Origins and processes of groundwater salinization in the urban coastal aquifers of Recife (Pernambuco, Brazil): a multi-isotope approach

Lise Cary (1) , Emmanuelle Petelet-Giraud (1) , Guillaume Bertrand (2) , Wolfram Kloppmann (1) , Luc Aquilina (3) , Veridiana Martins (2) , Ricardo Hirata (2) , Suzana Maria Gico Lima Montenegro (4) , Hélène Pauwels (1) , Eliot Chatton (3) , Melissa Franzen (5) , Axel Aurouet (6) , Eric Lasseur (1) , Géraldine Picot-Colbeaux (1) , Catherine Guerrot (1) , Christine Fléhoc (1) , Thierry Labasque (3) , Jeane Glaucia Santos (2) , Anderson Luiz Ribeiro Paiva (4) , Gilles Braibant (1) , Daniel Pierre (6)

1 BRGM - Bureau de Recherches Géologiques et Minières (BRGM)
2 USP - Universidade de São Paulo = University of São Paulo
3 GR - Géosciences Rennes
4 Departamento de Engenharia Civil
5 Brazilian Geological Survey - CPRM
6 Société GéoHyd

In the coastal multilayer aquifer system of a highly urbanized southern city (Recife, Brazil), where groundwaters are affected by salinization, a multi-isotope approach (Sr, B, O, H) was used to investigate the sources and processes of salinization. The high diversity of the geological bodies, built since the Atlantic opening during the Cretaceous, highly constrains the heterogeneity of the groundwater chemistry, e.g. Sr isotope ratios, and needs to be integrated to explain the salinization processes and groundwater pathways. A palaeoseawater intrusion, most probably the 120 ky B.P. Pleistocene marine transgression, and cationic exchange are clearly evidenced in the most salinized parts of the Cabo and Beberibe aquifers. All 87Sr/86Sr values are above the past and present-day seawater signatures, meaning that the Sr isotopic signature is altered due to additional Sr inputs from dilution with different freshwaters, and water-rock interactions. Only the Cabo aquifer presents a well-delimitated area of Na-HCO3 water typical of a freshening process. The two deep aquifers also display a broad range of B concentrations and B isotope ratios with values among the highest known to date (63-68.5‰). This suggests multiple sources and processes affecting B behaviour, among which mixing with saline water, B sorption on clays and mixing with wastewater. The highly fractionated B isotopic values were explained by infiltration of relatively salty water with B interacting with clays, pointing out the major role played by (palaeo)-channels for the deep Beberibe aquifer recharge. Based on an increase of salinity at end of the dry season, a present-day seawater intrusion is identified in the surficial Boa Viagem aquifer. Our conceptual model presents a comprehensive understanding of the major groundwater salinization pathways and processes, and should be of benefit for other southern Atlantic coastal aquifers to better address groundwater management issues.

Mots clés: Salinization origins; Salinization processes; Groundwater; Coastal aquifer; Strontium isotopes; Boron isotopes; Recife; Brazil

Domaines: Géochimie

Lise Cary, Emmanuelle Petelet-Giraud, Guillaume Bertrand, Wolfram Kloppmann, Luc Aquilina, et al.. Origins and processes of groundwater salinization in the urban coastal aquifers of Recife (Pernambuco, Brazil): a multi-isotope approach. Science of the Total Environment, 2015, 530-531, pp.411-429. ⟨10.1016/j.scitotenv.2015.05.015⟩. ⟨hal-01161949⟩