Crimson Publishers Blogger: Application of Raman Micro Spectroscopy and Micro-FTIR Mapping in the Bio-Hydrometallurgy of Copper Sulfide-Minerals

Monday, February 28, 2022

Application of Raman Micro Spectroscopy and Micro-FTIR Mapping in the Bio-Hydrometallurgy of Copper Sulfide-Minerals_Crimson Publishers

Application of Raman Micro Spectroscopy and Micro-FTIR Mapping in the Bio-Hydrometallurgy of Copper Sulfide-Minerals by Constantinos Varotsis in Aspects in Mining & Mineral Science_Mining and Mineral Science journals

Abstract

A combined application of μm-FTIR mapping and Raman microspectroscopy for the bioleaching behaviour of copper sulfide minerals such as chalcopyrite, bornite, chalcocite and covellite provides valuable information on the whole bio-hydrometallurgy Cu/Fe/S system. Both techniques provide label-free, nondestructive visualizations of the bio-hydrometallurgy dynamics for processing and storage of large spectral data sets which are valuable for evaluation of copper, iron and sulfur containing minerals. The results provide solid evidence that the techniques can be also applied to other Bio-hydrometallurgical extracted metals from Polymetallic Mineral Resources.

Keywords: Micro spectroscopy; Minerals; Metal ions; Copper

Introduction

New methods for maximizing copper extraction from whole ores and processing tails and sensory technologies for daily monitoring have been developed (Figure 1). Heap bioleaching is the most applicable technology to treat low grade copper sulfide ores and bearing chalcopyrite, idaite, bornite, chalcocite and covellite. A variety of biochemical processes in conjunction with state-of-the-art sensory technologies have been applied towards establishing the Bio- hydrometallurgy treatment of low-grade copper mixed ores and mineral processing tails [1,2]. High copper extractions are achieved with isolated and mixed cultures of the mesophilic iron and sulfur oxidizing bacteria Acidithiobacillus ferroxidans and Acidithiobacillus thiooxidans, and in the presence of moderately thermophilic microorganisms such as Acidithiobacillus caldus, Leptospirillum ferriphilum and their mixed cultures [1,2]. The elucidation of the mechanisms involved in the interactions of sulfur oxidizing bacteria with the mixed ores in the bioleaching procedure is important for understanding the bioleaching behavior between single and mixed ores and the origin of the existing differences [1,2]. Oxidation-reduction potential, temperature, pH and the origin of the microorganisms are crucial in our understanding the whole bio-hydrometallurgy system. Chalcopyrite [CuFeS₂] is the most abundant copper sulfide ore that has received extensive attention because there are considerable ore reserves that could be exploited. It has been suggested that the primary oxidation product of chalcopyrite leaching is chalcocite which is subsequently oxidized to covellite [2].The formation of the latter is confirmed by ore microscopy and by a number of structure sensitive techniques such as Raman and FTIR [1,2]. Raman spectra including the images can provide the information for identification of surface species/phases and spatial variations in composition of the bioleaching of chalcopyrite as well the formation of the passivation layers in Cu/Fe/S and Cu/S systems. (Figure 2) spectrum A, shows the Raman spectra of bornite and the 1-6 months bioleached bornite samples by a consortium of microorganisms consisted of Acidithiobacillus ferrooxidans, Acidithiobacillus thiooxidans, Acidithiobacillus caldus, Leptospirillum ferriphilum, Leptospirillum ferroodiazotrophum and Sulfobacillus thermosulfidooxidans. In the one month bioleaching period (spectrum A) there are several new Raman bands including those at 220 and 430cm^-1 which we assign to the ν(Fe-O) of K⁺_- jarosite respectively. We also assign the bands at 450, 624, 1004, 1097, and 1157cm^-1 to ν₂(SO₄^2-), ν₄(SO₄^2-), ν₁(SO₄^2-), ν₃(SO₄^2-) and ν₃(SO₄)^2- of K⁺_- jarosite, respectively. The marker band in the Raman data for distinguishing the K⁺ from NH₄⁺ jarosite is the ν₃(SO₄^2-) vibration observed at 1099cm^-1 in the spectra of K⁺_- jarosite and at 1091cm^-1 in the spectrum of NH₄⁺_-jarosite. The absence of NH₄⁺ marker bands in the spectrum strongly suggests that in one month period only K⁺_- jarosite is formed. The strong band at 473cm^-1 is attributed to ν(Cu-S) of covellite. Elemental sulphur and polysulfides contain S-S linkages and display the ν(S-S) and δ(S-S-S) which are characterized by equally strong intensities at 470 at 215cm^-1, respectively. The intensity of the ν(S-S)/δ(S-S-S) ratio has been applied used to distinguish the elemental sulphur from the other S-S and Cu-S bond containing species. At six months (spectrum B), the 220cm^-1 band attributed to K⁺_- jarosite has shifted to 218cm^-1 and gained intensity which is attributed to the formation of δ(S-S-S) of elemental sulphur. Given that the ν(S-S) and δ(S-S-S) are characterized by equally strong intensities we suggest that the band at 473cm^-1 has little contribution from the ν(Cu-S), and thus, we attributed it to ν(S-S) of elemental sulphur. This observation indicates that at six-months of bioleaching, the 474cm^-1 covellite band observed in spectrum A has disappeared. In addition, all bands attributed to K⁺_- jarosite including the ν(Fe-O) at 430cm^-1 have lost most of their peak intensity, and in contrast to the bioleaching behaviour of chalcopyrite, there is no evidence for the formation of NH₄⁺_- jarosite. Studies examining the dissolution behaviour of K⁺_- and NH₄⁺_- jarosites from the ore surface are limited. It is intriguing to propose that in our study more than one microorganism was involved in the biosynthesis of K⁺_- jarosite. The presence of K⁺_- jarosite at one month period and the lack of NH₄⁺_- jarosite formation suggest that K⁺_- jarosite is not subject to microbial reduction leading to intermediate mineral of the microbial process. In addition, the behavior of the K⁺_- jarosite marker bands at six months period indicates that either its presence is reduced substantially because it has broken down by converting to iron (III) oxide or oxyhydroxide phases or that is not part of the surface of the bioprocessed mineral, and thus, not detectable

