Novel reagents for iron and sulphur control in medium temperature leaching of sulphide concentrates

Hydrometallurgical leaching of sulphide concentrates of copper and nickel at medium temperature (150°C) produces residues that contain sulphur and iron-bearing minerals and phases. During leaching, and depending on various process parameters, iron may be precipitated as hematite, goethite, jarosite or other oxyhydroxides, which may be more or less crystalline. Hematite is the favoured iron precipitate, because it is the most environmentally stable and does not ad/absorb as much copper, nickel or other solution constituents during precipitation. However, the low solubility of iron during the medium temperature processing of sulphide ores can favour the formation of poorly crystalline, nano-scale iron oxide/oxyhydroxide phases. In some cases, these phases have been positively identified as the metastable ferrihydrite, which transforms into iron oxides such as goethite, hematite and magnetite over time. A better understanding of what may help drive this transformation during leaching would ultimately result in lower valuable metal losses and more stable leach residues. Higher acid concentrations result in increased copper extractions and favour the formation of hematite during concentrate leaching, rather than other metastable phases. Furthermore, commercially available water displacement formula ‘WD40®’ and other novel reagent(s) affect Fe precipitation and sulphur chemistry, leading to very different process outcomes such as improved extractions and larger, more easily separated, sulphur particles.