4.6 Article

Structural evolution of single-crystal RECrO3 (RE = Y, Eu-Lu) orthochromates

Journal

JOURNAL OF SOLID STATE CHEMISTRY
Volume 313, Issue -, Pages -

Publisher

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jssc.2022.123298

Keywords

Multiferroics; Orthochromates; X-ray diffraction; Crystal structures

Funding

  1. opening project of State Key Laboratory of High Performance Ceramics and Superfine Microstructure [SKL201907SIC]
  2. Science and Technology Development Fund, Macao SAR [0051/2019/AFJ, 0090/2021/A2, 0049/2021/AGJ]
  3. Guangdong Basic and Applied Basic Research Foundation [2020B1515120025]
  4. University of Macau [MYRG2020-00278-IAPME, EF030/IAPME-LHF/2021/GDSTIC]
  5. Guangdong-Hong Kong-Macao Joint Laboratory for Neutron Scattering Science and Technology [2019B121205003]

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In-house X-ray powder diffraction was used to study the room-temperature structural evolution of orthochromate RECrO3 (RE = Y, Eu-Lu) single crystals grown by the floating-zone method with a laser-diode furnace. An anomaly in the evolution of lattice parameters was found in the LuCrO3 single crystal, possibly due to the loss of both spin and orbital angular moments of Lu3+ ions leading to the disappearance of magnetostriction effect. The evolution of Bragg (0 2 0), (1 1 2), (2 0 0), and (0 2 1) peaks was monitored, showing regular variations with rare-earth ionic radius indicating changes in lattice constants.
In-house X-ray powder diffraction has been employed to study the room-temperature structural evolution of orthochromate RECrO3 (RE ?= ?Y, Eu-Lu) single crystals grown by the floating-zone method with a laser-diode furnace. Structural refinements reveal an anomaly in the evolution of lattice parameters versus RE ionic radius. This anomaly occurred to the LuCrO3 single crystal and may be attributed to the disappearance of magnetostriction effect due to the loss of both spin and orbital angular moments of Lu3+ ions. Moreover, we have monitored the evolution of Bragg (0 2 0), (1 1 2), (2 0 0), and (0 2 1) peaks, which has varied in a regular basis with rare-earth ionic radius indicative of changes in lattice constants.

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