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Article

Thermal, Structural, and Phase Evolution of the Y2(SO4)3*8H2O–Eu2(SO4)3*8H2O System via Dehydration and Volatilization to Y2(SO4)3–Eu2(SO4)3 and Y2O2(SO4)–Eu2O2(SO4) and Its Thermal Expansion

by
Andrey P. Shablinskii
1,
Olga Yu. Shorets
1,
Rimma S. Bubnova
1,
Maria G. Krzhizhanovskaya
2,
Margarita S. Avdontceva
2 and
Stanislav K. Filatov
2,*
1
Grebenchikov Institute of Silicate Chemistry, Makarova Embankment 2, Saint Petersburg 199034, Russia
2
Institute of Earth Sciences, St. Petersburg State University, Universitetskaya Embankment. 7/9, Saint Petersburg 199034, Russia
*
Author to whom correspondence should be addressed.
Minerals 2025, 15(12), 1304; https://doi.org/10.3390/min15121304 (registering DOI)
Submission received: 14 November 2025 / Revised: 9 December 2025 / Accepted: 10 December 2025 / Published: 14 December 2025
(This article belongs to the Special Issue Crystal Chemistry of Sulfate Minerals and Synthetic Compounds)

Abstract

The synthesis, crystal structure, phase transformations, and thermal expansion of (Y1–xEux)2(SO4)3*8H2O (where x = 0, 0.17, 0.33, 0.50, 0.66, 0.83, and 1) are presented. (Y1–xEux)2(SO4)3*8H2O solid solutions were synthesized via crystallization from an aqueous solution. (Y1–xEux)2(SO4)3*8H2O (C2/c) ↔ (Y1–xEux)2(SO4)3 (Pbcn) → (Y1–xEux)2O2SO4 (C2/c) and Eu2(SO4)3*8H2O (C2/c) ↔ Eu2(SO4)3 (C2/c) → Eu2O2SO4 (C2/c) phase transformations for all samples were investigated by high-temperature powder X-ray diffraction, differential scanning calorimetry and thermogravimetry in the temperature ranges of 25–750 and 25–1350 °C, respectively. The aim of this work is to identify the structural heredity of the phases formed during thermal transformations of (Y1–xEux)2(SO4)3*8H2O solid solutions, and to study the mechanisms of the thermal deformations of the crystal structure. Structural relations between these phases were found. The crystal structures of YEu(SO4)3*8H2O and (Y0.83Eu0.17)2(SO4)3*8H2O were refined at −173, −123, −73, −23, 27, and 77 °С. Thermal expansion coefficients for (Y1–xEux)2(SO4)3*8H2O, Eu2(SO4)3, (Y1–xEux)2O2SO4 (where x = 0, 0.17, 0.33, 0.50, 0.66, 0.83, and 1) compounds and solid solutions were calculated for the first time. The thermal expansion of Eu2(SO4)3 was highest in the direction approximately coinciding with the c-axis, because the Eu–O chains extended in this direction. As temperature increased, the crystal structure of (Y1–xEux)2(SO4)3*8H2O expanded significantly in the ac plane along directions close to the a and c axes, while thermal expansion along the b axis was relatively low. The distance between layers in the (Y1–xEux)2(SO4)3*8H2O crystal structure increased with increasing temperature, and corrugated layers (parallel to (101) direction) straightened out due to the rotation of the S2O4 tetrahedra. At high temperature, thermal expansion of Y2O2SO4 was highest along the longer diagonal of the ac parallelogram perpendicular to the plane of the oxo-centered 2[YO] layers.
Keywords: sulfates; rare earth; dehydration; crystal structure; thermal expansion; negative thermal expansion; structural evolution sulfates; rare earth; dehydration; crystal structure; thermal expansion; negative thermal expansion; structural evolution

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MDPI and ACS Style

Shablinskii, A.P.; Shorets, O.Y.; Bubnova, R.S.; Krzhizhanovskaya, M.G.; Avdontceva, M.S.; Filatov, S.K. Thermal, Structural, and Phase Evolution of the Y2(SO4)3*8H2O–Eu2(SO4)3*8H2O System via Dehydration and Volatilization to Y2(SO4)3–Eu2(SO4)3 and Y2O2(SO4)–Eu2O2(SO4) and Its Thermal Expansion. Minerals 2025, 15, 1304. https://doi.org/10.3390/min15121304

AMA Style

Shablinskii AP, Shorets OY, Bubnova RS, Krzhizhanovskaya MG, Avdontceva MS, Filatov SK. Thermal, Structural, and Phase Evolution of the Y2(SO4)3*8H2O–Eu2(SO4)3*8H2O System via Dehydration and Volatilization to Y2(SO4)3–Eu2(SO4)3 and Y2O2(SO4)–Eu2O2(SO4) and Its Thermal Expansion. Minerals. 2025; 15(12):1304. https://doi.org/10.3390/min15121304

Chicago/Turabian Style

Shablinskii, Andrey P., Olga Yu. Shorets, Rimma S. Bubnova, Maria G. Krzhizhanovskaya, Margarita S. Avdontceva, and Stanislav K. Filatov. 2025. "Thermal, Structural, and Phase Evolution of the Y2(SO4)3*8H2O–Eu2(SO4)3*8H2O System via Dehydration and Volatilization to Y2(SO4)3–Eu2(SO4)3 and Y2O2(SO4)–Eu2O2(SO4) and Its Thermal Expansion" Minerals 15, no. 12: 1304. https://doi.org/10.3390/min15121304

APA Style

Shablinskii, A. P., Shorets, O. Y., Bubnova, R. S., Krzhizhanovskaya, M. G., Avdontceva, M. S., & Filatov, S. K. (2025). Thermal, Structural, and Phase Evolution of the Y2(SO4)3*8H2O–Eu2(SO4)3*8H2O System via Dehydration and Volatilization to Y2(SO4)3–Eu2(SO4)3 and Y2O2(SO4)–Eu2O2(SO4) and Its Thermal Expansion. Minerals, 15(12), 1304. https://doi.org/10.3390/min15121304

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