4.5 Article

Pressure-induced structural modifications of rare-earth hafnate pyrochlore

期刊

JOURNAL OF PHYSICS-CONDENSED MATTER
卷 29, 期 25, 页码 -

出版社

IOP PUBLISHING LTD
DOI: 10.1088/1361-648X/aa7148

关键词

oxides; high pressure; pyrochlore

资金

  1. US Department of Energy, Office of Science, Basic Energy Science [DE-SC0001089]
  2. Stanford VPGE
  3. DOE-NNSA [DE-NA0001974]
  4. DOE-BES [DE-FG02-99ER45775]
  5. NSF
  6. Argonne National Laboratory [DE-AC02-06CH11357]
  7. DOE Office of Science User Facility [DE-AC02-05CH11231]
  8. EDGE-STEM

向作者/读者索取更多资源

Complex oxides with the pyrochlore (A(2)B(2)O(7)) and defect-fluorite ((A, B)(4)O-7) structure-types undergo structural transformations under high-pressure. Rare-earth hafnates (A(2)Hf(2)O(7)) form the pyrochlore structure for A = La-Tb and the defect-fluorite structure for A = Dy-Lu. High-pressure transformations in A(2)Hf(2)O(7) pyrochlore (A = Sm, Eu, Gd) and defect-fluorite (A = Dy, Y, Yb) were investigated up to similar to 50 GPa and characterized by in situ Raman spectroscopy and synchrotron x-ray diffraction (XRD). Raman spectra at ambient pressure revealed that all compositions, including the defect-fluorites, have some pyrochlore-type short-range order. In situ high-pressure synchrotron XRD showed that all of the rare earth hafnates investigated undergo a pressure-induced phase transition to a cotunnite-like (orthorhombic) structure that begins between 18 and 25 GPa. The phase transition to the cotunnite-like structure is not complete at 50 GPa, and upon release of pressure, the hafnates transform to defect-fluorite with an amorphous component. For all compositions, in situ Raman spectroscopy showed that disordering occurs gradually with increasing pressure. Pyrochlore-structured hafnates retain their short-range order to a higher pressure (30 GPa vs. <10 GPa) than defect-fluorite-structured hafnates. Rare earth hafnates quenched from 50 GPa show Raman spectra consistent with weberite-type structures, as also reported for irradiated rare-earth stannates. The second-order Birch-Murnaghan equation of state fit gives a bulk modulus of similar to 250 GPa for hafnates with the pyrochlore structure, and similar to 400 GPa for hafnates with the defect-fluorite structure. Dy2Hf2O7 is intermediate in its response, with some pyrochlore-type ordering, based on Raman spectroscopy and the equation of state, with a bulk modulus of similar to 300 GPa. As predicted based on the similar ionic radius of Zr4+ and Hf4+, rare-earth hafnates show similar behavior to that reported for rare earth zirconates at high pressure.

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