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March 18, 2026Journal of Sustainable Metallurgy0 citationsOpen Access

Fayalitic Minerals and Slags (Part II): Physical Properties and Metal Distribution Simulation

JWJoao WeissRWTH Aachen UniversityDMDaniel Dotto MünchenRWTH Aachen UniversityHLHugo LucasRWTH Aachen University

Key Points

  • This study aims to investigate the physical properties and metal distribution of fayalitic slags through thermochemical simulations.
  • Conducted thermochemical simulations based on available databases and literature on fayalitic slag composition.
  • Examined the effects of composition changes on properties such as melting temperature, viscosity, and density.
  • Derived equations from models to simplify complex calculations and assess discrepancies between predicted and experimental results.
  • Increased CaO leads to higher melting temperatures, reaching up to 1600 °C.
  • Higher SiO2 content significantly increases viscosity, observed at values up to 3 Pa·s.
  • Increasing FeO contributes to higher density, with values reaching 3.4 g·cm −3.
  • Adding fluxes like Al2O3 and Fe2O3 alters melting temperatures, viscosity, and density, improving mineral enrichment potential.

Abstract

Abstract The interaction between fayalitic slags and nonferrous metals during smelting presents a multifaceted challenge that necessitates comprehensive investigation to enhance metallurgical processes toward the recovery of valuable metals. This study builds on the literature review of the composition and mineralogy of fayalitic slags (Part I), examining the effect of these composition on thermodynamic and physical properties, which were generated through thermochemical simulations using available databases and known studies. The findings and models created have shown that small changes in composition have significant effects on properties. For each property studied an equation was derived from the model to summarize and simplify complex calculations. Differences between predicted values and experimental results were also commented. Melting temperature, for example, increases mainly with the CaO content increase, reaching up to 1600 °C. On the other hand, SiO 2 content increase plays a more significant role in the increase of viscosity, where values of up to 3 Pa·s were observed. Meanwhile, the FeO content increase has shown significant effect on density, up to 3.4 g·cm −3 . The addition of secondary compounds (fluxes) such as Al 2 O 3 , MgO, and Fe 2 O 3 have also influenced the melting temperature, viscosity, and density of fayalitic slags, with 9 mass% Al 2 O 3 notably expanding the low-viscosity area between 0.1 and 1 Pa·s and altering density ranges, while Fe 2 O 3 effectively reduces viscosity more than CaO. The combination of these compounds further modify the properties, enhancing the potential for targeted mineral enrichment in fayalitic slags. The study demonstrates how slag composition adjustments can lower melting temperatures and viscosity, while reducing the heat input and energy needs. Regression models enable efficient fayalitic slags designs aligned with sustainable goals, thereby reducing overall carbon footprint, facilitating slag reprocessing for metal extraction, minimizing waste, and environmental impact. Graphical Abstract

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Cite This Study

Weiss et al. (2026) studied this question.

synapsesocial.com/papers/69ba44154e9516ffd37a6061https://doi.org/10.1007/s40831-026-01461-8
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