“…The knowledge of the isotopic composition (δ 2 H, δ 18 O, and 3 H) in surface and groundwater in relation to the isotopic composition of the precipitations allows us to determine the average residence time of the water in the aquifers (Campbell et al, 2021 ; Krajcar Bronić & Barešić, 2021 ), the possible interconnections between different aquifers (Andries et al, 2021 ; Mahlangu et al, 2020 ), the origin of waters (Andries et al, 2021 ; Catalano et al, 2014 ), and the dynamics of processes in surface waters (Ramaroson et al, 2018 ; Schmidt et al, 2020 ). In addition, although the 3 H concentration in the atmosphere in recent years has reached values in line with the environmental threshold, thanks to the electrolytic enrichment methodologies it is possible to determine the low concentrations of 3 H using the liquid scintillation counting technique (Belachew et al, 2018 ; Lin et al, 2020 ).…”