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Article

Enhancing the Leaching of Chalcopyrite Using Acidithiobacillus ferrooxidans under the Induction of Surfactant Triton X-100

1
School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
2
School of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China
3
School of Energy and Environmental Engineering, University of Science and Technology Beijing, Beijing 100083, China
*
Author to whom correspondence should be addressed.
Minerals 2019, 9(1), 11; https://doi.org/10.3390/min9010011
Submission received: 27 October 2018 / Revised: 13 December 2018 / Accepted: 20 December 2018 / Published: 25 December 2018

Abstract

:
Chalcopyrite is the richest copper sulfide mineral in the world, but it is also the most resistant to biohydrometallurgical processing. To promote the bioleaching of chalcopyrite, a nonionic surfactant, t-octyl phenoxy polyethoxy ethanol (Triton X-100), was employed in this paper. Action of Triton X-100 in chalcopyrite leaching using Acidithiobacillus ferrooxidans was explored in shake flasks. Results showed that 30 mg·L−1 of Triton X-100 increased the bioleaching yield of copper by 42.21% compared to the process without additive after 24 days. Under the stress of Triton X-100, the bioleaching efficiency of chalcopyrite slightly dropped at an early stage, but remarkably increased afterwards. XRD and XPS analysis of the leach residues demonstrated that potassium jarosite and elemental sulfur resulted in surface leaching passivation. Surfactant Triton X-100 appeared to induce the oxidation of elemental sulfur by bacteria owing to the increase in the sulfur surface hydrophobicity. These results suggest that Triton X-100 itself has no ability to leach chalcopyrite, but under its induction, the bioleaching of chalcopyrite can be enhanced due to the removal of the passivation layer.

1. Introduction

Chalcopyrite (CuFeS2) is the richest copper-bearing mineral, accounting for nearly two-third of the world’s copper reserves [1], while it is also extremely recalcitrant to (bio)hydrometallurgical processing [2]. In practice, industrial-scale bioleaching is generally carried out by the use of mesophilic microorganisms like Acidithiobacillus ferrooxidans, Acidithiobacillus thiooxidans, and Leptospirillum ferrooxidans because they are dominant species at normal atmospheric temperatures [3]. Slow oxidation kinetics and low copper recovery are the bottlenecks of chalcopyrite’s commercial application in meso-acidophilic bioleaching [4]. These can be mainly attributed to two factors: (i) the high lattice energy of chalcopyrite, making it difficult to decompose; and (ii) the formation of a surface passivation film during chalcopyrite bioleaching, which is made up of sulfur-containing intermediates such as elemental sulfur, jarosite, polysulphides, and metal-deficient sulphides [5,6]. To prevent such passivation, many approaches have been proposed, for example, use of thermophilic microorganisms [7], lowering pH conditions [8], controlling the redox potential [9], and the addition of catalysts like silver and activated carbon [10,11]. Although each method possesses its own advantages of high activity of bacteria, high reaction efficiency, complete dissolution, or simple technique, it should be noted that they do have specific drawbacks such as a low metal tolerance capability, high acid consumption, complicated process, or high operation cost, which limit their application in industry.
Additionally, adding an appropriate amount of surfactant featuring specific structure has been found to be a potential way to promote the leaching [12]. Previous studies showed that the addition of surfactants such as polysorbate (Tween), p-octyl polyethylene glycol phenyl ether (emulsifier OP), o-phenylenediamine (OPD), or potassiumamyl xanthate (KAX), could result in the enhanced bioleaching of cobalt ore [13], arsenopyrite [14], marmatite [15], or zinc sulphide, respectively [16]. Most researchers have simply attributed this positive impact to the fact that surfactants can change surface properties of minerals and the interfacial tension of the leaching solution [13], but so far, no direct evidence can verify the cause-and-effect relationship between these changes and the leaching rate.
In the case of chalcopyrite, only the nonionic surfactants Tweens have been investigated. Hiroyoshi et al. reported that adding 20 mg∙L−1 of Tween 20 was favorable for the copper extraction from chalcopyrite [17]. The author believed that indirect leaching played the main role in the bioleaching, and the catalytic effect was attributed to the decrease in the bacterial adhesion to the chalcopyrite surface. Peng et al. also reported that 10 mg∙L−1 of Tween 80 increased the copper leaching efficiency by 16%, possibly due to the shortening of the lag stage of bacteria growth [18]. However, the catalytic capability of Tweens is rather limited, mainly due to its toxicity for bioleaching microorganisms [19]. Hence, there is a need to develop more effective but less toxic surfactants for catalyzing the bioleaching of chalcopyrite.
Triton X-100, formally named as t-octyl phenoxy polyethoxy ethanol, is a water-soluble nonionic surfactant with an aromatic hydrocarbon and branched alkyl substituent as a hydrophobic group and a polyethylene oxide chain as a hydrophilic group. Chemical structure of Triton X-100 is shown in Figure 1. It is widely used as a solubilizer, detergent, or dispersing or wetting agent due to its chemical stability, good wettability, and low toxicity [20,21]. Interestingly, our previous research showed that Triton X-100 could accelerate the bioleaching rate of chalcopyrite, though it has a detrimental impact on ferrous-oxidizing activity of bioleaching microorganisms [22]. However, little information has been done on its effect on the oxidation process, and on the formation of surface passivation films. It is clear that understanding its mechanism could offer a new alternative for the enhancement of copper recovery via bacterial leaching.
In this study, the influences of Triton X-100 on the chalcopyrite leaching via Acidithiobacillus ferrooxidans were investigated in shake flasks. Moreover, further analysis of the chalcopyrite surface after leaching were characterized using X-ray diffractometer (XRD), scanning electron microscope (SEM), X-ray photoelectron spectroscopy (XPS). Finally, a model for the catalytic action of Triton X-100 was proposed. This work would provide a deeper insight into the catalytic mechanism of surfactant (i.e., Triton X-100) in chalcopyrite bioleaching.

