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Crystal structure of undersubstituted sb-rich vikingite Vik40, Ag2.85 Pb12.35 (Bi9.52 Sb1.27)∑=10.80 S30: Site population and comparison with structure of vikingite Vik50, Ag3.5 Pb11.0 Bi11.5 S30

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60461373%3A22810%2F21%3A43923147" target="_blank" >RIV/60461373:22810/21:43923147 - isvavai.cz</a>

  • Alternative codes found

    RIV/68378271:_____/21:00548430

  • Result on the web

    <a href="http://doi.org/10.3190/jgeosci.329" target="_blank" >http://doi.org/10.3190/jgeosci.329</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3190/jgeosci.329" target="_blank" >10.3190/jgeosci.329</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Crystal structure of undersubstituted sb-rich vikingite Vik40, Ag2.85 Pb12.35 (Bi9.52 Sb1.27)∑=10.80 S30: Site population and comparison with structure of vikingite Vik50, Ag3.5 Pb11.0 Bi11.5 S30

  • Original language description

    Crystal structure of Sb-rich vikingite with lillianite substitution percentage L% below 50 % from Kutná Hora ore district, Czech Republic, was solved and refined from single-crystal diffraction data to determine the site populations of metal sites concerning a) the decreasing “lillianite“ substitution 2 Pb2+ = Ag+ + Bi3+ b) Sb content not known in vikingite from; other localities throughout the world. Vikingite is monoclinic, C2/m, with a = 13.5394(10), b = 4.0992(3), c = 25.506(3) Å, β = 95.597(8)°, V = 1408.9(2) Å3, Z = 1, Dc = 7.0412 g/cm3. The structural formula derived from the refinement is Ag2.85 Pb12.35 (Bi9.52 Sb1.27)Σ=10.80 S30, corresponding to Vik40.0. The structure of vikingite is composed of thinner slabs (4L) of four octahedra Me2–Me1–Me1–Me2 and thicker slabs (7L) of seven octahedra Me4–Me5–Me6–Me7–Me6–Me5–Me4 separated by Pb atoms Me3 in trigonal prismatic coordination. The refinement showed differences between the structures of Vik40 and the previously published structure of Vik50. The drop of L% below 50 % shows most profoundly in the marginal octahedral site Me2 of the thinner4L slabs, which becomes a Bi–Pb–Ag site with 28.6 % of silver next to 50 % of Bi and 21.4 % of Pb. The central Me1 site from4L slabs which is almost a pure Bi site in Vik50 (0.97 Bi + 0.3 Ag) becomes a Bi-Pb site with minor Sb (0.54 Bi + 0.06 Sb + 0.40 Pb) in Vik40. The Sb for Bi substitution was found to take place in the semimarginal site Me5 (0.74 Bi + 0.26 Sb) in the thicker7L slabs, which is a pure Bi site in Sb-free Vik50. Another important change against Vik50 occurs in central octahedral site Me6 (pure Pb site in Vik50), which becomes – despite the decrease in Bi content with decreasing L% – a Pb–Bi mix site. The correctness of the refined structural model was verified and the occupancies of mixed sites were fine-tuned employing charge distribution calculations in program ECoN21. In Vik40 weighted average bond lengths RAV of the marginal sites Me2 and Me4 and of the central site Me1 are significantly larger than in Vik50, reflecting the lower Ag content and the presence of Pb, while the Bi site Me5, which is partly substituted by Sb and the site Me6 with minor Bi at the expense of Pb exhibit adequately shortened RAV values. © 2021, Czech Geological Survey. All rights reserved.

  • 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

    10500 - Earth and related environmental sciences

Result continuities

  • Project

    <a href="/en/project/GA15-18917S" target="_blank" >GA15-18917S: Anomalous Bi-Sb substitution in sulphosalts of Kutna Hora ore district as an indicator of genetic conditions of the hydrotermal mineralization origin</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2021

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Journal of Geosciences

  • ISSN

    1802-6222

  • e-ISSN

    1803-1943

  • Volume of the periodical

    66

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    CZ - CZECH REPUBLIC

  • Number of pages

    10

  • Pages from-to

    175-184

  • UT code for WoS article

    000718259900005

  • EID of the result in the Scopus database

    2-s2.0-85119122852