Articles | Volume 385
https://doi.org/10.5194/piahs-385-393-2024
https://doi.org/10.5194/piahs-385-393-2024
Post-conference publication
 | 
19 Apr 2024
Post-conference publication |  | 19 Apr 2024

Multidisciplinary approach to understand the salinization of fractured crystalline aquifers in semi-arid region

Marjorie Beate Kreis, Jean-Denis Taupin, Nicolas Patris, Patrick Lachassagne, Virginie Vergnaud-Ayraud, Julien Daniel Pierre Burte, Christian Leduc, and Eduardo Sávio Passos Rodrigues Martins

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Isotopic signature of precipitation in the semi-arid region of Ceará, Northeastern Brazil
Marjorie B. Kreis, Jean-Denis Taupin, Nicolas Patris, and Eduardo S. P. R. Martins
Proc. IAHS, 385, 17–23, https://doi.org/10.5194/piahs-385-17-2024,https://doi.org/10.5194/piahs-385-17-2024, 2024
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Cited articles

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Araújo, A.: Mecanismos dominantes na salinização de água em rochas anisotrópicas com base em razões iônicas e número fuzzy, em área do sertão central no Ceará, PhD Thesis, Federal university of Ceará, 188 pp., http://repositorio.ufc.br/handle/riufc/53426, 2017. 
Burte, J.: Os pequenos aquiferos aluviais nas areas cristalinas semi-aridas: Funcionamento e estrategias de gestao, Estudo de caso no Nordeste brasileiro, PhD Thesis, University of Montpellier, https://agritrop.cirad.fr/547686/ (last access: 28 September 2023), 2008. 
Cavalcanti, J. A. D. and Cavalcante, J. C.: Evoluição geológica, in: Geodiversidade do estado do Ceará, CPRM, 19–34, https://rigeo.sgb.gov.br/handle/doc/16726, 2014. 
Chatton E., Aquilina L., Petelet-Giraud E., Cary, L., Bertrand, G., Labasque, T., Hirata, R., Martins, V., Montenegro, S., Vergnaud, V., Aurouet, A., and Kloppmann, W.: Glacial recharge, salinization and anthropogenic contamination in the coastal aquifers of Recife (Brazil), Sci. Total Environ., 569, 1114–1125, https://doi.org/10.1016/j.scitotenv.2016.06.180, 2016. 
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Short summary
This study used hydrodynamic and hydrogeochemical data to understand the salinization processes of the crystalline groundwater (GW) in Ceará, Brazil. Results demonstrate that GW is generally recent and recharged by meteoric waters mainly through localized infiltration. The study suggests that GW, originally bicarbonated, becomes progressively enriched in chloride due to the dissolution and leaching of salts that have precipitated in the unsaturated zone and pond sediments during dryer periods.