Publication at Faculty of Science, First Faculty of Medicine, Faculty of Mathematics and Physics |
2009
Abstract
Although the geological context is well known, there are still some gaps in the knowledge about the hydrogeochemical regime, groundwater average residence time and the palaeohydrological conditions prevailing during the recharge period of the aquifers which would help to secure sustainable exploiting of the resources. Environmental isotopes (18O, 2H, 3H, 13C) together with radiocarbon were used to evaluate hydrochemical evolution, residence time and palaeorecharge conditions for Jurassic and Cretaceous aquifer.