Structural investigation of cooperite (PtS) crystals
- Authors: Rozhdestvina V.I.1, Udovenko A.A.2, Rubanov S.V.3, Mudrovskaya N.V.1
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Affiliations:
- Institute of Geology and Nature Management, Far East Branch
- Institute of Chemistry, Far East Branch
- Bio21 Institute
- Issue: Vol 61, No 2 (2016)
- Pages: 193-202
- Section: Structure of Inorganic Compounds
- URL: https://journals.rcsi.science/1063-7745/article/view/189808
- DOI: https://doi.org/10.1134/S1063774516020176
- ID: 189808
Cite item
Abstract
The single-crystal structure of cooperite, a natural platinum sulfide PtS, is studied by X-ray diffraction supported by high-resolution scanning transmission electron microscopy and X-ray spectrum microanalysis. It is found that, in addition to the main reflections corresponding to the known tetragonal cell (a = 3.47 and c = 6.11 Å; space group P42/mmc), many weak reflections with intensities I ≤ 60σ(I) are clearly observed. These reflections fit the tetragonal cell (space group I4/mmm) with doubled parameters. In structures with small (P42/mmc) and large (I4/mmm) cells, the S atoms occupy statistically two special positions. It is shown that the chemical composition of the cooperite crystals deviates from the stoichiometric composition: sulfur-deficient specimens predominate.
About the authors
V. I. Rozhdestvina
Institute of Geology and Nature Management, Far East Branch
Author for correspondence.
Email: veronika@ascnet.ru
Russian Federation, ul. Zeiskaya 239, Blagoveshchensk, 675000
A. A. Udovenko
Institute of Chemistry, Far East Branch
Email: veronika@ascnet.ru
Russian Federation, pr. 100-letiya Vladivostoka, Vladivostok, 690022
S. V. Rubanov
Bio21 Institute
Email: veronika@ascnet.ru
Australia, Flemington Road 30, Melbourne, Victoria, 3052
N. V. Mudrovskaya
Institute of Geology and Nature Management, Far East Branch
Email: veronika@ascnet.ru
Russian Federation, ul. Zeiskaya 239, Blagoveshchensk, 675000