Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina
- Autores
- Álvarez, María del Pilar; Dapeña, Cristina; Bouza, Pablo J.; Ríos, Ileana; Hernández, Mario Alberto
- Año de publicación
- 2015
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The origin of the high salinity in the groundwater of a coastal wetland in an arid climate was studied in the Playa Fracasso marsh, located on the northwest coast of the extra-Andean Patagonia. Research was carried out by means of the design of a network of soil pits and short piezometers in the marsh and the surrounding landforms. Continuous fluctuations of the water table, in situ physical and chemical properties, major ions (Ca²⁺, Mg²⁺, Na⁺, K⁺, Cl⁻, SO₄²⁻, HCO₃⁻) and stable isotopes (¹⁸O and ²H) in groundwater, as well as soil salinity, were measured. The combined analysis of the hydrodynamics, the ion ratios rCa²⁺/rCl⁻ and rMg²⁺/rCa²⁺ vs. rCl⁻ and the isotopic composition made it possible to recognize an area within the high marsh in which the origin of groundwater is mainly marine and another in which the contributions are of mixed origin. By means of the analysis of rCl⁻ vs. δ¹⁸O, a salinization process with no change in isotopic composition was identified. Its interpretation, together with those of the soil salinity profiles and the records of the fluctuations in electrical conductivity associated with extraordinary tides, was used to define a conceptual model of salinization which could be useful to understand other coastal wetlands under similar arid climatic conditions. It consists in a cyclical mechanism of evapotranspiration, precipitation, dissolution and transport of salts during tides.
Facultad de Ciencias Naturales y Museo - Materia
-
Ciencias Naturales
Geohydrology
Hydrochemistry
Salt marsh
Patagonia
Arid climate - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/134737
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Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, ArgentinaÁlvarez, María del PilarDapeña, CristinaBouza, Pablo J.Ríos, IleanaHernández, Mario AlbertoCiencias NaturalesGeohydrologyHydrochemistrySalt marshPatagoniaArid climateThe origin of the high salinity in the groundwater of a coastal wetland in an arid climate was studied in the Playa Fracasso marsh, located on the northwest coast of the extra-Andean Patagonia. Research was carried out by means of the design of a network of soil pits and short piezometers in the marsh and the surrounding landforms. Continuous fluctuations of the water table, in situ physical and chemical properties, major ions (Ca²⁺, Mg²⁺, Na⁺, K⁺, Cl⁻, SO₄²⁻, HCO₃⁻) and stable isotopes (¹⁸O and ²H) in groundwater, as well as soil salinity, were measured. The combined analysis of the hydrodynamics, the ion ratios rCa²⁺/rCl⁻ and rMg²⁺/rCa²⁺ vs. rCl⁻ and the isotopic composition made it possible to recognize an area within the high marsh in which the origin of groundwater is mainly marine and another in which the contributions are of mixed origin. By means of the analysis of rCl⁻ vs. δ¹⁸O, a salinization process with no change in isotopic composition was identified. Its interpretation, together with those of the soil salinity profiles and the records of the fluctuations in electrical conductivity associated with extraordinary tides, was used to define a conceptual model of salinization which could be useful to understand other coastal wetlands under similar arid climatic conditions. It consists in a cyclical mechanism of evapotranspiration, precipitation, dissolution and transport of salts during tides.Facultad de Ciencias Naturales y Museo2015-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf7983-7994http://sedici.unlp.edu.ar/handle/10915/134737enginfo:eu-repo/semantics/altIdentifier/issn/1866-6280info:eu-repo/semantics/altIdentifier/issn/1866-6299info:eu-repo/semantics/altIdentifier/doi/10.1007/s12665-014-3957-3info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:31:57Zoai:sedici.unlp.edu.ar:10915/134737Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:31:57.253SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
title |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
spellingShingle |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina Álvarez, María del Pilar Ciencias Naturales Geohydrology Hydrochemistry Salt marsh Patagonia Arid climate |
title_short |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
title_full |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
title_fullStr |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
