Kinetic behaviour of the roasting/selective reduction process with the use of a mixture of bituminous coal and fuel oil as the additive

Lateritic ore is currently the main raw material that allows extraction of Ni by the Caron process. To date, the kinetic behaviour of the roasting/selective reduction process of lateritic nickeli-ferous ores on a pilot scale is largely unknown. In the present study, the kinetic behaviour, the contro...

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Bibliographic Details
Main Authors: Angulo-Palma Hugo Javier, Saldana Manuel, Legrá Ángel Legrá, Urgellés Alisa Lamorú, Pedrera Carlos Hernández, Gallegos Sandra, Galleguillos Madrid Felipe M., Toro Norman
Format: Article
Language:English
Published: Association of Chemical Engineers of Serbia 2025-01-01
Series:Hemijska Industrija
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Online Access:https://doiserbia.nb.rs/img/doi/0367-598X/2025/0367-598X2500005A.pdf
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Summary:Lateritic ore is currently the main raw material that allows extraction of Ni by the Caron process. To date, the kinetic behaviour of the roasting/selective reduction process of lateritic nickeli-ferous ores on a pilot scale is largely unknown. In the present study, the kinetic behaviour, the controlling stage and the mechanisms that describe this process with the use of a mixture of 2 wt.% bituminous coal and 1.25 wt.% fuel oil as a reducing additive were determined during the evaluation of the high and low thermal profiles, respectively. The phases of the reduced/le-ached minerals and the fed ore were analysed by X-ray powder diffraction. It was observed that the mixture used as a reducing additive guarantees an adequate transformation in both thermal profiles; the relationship between the residual Ni and residence time is described by a first-order reaction with the determination coefficients greater than 0.949. Although the influence of post-combustion air is not analysed, the controlling stage was diffusion through the ash layer with an activation energy of 14.4060 kJ mol-1. Thus, the most precise combination to describe the process is diffusion through the ash layer and the growth of the nuclei.
ISSN:0367-598X
2217-7426