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The Fennoscandian Shield has been subjected to several glaciations over the past million years, the last of which (Weichselian Ice Age) ended only at about 10Ka. Here we used boron isotopes and B contents to (a) establish the degree of water–rock interaction (WRI) and (b) clarify freezing processes within groundwaters from the Äspö site in Sweden and from various sites in Finland. The high δ 11...
The Palmottu uranium ore deposit, located within a granitic host rock in southern Finland, is an excellent setting for conducting analogue studies to assess radionuclide transport from the uranium deposit fractured crystalline host rock. In this context, Nd isotope ratios are used to establish the degree of water–rock interaction (WRI) and to clarify mixing processes within the groundwaters. Variations...
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