Mine Water and The Environment, Vol12, Annual Issue, 1993, pp 1-10
IMPACT OF LEADIZINC ORE MINING ON
GROUNDWATER QUALITY IN TRZEBIONKA
MINE (SOUTHERN POLAND)
Bogumil Gajowiec
State Geological Institute, Uppe Silesian Branch
Sosnowiec ul.Bialego 1, Poland
Andrzej Witkowski
Silesian University, Department of Hydrogeology and Engineering Geology,
Sosnowiec ul.Mielczarskiego 60 Poland
ABSTRACT
The intensive mining activity camed out by "Trzebionka" zinc-lead mine causes
chadges in the hydrodynamic regime of the massic aquifer as well as essential changes
in the chemical composition of the groundwater.The mine water, in comparison with
groundwaters collected directly from fractures and Karstic channels and with
groundwaters pumped out fkom wells situated in Chrzanow region, is characterized by
higher contents of almost all major dissolved constituents as, well as, many trace
elements. Hydrogeochemical background of massic carbonate series aquifer has been
elaborated. Largest anomalies in extent of almost all elements have occurred in area of
the "Tnebionka" mine. In this water general trend of increase of*pH, total dissolved
solids and SO42- concentration with simultanwus trends of decrease of ~n2+ and pb2+
concentrations have been noticed. Water pumped out from the mine in spite of its low
quality, is utilized in about 80% as potable water after undergoing complicated
treatment.
INTRODUCTION
Fissured - Karstic basin of the Triassic carbonate series in Chrzanow region (southern
Poland), is a very important source of potable water for this part of a great urban and
industrial agglomeration of the Upper Silcsian Coal Basin. It is subjected to a strong
anthropogenic pressure which leads to the degradation of water quality and depletion
of water reserves. This influence is exesperated at "Trzebionka" zinc-lead mine where
the impact of mining on groundwater regime and quality is particularly important in
considerationof fact that more than 50% of all water pumped out from the coal basin is
mine water
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