Naslov
Seasonal variations of tritium, uranium and stable isotopes in groundwater and spring waters in the Anthemountas Basin, Northern Greece

Autori
Kazakis, N. ; Krajcar Bronić, Ines ; Barešić, Jadranka ; Philippou, K. ; Paschalidis, I. ; Kalaitzidou, K. ; Mitrakas, M. ; Ioannidou, A.

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
International Symposium on Isotope Hydrology: Advancing the Understanding of Water Cycle Processes, CN-271 / - : International Atomic Energy Agency (IAEA), 2019

Skup
International Symposium on Isotope Hydrology: Advancing the Understanding of Water Cycle Processes

Mjesto i datum
Beč, Austrija, 20.05.2019. - 24.05.2019

Vrsta sudjelovanja
Poster

Vrsta recenzije
Recenziran

Ključne riječi
tritium ; uranium ; stable isotopes ; Greece

Sažetak
In this study, the hydrochemical and isotopic composition of groundwater and spring water was studied during the critical periods of a hydrological year in the Anthemountas basin in Northern Greece. Groundwater constitute a vital source of fresh water worldwide. However, it is vulnerable to climate change, mismanagement and human activities. Many studies have been focused on spatio-temporal variations of groundwater storage. However, groundwater quality can be also variable at the hydrological year scale, even in storm-event scale. Usually, it is considered insignificant in comparison with its spatial variability, while the high cost constitutes a limiting factor for frequent monitor of groundwater quality. Nevertheless, seasonal variability of groundwater quality can define the recharge and hydrogeochemical process of groundwater and function of springs. Another approach to determine the characteristics and origin of groundwater is the study of stable isotopes, tritium and isotopic ratios such as 234U/238U. Their variations have been widely used to determine the characteristics of groundwater and spring water. In this study, samples were collected from two springs and three boreholes during the period of September 2016, February, June and September of 2017. The highest value of 234U/238U ratio was 3.8 during the period of June and observed in groundwater impacted from geothermal fluids (sample 3 and 4), while in spring waters the ratio was up to 1.3. In all three samplings in 2017 samples/locations 3, 4 and 5 did not show measurable/detectable 3H activity concentrations. Samples/locations 1 and 2 showed in all samplings low but detectable 3H activity concentrations. The highest concentration of Tritium was observed in Voskina spring (Sample 2) during the February of 2017. According to the stable isotopes the recharge elevation of the springs and the aquifer is up to 350 m. In this study is highlighted the contribution of isotopes to determine the recharge and hydrogeochemical process of groundwater and spring water. The knowledge of these processes is the base for a sustainable water resource management plan and protection of the aquifer systems of the Anthemountas basin.

Izvorni jezik
Engleski

Znanstvena područja
Geologija, Interdisciplinarne prirodne znanosti

POVEZANOST RADA