A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge

Coastal aquifers are affected by seawater intrusion (SWI), which causes their salinization, and yield submarine groundwater discharge (SGD), which feeds marine ecosystems. Characterizing groundwater dynamics in coastal aquifers is fundamental for understanding both processes and their interaction. I...

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Autores: Martínez-Pérez, Laura, Luquot, Linda, Carrera, Jesús, Marazuela, Miguel Ángel, Goyetche, Tybaud, Pool, María, Palacios, Andrea, Bellmunt, Fabian, Ledo, Juanjo, Ferrer, Nuria, del Val, Laura, Pezard, Philippe A., García-Orellana, Jordi, Diego-Feliu, Marc, Rodellas, Valentí, Saaltink, Maarten W., Vázquez-Suñé, Enric, Folch, Albert
Formato: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2022
País:España
Recursos:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/306744
Acesso em linha:http://hdl.handle.net/10261/306744
https://api.elsevier.com/content/abstract/scopus_id/85124197418
Access Level:acceso abierto
Palavra-chave:Hydrogeochemistry
Borehole geophysics
Coastal alluvial aquifer
Conceptual model
Geological heterogeneity
http://metadata.un.org/sdg/6
Ensure availability and sustainable management of water and sanitation for all
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repository_id_str
dc.title.none.fl_str_mv A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
title A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
spellingShingle A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
Martínez-Pérez, Laura
Hydrogeochemistry
Borehole geophysics
Coastal alluvial aquifer
Conceptual model
Geological heterogeneity
http://metadata.un.org/sdg/6
Ensure availability and sustainable management of water and sanitation for all
title_short A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
title_full A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
title_fullStr A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
title_full_unstemmed A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
title_sort A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater discharge
dc.creator.none.fl_str_mv Martínez-Pérez, Laura
Luquot, Linda
Carrera, Jesús
Marazuela, Miguel Ángel
Goyetche, Tybaud
Pool, María
Palacios, Andrea
Bellmunt, Fabian
Ledo, Juanjo
Ferrer, Nuria
del Val, Laura
Pezard, Philippe A.
García-Orellana, Jordi
Diego-Feliu, Marc
Rodellas, Valentí
Saaltink, Maarten W.
Vázquez-Suñé, Enric
Folch, Albert
author Martínez-Pérez, Laura
author_facet Martínez-Pérez, Laura
Luquot, Linda
Carrera, Jesús
Marazuela, Miguel Ángel
Goyetche, Tybaud
Pool, María
Palacios, Andrea
Bellmunt, Fabian
Ledo, Juanjo
Ferrer, Nuria
del Val, Laura
Pezard, Philippe A.
García-Orellana, Jordi
Diego-Feliu, Marc
Rodellas, Valentí
Saaltink, Maarten W.
Vázquez-Suñé, Enric
Folch, Albert
author_role author
author2 Luquot, Linda
Carrera, Jesús
Marazuela, Miguel Ángel
Goyetche, Tybaud
Pool, María
Palacios, Andrea
Bellmunt, Fabian
Ledo, Juanjo
Ferrer, Nuria
del Val, Laura
Pezard, Philippe A.
García-Orellana, Jordi
Diego-Feliu, Marc
Rodellas, Valentí
Saaltink, Maarten W.
Vázquez-Suñé, Enric
Folch, Albert
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv Hydrogeochemistry
Borehole geophysics
Coastal alluvial aquifer
Conceptual model
Geological heterogeneity
http://metadata.un.org/sdg/6
Ensure availability and sustainable management of water and sanitation for all
topic Hydrogeochemistry
Borehole geophysics
Coastal alluvial aquifer
Conceptual model
Geological heterogeneity
http://metadata.un.org/sdg/6
Ensure availability and sustainable management of water and sanitation for all
description Coastal aquifers are affected by seawater intrusion (SWI), which causes their salinization, and yield submarine groundwater discharge (SGD), which feeds marine ecosystems. Characterizing groundwater dynamics in coastal aquifers is fundamental for understanding both processes and their interaction. In order to gain insights into SWI and SGD, we developed a 100 m-scale experimental field site located in a coastal alluvial aquifer at the mouth of an ephemeral stream on the Maresme coastline (Barcelona, Spain). Given the complexity of coastal aquifers and the dynamism of the processes occurring therein, understanding of the coupled processes can be achieved by combining methods and approaches across different hydrogeological disciplines. In this study, we conduct a detailed aquifer characterization based on the four pillars of hydrogeology: geology (lithological description and core samples analyses), geophysics (downhole and cross-hole measurements), hydraulics (pumping and tidal response tests) and hydrochemistry (major and minor elements, together with stable and Ra isotopes). Each discipline contributed to the characterization of the aquifer: (1) geological characterization revealed that the aquifer consists of fluvial sediments, organized in fining upwards sequences with alternating layers of gravel, sand and silt; (2) geophysics helped in identifying silt layers and their continuity, which play a segmenting role in the aquifer hydrodynamics; (3) hydraulics tests, specifically tidal response tests, evidenced that tidal loading, rather than hydraulic connection to the sea, drives the tidal response; and (4) hydrochemistry revealed a surprising high reactivity, as most ions reflect some reaction, beyond the expected cation exchange. The summary is that the aquifer, which initially looked like a homogeneous unconfined aquifer 22 m thick, effectively behaves as a multi-aquifer and reactive system with freshwater discharging beneath saltwater at several depths. The fact that thin silt layers caused such a significant impact opens new paths beyond this study both for coastal aquifer management (the possibility of transient pumping for freshwater resources) and marine ecology (expect diffuse groundwater discharge).
publishDate 2022
dc.date.none.fl_str_mv 2022
2023
2023
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Postprint
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/306744
https://api.elsevier.com/content/abstract/scopus_id/85124197418
url http://hdl.handle.net/10261/306744
https://api.elsevier.com/content/abstract/scopus_id/85124197418
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Journal of Hydrology
https://doi.org/10.1016/j.jhydrol.2022.127510

dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
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spelling A multidisciplinary approach to characterizing coastal alluvial aquifers to improve understanding of seawater intrusion and submarine groundwater dischargeMartínez-Pérez, LauraLuquot, LindaCarrera, JesúsMarazuela, Miguel ÁngelGoyetche, TybaudPool, MaríaPalacios, AndreaBellmunt, FabianLedo, JuanjoFerrer, Nuriadel Val, LauraPezard, Philippe A.García-Orellana, JordiDiego-Feliu, MarcRodellas, ValentíSaaltink, Maarten W.Vázquez-Suñé, EnricFolch, AlbertHydrogeochemistryBorehole geophysicsCoastal alluvial aquiferConceptual modelGeological heterogeneityhttp://metadata.un.org/sdg/6Ensure availability and sustainable management of water and sanitation for allCoastal aquifers are affected by seawater intrusion (SWI), which causes their salinization, and yield submarine groundwater discharge (SGD), which feeds marine ecosystems. Characterizing groundwater dynamics in coastal aquifers is fundamental for understanding both processes and their interaction. In order to gain insights into SWI and SGD, we developed a 100 m-scale experimental field site located in a coastal alluvial aquifer at the mouth of an ephemeral stream on the Maresme coastline (Barcelona, Spain). Given the complexity of coastal aquifers and the dynamism of the processes occurring therein, understanding of the coupled processes can be achieved by combining methods and approaches across different hydrogeological disciplines. In this study, we conduct a detailed aquifer characterization based on the four pillars of hydrogeology: geology (lithological description and core samples analyses), geophysics (downhole and cross-hole measurements), hydraulics (pumping and tidal response tests) and hydrochemistry (major and minor elements, together with stable and Ra isotopes). Each discipline contributed to the characterization of the aquifer: (1) geological characterization revealed that the aquifer consists of fluvial sediments, organized in fining upwards sequences with alternating layers of gravel, sand and silt; (2) geophysics helped in identifying silt layers and their continuity, which play a segmenting role in the aquifer hydrodynamics; (3) hydraulics tests, specifically tidal response tests, evidenced that tidal loading, rather than hydraulic connection to the sea, drives the tidal response; and (4) hydrochemistry revealed a surprising high reactivity, as most ions reflect some reaction, beyond the expected cation exchange. The summary is that the aquifer, which initially looked like a homogeneous unconfined aquifer 22 m thick, effectively behaves as a multi-aquifer and reactive system with freshwater discharging beneath saltwater at several depths. The fact that thin silt layers caused such a significant impact opens new paths beyond this study both for coastal aquifer management (the possibility of transient pumping for freshwater resources) and marine ecology (expect diffuse groundwater discharge).We acknowledge the contribution of all the members of the MEDISTRAES I, II and III project, from the Groundwater Hydrology Group of the Technical University of Catalonia (UPC) and the Spanish National Research Council (CSIC), the Autonomous University of Barcelona (UAB), the University of Barcelona (UB), the Geosciences Montpellier Laboratory, CNRS and the University of Rennes, for their support during experimental laboratory tests, the Argentona site creation, the setup of the electrodes during boreholes installation and for ensuring site maintenance. The final manuscript was significantly improved by critical, but constructive comments by two anonymous reviewers. This work was funded by the project PID2019-110212RB-C21, CGL2016-77122-C2-1-R/2-R and PID2019-110311RB-C22 of the Spanish Government and the project TerraMar (grant no. ACA210/18/00007) of the Catalan Water Agency. We would like to thank SIMMAR (Serveis Integrals de Manteniment del Maresme) and the Consell Comarcal del Maresme in the construction of the research site. This study contributes to the work carried out by the GHS (2017 SGR 1485) and MERS research group (2017 SGR 1588) for additional funding. M. Diego-Feliu acknowledges the economic support from the FI-2017 fellowships of the Generalitat de Catalunya autonomous government (2017FI_B_00365). V. Rodellas acknowledges financial support from the Beatriu de Pinós postdoctoral program of the Generalitat de Catalunya autonomous government (2019-BP-00241) The co-author Albert Folch is a Serra Húnter Fellow.Peer reviewedElsevierConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202320232022info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/306744https://api.elsevier.com/content/abstract/scopus_id/85124197418reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésJournal of Hydrologyhttps://doi.org/10.1016/j.jhydrol.2022.127510Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3067442026-05-22T06:33:51Z
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