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.Downloads
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Geochemia, mineralogia, petrologia