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• W3042815087 abstract "Abstract The intriguing functional nature of ceramics containing rare earth sesquioxide (RES) is associated with the type of polymorphic structure they crystallize into. They prefer to be in the cubic, monoclinic or hexagonal structure in the increasing order of cation size, R RE . Since the functional properties of these ceramics varies with R RE , temperature and pressure, a systematic investigation delineating the cation size effect is indispensable. In the present work we report the structural stability and compressibility behaviour of the RES ceramics, (Eu 1− x La x ) 2 O 3 , of RESs with dissimilar structure and significant difference in cationic radii. The selected compositions of (Eu 1− x La x ) 2 O 3 have been studied using the in-situ high pressure synchrotron X-ray diffraction and the structural parameters obtained through Rietveld refinement. The cubic structure, which is stable for 0.95 Å $$le$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mo>≤</mml:mo></mml:math> R RE $$<,0.98$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mrow><mml:mo><</mml:mo><mml:mspace /><mml:mn>0.98</mml:mn></mml:mrow></mml:math> Å at ambient temperature and pressure (ATP), prefers a cubic to hexagonal transition at high pressures. The biphasic region of cubic and monoclinic structure, which is stable for 0.98 Å $$le$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mo>≤</mml:mo></mml:math> R RE $$<,1.025$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mrow><mml:mo><</mml:mo><mml:mspace /><mml:mn>1.025</mml:mn></mml:mrow></mml:math> Å at ATP, prefers a cubic/monoclinic to hexagonal transition at high pressures. Further, in the biphasic region of monoclinic and hexagonal structure, observed for 1.025 Å $$le$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mo>≤</mml:mo></mml:math> R RE $$<,1.055$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mrow><mml:mo><</mml:mo><mml:mspace /><mml:mn>1.055</mml:mn></mml:mrow></mml:math> Å, the monoclinic phase is found to be progressing towards the hexagonal phase with increasing pressure. The pure hexagonal phase obtained for 1.055 Å $$le$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mo>≤</mml:mo></mml:math> R RE $$le$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mo>≤</mml:mo></mml:math> 1.10 Å is found to be structurally stable at high pressures. The bulk moduli are obtained from the Birch–Murnaghan equation of state fit to the compressibility data and its dependance on the cation size is discussed. The microstrain induced by the difference in cation size causes an internal pressure in the crystal structure leading to a reduction in the bulk modulus of $$textit{x}=0.2$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML><mml:mrow><mml:mi>x</mml:mi><mml:mo>=</mml:mo><mml:mn>0.2</mml:mn></mml:mrow></mml:math> and 0.6. A pressure–concentration (P– x ) phase diagram upto a pressure of 25 GPa is constructed for (Eu 1− x La x ) 2 O 3 . This would provide an insight to the fundamental and technological aspects of these materials and the RESs in general." @default.
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• W3042815087 date "2020-07-16" @default.
• W3042815087 modified "2023-10-16" @default.
• W3042815087 title "Structural phase transition, equation of state and phase diagram of functional rare earth sesquioxide ceramics (Eu1−xLax)2O3" @default.
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• W3042815087 doi "https://doi.org/10.1038/s41598-020-68400-9" @default.
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