ISSN 1105-2403
Vol. 16, Issue 1 (Jan-June 2006) Abstracts
The solid leach residue is a material consisting mainly of hematite, quartz and chromite. The present research is an investigation on the upgrading of the solid leach residue to a saleable iron concentrate. If proved successful, it will potentially relieve the environment from the disposal of such a large quantity of slag, which today is produced by the pyrometallurgical processing of laterites. The accomplishment of this target faces problems related mainly to the fine dissemination and interweaving of mineralogical phases and the present work is focused to addressing the associated mineralogical issues.
In brief, the ore was crushed to -10 mm and pelletized to allow sufficient permeability during column leaching with 2 N sulphuric acid. The solid residue of leaching was scrubbed and classified to different size fractions for magnetic separation. The rejected non-magnetic material consists mainly of quartz, while the magnetic product consists of low quality hematite due to the finely disseminated inclusions of quartz and some chromite. This magnetic product was ground to -70 ìm and treated again by magnetic separation. In this case, the liberation of hematite is good but the magnetic separation is not selective. Froth flotation is recommended for this separation and it is aimed for a future work.
An important finding of the present work is the detection of sub-micron kaolinite finely disseminated in hematite. Kaolinite is not visible by a microscope and is not detected by X-ray diffraction. Its existence is determined by electron-microscopy analysis, which shows the presence of Al and Si in the mass of hematite grains. The quantitative relation of Al to Si is the same with that found in kaolinite. The above finding means that a clean hematite concentrate may be not possible to be recovered after the separation of quartz from hematite.(Article in Greek.) © Mining & Metallurgical Annals, Hellenic Society of Mining & Metallurgical Engineers, 2006.
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