Composition and structure of Pt chloride complexes in hydrothermal solutions, according to X-ray absorption spectroscopy
- Авторы: Tagirov B.R.1, Trigub A.L.2, Selivanov P.V.1, Koroleva L.A.1
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Учреждения:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- National Research Center Kurchatov Institute
- Выпуск: Том 91, № 3 (2017)
- Страницы: 543-548
- Раздел: Structure of Matter and Quantum Chemistry
- URL: https://bakhtiniada.ru/0036-0244/article/view/169347
- DOI: https://doi.org/10.1134/S003602441703027X
- ID: 169347
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Аннотация
The local atomic environment of Pt in chloride solutions is studied at 25 and 300–350°C via X-ray absorption spectroscopy. A comparison of the Pt L3-edge XANES spectra for aqueous chloride solutions and reference compounds (K2PtCl4 and K2PtCl6) shows that platinum is in oxidation state +2 at all temperatures, and the complex composition remains unchanged in the experimental range of temperatures (25–350°С) and solution compositions (m(Cltot) > 0.4 mol kg−1 of H2O). Based on EXAFS spectral analysis, the composition of the complex being dominant in chloride solutions is found to be PtCl42- with interatomic Pt–Cl distances of 2.31 ± 0.01 Å, regardless of the temperature. It is concluded that the local environments of Pt and Pd in hydrothermal solutions are similar, and the main form of transfer for these metals is a square-planar complex with four Cl ligands and identical interatomic distances.
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B. Tagirov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Автор, ответственный за переписку.
Email: tagir@igem.ru
Россия, Moscow, 119017
A. Trigub
National Research Center Kurchatov Institute
Email: tagir@igem.ru
Россия, Moscow, 123182
P. Selivanov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tagir@igem.ru
Россия, Moscow, 119017
L. Koroleva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tagir@igem.ru
Россия, Moscow, 119017
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