Počet záznamů: 1  

Bioaccumulation of thallium in a neutral soil as affected by solid-phase association

  1. 1.
    SYSNO ASEP0464914
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevBioaccumulation of thallium in a neutral soil as affected by solid-phase association
    Tvůrce(i) Grösslová, Z. (CZ)
    Vaněk, A. (CZ)
    Mihaljevič, M. (CZ)
    Ettler, V. (CZ)
    Hojdová, Maria (GLU-S) RID, SAI
    Zádorová, T. (CZ)
    Pavlů, L. (CZ)
    Penížek, V. (CZ)
    Vaněčková, B. (CZ)
    Komárek, M. (CZ)
    Chrastný, V. (CZ)
    Ash, Ch. (CZ)
    Zdroj.dok.Journal of Geochemical Exploration. - : Elsevier - ISSN 0375-6742
    Roč. 159, December (2015), s. 208-212
    Poč.str.5 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.NL - Nizozemsko
    Klíč. slovabirnessite ; carbonate ; oxide ; plant ; uptake
    Vědní obor RIVDD - Geochemie
    Institucionální podporaGLU-S - RVO:67985831
    UT WOS000364896600017
    EID SCOPUS84945934187
    DOI10.1016/j.gexplo.2015.09.009
    AnotaceThe work focused on the biogeochemical behavior of synthetic Tl-modified phases, namely birnessite, ferrihydrite, and calcite, in a neutral soil Leptosol. The data presented here clearly demonstrate a strong relationship between the mineralogical position of Tl in the soil and its uptake by the studied plant (Sinapis alba L.). All tested Tl phases behaved as potential Tl sources in the rhizosphere, with a maximum for ferrihydrite and minimum for birnessite. Therefore, it can be concluded that Mn(III,IV) oxides, if present in the soil system,may reduce biological uptake of Tl to a substantial degree, including the case of Tl-accumulating species (i.e., Brassicaceae). It was proven that even Tl-enriched calcite present in the carbonate-rich soil is an important precursor for further contaminant mobilization, despite its relative resistance to degradation. Our data indicate that the fate of secondary Tl phases in the rhizosphere might be significantly influenced by the pH of the soil matrix, i.e., soils with lower pHs reduce their stability, making them more susceptible to further degradation by root exudates. Bulk soil mineralogy and the content and quality of soil organicmatter are thus suggested to be critical parameters controlling the bioaccumulation potential for
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2017
Počet záznamů: 1  

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