Hydrogeochemical features and groundwater renewal rate estimates from deep aquifers in the Pampean Plain, Córdoba Province, Argentina.

Abstract

In the Córdoba Province (Argentina), people use groundwater from confined aquifers systems (CAS) for different activities (irrigation, livestock, etc.). Therefore, comprehensive studies for a more sustainable use of these resources are necessary. The aim of this study is to assess the geochemistry, the water flow dynamic and the renewal rates of groundwater in the CAS of the Pampean plain of Córdoba. The CAS evaluated in this study are composed of two multilayered subsystems (A1 CAS and A2 CAS) of variable extent formed by thin (3–8 m) sandpebble lenses. The subsystems are associated with Neogene fluvial palaeosystems. These layers are situated at different depths (120–400 m) and are interbedded with thick clay strata, which generate different confinement grades. Groundwater is fresh and of good quality (EC < 2.000 μS/cm) because the geochemical processes that allow the transference of ions into solution are diminished by the grain size (sand and gravel) and the aquifer sediment mineralogy (quartz prevailing). A2 CAS has the best water and higher hydraulic conductivity resulting from coarser textures. The main geochemical processes that influence CAS groundwater composition are silicate weathering, carbonate dissolution, cation exchange and atmospheric input. The interpretations made from geochemistry, isotopes (2 H,18O,3 H and 14C) and hydraulic results, demonstrate that these systems are recharged in the piedmont areas and have groundwater ages from hundreds to thousands of years, that is, groundwater recharged during the Holocene. Even though the CAS are currently used for irrigation, no significant decreases are observed in groundwater levels. This situation would indicate that these systems are not yet being overexploited.