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A contribution to the interpretation of (super 14) C groundwater ages considering the example of a partially confirmed sandstone aquifer.
Keywords
Ar 39;argon;semi confined aquifers;unconfined aquifers;isotope exchange;sandstone;soil gas;mixing;noble gases;dissolved materials;West Germany;surveys;ground water;aquifers;clastic rocks;Germany;interpretation;Central Europe;soils;Europe;Cenozoic;Quaternary;geochronology;C 14;carbon;dates;isotopes;radioactive isotopes;carbon dioxide;absolute age;sedimentary rocks;geochemistry;carbonates;processes