Structural Transformations and Froodite (α-PdBi2)–Urvantsevite (β-PdBi2) Phase Transition at High Temperatures

The phase transition in structure of the PdBi2 compound has been studied using high-temperature in-situ methods (differential thermal analysis and high-temperature single-crystal X-ray diffraction). The structures of PdBi2 polymorphic modifications are refined at temperatures of 300, 373, 473, 573, and 637 K based on high-temperature single-crystal X-ray diffraction data. A low-temperature modification of α-PdBi2 corresponding to froodite occurs in a temperature range from 300K (27°C) to 573K (300°С) and is characterized by monoclinic syngony, space group C2/m (a = 12.726(1) Å, b = 4.2605(4) Å, c = 5.5668(5) Å, β = 102.51(1)°, V = 299.95(5) Å3, Z = 2). A high-temperature modification of β-PdBi2, which is registered at a temperature of 673K (400°C), has tetragonal syngony and space group I4/mmm (a = 3.3876(3) Å, c = 13.092(2) Å, V = 150.24(4) Å3, Z = 1) and is a structural analog of urvantsevite. The phase transition is referred to as type I and is a reconstructive polymorphic transformation with the rearrangement of the first coordination sphere.

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Journal
Moscow University Geology Bulletin
Published
2025-04-01
DOI
https://doi.org/10.3103/s0145875225700310
Primary Topic
Rare-earth and actinide compounds
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article
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article

Structural Transformations and Froodite (α-PdBi2)–Urvantsevite (β-PdBi2) Phase Transition at High Temperatures

N. S. Uporova, А. А. Межуева, Д. А. Чареев, O. V. Кarimova et al.
Moscow University Geology Bulletin
Rare-earth and actinide compounds
article

Structural Transformations and Froodite (α-PdBi2)–Urvantsevite (β-PdBi2) Phase Transition at High Temperatures

N. S. Uporova, А. А. Межуева, Д. А. Чареев, O. V. Кarimova, Anatoly A. Zolotarev, N. N. Eremin
article en

Abstract

The phase transition in structure of the PdBi2 compound has been studied using high-temperature in-situ methods (differential thermal analysis and high-temperature single-crystal X-ray diffraction). The structures of PdBi2 polymorphic modifications are refined at temperatures of 300, 373, 473, 573, and 637 K based on high-temperature single-crystal X-ray diffraction data. A low-temperature modification of α-PdBi2 corresponding to froodite occurs in a temperature range from 300K (27°C) to 573K (300°С) and is characterized by monoclinic syngony, space group C2/m (a = 12.726(1) Å, b = 4.2605(4) Å, c = 5.5668(5) Å, β = 102.51(1)°, V = 299.95(5) Å3, Z = 2). A high-temperature modification of β-PdBi2, which is registered at a temperature of 673K (400°C), has tetragonal syngony and space group I4/mmm (a = 3.3876(3) Å, c = 13.092(2) Å, V = 150.24(4) Å3, Z = 1) and is a structural analog of urvantsevite. The phase transition is referred to as type I and is a reconstructive polymorphic transformation with the rearrangement of the first coordination sphere.

Moscow University Geology BulletinVol. 80(2)
St Petersburg University (RU), Lomonosov Moscow State University (RU), Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry (RU), Institute of Experimental Mineralogy (RU), Zavaritsky Institute of Geology and Geochemistry (RU)
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Openalex Percentile: Top 88%
Rare-earth and actinide compounds
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Structural Transformations and Froodite (α-PdBi2)–Urvantsevite (β-PdBi2) Phase Transition at High Temperatures — N. S. Uporova, А. А. Межуева, et al. · Moscow University Geology Bulletin (2025) | TGRS Research Map | TGRS