2. Materials and Methods

2.1. Bacteria and Minerals

The meso-acidophilic strain Acidithiobacillus ferrooxidans XZ11, GenBank accession number KJ573102, used in this paper was isolated from the acid mine water of a Jiama copper mine in Tibet, China. The 0K medium was composed of 3.0 g∙L−1 (NH4)2SO4, 0.1 g∙L−1 KCl, 0.5 g∙L−1 K2HPO4, 0.5 g∙L−1 MgSO4∙7H2O, and 0.01 g∙L−1 Ca(NO3)2. The 9K medium was composed of the 0K medium with FeSO4∙7H2O (44.2 g·L−1) added as the sole energy resource for bacteria. Also, the sulfur medium consisted of the 0K medium and 1% (w/v) of sulfur powder. The initial pH of these three media was adjusted to 2.0 with sulphuric acid. All of the reagents were of analytical grade, which were purchased from Sinopharm Chemical Reagent Co., Ltd., Shanghai, China.
To obtain metabolite-free cells, bacteria inoculated in a bacterial adhesion (5 × 107 cells∙mL−1) and leaching experiments (2 × 107 cells∙mL−1) were cleaned as follows. First, bacteria cultured in 9K medium were collected in the stationary phase. Then, the culture was filtered through Whatman filter paper No. 42 to remove precipitates and centrifuged at 10,000 rpm for 15 min. Finally, the cells were washed and resuspended in the 0 K medium.
The highly pure chalcopyrite used in this paper was collected from Yunnan province in China. The sample was crushed, hand selected, and further purified using a shaking table. Then, the obtained high-purity chalcopyrite was ground until all particles passed through 74 μm before being used for leaching experiment. Powder X-ray diffraction data confirmed chalcopyrite to be the only detectable mineral phase. Chemical analysis showed that the chalcopyrite contained: Cu 32.84%; Fe 29.62%; S 33.10%.

2.2. Surface Tension and Contact Angle Measurements

The surface tension of Triton X-100 (chemically pure) solutions was measured in 0K medium at 30 ± 1 °C using the Wilhelmy plate technique with a tensiometer (JF99C, Zhongchen Digital Technology and Equipment Co., Ltd., Shanghai, China). The contact angles of elemental sulfur surface were measured by a contact angle analyzer (XG-CAMB, Xuanyi Digital Technology and Equipment Co., Ltd., Shanghai, China). Sulfur powders were pressed into pellets (5 mm thick and 10 mm in diameter), and successively polished with 400-, 800-, and 1000-grit silicon carbide papers, to ensure uniform smoothness. The deionized water and the aqueous solution containing Triton X-100 at various concentrations were dropped onto the pellets surface using a special syringe, and then the static contact angle was measured at room temperature (25 ± 2 °C). For each group, five measurements were carried out, and the average value was calculated.

2.3. Bacterial Adhesion Experiments

Bacterial adhesion to elemental sulfur was studied as described previously [23]. The experiments were carried out in 250-mL flasks containing 100 mL of 0K medium, 1% (w/v) of sulfur powder, 5 × 107 cells∙mL−1 of At. ferrooxidans, and a predetermined amount of Triton X-100. Each flask was shaken at 160 rpm and 30 °C for 30 min. Then, the mixture was filtered through a filter paper (Whatman No. 1) to remove cells-bearing sulfur powder. Finally, cell numbers in the filtrate was determined using a Neubauer-improved counting chamber (Cell depth: 0.1 mm; Ruling pattern 1/400 mm2; XB-K-25, Shanghai, China) under a microscope (Motic BA210, Xiamen, China). The bacterial adhesion percentage (η) was calculated using the equation η = (c0c)/c0 × 100%, where c0 and c represent the initial number and the cell number in the filtrate, respectively. Each group was carried out in triplicate, and the average value was reported.

