SciELO - Scientific Electronic Library Online

 
vol.72 número4Interpretación estructural de una sección geológica en las nacientes del río San Juan, a partir de datos geológicos y validación geofísicaGeología del prospecto vicuña muerta: emplazamiento múltiple y control estructural de cuerpos subvolcánicos miocenos en el borde oriental de la Puna Austral, Salta índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

  • No hay articulos citadosCitado por SciELO

Links relacionados

  • No hay articulos similaresSimilares en SciELO

Compartir


Revista de la Asociación Geológica Argentina

versión impresa ISSN 0004-4822versión On-line ISSN 1851-8249

Resumen

BECHER QUINODOZ, Fátima Noelia; BLARASIN, Mónica. T  y  PANARELLO, Héctor O. Modelado geoquímico e isotópico de las relaciones agua superficial-subterránea en la planicie arenosa del sur de Córdoba. Rev. Asoc. Geol. Argent. [online]. 2015, vol.72, n.4, pp.506-518. ISSN 0004-4822.

The sandy plain of the south of Cordoba is a palimpsest resulting from an Aeolian System (“Pampean Sand Sea”) and the Quinto River system’s juxtaposition. The aim of this work is to carry out the dynamic and geochemical characterization (general and isotopic) of surface water-groundwater relationships, validating with a numerical model. The Quinto River, with headwaters in the San Luis Mountains, develops its middle basin in the study area, registering flow variations between winter and summer. The average surface water velocity is 0.8 m/s and the geochemical type is sodium sulfate. The unconfined aquifer presented variable hydraulic gradients, low water velocity (0.2 m/d) and a complex geochemical pattern (sodium bicarbonate, sulfate or chloride types). Considering the hydraulic connection between the two hydrological systems (a predominantly gaining river) a dominance of surface water in summer is detected. Thus, surface water dilutes by hydrodynamic dispersion the salts supplied by the aquifer, due to differences in water velocity in both hydrological systems. Isotopes results show that the river and the aquifer lay on an evaporation line with origin in the upper basin water isotope composition, which indicates provenance. The low slope of the line indicates river-aquifer mixing processes. Thus, in Cordoba Province, it was observed the prevalence of surface water in summer (72 %), including contribution from dams, while the base flow is dominant in winter (82 %). This basin constitutes a paradigmatic case of natural and anthropogenic constraints, whose functioning does not recognize political boundaries, indicating the usefulness of inter-jurisdictional studies.

Palabras clave : Unconfined aquifer; Quinto river; Geochemical modeling; Stable isotopes.

        · resumen en Español     · texto en Español     · Español ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons