Podrobnosti záznamu

Název
    Sparkling mineral water at western rim of the Doupovské hory Mountains (Czech Republic): genesis by water-rock interaction and deep-seated CO2
Údaj o odpovědnosti
    Tomáš Pačes, Petr Möller, Andrea Fuganti, Giulio Morteani, Jan Pěček
Autor
    Fuganti, Andrea
    Möller, Petr
    Morteani, Giulio
    Pačes, Tomáš, 1937-
    Pěček, Jan
Jazyk
    anglicky
Zdrojový dokument - seriál
    Věstník Českého geologického ústavu (Bulletin of the Czech Geological Survey)
Svazek/č.
    Vol. 76, no. 4
Strany
    p. 189-202
Rok
    2001
Poznámky
    1 obr., 10 diagr., 7 tab., 36 bibl.
    il.
    Zkr. název ser.: Věst. Čes. geol. Úst. (Bull. Czech geol. Surv.)
Předmětová skupina
    bazalt
    granit
    interakce voda-hornina
    izotopy Pb
    izotopy stabilní
    krušnohorský pluton
    oxid uhličitý
    voda minerální
    vulkanity Doupovských hor
    vzácné zeminy
Geografické jméno
    ČR-Čechy
    Kyselka (Karlovy Vary)
    Velichovky (Náchod)
Klíčové slovo
    CO2
    Czech
    Deep-seated
    Doupovské
    Genesis
    Hory
    Interaction
    Mineral
    Mountains
    Republic
    Rim
    Sparkling
    Water
    Water-rock
    Western
Abstrakt (anglicky)
   Mineral water with dissolved CO2 is discharged from the variscian granite of the Karlovy Vary massif and from Tertiary basalts and pyroclastics of the stratovolcano of the Doupovské hory Mountains in the vicinity of Kyselka and Velichov. The sparkling mineral water is produced from numerous drill holes in the valley of the Lomnice creek, the Pstružný creek and the petrovský creek. the mineral water with the high content of CO2 is bottled as Mottoni sparkling mineral water. Atmospheric precipitation infiltrates either in outcrops of the granite or the basalt and the basaltic pyroclastics. Judged on the tritium content, the water is less than 50 years old. Where the ground water meets the ascending CO2 of post-volcanic origin, it iteracts more aggressively with the rocks of aquifer. The total dossilved solids of the mineral water increase to more than 1 g/l.
   The mineral water from the granite is characterized by the mass ratio of (Na+K) / (Ca+Mg) higher than 1 and increased concentration of fluorite ions. Mineral water from basaltic rocks has the ratio lower than 1 and the concentration of fluoride ions is low. isotopic composition of traces of He in Co2 gas indicates that about 35% of the He component probably originates from a mantle source. carbon dioxide is probably derived from a residual magmatic sources and not from deep-seated marine carbonates or organic matter undergoing thermal decomposition. Sulphate ions in the Kyselka and Velichov mineral waters differ isotopically from the sulphates in the thermal springs of Karlovy Vary
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    4. 7. 2007
Datum importu
    8. 8. 2012