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Metal(loid)s remobilization and mineralogical transformations in smelter-polluted savanna soils under simulated wildfire conditions

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    SYSNO ASEP0555414
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleMetal(loid)s remobilization and mineralogical transformations in smelter-polluted savanna soils under simulated wildfire conditions
    Author(s) Tuhý, M. (CZ)
    Ettler, V. (CZ)
    Rohovec, Jan (GLU-S) RID, SAI
    Matoušková, Šárka (GLU-S) RID, SAI
    Mihaljevič, M. (CZ)
    Kříbek, B. (CZ)
    Mapani, B. (NA)
    Article number112899
    Source TitleJournal of Environmental Management. - : Elsevier - ISSN 0301-4797
    Roč. 293, September (2021)
    Number of pages10 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsWildfire ; Soil ; Metal(loid)s ; Remobilization ; Smelter pollution
    OECD categoryEnvironmental sciences (social aspects to be 5.7)
    Method of publishingLimited access
    Institutional supportGLU-S - RVO:67985831
    UT WOS000677980900002
    EID SCOPUS85107693041
    DOI10.1016/j.jenvman.2021.112899
    AnnotationThe surroundings of mines and smelters may be exposed to wildfires, especially in semi-arid areas. The temperature-dependent releases of metal(loid)s (As, Cd, Cu, Pb, Zn) from biomass-rich savanna soils collected near a Cu smelter in Namibia have been studied under simulated wildfire conditions. Laboratory single-step combustion experiments (250–850 ◦C) and experiments with a continuous temperature increase (25–750 ◦C) were coupled with mineralogical investigations of the soils, ashes, and aerosols. Metals (Cd, Cu, Pb, Zn) were released at >550–600 ◦C, mostly at the highest temperatures, where complex aerosol particles, predominantly composed of slag-like aggregates, formed. In contrast, As exhibited several emission peaks at ~275 ◦C, ~370–410 ◦C, and ~580 ◦C, reflecting its complex speciation in the solid phase and indicating its remobilization, even during wildfires with moderate soil heating. At <500 ◦C, As was successively released via the transformation of As-bearing hydrous ferric oxides, arsenolite (As2./subO3) grains attached to the organic matter fragments, metal arsenates, and/or As-bearing apatite, followed by the thermal decomposition of enargite (Cu3AsS4) at >500 ◦C. The results indicate that the active and abandoned mining and smelting sites, especially those highly enriched in As, should be protected against wildfires, which can be responsible for substantial As re-emissions.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2022
    Electronic addresshttps://www.sciencedirect.com/science/article/pii/S0301479721009610?via%3Dihub
Number of the records: 1  

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