2.4. Ferrous Iron and Sulfur Oxidation Measurements

Ferrous iron or sulfur oxidation by At. ferrooxidans were determined in 250 mL Erlenmeyer flasks, in a shaking incubator with 160 rpm at 30 °C. Each flask contained 90 mL of 9K media or sulfur media, 10 mL of bacteria that was harvested during the stationary phase of growth, and a predetermined amount of Triton X-100. The ferrous iron concentration was measured by titration with a standard solution of potassium dichromate, and sodium diphenylamine sulphonate was employed as an indicator. The rate of sulfur oxidation was estimated by the decrease of pH value of the medium. Then, the pH value of each group was determined periodically using a digital pH meter (Sartorius PB-10, Goettingen, Germany). Each group was carried out in triplicate.

2.5. Leaching Experiments

Leaching experiments were carried out in 250 mL Erlenmeyer flasks, in a shaking incubator with 160 rpm at 30 °C. Each flask contained 100 mL of the 0K medium, 1% (w/v) of chalcopyrite and a predetermined amount of Triton X-100. The initial number of bacteria was adjusted to 2 × 107 cells∙mL−1 in the bioleaching systems, while 0.1 g·L−1 of NaF serving as a bacteriostat was added in abiotic leaching systems in the absence of cells. Each group was carried out in triplicate.
Samples were taken periodically to determine the concentrations of bacteria and metal ions. The concentrations of soluble copper and total iron were determined using inductively coupled plasma optical emission spectroscopy (Perkin Elmer, Waltham, MA, USA). Fe3+ concentration was calculated using the difference between total Fe and Fe2+ concentration. The water lost due to evaporation and sampling were compensated with deionized water and the 0K medium, respectively.
After 24 days of bioleaching, the pulp was filtered, and the residues were collected, washed carefully with deionized water, and then dried in a vacuum at 30 °C. Then, the residues were characterized using an X-ray diffractometer (PAN-alytical X’Pert Pro, Almelo, The Netherlands) and X-ray photoelectron spectroscopy (ESCALAB 250, Waltham, MA, USA), respectively. XRD measurements were tested with Cu Kα radiation (λ = 0.154 nm, 40 kV, 40 mA) and a scanning step of 2°/min. The results were analyzed using the built-in software X’Pert HighScorePlus. XPS measurements were conducted with a monochromatic Al-Kα source. All spectra were calibrated with the C 1s peak at 284.8 eV, and the obtained data was processed by fitting a Shirley background. In addition, after 24 days, a small amount of pulp containing minerals was deposited onto metallic substrates (1 cm × 1 cm) covered with a double-adhesive carbon tape, and then washed carefully with deionized water, and finally dried in a vacuum at 30 °C. Afterward, the dehydrated samples were covered with gold to be visualized using a scanning electron microscope (SEM, ZEISS Ultra Plus, Oberkochen, Germany). Further details can be found in previous works [24,25,26].

3. Results and Discussion

3.1. The Iron-Oxidizing Activity of At. ferrooxidans

Once an additive is added into the bacterial leaching system, the priority should be given to its possible toxic/inhibitory effect to the growth of bacteria. Influences of Triton X-100 on the iron-oxidizing activity of At. ferrooxidans are shown in Figure 2A. It was shown that the ferrous iron oxidation rate decreased with increasing Triton X-100 concentrations. Without the surfactant addition, the ferrous iron was completely oxidized in approximately 60 h, and the oxidation rate was up to 0.34 g∙L−1∙h−1. When the concentration fell within the range of 30 to 90 mg∙L−1, the oxidation rate was gradually decreased from 0.33 to 0.15 g∙L−1∙h−1. Exposure to 200 mg∙L−1 of Triton X-100 made the bacteria nearly lose the iron-oxidizing ability. These data indicated that the Triton X-100 addition was inhibitory for ferrous iron oxidation by At. ferrooxidans, even at low doses. As reported previously, most of organic compounds cannot be metabolized by At. ferrooxidans, as a chemosynthetic autotrophic bacterium, and usually inhibit the growth activity of the bacteria [27,28].
Figure 2B illustrates the change in surface tension of solution with the addition of varying concentrations of Triton X-100. It was shown that the higher the Triton X-100 concentration, the lower the surface tension of solution. In the presence of 200 mg∙L−1 of Triton X-100, the surface tension decreased from 67.84 (without additive) to 38.50 mN∙m−1. According to the reports by Torma and Liu et al., the bacterial activity of At. ferrooxidans and the surface tension of the medium were inversely proportional to the concentration of surfactants Tween 20, 40, 60, and 80 [19,29]. Thus, it was concluded that the decay in the iron-oxidizing ability of At. ferrooxidans in the presence of Triton X-100 is probably the consequence of the decrease in the surface tension of solution.

