Abstract

In this work, the effects of stoichiometry on phase evolution during the oxidation of mss (monosulfide solid solution) were investigated. A series of mss samples, ranging from Fe 7.9S 8 to Fe 2.37Ni 5.53S 8 were synthesized from pure components. Samples with grain size 53–90 μm were oxidized at 830 and 850 K in air in a muffle furnace. The Rietveld quantitative phase analysis method was used to identify and quantify the phase information from powder X-ray diffraction (XRD) profiles. Hematite was observed and accounted for most of the oxidized iron. Nickel in mss was not oxidized to NiO under current isothermal conditions; instead, it was finally transformed to Ni 17S 18. Hematite, Fe 2(SO 4) 3 and residual mss were identified in the final phases after 24 h oxidation of the mss composition Fe 7.9S 8; hematite and Ni 17S 18 for compositions Fe 6.15Ni 1.54S 8 and Fe 2.37Ni 5.53S 8; hematite, Ni 17S 18 and pentlandite for Fe 6.4Ni 1.6S 8. Given a constant iron to nickel atomic ratio of 4:1, the sample with lower metal concentration, Fe 6.15Ni 1.54S 8, showed a faster oxidation rate than its metal richer counterpart, Fe 6.4Ni 1.6S 8. The mean oxidation rates for these two samples are 1.85 × 10 −4 and 1.22 × 10 −4 s −1 respectively for 1.5 h heating at 830 K. Vyazovkin's theory of changing activation energy ( E a) with reaction extent ( y) was employed in the current kinetic study. The activation energy was determined using a model-free method. The oxidation of Fe 6.4Ni 1.6S 8 exhibited a higher E a than Fe 6.15Ni 1.54S 8 over the course of reaction. The activation energy increases with y from 67.1 to 103.3 kJ mol −1 for mss composition Fe 6.15Ni 1.54S 8; 76.1 to 195.0 kJ mol −1 for Fe 6.4Ni 1.6S 8. Bulk compositions Fe 7.9S 8, Fe 2.37Ni 5.53S 8 were selected to give a constant metal to sulfur atomic ratio of 7.9:8. Oxidation of Fe 2.37Ni 5.53S 8 achieved equilibrium within 1 h, compared to 5 h for Fe 7.9S 8.

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