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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Materials Map under construction

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)

  • 2017Field-induced structural transition and irreversible domain detwinning in the antiferromagnet Fe 1.1 Te6citations

Places of action

Chart of shared publication
Fabrèges, X.
1 / 3 shared
Detlefs, C.
1 / 10 shared
Knafo, W.
1 / 2 shared
Viennois, R.
1 / 2 shared
Duc, Fabienne
1 / 4 shared
Chart of publication period
2017

Co-Authors (by relevance)

  • Fabrèges, X.
  • Detlefs, C.
  • Knafo, W.
  • Viennois, R.
  • Duc, Fabienne
OrganizationsLocationPeople

article

Field-induced structural transition and irreversible domain detwinning in the antiferromagnet Fe 1.1 Te

  • Fabrèges, X.
  • Detlefs, C.
  • Knafo, W.
  • Viennois, R.
  • Duc, Fabienne
  • Roth, T.
Abstract

Single-crystal x-ray diffraction in pulsed magnetic fields of up to 31 T was used to investigate the iron telluride antiferromagnet Fe1.1Te, which is a parent of the Fe-based chalcogenide superconductors. At temperatures below the Néel temperature TN≃60 K, high magnetic fields perpendicular to the c axis lead to an irreversible detwinning of the crystal at the field HR, where magnetocrystalline domains are selected by a moment reorientation process. Just below TN, the onset of a structural transition at the critical field HC>HR, which delimits the antiferromagnet phase, indicates a partial restoration of the high-temperature tetragonal symmetry. The lattice and magnetic answers to an in-plane magnetic field are discussed, emphasizing the strength of magnetoelastic coupling in Fe1.1Te.

Topics
  • impedance spectroscopy
  • phase
  • x-ray diffraction
  • strength
  • iron