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Related Concept Videos

Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

12.6K
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
12.6K

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Updated: Aug 26, 2025

Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
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Samarium: from a distorted-fcc phase to melting under dynamic compression using in-situ x-ray diffraction.

Sakun Duwal1, Chad A McCoy2, Daniel H Dolan Iii2

  • 1Sandia National Laboratories, Albuquerque, NM, 87125, USA. sduwal@sandia.gov.

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|October 6, 2022
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Summary
This summary is machine-generated.

Researchers studied shocked samarium (Sm) using X-ray diffraction, revealing new phase transitions and melting points. This experimental data is crucial for refining theoretical models of lanthanide materials under extreme pressure.

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Area of Science:

  • Condensed Matter Physics
  • Materials Science
  • High-Pressure Physics

Background:

  • Understanding the behavior of f-electron systems in lanthanides is critical for developing accurate equations of state.
  • First-principles calculations like density functional theory (DFT) face challenges with f-electron interactions, necessitating precise experimental data.
  • Previous studies on shocked samarium (Sm) reported melting points that lacked direct experimental validation under shock conditions.

Purpose of the Study:

  • To experimentally determine the phase transitions and melting behavior of samarium (Sm) under shock compression.
  • To provide in-situ X-ray diffraction and temperature measurements along the Hugoniot of samarium.
  • To generate high-quality experimental data for constraining theoretical models and equations of state for lanthanides.

Main Methods:

  • In-situ X-ray diffraction measurements of shocked samarium (Sm).
  • Simultaneous measurement of temperature along the Hugoniot.
  • Analysis of diffraction patterns to identify phase transitions and melting points.

Main Results:

  • Direct experimental evidence of a distorted face-centered cubic (dfcc) phase in shocked samarium at 23 GPa.
  • Observation of melting initiation from the dfcc phase at 33 GPa (1333 K) and complete melting at 40 GPa (1468 K).
  • Significant discrepancy with previous shock melt estimations, highlighting the importance of in-situ X-ray measurements.

Conclusions:

  • The study provides the first direct experimental evidence of phase transitions and melting points for shocked samarium.
  • The obtained data offer critical benchmarks for validating and improving first-principles calculations and equation of state models for lanthanides.
  • Discrepancies with prior studies emphasize the necessity of advanced experimental techniques for accurate high-pressure material characterization.