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Accueil du site → Doctorat → États-Unis → 2003 → Geochemical and isotopic characterization of shallow basinal brines from the Makgadikgadi Pans complex, northeastern Botswana : Determination of the sources of salinity

Western Michigan University (2003)

Geochemical and isotopic characterization of shallow basinal brines from the Makgadikgadi Pans complex, northeastern Botswana : Determination of the sources of salinity

Molwalefhe, Loago N

Titre : Geochemical and isotopic characterization of shallow basinal brines from the Makgadikgadi Pans complex, northeastern Botswana : Determination of the sources of salinity

Auteur : Molwalefhe, Loago N

Université de soutenance : Western Michigan University

Grade : Doctor of Philosophy (PhD) 2003

Résumé
Isotopes and chemical tracers have been used to constrain the sources and causes of salinity in shallow groundwater brine from the Makgadikgadi Basin, northeastern Botswana. The brine is massively rich in chloride and sodium, and moderately rich in carbonates, sulphate and potassium, and is distinctively poor in divalent cationic species. Various models that have been advanced to explain the origin of the brines include evaporative enrichment at the surface and density-induced infiltration, dissolution of evaporites, and trapped connate water. This study presents the compositional variability and behaviors of the stable isotopes of carbon (δ13 C) and oxygen (δ 18 O), dissolved inorganic carbon (DIC) content, chloride, bromide and sodium in the brine from the northern part of Sua Pan, one of the Makgadikgadi Pans Complex. DIC concentrations in the brine reach 5 grams of carbon per liter and δ13 CDIC compositions average -1.6 ± 0.2[per thousand]. The values are compatible with dissolution and accumulation of carbon dioxide of geothermal origin. The halogen content of the brine (Cl/Br ratio) is consistent with studies of fluid-inclusion brines from magmatic rocks, and suggests significant magmatic influence in the formation of the brine. The sodium and chloride inventory on the other hand suggests additional sodium comes from intense weathering of silicate rocks. Spatial patterns in DIC concentrations and fluid conductivity show a linear anomaly of higher conductivity and DIC to the northeast of the study area. The anomaly may correlate with subsurface structural terminus in the bedrock where saline magmatic fluids are forced towards the surface along faults. Stable hydrogen and oxygen isotope relationships show that the brine is a mixture of local meteoric water and magmatic water from below. The conclusion of a deeper source is consistent with the geology and recent seismic evidence that indicates the area is structurally dynamic. Isotope results are also consistent with a climate-driven scenario, in which water is affected by evaporation at the surface prior to infiltration.

Mots clés : Makgadikgadi Pans, Salinity, Botswana, Geology, Earth sciences, Brines

Présentation (PROQUEST)

Page publiée le 11 février 2015, mise à jour le 4 septembre 2017