3.2. The Induction of Sulfur Oxidation by At. ferrooxidans

Apart from the oxidation of the ferrous iron (Fe2+), sulfur oxidation is the other important ability of At. ferrooxidans. It has been demonstrated that the oxidation of elemental sulfur (S0) by sulfur-oxidizing bacteria occurs at the cell envelope, thus the adhesion of bacterial cells to sulfur particles is necessary [30]. In such a process, the hydrophobic barrier must be overcome first.
Figure 3A illustrates the influences of Triton X-100 on S0 surface hydrophobicity (characterized by contact angle) and on the adhesion of At. ferrooxidans to S0. The results showed that the contact angle of S0 declined gradually with increasing Triton X-100 amount. The contact angle between water and S0 surface was 105.4°, suggesting that S0 surface was highly hydrophobic, whereas the contact angle decreased to 60.1° under the stress of 120 mg∙L−1 Triton X-100. Thus, it can be seen, Triton X-100 addition could significantly improve the surface hydrophilicity of S0. This might be because the hydrophobic part of Triton X-100, isooctyl phenyl ether, was absorbed on S0 surface by van der Waals interactions, and the hydrophilic part (i.e., oligo-ethylene oxide) was oriented toward the aqueous phase, forming a hydrophilic layer on the S0 surface.
Figure 3A also showed that Triton X-100 addition observably enhanced the bacterial adhesion performance, and the adhesion percentage increased with increasing Triton X-100 amount. The relative number of cells that adhered to S0 increased from 18.37% to 45.76% with the addition of 120 mg∙L−1 Triton X-100. This was because the increase in hydrophilicity of surface S0 led to an increase of attachment ability of At. ferrooxidans with a good hydrophilic surface [31]. Therefore, we confirmed that the hydrophobic interaction plays a principal role in the adhesion of cells to the hydrophobic S0 surface. Devasia et al. also reported that the greater hydrophobicity of bacterial cells could help in their adhesion to hydrophobic minerals like chalcopyrite and pyrite [32].
In sulfur medium, S0 is the sole energy source for At. ferrooxidans. When S0 is biooxidized into sulfate, the solution pH value decreases, as illustrated by Reaction (1). Therefore, the sulfur oxidation rate could be evaluated indirectly by the change of the pH value of the medium. Figure 3B shows the influences of Triton X-100 on sulfur oxidation in the absence and presence of At. ferrooxidans. The results showed that the solution pH value dropped much faster in the presence of 30 to 90 mg∙L−1 Triton X-100. Among them, the effect of 60 mg∙L−1 Triton X-100 was the most obvious, leading to a maximum drop in pH value from 1.5 to 1.36 on day 20. These data indicated that the oxidative activity of At. ferrooxidans could be improved under the stress of Triton X-100 at appropriate concentrations. When the addition was higher than 120 mg∙L−1, sulfate production was depressed.
2 S 0 + 3 O 2 + 2 H 2 O A t .   f e r r o o x i d a n s 2 S O 4 2 + 4 H +
Notably, in the absence of At. ferrooxidans, S0 was very slowly oxidized in acid solution, even when the Triton X-100 concentration increased to 200 mg∙L−1. This phenomenon demonstrates that S0 is inert and hardly oxidized at room temperature without a strong oxidizer, i.e., sulfur-oxidizing bacteria. This was in line with the observation by Knickerbocker et al. [33].
Based on the above results, it can be concluded that Triton X-100 did not accelerate the chemical oxidation of S0, but induced the biological oxidation of S0 owing to an increase in the bacterial adhesion to sulfur. The added Triton X-100 played a role of “bridge” in connecting S0 and cells. The positive correlation between the number of adhered bacteria and sulfur oxidation rate obtained by Porro et al. supported this hypothesis [34].

