A talajvizszint ingadozasanak vizsgalata matematikai modszerekkel a Felso-Tisza vidékén. (A mathematical investigation of groundwater table range in the Upper Tisza region)
LOKI J. ;
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 capacity of soils and vegetation showing alterations during the growing season. The influence of rivers is also studied. (DLO).
Article of periodic
published at : Acta geographica ac geologica et meteorologica debrecina Debrecen
Millesime : 1982, vol. 21 [pp. 39-73]
Bibliographic references : 19 réf.