Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach

The Tordera Desalination Plant located in Blanes (NE Spain) has seawater intake through 10 beach wells located a few meters inland on the shoreline at the Tordera River Delta. Between October 2002 and October 2003, the extracted groundwater showed a decrease in conductivity, especially in the wells...

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Autores: Otero Pérez, Neus, Soler i Gil, Albert, Corp, R.M., Mas-Pla, Josep, Garcia Solsona, E., Masqué, P.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2011
País:España
Institución:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repositorio:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:10256/12931
Acceso en línea:http://hdl.handle.net/10256/12931
Access Level:acceso embargado
Palabra clave:Aigua salada -- Dessalatge
Saline water conversion
Aigua -- Química
Water chemistry
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spelling Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approachOtero Pérez, NeusSoler i Gil, AlbertCorp, R.M.Mas-Pla, JosepGarcia Solsona, E.Masqué, P.Aigua salada -- DessalatgeSaline water conversionAigua -- QuímicaWater chemistryThe Tordera Desalination Plant located in Blanes (NE Spain) has seawater intake through 10 beach wells located a few meters inland on the shoreline at the Tordera River Delta. Between October 2002 and October 2003, the extracted groundwater showed a decrease in conductivity, especially in the wells located in the northern area, prompting the present study. A multi-isotopic approach (δD, δ18OH2O, 3H, δ34SSO4, 87Sr/86Sr and 228Ra/226Ra) coupled with chemical data was applied in order to assess the origin of the water collected for the desalination plant and to quantify the extent of freshwater collection from the Tordera aquifer, when applicable. Three multi-piezometers located in the Tordera aquifer were also sampled in order to characterize the freshwater end-member. A seasonal survey was performed in order to assess the evolution of mixed freshwater-seawater intake. Tritium isotopes showed values ranging from 0.6 to 2.5TU indicating recent origin of the collected waters. This was further confirmed using radium isotopes (226Ra and 228Ra), as the 228Ra/226Ra activity ratio (AR) indicated a continuous input of seawater on a yearly time scale. The water extracted from the beach wells was at least 95% seawater, except for wells 8-10. The latter two were extracting up to 15% of freshwater from the Tordera aquifer system. From a methodological point of view, while δ34S of dissolved sulphate and the ratio 87Sr/86Sr are good tracers of seawater mixing with freshwaters, the isotopic composition of water (δD and δ18OH2O) and the Cl-/Br- ratio are conservative tracers that allow for quantifying the contribution of freshwater to the extracted water. Although slight variations linked to seasonality were observed in all wells during the 3-year study period (November 2003 to December 2006), wells 1 and 7 showed an increase in freshwater contribution from 4% to 11% and well 10 a decrease from 15% to 10% over this periodThis study was funded by the Catalan Water Agency (Agència Catalana de l’Aigua), CICYT projects CGL-2008-06373-CO3-01/03-BTE from the Spanish Government, project 2009 SGR 103 from the Catalan Government, and the I3P Programme funded by the EUElsevierMinisterio de Educación y Ciencia (Espanya)infoinfo2011info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/10256/12931http://hdl.handle.net/10256/12931© Journal of Hydrology, 2011, vol. 397, núm. 1-2, p. 37-46Articles publicats (D-CCAA)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)Inglésinfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jhydrol.2010.11.020info:eu-repo/semantics/altIdentifier/issn/0022-1694info:eu-repo/grantAgreement/MICINN//CGL2008-06373-C03-03Tots els drets reservatsinfo:eu-repo/semantics/embargoedAccessoai:recercat.cat:10256/129312026-05-29T05:05:01Z
dc.title.none.fl_str_mv Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
title Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
spellingShingle Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
Otero Pérez, Neus
Aigua salada -- Dessalatge
Saline water conversion
Aigua -- Química
Water chemistry
title_short Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
title_full Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
title_fullStr Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
title_full_unstemmed Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
title_sort Origin and evolution of groundwater collected by a desalination plant (Tordera, Spain): A multi-isotopic approach
dc.creator.none.fl_str_mv Otero Pérez, Neus
Soler i Gil, Albert
Corp, R.M.
Mas-Pla, Josep
Garcia Solsona, E.
Masqué, P.
author Otero Pérez, Neus
author_facet Otero Pérez, Neus
Soler i Gil, Albert
Corp, R.M.
Mas-Pla, Josep
Garcia Solsona, E.
Masqué, P.
author_role author
author2 Soler i Gil, Albert
Corp, R.M.
Mas-Pla, Josep
Garcia Solsona, E.
Masqué, P.
author2_role author
author
author
author
author
dc.contributor.none.fl_str_mv Ministerio de Educación y Ciencia (Espanya)
dc.subject.none.fl_str_mv Aigua salada -- Dessalatge
Saline water conversion
Aigua -- Química
Water chemistry
topic Aigua salada -- Dessalatge
Saline water conversion
Aigua -- Química
Water chemistry
description The Tordera Desalination Plant located in Blanes (NE Spain) has seawater intake through 10 beach wells located a few meters inland on the shoreline at the Tordera River Delta. Between October 2002 and October 2003, the extracted groundwater showed a decrease in conductivity, especially in the wells located in the northern area, prompting the present study. A multi-isotopic approach (δD, δ18OH2O, 3H, δ34SSO4, 87Sr/86Sr and 228Ra/226Ra) coupled with chemical data was applied in order to assess the origin of the water collected for the desalination plant and to quantify the extent of freshwater collection from the Tordera aquifer, when applicable. Three multi-piezometers located in the Tordera aquifer were also sampled in order to characterize the freshwater end-member. A seasonal survey was performed in order to assess the evolution of mixed freshwater-seawater intake. Tritium isotopes showed values ranging from 0.6 to 2.5TU indicating recent origin of the collected waters. This was further confirmed using radium isotopes (226Ra and 228Ra), as the 228Ra/226Ra activity ratio (AR) indicated a continuous input of seawater on a yearly time scale. The water extracted from the beach wells was at least 95% seawater, except for wells 8-10. The latter two were extracting up to 15% of freshwater from the Tordera aquifer system. From a methodological point of view, while δ34S of dissolved sulphate and the ratio 87Sr/86Sr are good tracers of seawater mixing with freshwaters, the isotopic composition of water (δD and δ18OH2O) and the Cl-/Br- ratio are conservative tracers that allow for quantifying the contribution of freshwater to the extracted water. Although slight variations linked to seasonality were observed in all wells during the 3-year study period (November 2003 to December 2006), wells 1 and 7 showed an increase in freshwater contribution from 4% to 11% and well 10 a decrease from 15% to 10% over this period
publishDate 2011
dc.date.none.fl_str_mv 2011
info
info
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
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dc.identifier.none.fl_str_mv http://hdl.handle.net/10256/12931
http://hdl.handle.net/10256/12931
url http://hdl.handle.net/10256/12931
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jhydrol.2010.11.020
info:eu-repo/semantics/altIdentifier/issn/0022-1694
info:eu-repo/grantAgreement/MICINN//CGL2008-06373-C03-03
dc.rights.none.fl_str_mv Tots els drets reservats
info:eu-repo/semantics/embargoedAccess
rights_invalid_str_mv Tots els drets reservats
eu_rights_str_mv embargoedAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv © Journal of Hydrology, 2011, vol. 397, núm. 1-2, p. 37-46
Articles publicats (D-CCAA)
reponame:Recercat. Dipósit de la Recerca de Catalunya
instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
reponame_str Recercat. Dipósit de la Recerca de Catalunya
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