“…On the other hand, the smelting redox conditions were often inferred from the assemblage of slag mineralogical phases, using as references the oxygen buffer curves (e.g., Quartz-Fayalite-Magnetite oxygen buffer) in the oxygen fugacity-temperature space [15,16]. However, because equilibrium is rarely attained, it was suggested that a reliable proxy for oxygen fugacity is the iron oxidation state in slags, which can be expressed as the ferric/ferrous ratio (Fe 3+ /Fe 2+ ) [17,18]. This redox-sensitive ratio is usually measured by Mössbauer spectroscopy, XANES spectroscopy, and redox titration (i.e., "wet chemistry") [19,20].…”