Use of hydrochemistry and isotopes for improving the knowledge of groundwater flow in a semiconfined aquifer system of the Eastern Slavonia (Croatia)
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文摘

Recharge mechanism and groundwater flow evolution were studied.

Hydrogeological, hydrochemical and isotopic methods were combined successfully and used to improve conceptual model.

The results confirmed recharge by rainfall infiltration as the main source of water.

Groundwater residence time of several decades was confirmed by associated methods.

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