Figure 1: Proposed sequential pathway for the bioleaching evolution of chalcopyrite that involves idaite, bornite, chalcocite and covellite [2].

Figure 2: Raman spectra of bioleached bornite samples. The consortium of microorganisms consisted of Acidithiobacillus ferrooxidans, Acidithiobacillus ferrooxidans, Acidithiobacillus ferrooxidans, Leptospirillum ferriphilum, Leptospirillum ferroodiazotrophum and Sulfobacillus thermosulfidooxidans. Spectra A and B are at one and six months of bioleaching period, respectively.

Bioleaching of Cu/Fe/S minerals also leads to precipitation of Fe(III) hydroxysulfates and metal- deficient passivating layers which dramatically decrease the access of leaching agents and bacteria cells to the mineral surfaces, making the bioleaching procedure still not optimized and fully successful. FTIR imaging spectroscopy has been applied to monitor the formation of jarosite passivation layers which are of profound importance because despite great efforts, researchers have not reached a consensus on the control steps governing whole ore bioleaching [1,2]. Potassium Jarosite [KFe₃(SO₄)₂(OH)₆] is a mineral that is common in acidic, sulfate-rich environments, such as acid sulfate soils derived from pyrite-bearing sediments, weathering zones of sulfide ore deposits and acid mine rock drainage (ARD/AMD) sites. Jarosite typically is formed in ferric rich, acidic (pH<3) oxic environments and readily breaks down when removed from its stability region by presumably converting to iron (III) oxide or oxyhydroxide phases. K⁺_- jarosite converts to goethite through the following reaction

