Composition and structure of Pt chloride complexes in hydrothermal solutions, according to X-ray absorption spectroscopy


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Abstract

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.

About the authors

B. R. Tagirov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Author for correspondence.
Email: tagir@igem.ru
Russian Federation, Moscow, 119017

A. L. Trigub

National Research Center Kurchatov Institute

Email: tagir@igem.ru
Russian Federation, Moscow, 123182

P. V. Selivanov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tagir@igem.ru
Russian Federation, Moscow, 119017

L. A. Koroleva

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: tagir@igem.ru
Russian Federation, Moscow, 119017

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