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Thermally-induced release of arsenic from minerals and phases relevant to polluted natural systems affected by wildfires

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F25%3A00617939" target="_blank" >RIV/67985831:_____/25:00617939 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/25:10494624

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0883292725000411?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0883292725000411?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.apgeochem.2025.106318" target="_blank" >10.1016/j.apgeochem.2025.106318</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Thermally-induced release of arsenic from minerals and phases relevant to polluted natural systems affected by wildfires

  • Original language description

    Fire-induced arsenic (As) emission from contaminated biomass or soil is dependent on its solid-phase speciation. To quantify the nature of this release, environmentally relevant As-bearing compounds (sulfides, sulfosalts, As-oxides, arsenates, As-doped Fe-oxyhydroxides and organic material) were experimentally heated with a linear temperature increase (25–800 °C) and simultaneous detection of As and other emitted elements. Organic As-bearing materials (fungi, dimethylarsinic acid-DMAA) exhibited the peak of As release at the lowest temperatures of 275–350 °C, followed by arsenolite (As2O3) with the maximum As emission at ∼400 °C. Realgar (As4S4) and orpiment (As2S3) exhibited the maximum As release at 425–450 °C, while enargite (Cu3AsS4) and arsenopyrite (FeAsS) released As at much higher temperatures with emission peaks at ∼625 and > 725 °C, respectively. Similarly, As-bearing Fe-oxyhydroxides emitted As at temperatures exceeding 650 °C. Arsenic emission from arsenates was rather variable and peaked at ∼700 °C for conichalcite [CaCu(AsO4)(OH)], and scorodite (FeAsO4·2H2O), while for mimetite [Pb5(AsO4)3Cl], it peaked towards the upper limit of the temperature range. These results suggest that typical low intensity wildland fires would affect only organically bound As and arsenolite, while higher intensity wildland fires could cause the redistribution of As from all studied phases, thereby posing a significant environmental risk of As redistribution beyond contaminated sites.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10511 - Environmental sciences (social aspects to be 5.7)

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Applied Geochemistry

  • ISSN

    0883-2927

  • e-ISSN

    1872-9134

  • Volume of the periodical

    182

  • Issue of the periodical within the volume

    March

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    9

  • Pages from-to

    106318

  • UT code for WoS article

    001430935100001

  • EID of the result in the Scopus database

    2-s2.0-85217977562