2005
DOI: 10.1002/hyp.5971
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Origin of shallow groundwater of Csepel Island (south of Budapest, Hungary, River Danube): isotopic and chemical approach

Abstract: Abstract:The shallowest aquifer of the alluvial Csepel Island is used for drinking water supply for Budapest and the surrounding villages. A previous two-dimensional hydraulic model failed to explain many observations; therefore, a three-dimensional hydraulic model was constructed using the software application MODFLOW.

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Cited by 18 publications
(7 citation statements)
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“…Amin and Campana1996, Maloszewski et al 2002, Fórizs et al 2005, isotope data were observed for several years with a sampling frequency of 1 week or 1 month, and the modelled mean transit times represented an average value for several years. As mentioned previously, only a short time span with frequent (daily or daily calculated) sampling could be modelled in the present study.…”
Section: Modelling Results and Discussionmentioning
confidence: 94%
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“…Amin and Campana1996, Maloszewski et al 2002, Fórizs et al 2005, isotope data were observed for several years with a sampling frequency of 1 week or 1 month, and the modelled mean transit times represented an average value for several years. As mentioned previously, only a short time span with frequent (daily or daily calculated) sampling could be modelled in the present study.…”
Section: Modelling Results and Discussionmentioning
confidence: 94%
“…The observation site (multiple collector well) is located very close (45 m) to the river bank, while the water level of the Danube is variable. Thus, the modelling of the isotope data was performed by selecting single oxygen-isotope peaks observed during "steady-state" water levels, instead of using the whole continuous time series as in case studies by Amin et al (1996), Maloszewski et al (2002) and Fórizs et al (2005). Every input/output oxygen-isotope peak was considered as an independent signal characterized by its own travel time, dispersion parameter and Danube water proportion.…”
Section: Introductionmentioning
confidence: 99%
“…The infiltration of surface water to groundwater systems and water passage through the aquifer media causes improvements in water quality by a set of processes including: sorption, redox processes and biodegradation [3,4]. The mixing of bank filtrates with ambient, usually unpolluted groundwater, also takes place [5,6]. Nevertheless, the quality of bank filtrate is strongly dependent on surface water quality.…”
Section: Introductionmentioning
confidence: 99%
“…First in the riverbed and then in the aquifer, the water undergoes combined physical, biological, and chemical processes such as dissolution, sorption, redox processes, and biodegradation [1]. Additionally, mixing with ambient groundwater usually occurs to some degree [2,3].…”
Section: Introductionmentioning
confidence: 99%