Naslov
Isotope studies of karst springs included in the water supply system of the City of Rijeka (Croatia)

Autori
Mance, Diana ; Lenac, Danijela ; Rubinić, Josip

Izvornik
Southeastern European Medical Journal (2459-9484) 1 (2017), 2; 46-54

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
drinking water, isotopes, radioisotopes

Sažetak
Aim: To provide information about the results of isotopic analyses of karst springs, Rječina Spring and Zvir, which ensure potable water for more than 200, 000 people in Rijeka County (Croatia) Methods: Specific activities of selected radionuclides were determined by high resolution gamma spectrometric analysis and radiochemical separation method. Values of hydrogen and stable isotope contents were determined by water equilibration method on isotope ratio mass spectrometer in conjunction with dual inlet and equilibration peripheral unit. Results: Anthropogenic radionuclides were detected in trace amounts. The results of the analysis show that the calculated yearly dose introduced to an adult human consuming 2 liters of water per day is approximately 20 microSv. Stable isotopes content of the spring waters indicates a dominant recharge of the analyzed hydrological system by winter precipitation. Different isotopic variations of spring water as a consequence of sudden precipitation inputs in summer and autumn indicate that water discharged at Rječina Spring mainly originates from a big water reservoir situated in the wide mountainous region in the hinterland of the spring.Conclusion: The examined water is potable and radiologically safe. Stable isotope variations of the spring water show a fast reaction to sudden precipitation inputs, confirming the ecological vulnerability of karst springs. In light of recent heavy precipitation and flooding in different parts of Croatia, a more systematic research on isotopic water composition should be encouraged.

Izvorni jezik
Engleski

Znanstvena područja
Fizika, Interdisciplinarne prirodne znanosti

POVEZANOST RADA