Helium Incorporation into Scandium Fluoride, a Model Negative Thermal Expansion Material

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Abstract

Scandium trifluoride is a model negative thermal expansion (NTE) material. Its simple structure can be described as an A-site vacant perovskite, and it shows isotropic NTE over a very wide temperature range (up to ∼1100 K), due to transverse vibrational motion of the fluoride. Like many framework NTE materials, it undergoes a phase transition at low pressures, adopting a rhombohedral (R3̅c) structure at >0.7 GPa and 300 K in commonly used nonpenetrating pressure media, such as silicone oil. High pressure X-ray diffraction data and gas uptake/release measurements indicate that, on compression in helium above ∼200 K, helium is inserted into ScF3 to form the defect perovskite HexScF3. The incorporation of helium stiffens the structure and changes its phase behavior. At room temperature, complete filling of the structure with helium does not occur until >1.5 GPa. On compression, a cubic perovskite structure is maintained until ∼5 GPa. As the pressure was increased to ∼9.5 GPa, a further transition occurred at ∼7 GPa. The first transition at ∼5 GPa is likely to a tetragonal (P4/mbm) perovskite, but the detailed structure of the perovskite phase formed on compression above ∼7 GPa is unclear. Cooling down from 300 to 100 K in helium at ∼0.4 GPa leads to an approximate composition of He0.1ScF3. High pressure neutron diffraction measurements, in the temperature range 15-150 K show that the incorporation of helium increases the pressure at which the cubic (Pm3̅m) to rhombohedral (R3̅c) putative quantum structural phase transition occurs from close to 0 GPa to ∼0.2 GPa at 0 K.

Original languageEnglish
Pages (from-to)1657-1666
Number of pages10
JournalChemistry of Materials
Volume37
Issue number4
DOIs
StatePublished - Feb 25 2025

Funding

The work at Georgia Tech was partially supported under NSF DMR-1607316 and NSF DMR-2002739. Use of the COMPRES-GSECARS gas loading system was supported by COMPRES under NSF Cooperative Agreement EAR-1661511 and by GSECARS through NSF grant EAR-1634415. Portions of this work were performed at HPCAT (Sector 16) and at GeoSoilEnviroCARS (The University of Chicago, Sector 13), Advanced Photon Source (APS), Argonne National Laboratory. HPCAT operations are supported by DOE-NNSA’s Office of Experimental Sciences. The Advanced Photon Source is a U.S. Department of Energy (DOE) Office of Science User Facility operated for the DOE Office of Science by Argonne National Laboratory under Contract no. DE-AC02-06CH11357. We are grateful for assistance from sample environment team members, Mark Loguillo and Matt Rucker, at the Spallation Neutron Source, Oak Ridge National Laboratory. A portion of this research used resources at the Spallation Neutron Source, a DOE Office of Science User Facility operated by the Oak Ridge National Laboratory. Neutron beam time was allocated to the SNAP Instrument under proposal number IPTS-30415 and the helium uptake a release measurements were performeed under proposal number IPTS-31233.

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