Identification of the ascent of groundwater from the mesozoic to the neogene layer in Poznan based on determinations of micro- and macro-components

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F07%3A00022754" target="_blank" >RIV/00216224:14310/07:00022754 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Identification of the ascent of groundwater from the mesozoic to the neogene layer in Poznan based on determinations of micro- and macro-components
Original language description
The comunication presents the results of determinations of the following physico-chemical parameters: pH reaction, temperature, electrolytic conductivity, colour, basicity, total solids, total dissolved solids, total organic carbon, Cl, SO4, F, PO4, NO3,NH4, Na, K, Ca, Mg, CaCO3, Fe, Mn, Cd, Cu, Cr, Ni, Pb, Zn, Al, Ag, Ba, Be, Li, Mo, Tl, V, Hg, Ce, Cs, La, Nd, Pr and Sm in groundwater of the Neogene layer in Poznan city. The water plays an important supplementary role in providing drinking and industrial water to residents, industrial plants, service establishments and public institutions located in some peripheral parts of the city where the Miocene level is used as the principal water-bearing horizon. Years of exploitation have produced a change inthe hydrochemical zonality of the aquifers.
Czech name
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Czech description
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Publication year
2007
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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