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The Danube-Tisza Interfluves is one of the largest recharge areas in Europe. The aim of this study was to build a flow and transport model for an agricultural field. In previous studies in Méntelek the derived average groundwater recharge has been obtained to be 53 mm/year, and the vertical dispersivity is 0.3 m [1]. Close to this natural environment, about 16 km apart, there is an agricultural field close to a larger city, Kecskemét, where artificial irrigation occurred between the middle 1970 and 1980 (Fig. 1-2.).

Tritium Peak Method and 3H/3HE Dating Technique use for Estimating Shallow Groundwater Recharge