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Isotopic Tracing of Thallium Contamination in Soils Affected by Emissions from Coal-Fired Power Plants

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    SYSNO ASEP0464985
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleIsotopic Tracing of Thallium Contamination in Soils Affected by Emissions from Coal-Fired Power Plants
    Author(s) Vaněk, A. (CZ)
    Grösslová, Z. (CZ)
    Mihaljevič, M. (CZ)
    Trubač, J. (CZ)
    Ettler, V. (CZ)
    Teper, L. (PL)
    Cabala, J. (PL)
    Rohovec, Jan (GLU-S) RID, SAI
    Zádorová, T. (CZ)
    Penížek, V. (CZ)
    Pavlů, L. (CZ)
    Holubík, O. (CZ)
    Němeček, K. (CZ)
    Houška, J. (CZ)
    Drábek, O. (CZ)
    Ash, C. (CZ)
    Source TitleEnvironmental Science and Technology - ISSN 0013-936X
    Roč. 50, č. 18 (2016), s. 9864-9871
    Number of pages8 s.
    Publication formPrint - P
    Languageeng - English
    CountryUS - United States
    Keywordsenvironmental implications ; isotope ; fractionation ; combustion ; utility ; health ; oxides ; silver ; lead
    Subject RIVDD - Geochemistry
    Institutional supportGLU-S - RVO:67985831
    UT WOS000384037900009
    EID SCOPUS84988592724
    DOI10.1021/acs.est.6b01751
    AnnotationHere, for the first time, we report the thallium (Tl) isotope record in moderately contaminated soils with contrasting land management (forest and meadow soils), which have been affected by emissions from coal-fired power plants. Our findings clearly demonstrate that Tl of anthropogenic (high-temperature) origin with light isotope composition was deposited onto the studied soils, where heavier Tl (epsilon205Tl ∼ -1) naturally occurs. The results show a positive linear relationship (R2 = 0.71) between 1/Tl and the isotope record, as determined for all the soils and bedrocks, also indicative of binary Tl mixing between two dominant reservoirs. We also identified significant Tl isotope variations within the products from coal combustion and thermo-desorption experiments with local Tl-rich coal pyrite. Bottom ash exhibited the heaviest Tl isotope composition (epsilon205Tl ∼ 0), followed by fly ash (epsilon205Tl between -2.5 and -2.8) and volatile Tl fractions (epsilon205Tl between -6.2 and -10.3), suggesting partial Tl isotope fractionations. Despite the evident role of soil processes in the isotope redistributions, we demonstrate that Tl contamination can be traced in soils and propose that the isotope data represent a possible tool to aid our understanding of postdepositional Tl dynamics in surface environments for the future.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2017
Number of the records: 1  

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