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

Kód výsledku v 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>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

O - Ostatní výsledky

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2007

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů