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)

  • 2021A pressure induced reversal to the 9R perovskite in Ba3MoNbO8.54citations

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Chart of shared publication
Skakle, Jan
1 / 11 shared
Bull, C. L.
1 / 6 shared
Fop, Sacha
1 / 4 shared
Wildman, Eve
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Ridley, C. J.
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Mclaughlin, Abbie
1 / 13 shared
Chart of publication period
2021

Co-Authors (by relevance)

  • Skakle, Jan
  • Bull, C. L.
  • Fop, Sacha
  • Wildman, Eve
  • Ridley, C. J.
  • Mclaughlin, Abbie
OrganizationsLocationPeople

article

A pressure induced reversal to the 9R perovskite in Ba3MoNbO8.5

  • Skakle, Jan
  • Bull, C. L.
  • Fop, Sacha
  • Sherwood, Brent
  • Wildman, Eve
  • Ridley, C. J.
  • Mclaughlin, Abbie
Abstract

Ba3MoNbO8.5 is an oxide ion conductor with an unconventional hybrid crystal structure that is intermediate between the 9R-perovskite (A3B3O9) and the palmierite (A3B2O8). The crystal structure is highly disordered with vacancies distributed across two cation (M(1) and M(2)) and oxygen sites (O(2) and O(3)), with Mo and Nb in variable coordinate environments. M(1)–O(1)–O(2) and M(2)–O(1) sites are associated with the formation of (Mo,Nb)O6 octahedra, whilst tetrahedral units are composed of M(1)–O(1)–O(3) atoms. Upon increasing the temperature, the structure undergoes a change in occupancy in favour of the O(3) site, which results in a change in metal co-ordination as the tetrahedral to octahedral ratio increases. We demonstrate that the structure can also be tuned using externally applied pressure. Variable pressure studies ≤4.8 GPa indicate that densification of the unit cell induces the reverse effect, as the occupancy of the O(2) site increases and the palmierite contribution is suppressed. Our results strongly suggest that by 5.2 GPa the O(3) position will be completely empty as the 9R unit cell stabilises with a network of octahedral MO6 units. Pressure induces a flattening of M(1)O4 tetrahedra in the palmierite layers, as M(1)O6 octahedra become more regular in geometry. Bond valence site energy calculations show that pressure increases the height of all energy barriers to migration along the three-dimensional diffusion pathways, increasing the energy of the dominant pathway from 0.35 to 0.95 eV. The relaxation energy, E2, disappears above 2.8 GPa, when the average polyhedral distortion (σ(R)) falls below 0.07 Å, indicating the existence of a critical minimum. The bulk modulus of Ba3MoNbO8.5 is exceptionally low (50(2) GPa) for a layered oxide material and is closer to that of the halide perovskites. These results demonstrate a high degree of flexibility, in terms of the softness of the lattice and variable metal coordination, emphasising the potential for these materials in multi sensory and thin film applications.

Topics
  • perovskite
  • impedance spectroscopy
  • thin film
  • Oxygen
  • layered
  • densification
  • bulk modulus