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    Spatial Radiocarbon and Stable Carbon Isotope Variability of Mineral and Thermal Waters in Slovakia

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    Author
    Povinec, P. P.
    Franko, O.
    Šivo, A.
    Richtáriková, M.
    Breier, R.
    Aggarwal, P. K.
    Araguás-Araguás, L.
    Issue Date
    2010-01-01
    
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    Citation
    Povinec, P. P., Franko, O., Šivo, A., Richtáriková, M., Breier, R., Aggarwal, P. K., & Araguás-Araguás, L. (2010). Spatial radiocarbon and stable carbon isotope variability of mineral and thermal waters in Slovakia. Radiocarbon, 52(3), 1056-1067.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 20th International Radiocarbon Conference held in Kona, Hawaii, USA, May 31-June 3, 2009.
    URI
    http://hdl.handle.net/10150/654329
    DOI
    10.1017/S0033822200046130
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Isotope hydrology investigations were carried out with the aim to study isotope variability in mineral and thermal waters (MTW) of Slovakia. The aquifers of MTW were formed by Triassic limestones and dolomites, which are found in the mountains as well as in the pre-Tertiary substratum of depressions and lowlands. The MTW were of artesian and/or open structures. At present, there are only boreholes available, as natural outflows have already been captured by them. Large spatial isotope variability (14C between 2 and 33.6 pMC, 18O between -11.8 and -9.8, and 13C between -12.7 and -3.4 for bicarbonates and -21 and -4.9 for free CO2) and heterogeneity of MTW was observed, indicating different origins of MTW. Corrected radiocarbon apparent ages of MTW indicate that they mostly infiltrated during the Würm and Holocene periods.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200046130
    Scopus Count
    Collections
    Radiocarbon, Volume 52, Number 3 (2010)

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