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Author Nisi, B.; Raco B.; Dotsika, E.
Title Groundwater Contamination Studies by Environmental Isotopes: A review Type Book Chapter
Year 2014 Publication Environment, Energy and Climate Change I: Environmental Chemistry of Pollutants and Wastes Abbreviated Journal
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Publisher Springer-Verlag Berlin Heidelberg Place of Publication Editor E. Jimenez
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Call Number THL @ christoph.kuells @ Serial 186
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Author Richter, B. C.; Kreidler, C.W.
Title Identification of Sources of Groundwater Salinization using Geochemical Techniques Type Journal Article
Year 1991 Publication EPA/600/2-91/064 Abbreviated Journal
Volume Issue Pages 259
Keywords Geochemistry, USA, isotopes, salinization, ground water
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Corporate Author Bureau of Economic Geology, Univ. of Austin, Texas Thesis
Publisher EPA Place of Publication Editor Bledsoe, B.E.
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Call Number THL @ christoph.kuells @ Serial 187
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Author Carreira, P. M.; Lobo de Pina, A.; Mota Gomes, A.; Marques, J.M.; Monteiro Santos, F.
Title Geochemical and Isotopic Marks for Tracing Groundwater Salinization: Santiago Island, Republic of Cape Verde, Case Study Type Book Chapter
Year 2019 Publication Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources Abbreviated Journal
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Publisher Verlag: Springer International Publishing Place of Publication Editor Drioli,E.; Macedonio, F.
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Series Editor Series Title Innovation in Process Engineering for Hydrology Abbreviated Series Title
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Call Number THL @ christoph.kuells @ Serial 188
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Author Bahir, M.; Ouhamdouch, S.; Carreira, P.M.
Title Isotopic and geochemical methods for studying water–rock interaction and recharge mode: application to the Cenomanian–Turonian and Plio-Quaternary aquifers of Essaouira Basin, Morocco Type Journal Article
Year 2018 Publication Mar. Freshwater Res. Abbreviated Journal
Volume 69 Issue 8 Pages 1290-1300
Keywords geochemistry, semi-arid area, stable isotopes, water resources.
Abstract Study of the Cenomanian–Turonian and Plio–Quaternary aquifers of Essaouira basin (Western Morocco), based on the interpretation of geochemical (major elements) and isotopic (18O, 2H, 13C and 14C) data, has aided the understanding of the hydrodynamics of these aquifers, which is greatly affected by tectonics. Hydrochemical characteristics based on the bivariate diagrams of major ions (Cl–, SO42–, NO3–, HCO3–, Na+, Mg2+, K+ and Ca2+) and electrical conductivity and mineral saturation indices indicate that the origins of groundwater mineralisation are the result of: (1) evaporite dissolution; (2) cation exchange reactions; (3) and evaporation processes. Radiogenic isotopes (3H and 14C) have highlighted the presence of significant recent recharge in the eastern part of the basin, with groundwater moving according to the general flow path (south-east to north-west). Stable isotope data from the Essaouira basin plot along the Global Meteoric Water Line and below the Local Meteoric Water Line. This suggests that groundwater has been recharged under several different climate regimes.
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Call Number THL @ christoph.kuells @ Serial 191
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Author Kloppmann, W.; Petelet-Giraud, E.; Guerrot, C.; Cary, L.; Pauwels, H.
Title Extreme Boron Isotope Ratios in Groundwater Type Journal Article
Year 2015 Publication Procedia Earth and Planetary Science Abbreviated Journal
Volume 13 Issue Pages
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Abstract Kloppmann, W. , Petelet-Giraud, E. , Guerrot, C. , Cary, L. , & Pauwels, H. (2015). Extreme Boron Isotope Ratios in Groundwater. Procedia Earth and Planetary Science, 13 . doi: 10.1016/j.proeps.2015.07.069
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Call Number THL @ christoph.kuells @ Serial 193
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