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Natural concentrations of major and trace elements in some Norwegian bedrock groundwaters
Affiliation:1. Institut des Sciences de la Terre, Centre d''Etudes et de Recherches de Djibouti (CERD), Route de l''aéroport, B.P. 486, Djibouti – ville, République de Djibouti;2. Département des génies civil, géologique et des mines, Polytechnique Montréal, C.P. 6079, succ. Centre-Ville, Montréal, QC H3C 3A, Canada;3. UMR G-EAU, BP 5095, 34196 Montpellier Cedex 5, France;4. GEOTOP Research Center, Montréal, Canada;5. Département de biologie, chimie et géographie, Université du Québec à Rimouski, 300, Allée des Ursulines, Rimouski, QC G5L 3A1, Canada;6. Department of Physics and Earth Sciences “Macedonio Melloni”, University of Parma, Parco Area delle Scienze 157/a, 43124 Parma, Italy;1. School of Earth Science and Geological Engineering, Sun Yat-sen University, Guangzhou 510275, China;2. Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China
Abstract:Twenty-eight groundwater samples have been collected from boreholes in bedrock aquifers in Nord Trøndelag (Central Norway), the Hvaler archipelago and other areas around Oslofjord (South-eastern Norway). A clear relationship is demonstrated between many chemical parameters and lithology or geographical location. The parameters electrical conductivity, Cl, SO42−, F, Na, Al, Fe, Be, Bi, Cd, Cu, La, Mo, Pb, Th, Tl, U, Y, Zn, Zr, B, Rn, and Si have generally higher values in the Iddefjord Granite of Hvaler, while pH, alkalinity, Ca, Mg, Cs, Rb, and Sr are highest in Trøndelag. Several parameters such as F, Na, Fe, U, Rn and possibly Al exceed drinking water norms on Hvaler. Measured values of the analyzed parameters compare well (except F) with the Dutch “A” (background) values, developed for assessment of anthropogenic contamination. The authors warn, however, against uncritical use of “norms” developed in countries with other dominant lithologies than Norway.
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