3.3. The Leaching Efficiency of Chalcopyrite

Figure 4 shows the influences of Triton X-100 at various concentrations on the copper extraction yield from chalcopyrite in the presence and absence of At. ferrooxidans. In the case of bacterial leaching, the leaching efficiency was sensitive to the concentration of Triton X-100. The surfactant at the dosage of 30 to 90 mg∙L−1 exerted remarkable catalytic effects. The optimum concentration was found to be 30 mg∙L−1, under which the copper extraction yield increased by 42.21% after 24 days of leaching. However, when the addition was above 120 mg∙L−1, there was a decrease in the copper extraction yield. This inhibition was associated with the negative effect of Triton X-100 on the iron oxidation activity of At. ferrooxidans (Figure 2).
In chemical leaching systems, the leaching efficiency was hardly influenced by Triton X-100 addition. Even at the 200 mg∙L−1 of dosage, the copper extraction yield increased from 75.50 mg∙L−1 to 81.22 mg∙L−1 in 24 days. Zhang et al. reported that polyethylene glycol could promote the chemical leaching of chalcopyrite, but not by much [23]. In contrast, the addition of another nonionic surfactant, Tween 20, had a negative effect toward chalcopyrite dissolution [17]. Hence, we believe that the key factor influencing the surfactant performance is its molecular structure rather than the ionic type. In addition, by comparing Figure 2 and Figure 4, it can be seen that the decrease in the surface tension of solution has little benefit on the dissolution of chalcopyrite.

3.4. The Induction of Chalcopyrite Bioleaching

A more detailed study of the optimal concentration (30 mg∙L−1) of Triton X-100 was conducted in systems without any energy substance like Fe2+ and S0. Changes in the solution pH, the number of planktonic bacteria, and the concentrations of Fe2+, Fe3+, and Cu2+ ions are shown in Figure 5. Based on the variation regularity of these parameters, the whole process was divided into three stages: the first stage (day 0–3), the second stage (day 3–9), and the third stage (day 9–24).
In the first stage (day 0–3), the concentration of bacteria remained invariable due to the bacterial adaptive period both in the absence and presence of Triton X-100, as shown in Figure 5A. Moreover, it was observed that the solution pH and the concentration of Fe2+ increased. This was because the active sites like micro-pores, micro-cracks, and lattice defects on the chalcopyrite surface were first attacked by protons and dissolved oxygen (Reaction (2)), and at the same time Fe2+ and S0 were released. However, in terms of copper extraction, little change was observed between the control and the Triton X-100 addition in this stage.
CuFeS 2 + 4 H + + O 2 c h e m i c a l Cu 2 + + Fe 2 + + 2 S 0 + 2 H 2 O
In the second stage (day 3–9), although S0 also existed in the leaching system, water-soluble Fe2+ was more readily usable by At. ferrooxidans [35]. The accumulation of Fe2+ created a favorable condition for bacteria growth, and thus the number of bacteria increased rapidly, as shown in Figure 5A. However, the Triton X-100 addition delayed the bacteria growth, owing to its inhibition on the bacterial iron-oxidizing activity (Figure 2). As a result, the presence of Triton X-100 inhibited copper extraction from chalcopyrite to a certain degree.
In the third stage (day 9–24), the leaching solution pH declined gradually both with and without the Triton X-100 addition. This could be attributed to the fact that, although the oxidation of Fe2+ led to H+ consumption (Reaction (3)), the oxidation of S0 into sulfate took place simultaneously (Reaction (1)). Remarkably, the solution pH declined from 1.90 (without Triton X-100) to 1.84 (with Triton X-100) after 24 days of leaching, suggesting an increase in the acid production due to S0 oxidation. This evidence proved that Triton X-100 addition could induce the oxidative dissolution of S0 formed in the leaching process. The increase of the bioavailability of S0 provided more energy substrate to the bacteria growth in turn. Thus, without Triton X-100, the bacterial concentration reached a maximum of 9.5 × 107 cells∙mL−1 at day 9, and then decreased afterward. By contrast, with Triton X-100, the bacterial concentration rose again after 9 days of leaching and reached a maximum of 1.3 × 108 cells∙mL−1 at day 18.
In the meantime, the rate of Fe2+ ions biooxidation (Reaction (3)) was enhanced because of higher a concentration of bacteria. Therefore, it was shown that the Fe3+ ions concentration increased from 101.41 mg∙L−1 (without Triton X-100) to 179.85 mg∙L−1 (with Triton X-100) on day 24. However, in the absence of Triton X-100, the concentration of Fe3+ ions no longer increased after 15 days, owing to the precipitation of jarosite, as expressed by Reaction (4). According to Vera et al. [36], the increase in concentration of Fe3+ ions, as an oxidant, could help the chemical oxidation of chalcopyrite, as expressed by Reaction (5). As a result, the addition of Triton X-100 could effectively enhance the dissolution of chalcopyrite between day 9 and day 24, and the final copper leaching recovery was 223.24 and 317.46 mg∙L−1 without and with Triton X-100 addition, respectively.
4 Fe 2 + + O 2 + 4 H + A t .   f e r r o o x i d a n s 4 Fe 3 + + 2 H 2 O
3 Fe 3 + + 2 SO 4 2 + 6 H 2 O + M + M Fe 3 ( SO 4 ) 2 ( OH ) 6 + 6 M +
CuFeS2 + 4Fe3+ → Cu2+ + 5Fe2+ + 2S0
where M represents K+, NH4+, Na+, or H3O+.

