Synthesis and Low-Temperature Thermodynamic Functions of Platinum Ditelluride
- Authors: Chareev D.A.1,2,3,4, Tyurin A.V.5, Polotnyanko N.A.1, Chareeva P.V.6
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Affiliations:
- Dubna State University
- Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences
- Institute of Physics and Technology, Yeltsin Federal University
- Kazan (Volga Region) Federal University
- Kurnakov Institute of General and Inorganic Chemistry, Russian Academy of Sciences, Moscow, Russia
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
- Issue: Vol 59, No 8 (2023)
- Pages: 859-865
- Section: Articles
- URL: https://journals.rcsi.science/0002-337X/article/view/231965
- DOI: https://doi.org/10.31857/S0002337X23080031
- EDN: https://elibrary.ru/SIADFD
- ID: 231965
Cite item
Abstract
In this paper, we report the synthesis of crystalline platinum ditelluride, PtTe2, a synthetic analog of the mineral moncheite, and its thermodynamic properties. Using the isobaric heat capacity of PtTe2 determined in the range 2–305 K by the relaxation and adiabatic calorimetry methods, we have evaluated its standard thermodynamic functions: entropy, enthalpy increment, and reduced Gibbs energy. The following parameters have been obtained for PtTe2 at 298.15 K:
= 75.11 ± 0.15 J/(K mol), S° = 121.5 ± 0.2 J/(K mol), Н°(298.15 K) − Н°(0) = 16.69 ± 0.03 kJ/mol, and Ф° = 65.55 ± 0.13 J/(K mol). Using data in the literature and handbooks, we have estimated the standard Gibbs energy of formation of PtTe2: ΔfG°(PtTe2, cr, 298.15) = –75.4 ± 0.8 kJ/mol. Fractal analysis of the heat capacity data indicates that PtTe2 has a layered structure and that its Debye temperature is 250 K.
About the authors
D. A. Chareev
Dubna State University; Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences; Institute of Physics and Technology, Yeltsin Federal University; Kazan (Volga Region) Federal University
Email: d.chareev@gmail.com
141982, Dubna, Moscow oblast, Russia; 142432, Chernogolovka, Noginskii raion, Moscow oblast, Russia; 620002, Yekaterinburg, Russia; 420008, Kazan, Tatarstan, Russia
A. V. Tyurin
Kurnakov Institute of General and Inorganic Chemistry, Russian Academy of Sciences, Moscow, Russia
Email: fomina@igic.ras.ru
119991, Moscow, Russia
N. A. Polotnyanko
Dubna State University
Email: d.chareev@gmail.com
141982, Dubna, Moscow oblast, Russia
P. V. Chareeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
Author for correspondence.
Email: d.chareev@gmail.com
119017, Moscow, Russia
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