Structural transformations of dysprosium up to 337 GPa

The structures and equations of states of dysprosium have been studied up to 337 GPa without a pressure transmitting medium using synchrotron x-ray diffraction. Beyond the previously reported transition sequences, namely hP2 \ensuremath{\rightarrow} hR9 \ensuremath{\rightarrow} hP4 \ensuremath{\rightarrow} hR24 \ensuremath{\rightarrow} oF16, we herein disclose an isosymmetric structural transition that occurs above 195.5 GPa, wherein the structure transforms from orthorhombic face-centered oF16 to oF8. The oF8 phase comprises eight atoms per unit cell and belongs to the space group Fddd, being isostructural with lanthanides Nd-VI, Sm-VI, and actinides Am-III, Cf-III, and Cm-IV. During the phase transition, the reduction in lattice volume occurs continuously and is concomitant with the expansion along the $b$ axis, manifesting negative linear compressibility and an increasing degree of anisotropy. Our finding further corroborates the intimate structural correlation between lanthanides and actinides.

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Publication Details

Journal
Physical review. B./Physical review. B
Published
2025-02-20
DOI
https://doi.org/10.1103/physrevb.111.064112
Citations
2
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
3.73

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article

Structural transformations of dysprosium up to 337 GPa

Yongjun Tian, Jing Song, Bing Li, Hechong Wang et al.
2 citations
Physical review. B./Physical review. B
High-pressure geophysics and materials
3.73
article

Structural transformations of dysprosium up to 337 GPa

Yongjun Tian, Jing Song, Bing Li, Hechong Wang, Hongkai Li, Saori I. Kawaguchi, Guoying Gao, Zhongyan Wu, Mingyu Li, Lin Wang, Shaojie Wang, Ke Yang
article en
2 citations

Abstract

The structures and equations of states of dysprosium have been studied up to 337 GPa without a pressure transmitting medium using synchrotron x-ray diffraction. Beyond the previously reported transition sequences, namely hP2 \ensuremath{\rightarrow} hR9 \ensuremath{\rightarrow} hP4 \ensuremath{\rightarrow} hR24 \ensuremath{\rightarrow} oF16, we herein disclose an isosymmetric structural transition that occurs above 195.5 GPa, wherein the structure transforms from orthorhombic face-centered oF16 to oF8. The oF8 phase comprises eight atoms per unit cell and belongs to the space group Fddd, being isostructural with lanthanides Nd-VI, Sm-VI, and actinides Am-III, Cf-III, and Cm-IV. During the phase transition, the reduction in lattice volume occurs continuously and is concomitant with the expansion along the $b$ axis, manifesting negative linear compressibility and an increasing degree of anisotropy. Our finding further corroborates the intimate structural correlation between lanthanides and actinides.

Physical review. B./Physical review. BVol. 111(6)
Changchun Normal University (CN), Yanshan University (CN), Japan Synchrotron Radiation Research Institute (JP), Shanghai Synchrotron Radiation Facility
National Natural Science Foundation of China, Natural Science Foundation of Hebei Province
Openalex Percentile: Top 10%
High-pressure geophysics and materials
3.73
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