3.5. Analysis of Chalcopyrite Surface after Leaching

Figure 6 presents the XRD results of chalcopyrite after being bioleached with and without Triton X-100. The original chalcopyrite sample was used as a control. Results showed that potassium jarosite (KFe3(SO4)2(OH)6) and elemental sulfur (S0) were generated in the process of chalcopyrite biooxidation, in accordance with the finding of Bevilaqua et al. [37]. This also indicated that S0 formed in the process could not be efficiently oxidized and dissolved even in the presence of At. ferrooxidans. By contrast, in the presence of Triton X-100, S0 was not found in the leaching residue, suggesting that the proposed surfactant could induce the biooxidation of S0. These observations agreed well with the results shown in Figure 3.
Figure 7 presents the surface micro-morphologies of the chalcopyrite bioleached without and with Triton X-100. Without the surfactant, the surface of mineral particles was covered with a large accumulation of flocculent precipitates. These insoluble precipitates (i.e., potassium jarosite and elemental sulfur) were detrimental to the leaching reaction, resulting in a decrease of the leaching rate (Figure 5B). Meanwhile, only a few signs of corrosion were observed on the surface of chalcopyrite. However, in the presence of Triton X-100, the surface was eroded strongly. Scale- and ladder-like structure was displayed, and only a small amount of precipitate was observed on the mineral surface. These results indicated that the appearance of leached chalcopyrite surface was notably changed by the addition of Triton X-100.
It is worth noting that few cells can be observed in Figure 7. The similar phenomenon can also be observed in other studies [38,39,40]. However, if the samples after bioleaching were pretreated using a series of operations including fixing, dehydrating, critical point drying, or freeze-drying, the cells attached to mineral surfaces would be clearly visible [41,42,43]. Thus, the loss of cells was probably due to the damage of cell structure, but this hardly affected the observation of the passivation layer formed on the mineral surface.
Figure 8 represents the XPS spectra of the surface of chalcopyrite bioleached with and without Triton X-100. In terms of Cu 2p, two spectra peaks of 932.1 and 951.95 eV existed whether Triton X-100 was added or not. This observation indicated that copper on the mineral surface might be in a +2 valence state, according to Todd et al. [44]. Thus, it was considered that the Triton X-100 addition could not change migration path of copper during the oxidation of chalcopyrite.
There are numerous studies on the oxidation state for Cu, Fe, and S in the bulk structure of chalcopyrite, but two different opinions exist on its structure: one is Cu+Fe3+S2 [45], the other is Cu2+Fe2+S2 [44,46]. Remarkably, the small separation of the energies between the main peak of Cu(II)-oxides and sulfides compared to the peak of Cu(I)-oxides and sulfides requires extreme care [45]. Coincidentally, the main Cu 2p peaks of these two samples were centered at 932.1 eV, which were in good agreement with the value of the Cu 2p peak of CuS, according to the studies of Zhao and Ghahremaninezhad et al. [47,48]. This indicated that CuS might be generated, as an intermediate product at a late stage of chalcopyrite leaching. Córdoba and He et al. [38,49] also demonstrated the presence of CuS during the oxidation of chalcopyrite, though short-lived. Thus, Reaction (5) should be amended and divided into two steps. First, it was oxidized, forming CuS as an intermediary product:
CuFeS2 + 2Fe3+ → CuS + 3Fe2+ + S0
Then, CuS was oxidized by ferric ion, releasing copper ions:
CuS + 2Fe3+ → Cu2+ + 2Fe2+ + S0
From the results of Fe 2p spectra, the strongest peak appeared near 711.5 eV, as the emission characteristics of Fe3+, indicating that iron(III) (hydro)oxide productions at the surface had been formed at the mineral’s surface [50]. In this study, this mainly referred to potassium jarosite, as shown in Figure 6. The peak at 708.6 ± 0.2 eV was assigned to Fe(II)-S, which came from the chalcopyrite crystal structure [51]. Also, the peak at 724.4 eV could be attributed to the other spin orbit component of iron bulk chalcopyrite, according to the result of Harmer et al. [51]. The increase in intensity of the Fe2+ peak indicated that more fresh surface was exposed from the passivation layer under the effect of Triton X-100.
From the results of S 2p spectra, it was shown that S0 (164.5 eV) was detected when chalcopyrite was bioleached without additives [52]. This phenomenon demonstrated that S0, as an intermediate in the leaching process, was not efficiently oxidized by the sulfur-oxidizing bacteria (i.e., At. ferrooxidans) and easily stored on the mineral surface. However, in the presence of Triton X-100, S0 was not detected, confirming that Triton X-100 addition could eliminate S0 from the mineral surface, which was accordant with XRD results of the leach residues in Figure 6.
Furthermore, Triton X-100 decreased the intensity of the SO 4 2 peak (168.4 eV), which suggested that the amount of jarosite formed on the mineral surface had been removed [53]. This can be attributed to two reasons: (i) the solubilization of formed S0 dispersed the oxidation products from the mineral surface, which was similar with the role of Tweens in cobalt ore bioleaching [29]; and (ii) the decrease in solution pH value (below 1.9) delayed the jarosite formation to a certain extent [54].
In addition, monosulfid S2− (161.3 eV), disulfide S 2 2 (162.5 eV), and polysulfide S n 2 (163.4 eV) were also present on the surface whether Triton X-100 was added or not [50]. The peak at 161.3 eV was generated from the chalcopyrite crystal structure [53]. Previous studies showed that the oxidation reaction of sulfide minerals followed two pathways: (i) the thiosulfate pathway, S2− → S2+ → S6+; and (ii) the polysulfide pathway, S2− → S0 → S6+ [36,55]. In the present study, we speculated that the oxidation of chalcopyrite occurred in the second way, and the valence-state changes of sulfur followed the order as below: S2− S 2 2 S n 2 → S0 SO 4 2 . However, it was important to note that neither disulfide S 2 2 nor polysulfide S n 2 species were directly detected by XRD results, indicating that these intermediates were amorphous and unstable which would be ultimately oxidized into sulfate.

