Materials Map

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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 (4/4 displayed)

  • 2024Phase equilibria and thermodynamic modelling of the PbO-ZnO-FeO-FeO1.5-SiO2 system and its subsystems in equilibrium with air/metallic lead/iron3citations
  • 2023Phase equilibria and thermodynamic modelling of the PbO–ZnO-“CuO0.5”-SiO2 system13citations
  • 2023Experiment and thermodynamic modelling of phase equilibria in PbO−“CuO0.5” and PbO−“CuO0.5”−“FeO1.5” slag systems with metal7citations
  • 2021Experimental study of “CuO0.5”-“FeO”-SiO2 and “FeO”-SiO2 systems in equilibrium with metal at 1400–1680 °C11citations

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Shevchenko, Maxim
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Jak, Evgueni
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  • Shevchenko, Maxim
  • Jak, Evgueni
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article

Experimental study of “CuO0.5”-“FeO”-SiO2 and “FeO”-SiO2 systems in equilibrium with metal at 1400–1680 °C

  • Shevchenko, Maxim
  • Jak, Evgueni
  • Wen, Xi Rui
Abstract

The phase equilibria of the “CuO”-“FeO”-SiO slag system in equilibrium with metallic copper and tridymite/cristobalite (SiO), and the “FeO”-SiO slag system in equilibrium with metallic iron and tridymite/cristobalite (SiO) were investigated between 1400 and 1680 °C. High temperature equilibration in closed silica ampoules, followed by quenching and the direct measurement of the phase compositions with the electron probe X-ray microanalysis (EPMA) was used. The liquidus isotherms in the tridymite and cristobalite (SiO) primary phase fields were measured, and the shape of the two liquid slags miscibility gap over cristobalite was determined for the “CuO”-“FeO”-SiO and “FeO”-SiO systems in equilibrium with metallic copper and iron respectively. The two liquid slags miscibility gap over cristobalite was found to be present at all Cu/(Cu+Fe) molar ratios in the slag. However, the difference in the SiO concentration between the low- and high-SiO slag was found to decrease as the Cu/(Cu+Fe) molar ratio in slag approached 0.5, with the minimal difference assessed to be approximately 4 mol.%. Additionally, new phase equilibria data obtained for the “FeO”-SiO subsystem in equilibrium with metallic iron suggested that the monotectic temperature of the subsystem is 1673 ± 3 °C, and that the low- and high- SiO slags contain 59.7 mol.% and 96.4 mol.% SiO respectively. The present study was a continuation of previous investigations by the authors into the Cu-Fe-Si-O multicomponent slag system, aimed at providing information for improving the thermodynamic models for all phases in this system.

Topics
  • impedance spectroscopy
  • phase
  • copper
  • iron
  • quenching
  • electron probe micro analysis