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Reversible reactions between pyrite and pyrrhotite in SO sub 2

Journal Article · · JOM (Journal of the Minerals, Metals and Materials Society); (United States)
DOI:https://doi.org/10.1007/BF03220544· OSTI ID:5467712
Differential thermal analysis (DTA) of iron sulfides in inert atmospheres containing varying amounts of SO{sub 2} indicates temperature-dependent reversible reactions between pyrite and pyrrhotite in the range from 350{degrees} C to 520{degrees} C. Hexagonal pyrrhotite (troilite) and sulfur dioxide interact above 350{degrees} C to form pyrite and magnetite. Pyrite decomposes endothermically to pyrrhotite and sulfur above 520{degrees} C in the same atmosphere. The sulfurization of hexagonal pyrrhotite to pyrite has been investigated kinetically by DTA and confirmed by x-ray diffraction and wet chemical analyses. This paper reports on reversibility of this pyrrhotite-pyrite reaction in a sulfur dioxide atmosphere.
OSTI ID:
5467712
Journal Information:
JOM (Journal of the Minerals, Metals and Materials Society); (United States), Journal Name: JOM (Journal of the Minerals, Metals and Materials Society); (United States) Vol. 43:4; ISSN JOMME
Country of Publication:
United States
Language:
English