3.6. Model of the Enhancement of Bioleaching

Based on the above investigations, a model for enhancing chalcopyrite bioleaching using surfactant Triton X-100 was proposed, as shown in Figure 9. The chalcopyrite bioleaching process could be regarded as a three-step process:
(i)
In the first stage, the addition of Triton X-100 could hardly influence chalcopyrite leaching. Chalcopyrite was initially attacked by protons, simultaneously releasing ferrous iron and elemental sulfur, as Reaction (2) proceeded.
(ii)
In the second stage, the bacterial leaching of chalcopyrite is slightly prevented by the addition of Triton X-100. This was mainly because the surfactant addition had a negative effect on iron-oxidizing activity of the leaching bacteria, and the bacteria would first use soluble Fe2+ rather than insoluble S0 as the energy resource, as illustrated by Reactions (1) and (3).
(iii)
In the third stage, chalcopyrite bioleaching was promoted under the induction of Triton X-100, and the copper extraction efficiency increased remarkably. Triton X-100 induced the bioavailability of formed S0, consequently destroying the structure of the passivation layer. On the other hand, the decrease of the leaching solution pH delayed jarosite formation (Reaction (4)), and favored the “indirect” oxidation of chalcopyrite (Reaction (5)), which in turn maintained the ongoing dissolution of chalcopyrite.

4. Conclusions

The presented work gives insights into the mechanism of enhancing meso-acidophilic chalcopyrite bioleaching using the surfactant Triton X-100. Results showed that the optimum dosage of Triton X-100 was 30 mg∙L−1, and the copper extraction yield increased by 42.21% compared to the normal bioleaching without an additive. However, the surfactant itself had no ability to leach chalcopyrite. The presence of Triton X-100 induced the biooxidation of S0, owing to more rapid contact between the bacteria and sulfur particle, but it decreased the iron-oxidizing activity of At. ferrooxidans. During the bioleaching process, the addition of Triton X-100 increased the concentrations of bacteria and removed inhibitory jarosite and S0 from the mineral surface, thereby accelerating the chalcopyrite oxidation. This study indicates that increasing the sulfur-oxidizing activity of bacteria can enhance chalcopyrite bioleaching, and the application of the surfactant Triton X-100 is a potential method.

Author Contributions

R.Z. and C.S. designed the experiment, performed the study, and wrote the manuscript. J.K. and H.Z. performed the experiment and the analyses of leached chalcopyrite surface. D.W. and Y.X. coordinated the study and modified the draft of the manuscript. All authors gave final approval for publication.

Funding

This research was funded by the National Natural Science Foundation of China (No. 51804020), the China Postdoctoral Science Foundation (No. 2018M631343), and the Fundamental Research Funds for the Central Universities (No. FRF-TP-17-025A1).

