Abstract

The purpose of this study was to liberate gold from sulfide minerals in a gold concentrate through microwave-nitric acid leaching and to separate the light minerals in an insoluble residue using a hydro-separation process. The representative sulfide minerals in the gold concentrate were pyrite with minor galena. Mineralogical characterization was conducted on the gold concentrate using 1715.20 g/t based on lead-fire assays. During the leaching experiment, the effect of nitric acid concentration was studied. The results indicated that the metal leaching rate of the gold concentrate increased with increasing nitric acid concentration. After the microwave-nitric acid leaching, the resulting main feature was consistent with the increased exposure to reactive sulfide minerals and decrease in weight. Characterization techniques such as X-ray diffraction (XRD), scanning electron microscope energy dispersive spectroscopy (SEM-EDS) and scanning electron microscope backscattered electron imaging (SEM-BSE) were performed to characterize the minerals in the insoluble residue using microwave-nitric acid leaching and the hydro-separation process. The XRD patterns of the insoluble residues were compared. The intensities of the pyrite peak decreased and disappeared under different nitric acid concentrations, whereas intensities of the quartz peak increased. The hydro-separation process focused on the separation of heavy (e.g., native gold) and light (e.g., quartz) minerals from the insoluble residues. After the hydro-separation treatment process, the heavy minerals exhibited typical diffraction lines of gold, as obtained using the XRD analysis.

Highlights

  • IntroductionThe gold produced from sulfide minerals is divided into visible and invisible gold [2]

  • Gold is mainly produced from pyrite and arsenopyrite [1]

  • The observation of the ore minerals by polarization microscopy revealed that the main sulfide minerals consisted of small quantities of pyrite and chalcopyrite

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Summary

Introduction

The gold produced from sulfide minerals is divided into visible and invisible gold [2]. Whereas visible gold can be observed using an optical microscope or a scanning electron microscope (SEM), invisible gold is very difficult to observe using these techniques. The fact that gold is present as microparticles makes it difficult to observe using an optical microscope (detection limit = 1 μm or less) or SEM (detection limit = 0.1 μm) [3]. Gold that is produced in these states cannot be observed with the resolutions of these microscopes [4]. When gold is produced in a microparticle size, its presence can be confirmed through qualitative or quantitative analysis based on energy dispersive spectroscopy (EDS) or electron microprobe analysis (EPMA) after selecting the bright gold microparticles using backscattered electron (BSE) imaging. In the SEM-BSE images, minerals with low average atomic numbers, such as quartz, Minerals 2020, 10, 327; doi:10.3390/min10040327 www.mdpi.com/journal/minerals

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