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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Lashgari, V. A.

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in Cooperation with on an Cooperation-Score of 37%

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Publications (1/1 displayed)

  • 2014Kinetics of internal oxidation of Mn-steel alloys25citations

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Kwakernaak, C.
1 / 20 shared
Zimbitas, Georgina
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Sloof, W. G.
1 / 29 shared
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2014

Co-Authors (by relevance)

  • Kwakernaak, C.
  • Zimbitas, Georgina
  • Sloof, W. G.
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article

Kinetics of internal oxidation of Mn-steel alloys

  • Lashgari, V. A.
  • Kwakernaak, C.
  • Zimbitas, Georgina
  • Sloof, W. G.
Abstract

<p>Internal oxidation of three Mn-steel alloys with 1.7, 3.5 and 7.0 wt% Mn concentration at 950 °C in a gas mixture composed of nitrogen, hydrogen and water vapor with a dew point of +10°C was evaluated. For these alloys, the kinetics of internal oxidation are diffusion-controlled and obey parabolic growth rate law. The diffusion coefficient of oxygen and manganese determined from the observed internal oxidation kinetics are 3.35 × 10<sup>−7</sup> and 4.14 × 10<sup>−12</sup>cm<sup>2</sup>/s at 950 °C, respectively. The formed internal oxide precipitates are mainly composed of MnO. The solubility product of MnO in an austenitic iron matrix is estimated to be (7.66 ± 0.18) × 10<sup>−9</sup> mol fraction<sup>2</sup> at 950 °C. The numerical simulation of concentration depth profiles of precipitated oxygen is in agreement with depth profiles determined with image analysis and X-ray microanalysis. Validity of the numerical simulation in case of the phase transformation was also tested. When a 1.7 wt% Mn-steel alloy is oxidized at 850 °C (instead of 950 °C) with a dew point of +12 °C partial phase transformation from austenite to ferrite takes place due to the Mn depletion. The associated precipitated oxygen concentration depth profile can be predicted accurately with numerical simulation.</p>

Topics
  • impedance spectroscopy
  • phase
  • simulation
  • Oxygen
  • Nitrogen
  • steel
  • Hydrogen
  • precipitate
  • iron
  • Manganese