Żelazo w wodach wysokiego tarasu Wisły na wschód od Krakowa
Abstract
Iron in the Walters of the high terrace of the Vistula east of Cracow
The iron in waters under investigation is derived from rocks present in infiltration and water-bearing zones. Fluctuations of Fe content during exploitation of wells are observed and discussed. Only analyses of samples taken from special sampling taps are considered to be reliable.
The iron in waters under investigation is derived from rocks present in infiltration and water-bearing zones. Fluctuations of Fe content during exploitation of wells are observed and discussed. Only analyses of samples taken from special sampling taps are considered to be reliable.