Research demonstrates improved nickel recovery in FeNi50 alloy from laterite, suggesting reduction kinetics and oxides play key roles.
Owing to the superior reduction kinetics of limonite and goethite relative to silicates, coupled with the poor beneficiation performance of saprolite-type laterite, the direct carbothermal reduction of saprolite-type laterite exhibits limited nickel selectivity. This study leverages the selective oxidation effect of CO-CO2 atmosphere on metallic iron and its suppression of Fe2+ reduction to promote iron migration from oxides into the silicate phase, achieving homogenization and thereby negating its kinetic advantage in reduction. Parameter optimization experiments revealed that treating pre-reduced minerals with a 30 vol% CO atmosphere at 1200 °C for 20 minutes achieves complete iron homogenization within the silicate phase. Compared with the nickel-iron alloy (containing less than 10 wt% Ni) obtained via RKEF process, the combination of pre-reduction, CO-CO2 treatment, and melting reduction process yielded nickel-iron alloys with nickel contents of 52.1 wt% (FeNi50 alloy) and 64.2 wt% at carbon consumptions of 4.0 wt% and 3.83 wt%, respectively, accompanied by nickel recovery rates of 95.5% and 91.2%. Furthermore, the enrichment of Fe2+ in the slag significantly reduces its melting point to approximately 1450 °C, enabling complete slag-metal separation after smelting at 1550 °C for 10 minutes.
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Hu et al. (2025) studied this question.
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