Bacterial cell finds a way to protect itself from the infiltration of toxic metal ions by covering its peripheral surface with a shield of EPS. Structural and compositional makeup of EPS favors the sequestration of metal ions and hence obstructs them from penetrating the cell surface. The mixed culture microbial biofilms and their extracellular polymeric substances associated with the solid-liquid interfaces have several key properties and functions. A close inspection of the intensity of the respective peaks in the 1000- 1200cm-1 region in the FTIR spectra illustrated that the relative contents of chemical groups are distinctly different between bornite, chalcocite and covellite [1,2]. The mixed culture biofilms are spatially structured communities of microbes whose function is dependent upon a complex web of symbiotic interactions. Apart from cellular constituents, a major component of biofilm systems is the EPS produced by the members. The extracellular polymeric substances (EPS) of the biofilm matrix appear to have several key properties and functions. Extracellular polymeric substances (EPS) are complex high molecular weight microbial biopolymers which occur in a range of molecular sizes, conformations and physicochemical properties, and polysaccharides, proteins, lipids, and even nucleic acids are actively secreted components. The physical ultrastructure of how individual EPS interact with each other is poorly understood. The major components present in EPS are proteins, polysaccharides, uronic acids, lipids and humic substances. Little is known about the mineral-humic substances interactions. One of its essential constituent is the exopolysaccharide (EPS) released out of self defence against harsh conditions of starvation, pH and temperature, hence it displays physiological, rheological and physico-chemical properties (Figure 3).

Figure 3: Collective image of the surface of bioleached covellite and the FTIR spectra collected from the surface of the mineral at seven week period time. The consortium of microorganisms consisted of Acidithiobacillus ferrooxidans, Acidithiobacillus thiooxidans, Acidithiobacillus caldus, Leptospirillum ferriphilum, Leptospirillum ferroodiazotrophum and Sulfobacillus thermosulfidooxidans. Each spectrum represents the infrared fingerprint of an area of 0.01mm2 of the mineral surface with spectral resolution 4cm^-1.

The FTIR analysis was carried out to probe the chemical structures of the various mixed culture biofilms and their EPS on the surfaces of covellite. The positions and number of FTIR peaks for the different biofilms and EPS appeared to be quite different, implying that the types of chemical groups involved are quite different. Several strong bands associated with proteins and polysaccharides were observed in the marker bands, among which are the stretching vibration C=O (1637cm^-1) and the C-O-C stretching vibration of polysaccharides (960^-1150cm^-1) [1,2]. The intensity and peak positions in the μm-FTIR data clearly demonstrated that the relative contents of chemical groups are distinctly different. These observations demonstrate that the biofilms and the associated EPS consisted of different components. On the mechanism of EPS attachment on the mineral, the most reasonable interpretation is that charge effects are involved whereas molecules acting as Lewis acids by accepting electrons from the mineral-sulfur, like EPS-complexed iron species, will preferentially strongly attracted. The selective attachment to mineral ores is associated with the occurrence of distinct dislocation sited, where sulphur atoms are accumulated.

Conclusion

Raman microspectroscopy and micro-FTIR mapping/imaging are structure sensitive techniques that have been applied successfully in our laboratory for over 30 years towards our understanding of the characterization of the structure-function relationship in biomolecules, and recently in minerals, and in monitoring the steps governing whole ore bioleaching [1-14]. FTIR is well established as a method for studying solid state transformations in minerals and bio minerals and micro-FTIR extends this functionality to include spectroscopic mapping at the micrometer length scale. The achievement of chemical and structural mapping of (bio)-minerals opens new horizons for our understanding of mineral arrangements and variability in biological systems. Based on our results we propose a mechanism for the sequential steps for chalcopyrite bioleaching in which chalcopyrite is converted initially to Cu₂S, and subsequently to CuS. K⁺_- jarosite formation is not followed by the formation of NH₄⁺_- jarosite as it was observed in the case of chalcopyrite. The role of the microenvironment filled with EPS which contains sugars, fatty acids and lipids and formed between the bacterium and the metal sulfide surface is distinct in each case. The dynamics of the EPS which are essential for cell attachment and metal sulfide leaching is time-dependent.

Acknowledgement

Financial support by the European Regional Development Fund and the Republic of Cyprus through the Research Promotion Foundation (Grant No ENTERPRISES/0916/0069) is gratefully acknowledged.