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Pohyb důlních vod v mělkém středověkém Dole Jeroným (Česká republika)
Kaláb, Zdeněk ; Hrubešová, E. ; Knejzlík, Jaromír ; Kořínek, R. ; Kukutsch, Radovan ; Lednická, Markéta ; Žůrek, P.
Mine waters in the Jeroným Mine can be divided into following types: running, influent and flowing waters, water accumulated in closed drainless expanses, waters in expanses with natural or man-made outflow. Mine water flow is significant, small drain exists in some parts during the whole year. First sudden and significant increasing of mine water level is obviously related with marked changes of surface water amount (spates or snow-melt). Low increases of water level are not always dependent on precipitation amount and there other influencing factors exist probably.
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Mine Waters in Medieval Mine Jeroným
Kukutsch, R. ; Lednická, Markéta ; Kořínek, R. ; Žůrek, P.
In this paper we presented summary about mine waters in medieval Mine Jeroným near Čistá. It is documented current measurement of changes of individual water accumulations and correlation of these changes with weather conditions. Connection of two separated parts of Mine Jeroným through water channels is documented using application of tinted lotion.
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