Mossbauer Study of Iron Sulphides in Mining Ores

"Mineral samples were obtained from different stages of a mineral processing circuit used to extract the copper and gold rich mineralogical phases. The aim of this work is to characterise the quality of the samples at different stages of processing. The samples were taken of the head grade, tailings, cyclone overflow and the final concentrate.Characterisation of the samples was determined using Cu-Ka X-ray powder diffraction and Fe57 Mossbauer spectroscopy. These measurements will be presented and discussed in terms of the enrichment of the ore, showing the removal of magnetite and quartz through the processing, the final concentrate being rich in chalcopyrite and pyrite. This data also shows the utility of Mossbauer spectroscopy to provide mineralogical phase information directly.Mossbauer spectroscopy is a tool to determine the material phases of a sample. It is a nuclear based technique which measures the amount of attenuation of a narrow Doppler shifted source energy as it passes through a sample. The attenuation depends on the amount of resonantly absorbing material in the nuclear radiation path from the source to the detector. Synchronous detection of the doppler shifting velocity and the nuclear radiation count gives a Mossbauer spectrum. By convention, the energy axis of the Mossbauer spectrum is displayed in units of velocity.Figure 1 shows Mossbauer spectra obtained for a sequence of samples throughout a processing plant. These spectra show the removal of magnetite and the concentration of chalcopyrite and pyrite. Optical microscopy results indicated a significant component of bornite not witnessed with Mossbauer spectroscopy. Closer examination showed that optical microscopy assays over estimate the bornite component."