Materials Map

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (1/1 displayed)

  • 2011The influence of the Jahn-Teller effect at Fe2+ on the structure of chromite at high pressure44citations

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Chart of shared publication
Yamanaka, T.
1 / 1 shared
Gramsch, S. A.
1 / 1 shared
Hemley, R. J.
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Mysen, B. O.
1 / 2 shared
Ahart, M.
1 / 1 shared
Mao, H. K.
1 / 2 shared
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2011

Co-Authors (by relevance)

  • Yamanaka, T.
  • Gramsch, S. A.
  • Hemley, R. J.
  • Mysen, B. O.
  • Ahart, M.
  • Mao, H. K.
OrganizationsLocationPeople

article

The influence of the Jahn-Teller effect at Fe2+ on the structure of chromite at high pressure

  • Yamanaka, T.
  • Gramsch, S. A.
  • Hemley, R. J.
  • Mysen, B. O.
  • Kyono, A.
  • Ahart, M.
  • Mao, H. K.
Abstract

The crystal structure of chromite FeCr2O4 was investigated to 13.7 GPa and ambient temperature with single-crystal x-ray diffraction techniques. The unit-cell parameter decreases continuously from 8.3832(5) to 8.2398(11) A up to 11.8 GPa. A fit to the Birch-Murnaghan equation of state (EoS) based on the P-V data gives: K0 = 209(13) GPa, K' = 4.0 (fixed), and V0 = 588(1) A3. The FeO4 tetrahedra and CrO6 octahedra are compressed isotropically with pressure with their Fe-O and Cr-O bond distances decreasing from 1.996(6) to 1.949(7) A and from 1.997(3) to 1.969(7) A, respectively. The tetrahedral site occupied by the Fe2+ cation is more compressible than the octahedral site occupied by the Cr3+ cation. The resulting EoS parameters for the tetrahedral and the octahedral sites are K0 = 147(9) GPa, K' = 4.0 (fixed), V0 = 4.07(1) A3 and K0 = 275(24) GPa, K' = 4.0 (fixed), V0 = 10.42(2) A3, respectively. A discontinuous volume change is observed between 11.8 and 12.6 GPa. This change indicates a phase transition from a cubic (space group Fd-3m) to a tetragonal structure (space group I41/amd). At the phase transition boundary, the two Cr-O bonds parallel to the c-axis shorten from 1.969(7) to 1.922(17) A and the other four Cr-O bonds parallel to the ab plane elongate from 1.969(7) to 1.987(9) A. This anisotropic deformation of the octahedra leads to tetragonal compression of the unit cell along the c-axis. The angular distortion in the octahedron decreases continuously up to 13.7 GPa, whereas the distortion in the tetrahedron rises dramatically after the phase transition. At the pressure of the phase transition, the tetrahedral bond angles along the c-axis direction of the unit cell begin decreasing from 109.5° to 106.6 (7)°, which generates a "stretched" tetrahedral geometry. It is proposed that the Jahn-Teller effect at the tetrahedrally coordinated Fe2+ cation becomes active with compression and gives rise to the tetrahedral angular distortion, which in turn induces the cubic-to-tetragonal transition. A qualitative molecular orbital model is proposed to explain the origin and nature of the Jahn-Teller effect observed in this structure and its role in the pressure-induced phase transition.

Topics
  • impedance spectroscopy
  • phase
  • x-ray diffraction
  • anisotropic
  • phase transition
  • space group