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dc.rights.licenseReconocimiento 4.0 Internacional
dc.rights.licenseReconocimiento 4.0 Internacional
dc.contributor.advisorVélez Upegui, Jaime Ignacio
dc.contributor.advisorVelásquez Girón, Nicolás
dc.contributor.authorSalamanca Jiménez, Sandra Patricia
dc.date.accessioned2020-08-21T20:20:00Z
dc.date.available2020-08-21T20:20:00Z
dc.date.issued2020-08-12
dc.identifier.citationSalamanca, Sandra. Efectos de escala espacial y temporal en la modelación hidro-sedimentológica distribuida de una cuenca tropical. Caso de estudio San Lorenzo. Universidad Nacional de Colombia, Sede Medellín, Tesis de Grado, 2020. – 100 p.
dc.identifier.urihttps://repositorio.unal.edu.co/handle/unal/78159
dc.descriptionilustraciones, diagramas, mapas, tablas
dc.description.abstractEn Colombia una de las principales causas de degradación del suelo es la erosión, afecta cerca de 32 millones de hectáreas. Sin embargo, a nivel nacional no existe un consenso en cuanto a la escala espacial y temporal apropiada para representar este proceso a escala de cuenca. En este contexto, se han desarrollado diferentes modelos basados en datos empíricos para representar la erosión, transporte y depositación de sedimentos; entre estos se encuentran Universal Soil Loss Equation -USLE y CASC2D-SED. Sin embargo, la mayoría de trabajos encontrados en el estado del arte se enfocan en cuencas extra-tropicales cuyos conclusiones no se puedan aplicar a cuencas de la región andina Colombiana. En este trabajo de investigación se realizó un análisis de escala espacial y temporal de la cuenca del río Nare, afluente del embalse San Lorenzo. En la metodología se usaron dos modelos para evaluar la variabilidad espacial de la pérdida del suelo, Revised USLE -RUSLE y CASC2D-SED. RUSLE se usó como una aproximación para identificar zonas de producción de sedimentos dentro de la cuenca sin tener en cuenta variabilidad en los campos de precipitación y CASC2D-SED, para evaluar el efecto de la escorrentía superficial que produce los eventos de tormenta. En el estudio de la escala temporal, se usaron 5 escalas desde diaria a horaria. En los resultados de la investigación se demuestra que la escala espacial y temporal para representar procesos erosivos debe seleccionarse de acuerdo al objeto del análisis. Para identificar zonas de producción, escalas espaciales finas, sin importar el modelo, logran delimitar entre 10 y 100 veces más zonas con producciones mayores a 0.5 kton/Año km2 respecto a escalas más gruesas. Si el interés es en el transporte de sedimentos en un punto específico durante eventos, una escala temporal fina, logra identificar caudales sólidos con picos 10% mayores que una escala gruesa. Los resultados de este estudio son insumo para la gestión del recurso hídrico de una importante empresa de generación eléctrica del país. (Texto tomado de la fuente)
dc.description.abstractThe erosion is one of the main soil degradation causes in Colombia affecting nearly 32 million hectares, however, at a national level, there is no consensus regarding the appropriate temporal and spatial scale to represents this process.  At basin level, different empirical data-based models have been developed to represent sediment erosion, transport, and deposition. Among the most common are -USLE and CASC2D-SED. Most of the research works found in the state of the art were focused on extra-tropical basins whose conclusions cannot be applied to basins in the Colombian Andean region. In this research, a spatial-temporal analysis of the Nare River (a tributary of the San Lorenzo reservoir) basin was carried out. Two models were used in the methodology to assess the spatial variability of soil loss. RUSLE- was used to identify sediment production zones within the basin without considering variability in precipitation fields. CASC2D-SED was used to evaluate the effect of runoff produced by storm events. In the temporal scale study, 5 temporal scales were used in the CASC2D-SED model. The research results show the goal of the analysis influences the selection of the spatial and temporal scale to represent erosive processes. Finer scales, regardless of the model, achieve between 10 and 100 times more areas delimitation with productions greater than 0.5 kton/Year km2 than coarser scales. If the interest is in the sediment transportation at a specific point during events, a fine time scale identifies soil flows peaks 10% greater than a coarser scale.The research results are used for resource management of an important energy generation company in the country.
dc.format.extentx, 62 páginas + 1 Anexo/PDF
dc.format.mimetypeapplication/pdf
dc.language.isospa
dc.publisherUniversidad Nacional de Colombia
dc.rightsDerechos reservados - Universidad Nacional de Colombia
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subject.ddc620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
dc.titleEfectos de escala espacial y temporal en la modelación hidro-sedimentológica distribuida de una cuenca tropical. Caso de estudio San Lorenzo
dc.typeTrabajo de grado - Maestría
dc.rights.spaAcceso abierto
dc.type.driverinfo:eu-repo/semantics/masterThesis
dc.type.versioninfo:eu-repo/semantics/acceptedVersion
dc.publisher.programMedellín - Minas - Maestría en Ingeniería - Recursos Hidráulicos
dc.contributor.researchgroupPosgrado en Aprovechamiento de Recursos Hidráulicos (PARH)
dc.coverage.regionAntioquia, Colombia
dc.description.degreelevelMaestría
dc.description.degreenameMagíster en Ingeniería - Recursos Hidráulicos
dc.identifier.instnameUniversidad Nacional de Colombia
dc.identifier.reponameRepositorio Institucional Universidad Nacional de Colombia
dc.identifier.repourlhttps://repositorio.unal.edu.co/
dc.publisher.departmentDepartamento de Geociencias y Medo Ambiente
dc.publisher.facultyFacultad de Minas
dc.publisher.placeMedellín, Colombia
dc.publisher.branchUniversidad Nacional de Colombia - Sede Medellín
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dc.rights.accessrightsinfo:eu-repo/semantics/openAccess
dc.subject.proposalErosión de suelos
dc.subject.proposalRUSLE
dc.subject.proposalEscala temporal y espacial
dc.subject.proposalSHIA
dc.subject.proposalCASC2DSED
dc.subject.proposalSoil erosion
dc.subject.proposalTemporal And Spatial Scale
dc.title.translatedEfects of spatial and temporal scale in the distributed hydro-sedimentological modeling of a tropical basin. Case study: San Lorenzo
dc.type.coarhttp://purl.org/coar/resource_type/c_1843
dc.type.coarversionhttp://purl.org/coar/version/c_ab4af688f83e57aa
dc.type.contentText
oaire.accessrightshttp://purl.org/coar/access_right/c_abf2
dcterms.audience.professionaldevelopmentInvestigadores
dc.description.curricularareaÁrea Curricular de Medio Ambiente


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