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• W2079561131 abstract "Horizontal and vertical variations in the distribution of 14 C, δ 13 C, δ 18 O, and δ 2 H in groundwater of Žitný Island (Rye Island) have been studied. Žitný Island, situated in the Danube River Basin, is the largest island in Europe that is formed by interconnected rivers. It is also the largest groundwater reservoir in central Europe (∼10 10 m 3 of drinking water). The δ 2 H vs. δ 18 O plot made from collected groundwater samples showed an agreement with the Global Meteoric Water Line. In the eastern part of the island, it was found that subsurface water profiles (below 10 m water depth) showed enriched δ 18 O levels, which were probably caused by large evaporation losses and the practice of irrigating the land for agriculture. The core of the subsurface 14 C profile represents contemporary groundwater with 14 C values >80 pMC, indicating that the Danube River during all its water levels feeds most of the groundwater of Žitný Island. However, on the eastern part of the island a small area was found where the δ 13 C and 14 C data (down to ∼30 pMC) helped to identify a groundwater aquifer formed below the Neogene clay sediments. This is the first time that vertical distributions of isotopes in different groundwater horizons have been studied." @default.
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• W2079561131 date "2013-01-01" @default.
• W2079561131 modified "2023-09-28" @default.
• W2079561131 title "Radiocarbon and Stable Isotopes as Groundwater Tracers in the Danube River Basin of SW Slovakia" @default.
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• W2079561131 doi "https://doi.org/10.1017/s003382220005815x" @default.
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