Aluminium in the water of the neogene-paleogene aquifer of Wielkopolska

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F09%3A00043770" target="_blank" >RIV/00216224:14310/09:00043770 - 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

Aluminium in the water of the neogene-paleogene aquifer of Wielkopolska

Popis výsledku v původním jazyce

The Neogene-Paleogene aquifer plays an important role in supplying the population of Wielkopolska, Poland, with water, both potable and for domestic purposes. This especially concerns the areas where there are no aquifers in the Quaternary layer, or where the level of water in the existing aquifers is low, or their chemical composition is of poor quality. The hydrogeochemical environment of the Neogene-Paleogene aquifer displays considerable variability determined by geogenic factors and manifested by large differences in water chemistry, especially its colour, hardness, and the levels of chlorides, iron and manganese. The differences in quality are particularly significant in the region of the Poznań-Oleśnica graben, where water ascends from the deeper Mesozoic aquifers.

Název v anglickém jazyce

Aluminium in the water of the neogene-paleogene aquifer of Wielkopolska

Popis výsledku anglicky

The Neogene-Paleogene aquifer plays an important role in supplying the population of Wielkopolska, Poland, with water, both potable and for domestic purposes. This especially concerns the areas where there are no aquifers in the Quaternary layer, or where the level of water in the existing aquifers is low, or their chemical composition is of poor quality. The hydrogeochemical environment of the Neogene-Paleogene aquifer displays considerable variability determined by geogenic factors and manifested by large differences in water chemistry, especially its colour, hardness, and the levels of chlorides, iron and manganese. The differences in quality are particularly significant in the region of the Poznań-Oleśnica graben, where water ascends from the deeper Mesozoic aquifers.

Druh

O - Ostatní výsledky

CEP obor

CB - Analytická chemie, separace

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2009

Kód důvěrnosti údajů

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