Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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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)

  • 2022Variable Temperature Neutron Diffraction Study of the Oxide Ion Conductor Ba3VWO8.511citations

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Fop, Sacha
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Ritter, Clemens
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Gilane, Asma
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Mclaughlin, Abbie
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2022

Co-Authors (by relevance)

  • Fop, Sacha
  • Ritter, Clemens
  • Gilane, Asma
  • Mclaughlin, Abbie
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article

Variable Temperature Neutron Diffraction Study of the Oxide Ion Conductor Ba3VWO8.5

  • Fop, Sacha
  • Ritter, Clemens
  • Gilane, Asma
  • Mclaughlin, Abbie
  • Tawse, Dylan
Abstract

Ba3VWO8.5 is an oxide ion conductor with a bulk conductivity of 5.0 x 10-5 S cm-1 at 600 °C. Ba3VWO8.5 is anomalous to the other Ba3M’M’’O8.5 (M’ = Nb; M’’= Mo, W) oxide ionic conductors, as it exhibits cation order with vanadium and tungsten on the M1 site only. Here we report a variable temperature neutron diffraction study of Ba3VWO8.5 that demonstrates cation order is retained up to 800 °C. We show for the first time that the structural rearrangements reported for hexagonal perovskite derivatives Ba3M’M’’O8.5 are dictated by water absorption. The significant water uptake in Ba3M’M’’O8.5 (M’ = Nb; M’’= Mo, W) arises due to the flexibility of the crystal structure, whereby upon absorption of water, a fraction of the transition metal cations moves from the M1 site to the octahedral M2 site. The results presented here demonstrate that the presence of 50% V5+ on the M1 site, which has a strong preference for tetrahedral geometry, is enough to disrupt the flexibility of the cation sublattice resulting in the ordering of the cations exclusively on the M1 site and no significant water absorption.

Topics
  • perovskite
  • impedance spectroscopy
  • neutron diffraction
  • tungsten
  • vanadium