Composition and structure of Pt chloride complexes in hydrothermal solutions, according to X-ray absorption spectroscopy
- Авторлар: Tagirov B.R.1, Trigub A.L.2, Selivanov P.V.1, Koroleva L.A.1
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Мекемелер:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- National Research Center Kurchatov Institute
- Шығарылым: Том 91, № 3 (2017)
- Беттер: 543-548
- Бөлім: Structure of Matter and Quantum Chemistry
- URL: https://journal-vniispk.ru/0036-0244/article/view/169347
- DOI: https://doi.org/10.1134/S003602441703027X
- ID: 169347
Дәйексөз келтіру
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.
Негізгі сөздер
Авторлар туралы
B. Tagirov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Хат алмасуға жауапты Автор.
Email: tagir@igem.ru
Ресей, Moscow, 119017
A. Trigub
National Research Center Kurchatov Institute
Email: tagir@igem.ru
Ресей, Moscow, 123182
P. Selivanov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tagir@igem.ru
Ресей, Moscow, 119017
L. Koroleva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: tagir@igem.ru
Ресей, Moscow, 119017
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