SciELO - Scientific Electronic Library Online

 
vol.44 número2Factor analysis and multifractal concentration-area modeling for the delimitation of complex pedogeochemical anomalies in the Loma Roja-Loma Hierro sector, Western CubaRainfall thresholds as triggering factor in the Central cordillera of the Colombian Andes índice de autoresíndice de assuntospesquisa de artigos
Home Pagelista alfabética de periódicos  

Serviços Personalizados

Journal

Artigo

Indicadores

Links relacionados

  • Em processo de indexaçãoCitado por Google
  • Não possue artigos similaresSimilares em SciELO
  • Em processo de indexaçãoSimilares em Google

Compartilhar


Boletín de Geología

versão impressa ISSN 0120-0283versão On-line ISSN 2145-8553

Resumo

BENAVIDES-GUERRERO, Carlos Esteban; CARO-CARO, Linda Elizabeth  e  MARINO-MARTINEZ, Jorge Eliecer. Towards the elaboration of a hydrogeological model of the Guachiria river basin (Colombia). Bol. geol. [online]. 2022, vol.44, n.2, pp.161-182.  Epub 18-Jul-2022. ISSN 0120-0283.  https://doi.org/10.18273/revbol.v44n2-2022008.

In recent years, extreme climatic variations have generated obvious effects on natural resources, harming one of the most important: water. A clear example of this is the Guachiria River Basin, located in Colombia, the prolonged dry seasons of the last decade have harmed both the biota and the civilian population, since they depend mainly on this resource. The present study aims to increase the state of the art on hydrometeorological, hydraulic variables and, in general, to understand the hydrogeological conditions of the Guachiria River Basin, this with the purpose of providing information that serves as baseline for the elaboration of a conceptual hydrogeological model (CHM) that helps in decision-making by the entities in charge of water resource management. First, the morphometric and geological conditions of the area were determined, finding that there is a predominance of flat areas with little slope, made up of unconsolidated deposits, extensive flood zones and wind influence on fluvial deposits. Then, starting from a mass balance, a water balance was carried out in the basin to quantify the resource in the area; In turn, favorable recharge zones were identified in several sectors: one part towards the foothills in the area of high slopes and another towards the deposits with eolian influence, made up of sandy and sandy loam soils that overlie the Guayabo Formation. In addition, through pumping tests, different hydraulic parameters were determined, and the aquifers were classified as free, confined, and semi-confined, linked to the lithology of the area, due to their extension and lithological complexity. Finally, a hydrogeochemical sampling was carried out, where mostly relatively young waters, with little transport and high iron content were found.

Palavras-chave : Hydrogeology; Hydrology; Potential recharge; Hydrogeochemistry; Eastern plains; Orinoquia.

        · resumo em Espanhol     · texto em Espanhol     · Espanhol ( pdf )