueva, Virginia es_ES
dc.contributor.author Rojas, Iván es_ES
dc.coverage.spatial east=-72.7095437; north=-42.918234; name=Chaitén, Chaiten, Chaitén, Los Lagos, Xile es_ES
dc.date.accessioned 2023-05-08T06:42:55Z
dc.date.available 2023-05-08T06:42:55Z
dc.date.issued 2023-04-28
dc.identifier.issn 1134-2196
dc.identifier.uri http://hdl.handle.net/10251/193174
dc.description.abstract [EN] This work explored the hydrodynamic response of the Blanco River to three-phase flows (water, sediment, and wood), in a context of volcanic disturbance. The scarce hydrological information makes the use of traditional methods difficult, so an alternative methodological approach was defined to determine the flood hazard through numerical modelling (Iber) and scenario design. The results showed that the discharge required to flood the town varied between 850 and 950 m3/s for single-phase flows (water only), while for three-phase flows the discharge was much lower (between 700 and 800 m3/s). In addition, significant differences in flooded areas were observed between scenarios with different roughness and proportion of sediment and wood in the flow. The results show the great complexity and sensitivity of the Rio Blanco River system. es_ES
dc.description.abstract [ES] En este trabajo se exploró la respuesta hidrodinámica del Río Blanco ante flujos trifásicos (agua, sedimento y madera), en un contexto de perturbación volcánica. La escasa información hidrológica dificulta el uso de métodos tradicionales, por lo que se definió una alternativa metodológica para determinar la peligrosidad de inundaciones a través de modelos numéricos (Iber) y el diseño de escenarios. Los resultados mostraron que el caudal necesario para el desborde del río varía entre 850 y 950 m3/s para flujos monofásicos (solo agua), mientras que para los flujos trifásicos el caudal fue mucho menor (entre 700 y 800 m3/s). Además, se observaron diferencias significativas en el área inundada entre los escenarios con distintas rugosidades y proporción de sedimento y madera en el flujo. Los resultados evidencian la gran complejidad y sensibilidad del sistema fluvial del Río Blanco. es_ES
dc.description.sponsorship Esta investigación fue financiada por ANID/CONICYT con el Proyecto FONDECYT REGULAR - Folio 1200091 -“Unravelling the dynamics and impacts of sediment-laden flows in urban areas in Southern Chile as a basis for innovative adaptation (SEDIMPACT)” del Investigador Responsable Bruno Mazzorana. es_ES
dc.language Español es_ES
dc.publisher Universitat Politècnica de València es_ES
dc.relation.ispartof Ingeniería del Agua es_ES
dc.rights Reconocimiento - No comercial - Compartir igual (by-nc-sa) es_ES
dc.subject Chaitén es_ES
dc.subject Hazardouness es_ES
dc.subject Thriphasic flows es_ES
dc.subject Iber es_ES
dc.subject Hydrodynamic sensitivity es_ES
dc.subject Peligrosidad es_ES
dc.subject Flujos trifásicos es_ES
dc.subject Sensibilidad hidrodinámica es_ES
dc.title Explorando la respuesta hidrodinámica de un río altamente perturbado por erupciones volcánicas: el Río Blanco, Chaitén (Chile) es_ES
dc.title.alternative Exploring the hydrodynamic response of a highly perturbed river due to volcanic eruptions: the Blanco River, Chaitén (Chile) es_ES
dc.type Artículo es_ES
dc.identifier.doi 10.4995/ia.2023.18866
dc.relation.projectID info:eu-repo/grantAgreement/FONDECYT//1200091/Unravelling the dynamics and impacts of sediment-laden flows in urban areas in Southern Chile as a basis for innovative adaptation (SEDIMPACT) es_ES
dc.rights.accessRights Abierto es_ES
dc.description.bibliographicCitation Mazzorana, B.; Bahamondes Rosas, D.; Montecinos, L.; Ruiz-Villanueva, V.; Rojas, I. (2023). Explorando la respuesta hidrodinámica de un río altamente perturbado por erupciones volcánicas: el Río Blanco, Chaitén (Chile). Ingeniería del Agua. 27(2):73-92. https://doi.org/10.4995/ia.2023.18866 es_ES
dc.description.accrualMethod OJS es_ES
dc.relation.publisherversion https://doi.org/10.4995/ia.2023.18866 es_ES
dc.description.upvformatpinicio 73 es_ES
dc.description.upvformatpfin 92 es_ES
dc.type.version info:eu-repo/semantics/publishedVersion es_ES
dc.description.volume 27 es_ES
dc.description.issue 2 es_ES
dc.identifier.eissn 1886-4996
dc.relation.pasarela OJS\18866 es_ES
dc.contributor.funder Fondo Nacional de Desarrollo Científico y Tecnológico, Chile es_ES
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