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Wyszukujesz frazę "Klodzko Region" wg kryterium: Wszystkie pola


Wyświetlanie 1-2 z 2
Tytuł:
Silicon and aluminium in groundwater of the Kłodzko Region (the Sudetes, )land) - partial geochemical equilibrium with secondary solid phases
Autorzy:
Dobrzyński, D.
Powiązania:
https://bibliotekanauki.pl/articles/2059234.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Sudetes
groundwater geochemistry
aluminosilicate phases
hydroxyaluminosilicate HAS
silicon
aluminium
Opis:
The chemistry of shallow, cold groundwater in the eastern part of the Kłodzko Region (the Sudetes, SW Poland) was investigated, Groundwaters occur in the short turn-over time zone of the hydrogeological systems. The aquifers are composed of various bedrock types (metamorphic, igneous and sedimentary). Silicon and aluminium concentrations in the waters of particular aquifers are documented. The aqueous chemistry is interpreted in terms of the solubility of solid phases to indicate phases that are responsible for silicon and/or aluminium solubility control. Locally and/or periodically (seasonally) partial geochemical equilibrium between the groundwater and the secondary solid phases might be reached and maintained. In groundwater with a pH below 6.7, aluminium activity is usually controlled by the reversible congruent dissolution of A1(OH)3 forms, whereas silicon activity is probably controlled by the solubility the SiO2 form (chalcedony). At pHs above 6.7, the incongruent reaction between the hydroxyaluminosilicate colloid (HASB) and forms of Al(OH), controls both silicon and aluminium activities.
Źródło:
Geological Quarterly; 2006, 50, 3; 369-382
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The main hydrogeochemical processes affecting the composition of certain naturally carbonated waters of southwestern Poland
Autorzy:
Kiełczawa, B.
Powiązania:
https://bibliotekanauki.pl/articles/2059141.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polska
Kłodzko Region
groundwater
ion exchange
water-rock interaction
mineral equilibrium
Opis:
Kłodzko region is a historical region in southwestern Poland, cutting into the territory of the Czech Republic. In geological terms, it contains (within the Polish borders) the Upper Nysa Kłodzka Graben and the Orlica-Śnieżnik Metamorphic Unit. The region abounds in naturally carbonated waters, whose composition is dominated by HCO-3, Na+, Ca2+ and Mg2+ ions. This study concerns the chemical composition of waters from particular intakes situated in Kudowa-Zdrój, Jeleniów, Duszniki-Zdrój, Polanica-Zdrój and Gorzanów. Chemical data were analysed mathematically and by hydrochemical modelling performed with the help of the AquaChem5.1 and PhreeqC codes. The chemical composition of the waters studied is shaped chiefly by hydrolysis of aluminosilicates. The major ion composition is also influenced by ion exchange (adsorption and desorption) with and dissolution of carbonate minerals. Analysis of saturation indexes showed that these waters are in equilibrium with kaolinite. Generally speaking, the chemical composition of waters in this region is determined by dissolution and precipitation of carbonates (mostly secondary) and aluminosilicates in the presence of carbon dioxide, as well as by ion exchange.
Źródło:
Geological Quarterly; 2011, 55, 3; 203-212
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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