Mária Fröhlichová

COMPARISON OF IRON ORE SINTER MINERALOGY QUANTIFICATION

At present, the powder XRD is widely used analytical method for iron ore sinter mineralogy determination. In many researches, diffraction data for SFCA and SFCA-I phases were not available and diffraction data for other calcium ferrites were used instead. Therefore, the aim of this paper is to bring a comparison between evaluation of diffractograms, when SFCA/SFCA-I, and, other calcium ferrites, respectively, are considered. As a result, the quantification of phases is quite comparable, when minerals are collected into groups, i.e. hematite, magnetite, calcium ferrites, silicates and non-assimilated non-ferrous phases. Only in the case of silicates a comparison tends to be dissatisfactory.

Microstructure of Agglomerate Produced with Charcoal as Substitution Fuel

Worldwide laboratory research proves that replacement of coke breeze by solid biomass in the process of agglomeration is possible [1,2,3]. One possibility of solid biomass use is the charcoal. Literature indicates that coke breeze can be replaced by charcoal up to 40% based on calorific value [4]. This paper deals with the poblems of coke breeze substitution by charcoal in laboratory conditions sintering and the impact of such substitution on the resulting agglomerate properties, i.e. microstructure. Agglomerate microstructure consists of mineralogical phases; hematite, magnetite, calcium and aluminum silico-ferrites, and silicates. Substituting coke breeze for charcoal up to 40% in the process of agglomeration, slight changes occur in the volume fractions of individual phases of the agglomerates. Volume fractions of agglomerate phases change significantly above 40% substitution by charcoal. Phase composition has an effect on the quality characteristics of the produced agglomerate. The amount of calcium and aluminum silico-ferrites influences the strength of the agglomerate [5].