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)

  • 2014In situ synchrotron X-ray diffraction and dilatometric study of austenite formation in a multi-component steel: Influence of initial microstructure and heating rate62citations

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Aeby-Gautier, Elisabeth
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Geandier, Guillaume
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Teixeira, Julien
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Denand, Benoît
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Dehmas, Moukrane
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Esin, Vladimir A.
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Denis, Sabine
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Sourmail, T.
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2014

Co-Authors (by relevance)

  • Aeby-Gautier, Elisabeth
  • Geandier, Guillaume
  • Teixeira, Julien
  • Denand, Benoît
  • Dehmas, Moukrane
  • Esin, Vladimir A.
  • Denis, Sabine
  • Sourmail, T.
OrganizationsLocationPeople

article

In situ synchrotron X-ray diffraction and dilatometric study of austenite formation in a multi-component steel: Influence of initial microstructure and heating rate

  • Aeby-Gautier, Elisabeth
  • Geandier, Guillaume
  • Teixeira, Julien
  • Denand, Benoît
  • Dehmas, Moukrane
  • Bihan, Quentin Le
  • Esin, Vladimir A.
  • Denis, Sabine
  • Sourmail, T.
Abstract

The formation of austenite during both slow and fast heating (0.25–100 °C s−1) was investigated for different microstructures of a selected low-alloy steel. With the simultaneous use of dilatometry and high-energy X-ray diffraction, it was possible to follow not only the global progress of the austenitization, but also the individual evolutions of each phase (ferrite, cementite and retained austenite if present in the initial microstructure). The results confirm earlier published data regarding the ease of austenitization of different initial microstructures (ferrite–pearlite, bainite and tempered martensite). More importantly, two stages were clearly identified, corresponding to the simultaneous transformation of ferrite and cementite, followed by the progressive disappearance of the remaining ferrite. While this is well known for ferrite–pearlite microstructures, it is not yet documented for bainite and tempered martensite. Microstructure evolution calculations based on a diffusion-controlled mechanism helped rationalize the differences observed between the three initial microstructures. In addition, they also strongly suggested the existence of a critical carbide size beyond which the second austenitization phase would correspond to carbide dissolution instead of ferrite transformation.

Topics
  • impedance spectroscopy
  • microstructure
  • phase
  • x-ray diffraction
  • carbide
  • steel
  • dilatometry