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 (3/3 displayed)

  • 2012Isothermal martensite formation at sub-zero temperatures1citations
  • 2011Isothermal martensite formation at sub-zero temperatures12citations
  • 2010Isothermal martensite formation at sub-zero temperaturescitations

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Somers, Marcel Adrianius Johannes
3 / 195 shared
Hansen, Mikkel Fougt
3 / 36 shared
Stojko, Allan
3 / 4 shared
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2012
2011
2010

Co-Authors (by relevance)

  • Somers, Marcel Adrianius Johannes
  • Hansen, Mikkel Fougt
  • Stojko, Allan
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document

Isothermal martensite formation at sub-zero temperatures

  • Somers, Marcel Adrianius Johannes
  • Hansen, Mikkel Fougt
  • Stojko, Allan
  • Slycke, Jan
Abstract

Sub-zero treatment of steels with an Mf below zero degrees Celsius relies (partly) on a continuation of the martensite formation. The present work reports on the observation of isothermal martensite formation in the sub-zero temperature regime for two steels: AISI 1070 and AISI 52100. Samples were austenitized and quenched in oil and thereafter investigated with vibrating sample agnetometry, which allows a quantitative assessment of the fraction of retained austenite as a function of the subzero temperature and time. Isothermal martensite formation was observed on interrupting the continuous cooling (5 K/min) with vibrating sample magnetometry at several temperatures in the range 80-233 K. The kinetics of isothermal martensite formation depends strongly on the temperature. Similar isothermal experiments with dilatometry indicated the occurrence of volume increase on isothermal holding, consistent with a continuation of the martensitictransformation. On prolonged isothermal holding a volume reduction was observed for AISI 52100, but not for AISI 1070. A mechanism is proposed that explains the occurrence of isothermal martensite formation.

Topics
  • impedance spectroscopy
  • experiment
  • steel
  • dilatometry