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Updated: Jan 12, 2026

Synthesis and Microdiffraction at Extreme Pressures and Temperatures
Published on: October 7, 2013
Mfergusonite DyTaO4under compression: an insight from experiment and theory
Saheli Banerjee1, Alka B Garg1,2, Boby Joseph3
1High Pressure & Synchrotron Radiation Physics Division, Bhabha Atomic Research Centre, Mumbai 400085, India.
Dysprosium tantalate (DyTaO4) exhibits a pressure-induced structural phase transition near 24 GPa, transitioning from a monoclinic to a tetragonal phase. This study details its high-pressure behavior and structural evolution.
Area of Science:
- Materials Science
- Solid State Physics
- Crystallography
Background:
- Dysprosium orthotantalate (DyTaO4) is a rare-earth tantalate with valuable optical, dielectric, and thermal properties.
- Understanding its behavior under extreme conditions is crucial for advanced applications.
Purpose of the Study:
- To synthesize and characterize both M- and M'-type monoclinic phases of DyTaO4.
- To investigate the high-pressure behavior of the M-type DyTaO4 phase using experimental and computational methods.
Main Methods:
- Synchrotron-based X-ray diffraction (XRD) up to ~28 GPa.
- Raman spectroscopy up to ~38 GPa.
- First-principles density functional theory (DFT) calculations.
Main Results:
- Observed a pressure-induced structural phase transition near 24 GPa.
- DFT calculations predicted a transition to a tetragonal structure (P4/nbm) around 15 GPa.
- Anisotropic lattice compression was observed in the low-pressure monoclinic phase (I2/a).
- Determined the bulk modulus for the M-phase and reported Grüneisen parameters.
Conclusions:
- The study provides comprehensive insights into the high-pressure structural evolution of DyTaO4.
- Results contribute to the understanding of pressure effects on rare-earth orthotantalates.
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