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Oferta hídrica superficial del humedal el Gallinazo

dc.contributor.authorSALDANA ESCORCIA, ROSSEMBER
dc.contributor.authorOTALVAREZ HERRERA, ROSANA
dc.contributor.authorHERRERA GALVIZ, JUAN DAVID
dc.coverage.spatialColombiaen_US
dc.date.accessioned2026-02-23T15:53:45Z
dc.date.available2026-02-23T15:53:45Z
dc.date.issued2023
dc.identifier.issn2145-6453en_US
dc.identifier.urihttps://repositorioinstitucional.ufpso.edu.co/xmlui/handle/20.500.14167/6097
dc.description.abstractContextualización: los humedales se encuentran en deterioro a causa, princi-palmente, de las actividades humanas que provocan procesos de degradación de estos, por los cambios en el uso de los suelos. Esto ocasiona conflictos en-tre quienes viven cerca al humedal y tiene consecuencias en el suministro de los recursos para las poblaciones ale-dañas. En especial, las actividades hu-manas afectan al recurso hídrico, lo que limita los servicios ecosistémicos que los humedales prestan.Vacío de conocimiento: información inexistente sobre la disponibilidad del recurso hídrico en la zona del humed-al, la cual serviría para una gobernan-za del agua eficiente e inclusiva en la zona, que contribuya en la formulación de políticas públicas para la gestión in-tegral del recurso hídrico, y maximice así el bienestar social y económico en el municipio. Para lograr los objetivos mencionados se hace necesario la de-terminación de dicha disponibilidad, con el fin de conservar los ecosistemas de humedal con importancia regional.Propósito: este trabajo estimó la ofer-ta hídrica superficial [neta] disponible, mediante el método lluvia-escorrentía, en el humedal El Gallinazo, ubicado en Aguachica (Cesar–Colombia), como aporte para la gestión integral del re-curso hídrico.Metodología: se identificó de la cober-tura vegetal de la zona por medio de la metodología «Corine Land Cover» adaptada para Colombia y se deter-minó el grupo hidrológico mediante la textura del suelo; con estos dos insu-mos se determinó, a través de tablas, el número de curvas. La investigación incluyó el cálculo de la precipitación media anual, empleando el método de interpolación de Kriging, con ayu-da del software ArcGIS y la evaluación de los datos meteorológicos extraídos de estaciones del IDEAM [Instituto de Hidrología, Meteorología y Estudios Ambientales] para determinar la pre-cipitación efectiva de la zona. Además, se utilizó el método lluvia-escorrentía en función del número de curvas [SCS-CN] y se examinó la resolución 865 de 2004 (Ministerio de Ambiente Vivienda y Desarrollo Territorial, 2004) para esta-blecer la oferta hídrica neta disponible del humedal El Gallinazo.Resultados y conclusiones: la zona po-see dos tipos de coberturas vegetales, tres grupos hidrológicos de suelo y un CN promedio de 59,29, demostrando un potencial de escorrentía modera-damente alto y una capacidad de in-filtración moderada; la oferta hídrica m3. El comportamiento de la disponib-ilidad del agua depende de las activi-dades antrópicas desarrolladas dentro y fuera del humedal, así como del régi-men de precipitación.en_US
dc.language.isoengen_US
dc.relationhttps://hemeroteca.unad.edu.co/index.php/riaa/article/view/5959en_US
dc.titleOferta hídrica superficial del humedal el Gallinazoen_US
dc.title.translatedSurface water supply of the Gallinazo wetlanden_US
dc.contributor.cvlac0000116197en_US
dc.contributor.cvlac0000116200en_US
dc.contributor.cvlac0001541907en_US
dc.contributor.googlescholardHFj0ycAAAAJ&hlen_US
dc.contributor.googlescholaruzH7pZcAAAAJ&hlen_US
dc.contributor.orcid0000-0002-5290-7072en_US
dc.contributor.orcid0000-0002-7636-5853en_US
dc.contributor.researchgateRossember-Saldana-Escorciaen_US
dc.contributor.researchgateRosana-Herreraen_US
dc.contributor.researchgateJuan-Herrera-Galvizen_US
dc.contributor.scopus57212698376en_US
dc.description.abstractenglishContext: Wetlands are deteriorating primarily due to human activities that cause degradation processes through changes in land use. This leads to conflicts among those living near the wetland and has consequences for the supply of resources to neighboring populations. In particular, human activities affect water resources, limiting the ecosystem services that wetlands provide. Knowledge gap: There is a lack of information on the availability of water resources in the wetland area, which would be useful for efficient and inclusive water governance in the area. This would contribute to the formulation of public policies for the integrated management of water resources, thereby maximizing social and economic well-being in the municipality. To achieve the aforementioned objectives, it is necessary to determine this availability in order to conserve wetland ecosystems of regional importance. Purpose: This work estimated the available [net] surface water supply, using the rainfall-runoff method, in the El Gallinazo wetland, located in Aguachica (Cesar–Colombia), as a contribution to the integrated management of the water resource. Methodology: The vegetation cover of the area was identified using the "Corine Land Cover" methodology adapted for Colombia, and the hydrological group was determined by soil texture; with these two inputs, the number of curves was determined using tables. The research included calculating the average annual precipitation using the Kriging interpolation method with the aid of ArcGIS software and evaluating meteorological data from IDEAM (Institute of Hydrology, Meteorology and Environmental Studies) stations to determine the effective precipitation of the area. Additionally, the rainfall-runoff method based on the number of curves (SCS-CN) was used, and Resolution 865 of 2004 (Ministry of Environment, Housing and Territorial Development, 2004) was examined to establish the net available water supply of the El Gallinazo wetland. Results and conclusions: the area has two types of vegetation cover, three hydrological soil groups, and an average CN of 59.29, demonstrating a moderately high runoff potential and a moderate infiltration capacity; the water supply is [m3]. The behavior of water availability depends on human activities carried out inside and outside the wetland, as well as the precipitation regime.en_US
dc.subject.proposalCobertura vegetal, disponibilidad de agua, humedal, llu-via-escorrentía, método SCS-CN.en_US
dc.subject.proposalCobertura vegetal, disponibilidad de agua, humedal, llu-via-escorrentía, método SCS-CN.en_US
dc.subject.keywordsVegetation cover, water availability, wetland, rainfall-via-runoff, SCS-CN method.en_US
dc.subject.keywordsVegetation cover, water availability, wetland, rainfall-via-runoff, SCS-CN method.en_US
dc.publisher.facultyFacultad ciencias agrarias y del ambienteen_US
dc.type.redcolhttp://purl.org/redcol/resource_type/ARTen_US
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