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By Markus A. Reuter, Yongxiang Yang, Jim R. Post

In the upper part of an iron making blast furnace, sinter, coke and pellets are charged. While descending, the burden is heated and the iron oxides are reduced by the rising gases. The iron oxides start to soften and eventually melt. The melt and the remaining coke collect in the lower part of the blast furnace: the hearth. The remaining coke forms a porous bed: the dead man (see Figure 2). The melt flow through the dead man can affect substantially the hearth lining life, the furnace productivity and product (i.e. hot metal) quality. Physical characteristics like porosity and particle size distribution of the porous coke bed play a critical role. Because of the distributed nature of the coke properties, the bed packing structure and porosity will not be constant.

Jan 1, 2003

By N. T. Beukes, W. Banda

Recovery of Co from slag is a recent advancement in the extractive metallurgy of nonferrous metals. In this study a DC arc technology at laboratory scale has been applied to investigate the selective recovery of Co from slag, under three different flux types with an emphasis on influencing the activity of FeOx, SiO2 and CoO in the slag. It is known that reduction of slag by carbon is only up to a certain level after which, the recovery will depend on the chemistry of the slag, hence the need to modify the slag chemistry. Two power settings were employed to induce higher temperatures and aggressive agitation. The results were interpreted by comparing how much Co and Fe was in the slag and alloy. TiO2 reduced the amount of Fe in the product alloy compared to when CaO and CaF2 were used. The change in power did not seem to have had a major effect on the recovery although the amount of material lost to flue dust was more at a higher power rate.

Jan 1, 2003

By N. Kgabi, F. B. Waanders, E. Vinken, A. Mans

"Mössbauer and SEM identification of the iron mineral phases present in South African coal fractions from the Free State, Gauteng, Mmpumalanga, Natal and Waterberg coal fields, as well as from ash samples from coal used in the Lethabo power plant, containing a large amount of inorganic matter, was conducted. The iron is mainly associated with sulphur in the mineral but the amounts of these and other minerals vary considerably in coals from diverse origins. By means of Mössbauer analyses the iron bearing minerals were identified as pyrite, jarosite, illite and ankerite. In the SEM analyses quartz, associated with various clay minerals was identified with differences in abundance found between the coals from the different locations.The fly ash, produced at the high combustion temperatures in the power plant, gave rise to a spectrum, typical of a glass. SEM analyses showed that agglo- meration of the fly ash was due to the presence of Ca in the coal. The lab. produced fly ash was combusted at temperatures ranging from 200-1 200°C and the pyrite changed partially to hematite and partly into the glass due to the presence of the quarts and the clay minerals. A similar spectrum as the power plant fly ash spectrum was obtained.In the weathering experiments the pyrite changed to a sulphate component in a very short time during air drying."

Jan 1, 2003