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Accurate identification of the origin of groundwater samples is not always possible in complex multilayered aquifers.
This work aims to investigate the origin of groundwater salinity and the major hydrogeochemical processes controlling the groundwater evolution in the confined basal aquifer of the PRD.
This study has significantly advanced our understanding of the origin of groundwater recharge in a semi-arid zone region of the Darling River catchment, Australia.
This study investigates the origin of groundwater from the Lower Cambrian carbonate aquifer of the Lakhssas Plateau in the Anti-Atlas Mountains of southwestern Morocco.
In order to investigate the origin of groundwater, its circulation patterns, and to understand the connectivity and compartmentalization of a karst system, a multi-tracer approach was used to describe the hydrogeology of the Lez karst system.
The transport of salts from land to sea (by erosion of rocks and surface runoff) and from sea to land (by evaporation, cloud formation, and precipitation), the age and origin of groundwater in desert regions, and the paleotemperature determinations based on isotope analyses of ice sheets and glaciers are a few examples.
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This serves as the basis for discussion on the possible origin of groundwaters in the Gushegu District.
Hence, there is the need for hydrochemical investigation to determine the quality of the groundwater in the study area, the possible sources of the ions as well as the origin of the groundwater.
Fresh groundwater stable isotope signatures (δ18O, δ2H) reflect local amount weighted rainfall signatures (δ18O: −3.8‰; δ2H: −15.1‰), and confirm rainfall as the origin of fresh groundwater (δ18O: −4.47 to −3.82‰; δ2H: −20.0 to −16.6‰).
The study aims to reveal the origin of the groundwater, salinity sources, and the residence time of the water.
This group indicates the meteoric origin of the groundwater.
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