1. Identification of palaeo-seawater intrusion in groundwater using minor ions in a semi-confined aquifer of the Río de la Plata littoral (Argentina)
- Author
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Eleonora Silvina Carol, Eduardo Emilio Kruse, and Lucía Santucci
- Subjects
Environmental Engineering ,Soil salinity ,Coastal plain ,PALAEO-SEAWATER INTRUSION ,0208 environmental biotechnology ,HYDROGEOCHEMISTRY ,Aquifer ,02 engineering and technology ,010501 environmental sciences ,01 natural sciences ,MIDDLE RÍO DE LA PLATA ESTUARY ,Ciencias de la Tierra y relacionadas con el Medio Ambiente ,Loess ,SALINIZATION ,Littoral zone ,Environmental Chemistry ,Waste Management and Disposal ,0105 earth and related environmental sciences ,Hydrology ,geography ,ARGENTINA ,geography.geographical_feature_category ,Estuary ,Pollution ,020801 environmental engineering ,Seawater ,Meteorología y Ciencias Atmosféricas ,Groundwater ,Geology ,CIENCIAS NATURALES Y EXACTAS - Abstract
The hydrochemistry of minor elements and traces such as bromide, lithium, strontium, uranium and selenium, together with the chemical analysis of major ions, has been used in the study of salinization process. This process occurs in a semi-confined aquifer that corresponds to a Pliocene–Pleistocene fluvial environment. The semi-confined aquifer is located in the littoral of the cities of Ensenada and Berisso, in the region of the middle Río de la Plata estuary, Argentina. Groundwater salinization was detected in the semi-confined aquifer in the coastal plain area, with salt contents that increase from the loess plain towards the river. The content of major ions that predominate in sea water (Cl−, Na+ and Mg2 +), as well as the Cl−/Br− and U vs. Cl− ratios, demonstrates that such salinization is related to sea water, which shows no correspondence with estuary water. In the salinized area, Li, Sr and Se enrichments occur, and are used as tracers of the average time that a substance remains in solution in sea water in the aquifer. The study of such minor ions together with the geological evolution of the area made it possible to recognize that the salt water in the semi-confined aquifer corresponds to a palaeo-intrusion of sea water associated with the Pleistocene–Holocene ingressions caused by the climate changes occurring during the Quaternary. Fil: Santucci, Lucía. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Carol, Eleonora Silvina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Kruse, Eduardo Emilio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Cátedra de Hidrología General; Argentina
- Published
- 2016