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Radiation damage in sulfides: Radioactive galena from burning heaps, after coal mining in the Lower Silesian basin (Czech Republic)

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388980%3A_____%2F17%3A00478666" target="_blank" >RIV/61388980:_____/17:00478666 - isvavai.cz</a>

  • Alternative codes found

    RIV/00025798:_____/17:00000224 RIV/00216224:14310/17:00100317 RIV/00216208:11310/17:10369548 RIV/00216208:11320/17:10369548

  • Result on the web

    <a href="http://dx.doi.org/10.2138/am-2017-6036" target="_blank" >http://dx.doi.org/10.2138/am-2017-6036</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.2138/am-2017-6036" target="_blank" >10.2138/am-2017-6036</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Radiation damage in sulfides: Radioactive galena from burning heaps, after coal mining in the Lower Silesian basin (Czech Republic)

  • Original language description

    The isotopic composition of lead (Pb-207/Pb-206, Pb-208/Pb-206, and Pb-210) in a recently formed galena from burning heaps after coal mining in Radvanice, Markousovice, and Rybnicek, the Lower Silesian basin, Czech Republic, was studied in detail. 210Pb activity in galena varied from 135 +/- 9 to 714 +/- 22 Bq/g and calculated integral doses ranged from 2.21 x 10(11) to 6.11 x 10(11) alpha/g. The radioactivity of the galena causes micro-deformations in its crystal structure as indicated by the Williamson-Hall graphs, showing that the level of micro-strain depends on the length of time that galena samples were exposed to the radiation. However, the crystal structure of galena is affected very inhomogenously, according to TEM investigations there are domains of fully crystalline, polycrystalline, and fully metamict galena within one crystal. Inductively coupled plasma-mass spectrometry (ICP-MS) was used to determine the isotopic composition of the studied galena. The stable isotope ratios of Pb varied for Pb-207/Pb-206 from 0.8402 to 0.8435 and for Pb-208/Pb-206 from 2.0663 to 2.0836. The average ratios Pb-207/Pb-206 = 0.8312 and Pb-208/Pb-206 = 2.0421 were obtained for coal from the same localities. These isotope ratios show that there is no isotopic fractionation taking place during the coal burning and subsequent galena crystallization from hot gases.

  • 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

    10402 - Inorganic and nuclear chemistry

Result continuities

  • Project

    <a href="/en/project/GA15-11674S" target="_blank" >GA15-11674S: A model of mobilization and geochemical cycles of potentially hazardous elements and organic compounds in burned coal heaps</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    American Mineralogist

  • ISSN

    0003-004X

  • e-ISSN

  • Volume of the periodical

    102

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    7

  • Pages from-to

    1788-1795

  • UT code for WoS article

    000410608000004

  • EID of the result in the Scopus database

    2-s2.0-85029350111