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A talajvizszint ingadozasanak vizsgalata matematikai modszerekkel a Felso-Tisza vidékén. (A mathematical investigation of groundwater table range in the Upper Tisza region)
(supprimer)
Average groundwater depth in the clayey sediments of the area is 2 to 3 m, but large deviations occur. Changes in groundwater table are similar to those observed in the Great Plain. The range depends on precipitation, lithology, water retention