title_full_unstemmed |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
title_sort |
Groundwater salinization in arid coastal wetlands: a study case from Playa Fracasso, Patagonia, Argentina |
dc.creator.none.fl_str_mv |
Álvarez, María del Pilar Dapeña, Cristina Bouza, Pablo J. Ríos, Ileana Hernández, Mario Alberto |
author |
Álvarez, María del Pilar |
author_facet |
Álvarez, María del Pilar Dapeña, Cristina Bouza, Pablo J. Ríos, Ileana Hernández, Mario Alberto |
author_role |
author |
author2 |
Dapeña, Cristina Bouza, Pablo J. Ríos, Ileana Hernández, Mario Alberto |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales Geohydrology Hydrochemistry Salt marsh Patagonia Arid climate |
topic |
Ciencias Naturales Geohydrology Hydrochemistry Salt marsh Patagonia Arid climate |
dc.description.none.fl_txt_mv |
The origin of the high salinity in the groundwater of a coastal wetland in an arid climate was studied in the Playa Fracasso marsh, located on the northwest coast of the extra-Andean Patagonia. Research was carried out by means of the design of a network of soil pits and short piezometers in the marsh and the surrounding landforms. Continuous fluctuations of the water table, in situ physical and chemical properties, major ions (Ca²⁺, Mg²⁺, Na⁺, K⁺, Cl⁻, SO₄²⁻, HCO₃⁻) and stable isotopes (¹⁸O and ²H) in groundwater, as well as soil salinity, were measured. The combined analysis of the hydrodynamics, the ion ratios rCa²⁺/rCl⁻ and rMg²⁺/rCa²⁺ vs. rCl⁻ and the isotopic composition made it possible to recognize an area within the high marsh in which the origin of groundwater is mainly marine and another in which the contributions are of mixed origin. By means of the analysis of rCl⁻ vs. δ¹⁸O, a salinization process with no change in isotopic composition was identified. Its interpretation, together with those of the soil salinity profiles and the records of the fluctuations in electrical conductivity associated with extraordinary tides, was used to define a conceptual model of salinization which could be useful to understand other coastal wetlands under similar arid climatic conditions. It consists in a cyclical mechanism of evapotranspiration, precipitation, dissolution and transport of salts during tides. Facultad de Ciencias Naturales y Museo |
description |
The origin of the high salinity in the groundwater of a coastal wetland in an arid climate was studied in the Playa Fracasso marsh, located on the northwest coast of the extra-Andean Patagonia. Research was carried out by means of the design of a network of soil pits and short piezometers in the marsh and the surrounding landforms. Continuous fluctuations of the water table, in situ physical and chemical properties, major ions (Ca²⁺, Mg²⁺, Na⁺, K⁺, Cl⁻, SO₄²⁻, HCO₃⁻) and stable isotopes (¹⁸O and ²H) in groundwater, as well as soil salinity, were measured. The combined analysis of the hydrodynamics, the ion ratios rCa²⁺/rCl⁻ and rMg²⁺/rCa²⁺ vs. rCl⁻ and the isotopic composition made it possible to recognize an area within the high marsh in which the origin of groundwater is mainly marine and another in which the contributions are of mixed origin. By means of the analysis of rCl⁻ vs. δ¹⁸O, a salinization process with no change in isotopic composition was identified. Its interpretation, together with those of the soil salinity profiles and the records of the fluctuations in electrical conductivity associated with extraordinary tides, was used to define a conceptual model of salinization which could be useful to understand other coastal wetlands under similar arid climatic conditions. It consists in a cyclical mechanism of evapotranspiration, precipitation, dissolution and transport of salts during tides. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-06 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://sedici.unlp.edu.ar/handle/10915/134737 |
url |
http://sedici.unlp.edu.ar/handle/10915/134737 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
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info:eu-repo/semantics/altIdentifier/issn/1866-6280 info:eu-repo/semantics/altIdentifier/issn/1866-6299 info:eu-repo/semantics/altIdentifier/doi/10.1007/s12665-014-3957-3 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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openAccess |
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http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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