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• W2493661033 abstract "The carbonate hydrochemistry of groundwater from the Hvinningdal aquifer (Denmark) was studied by radiocarbon (accelerator mass spectrometry (AMS)) and δ 13 C measurements as a preliminary step towards 14 C groundwater dating. The 14 C concentrations varied between 30 and 100 percent modern carbon (pMC) in apparent contradiction with tritium ( 3 H) data, which in most cases indicate a post-bomb date. The dilution of 14 C can be explained as being due to the combined effect of dissolution of old soil carbonate and oxidation of old organic carbon. The last effect proved to be essential. To calculate this correction the dissolved oxygen concentration was used together with the δ 13 C values. The combined corrections bring the 14 C concentrations up to post-bomb levels in better agreement with the 3 H data." @default.
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• W2493661033 date "1997-01-01" @default.
• W2493661033 modified "2023-10-17" @default.
• W2493661033 title "Study of the Effect of Fossil Organic Carbon on ¹⁴C in Groundwater from Hvinningdal, Denmark" @default.
• W2493661033 cites W1570458174 @default.
• W2493661033 doi "https://doi.org/10.1017/s0033822200018889" @default.
• W2493661033 hasPublicationYear "1997" @default.
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