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)

  • 2002Back stress evolution and iso-volume fraction lines in a Cr-Ni-Mo-Al-Ti maraging steel in the process of martensitic transformation15citations

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Terasaki, T.
1 / 3 shared
Nagayama, K.
1 / 3 shared
Cailletaud, G.
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Tanaka, K.
1 / 15 shared
Fischer, Franz Dieter
1 / 19 shared
Antretter, Thomas
1 / 37 shared
Goto, S.
1 / 11 shared
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2002

Co-Authors (by relevance)

  • Terasaki, T.
  • Nagayama, K.
  • Cailletaud, G.
  • Tanaka, K.
  • Fischer, Franz Dieter
  • Antretter, Thomas
  • Goto, S.
OrganizationsLocationPeople

article

Back stress evolution and iso-volume fraction lines in a Cr-Ni-Mo-Al-Ti maraging steel in the process of martensitic transformation

  • Terasaki, T.
  • Nagayama, K.
  • Cailletaud, G.
  • Azzouz, F.
  • Tanaka, K.
  • Fischer, Franz Dieter
  • Antretter, Thomas
  • Goto, S.
Abstract

<p>The quantitative identification of the back stress evolution is carried out for a Cr-Ni-Mo-Al-Ti maraging steel in the process of martensitic transformation under thermomechanical loading conditions. The evolution depends on the direction of the applied stress: tensile, compressive or shear. The iso-volume fraction lines (the iso-ξ lines) are determined between the transformation-start and -finish lines on the applied stress-temperature plane. The iso-ξ lines are composed of a tensile-branch and a compressive-branch, each of which is parallel to the martensite-start line. The interaction point of the tensile- and compressive-branches of the iso-ξ line shifts to the direction of the back stress evolution. The almost hold stress-independent martensite-finish line, identified in a previous paper (Mater. Sci. Eng. A308 (2001) 25) is proved to be attributed to the back stress evolution.</p>

Topics
  • impedance spectroscopy
  • steel