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- W4386323336 abstract "Shallow crystalline groundwater of semi-arid hinterland of Ceará exhibits brackish or saline water with mixed-chloride or sodium-chloride facies. Very few hydrochemical data are available in the area and the drivers behind this salinity are not clearly identified. In this study, an extensive field data collection work was performed to provide new information about the hydrogeological functioning and the salinization processes, through the implementation of piezometric, hydrogeochemical, isotopic (18O, 2H) and multi-tracer dating (14C, 3H, CFC, SF6) monitoring. Piezometric and isotopic data evidence fast flow circulation processes and a high contribution of evaporated surface water to aquifer recharge. Multi-tracer dating shows that groundwater is essentially composed of seasonal vertical infiltration flows that mix with older waters stored in the aquifer. Chemical analyses suggest that groundwater, originally low mineralized, has become progressively saltier due to leaching of salts that were evapoconcentrated either in surface waters or the unsaturated zone during drier periods." @default.
- W4386323336 created "2023-09-01" @default.
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- W4386323336 date "2023-08-31" @default.
- W4386323336 modified "2023-09-29" @default.
- W4386323336 title "Explaining the groundwater salinity of hard-rock aquifers in semi-arid hinterlands using a multidisciplinary approach" @default.
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- W4386323336 doi "https://doi.org/10.1080/02626667.2023.2253227" @default.
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