Assessing interactions between groundwater and surface water in a Pampean stream
In the south of Córdoba (Argentina), groundwater from the unconfined aquifer, presents scarce suitability due to high values of salts, sulfates, arsenic and fluorides. This situation makes it necessary to explore other possibilities, for example, conjunctive use of groundwater and surface water. The...
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2017
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_19989563_v48_n4_p1045_BecherQuinodoz http://hdl.handle.net/20.500.12110/paper_19989563_v48_n4_p1045_BecherQuinodoz |
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paper:paper_19989563_v48_n4_p1045_BecherQuinodoz2023-06-08T16:32:54Z Assessing interactions between groundwater and surface water in a Pampean stream Geochemical modeling Groundwater Radon Stable isotope Surface water Aquifers Carbonates Geochemistry Groundwater Groundwater resources Isotopes Mixing Numerical models Radon Rivers Sodium bicarbonate Stream flow Surface waters Activity results Conceptual model Conjunctive use Geochemical modeling Groundwater supply Stable isotopes Surface water and groundwaters Unconfined aquifers Hydrochemistry bicarbonate chemical composition conceptual framework groundwater groundwater-surface water interaction hydrogeochemistry hydrological modeling inorganic compound mixing numerical model radon river basin salt sodium chloride stable isotope stream surface water unconfined aquifer Aji Basin Argentina Cordoba [Argentina] East Azerbaijan Iran Pampas In the south of Córdoba (Argentina), groundwater from the unconfined aquifer, presents scarce suitability due to high values of salts, sulfates, arsenic and fluorides. This situation makes it necessary to explore other possibilities, for example, conjunctive use of groundwater and surface water. The objective of this work was to describe the dynamic and geochemical relationships between surface water and groundwater in the medium-low basin of the Ají stream. The conceptual model was supported by the use of stable 18O/16O and 2H/1H isotopes and it was validated through numerical modeling and 222Rn activity results. The stream water is sodium bicarbonate fresh type (460-1, 400 μS/cm). The aquifer presents fresh to salt water (720-14, 000 μS/cm), from sodium bicarbonate to sodium chloride type. The isotopic results show that there is a straight mixing line between surface water and groundwater samples. The geochemical numerical modeling revealed that in the mixing models between stream and aquifer, for hydraulically linked samples, the aquifer only provides 2% of the total stream flow. This was validated through 222Rn results, which led us to the estimation of about 2% of groundwater supply in summer. © IWA Publishing 2017. 2017 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_19989563_v48_n4_p1045_BecherQuinodoz http://hdl.handle.net/20.500.12110/paper_19989563_v48_n4_p1045_BecherQuinodoz |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
Geochemical modeling Groundwater Radon Stable isotope Surface water Aquifers Carbonates Geochemistry Groundwater Groundwater resources Isotopes Mixing Numerical models Radon Rivers Sodium bicarbonate Stream flow Surface waters Activity results Conceptual model Conjunctive use Geochemical modeling Groundwater supply Stable isotopes Surface water and groundwaters Unconfined aquifers Hydrochemistry bicarbonate chemical composition conceptual framework groundwater groundwater-surface water interaction hydrogeochemistry hydrological modeling inorganic compound mixing numerical model radon river basin salt sodium chloride stable isotope stream surface water unconfined aquifer Aji Basin Argentina Cordoba [Argentina] East Azerbaijan Iran Pampas |
| spellingShingle |
Geochemical modeling Groundwater Radon Stable isotope Surface water Aquifers Carbonates Geochemistry Groundwater Groundwater resources Isotopes Mixing Numerical models Radon Rivers Sodium bicarbonate Stream flow Surface waters Activity results Conceptual model Conjunctive use Geochemical modeling Groundwater supply Stable isotopes Surface water and groundwaters Unconfined aquifers Hydrochemistry bicarbonate chemical composition conceptual framework groundwater groundwater-surface water interaction hydrogeochemistry hydrological modeling inorganic compound mixing numerical model radon river basin salt sodium chloride stable isotope stream surface water unconfined aquifer Aji Basin Argentina Cordoba [Argentina] East Azerbaijan Iran Pampas Assessing interactions between groundwater and surface water in a Pampean stream |
| topic_facet |
Geochemical modeling Groundwater Radon Stable isotope Surface water Aquifers Carbonates Geochemistry Groundwater Groundwater resources Isotopes Mixing Numerical models Radon Rivers Sodium bicarbonate Stream flow Surface waters Activity results Conceptual model Conjunctive use Geochemical modeling Groundwater supply Stable isotopes Surface water and groundwaters Unconfined aquifers Hydrochemistry bicarbonate chemical composition conceptual framework groundwater groundwater-surface water interaction hydrogeochemistry hydrological modeling inorganic compound mixing numerical model radon river basin salt sodium chloride stable isotope stream surface water unconfined aquifer Aji Basin Argentina Cordoba [Argentina] East Azerbaijan Iran Pampas |
| description |
In the south of Córdoba (Argentina), groundwater from the unconfined aquifer, presents scarce suitability due to high values of salts, sulfates, arsenic and fluorides. This situation makes it necessary to explore other possibilities, for example, conjunctive use of groundwater and surface water. The objective of this work was to describe the dynamic and geochemical relationships between surface water and groundwater in the medium-low basin of the Ají stream. The conceptual model was supported by the use of stable 18O/16O and 2H/1H isotopes and it was validated through numerical modeling and 222Rn activity results. The stream water is sodium bicarbonate fresh type (460-1, 400 μS/cm). The aquifer presents fresh to salt water (720-14, 000 μS/cm), from sodium bicarbonate to sodium chloride type. The isotopic results show that there is a straight mixing line between surface water and groundwater samples. The geochemical numerical modeling revealed that in the mixing models between stream and aquifer, for hydraulically linked samples, the aquifer only provides 2% of the total stream flow. This was validated through 222Rn results, which led us to the estimation of about 2% of groundwater supply in summer. © IWA Publishing 2017. |
| title |
Assessing interactions between groundwater and surface water in a Pampean stream |
| title_short |
Assessing interactions between groundwater and surface water in a Pampean stream |
| title_full |
Assessing interactions between groundwater and surface water in a Pampean stream |
| title_fullStr |
Assessing interactions between groundwater and surface water in a Pampean stream |
| title_full_unstemmed |
Assessing interactions between groundwater and surface water in a Pampean stream |
| title_sort |
assessing interactions between groundwater and surface water in a pampean stream |
| publishDate |
2017 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_19989563_v48_n4_p1045_BecherQuinodoz http://hdl.handle.net/20.500.12110/paper_19989563_v48_n4_p1045_BecherQuinodoz |
| _version_ |
1768546229887696896 |