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Influence of Carbon and Pyrite on Desulfurization Behavior of Red Gypsum at High Temperature

Red gypsum is generated from TiO 2 production industry by the sulfate method, which contains iron, calcium, and sulfur elements. The iron and calcium elements can be reused as iron-making raw materials, but the sulfur element in the gypsum is required to be removed as it has a harmful effect on the...

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Bibliographic Details
Published in:Journal of sustainable metallurgy 2022-03, Vol.8 (1), p.409-418
Main Authors: Ma, Xiaoling, Tan, Hongbin, Dong, Faqin, Yang, Feihua
Format: Article
Language:English
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Summary:Red gypsum is generated from TiO 2 production industry by the sulfate method, which contains iron, calcium, and sulfur elements. The iron and calcium elements can be reused as iron-making raw materials, but the sulfur element in the gypsum is required to be removed as it has a harmful effect on the properties of iron. Herein, the influence of carbon and pyrite on the desulfurization behavior of red gypsum is systematically investigated by high-temperature decomposition. In the absence of carbon, a small amount of anhydrite (CaSO 4 ) phase is decomposed after sintering at 1200 °C for 2 h. However, the undesirable oldhamite (CaS) phase is observed in the entombed RG/carbon50 mixture after sintering at 800 °C for 2 h, which implies that a strong reducing atmosphere can promote oldhamite to get generated. Overall, anhydrite decomposition is influenced by the carbon content, sintering temperature, and holding time. In the case of RG/carbon100 mixture, the diffraction peaks of anhydrite are not observed after sintering at 1100 °C for 2 h and 1200 °C for 0.5 h. Moreover, the main phases in RG/carbon100 mixture are found to be gehlenite (Ca 2 Al(AlSiO 7 ), magnetite (Fe 3 O 4 ), dicalcium diiron oxide (Ca 2 Fe 2 O 5 ), and lime (CaO). In addition, the phase composition of RG/carbon100 mixture is not influenced by the addition of different amounts of pyrite (FeS 2 ) after sintering at 900, 1000, and 1100 °C. Graphical Abstract
ISSN:2199-3823
2199-3831
DOI:10.1007/s40831-021-00483-8