Rekultywacja warunków hydrogeologicznych w dolinie Kaczawy
Abstract
RECULTIVATION OF HYDROGEOLOGICAL CONDITIONS IN THE KACZAWA RIVER VALLEY
Summary
The results of calculations of permeability coefficient "k" by means of a field method (Maag's method) are given for the Quaternary formations found to occur within the Kaczawa river valley in the vicinity of Nowy Kościół; and the intensity of water inflow into the individual bore holes made within the alluvial deposits of this area is presented: Moreover, the problem of water disappearance and its reappearance in the wells within the Kaczawa river valley is discussed too.
Summary
The results of calculations of permeability coefficient "k" by means of a field method (Maag's method) are given for the Quaternary formations found to occur within the Kaczawa river valley in the vicinity of Nowy Kościół; and the intensity of water inflow into the individual bore holes made within the alluvial deposits of this area is presented: Moreover, the problem of water disappearance and its reappearance in the wells within the Kaczawa river valley is discussed too.