Acknowledgements

We thank Emre Naci Altun (Middle East Technical University, Turkey) for providing advice on manuscript preparation.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Chemical structure of surfactant Triton X-100.
Figure 1. Chemical structure of surfactant Triton X-100.
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Figure 2. Influences of Triton X-100 on iron-oxidizing activity of At. ferrooxidans and on the surface tension of solution: (A) bacteria inoculation 10% (v/v), initial Fe2+ 8.9 g∙L−1, initial pH 2.0, rotational speed 160 rpm, and temperature 30 °C; (B) Fe2+ 0 g∙L−1, pH 2.0, and temperature 30 °C.
Figure 2. Influences of Triton X-100 on iron-oxidizing activity of At. ferrooxidans and on the surface tension of solution: (A) bacteria inoculation 10% (v/v), initial Fe2+ 8.9 g∙L−1, initial pH 2.0, rotational speed 160 rpm, and temperature 30 °C; (B) Fe2+ 0 g∙L−1, pH 2.0, and temperature 30 °C.
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Figure 3. Influences of Triton X-100 on contact angle of S0 and bacterial attachment to S0, as well as on the oxidation of S0: (A) S0 1% (w/v), bacteria inoculation 5 × 107 cells·mL−1, temperature 30 °C, and adsorption time 30 min; (B) S0 1% (w/v), bacteria inoculation 10% (v/v), initial pH 2.1, and temperature 30 °C.
Figure 3. Influences of Triton X-100 on contact angle of S0 and bacterial attachment to S0, as well as on the oxidation of S0: (A) S0 1% (w/v), bacteria inoculation 5 × 107 cells·mL−1, temperature 30 °C, and adsorption time 30 min; (B) S0 1% (w/v), bacteria inoculation 10% (v/v), initial pH 2.1, and temperature 30 °C.
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Figure 4. Influences of Triton X-100 on Cu extraction from chalcopyrite in the absence and presence of bacteria. Chalcopyrite 1% (w/v), bacteria inoculation 2 × 107 cells∙mL−1 for bioleaching systems, NaF 0.1 g·L−1 for abiotic leaching systems, initial Fe2+ 0 g·L−1, initial pH 2.0, and leaching for 24 days.
Figure 4. Influences of Triton X-100 on Cu extraction from chalcopyrite in the absence and presence of bacteria. Chalcopyrite 1% (w/v), bacteria inoculation 2 × 107 cells∙mL−1 for bioleaching systems, NaF 0.1 g·L−1 for abiotic leaching systems, initial Fe2+ 0 g·L−1, initial pH 2.0, and leaching for 24 days.
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Figure 5. Influences of Triton X-100 on the bioleaching behavior of chalcopyrite. (A) Variation of pH and cell density; (B) Variation of the concentrations of Fe2+, Fe3+ and Cu2+. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, and temperature 30 °C).
Figure 5. Influences of Triton X-100 on the bioleaching behavior of chalcopyrite. (A) Variation of pH and cell density; (B) Variation of the concentrations of Fe2+, Fe3+ and Cu2+. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, and temperature 30 °C).
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Figure 6. XRD analysis of (a) the original chalcopyrite, and the chalcopyrite bioleached (b) without Triton X-100 and (c) with Triton X-100. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, temperature 30 °C, and leaching for 24 days).
Figure 6. XRD analysis of (a) the original chalcopyrite, and the chalcopyrite bioleached (b) without Triton X-100 and (c) with Triton X-100. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, temperature 30 °C, and leaching for 24 days).
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Figure 7. SEM results of chalcopyrite bioleached (A) without Triton X-100 and (B) with Triton X-100. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, temperature 30 °C, and leaching for 24 days).
Figure 7. SEM results of chalcopyrite bioleached (A) without Triton X-100 and (B) with Triton X-100. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, temperature 30 °C, and leaching for 24 days).
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Figure 8. Cu 2p, Fe 2p and S 2p XPS spectra of chalcopyrite bioleached without and with Triton X-100. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, temperature 30 °C, and leaching for 24 days).
Figure 8. Cu 2p, Fe 2p and S 2p XPS spectra of chalcopyrite bioleached without and with Triton X-100. (Chalcopyrite 1% (w/v), Triton X-100 30 mg∙L−1, initial cell density 2 × 107 cells∙mL−1, initial Fe2+ 0 g∙L−1, initial pH 2.0, rotational speed 160 rpm, temperature 30 °C, and leaching for 24 days).
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Figure 9. Proposed schematic diagram of enhancing chalcopyrite bioleaching under the induction of Triton X-100. The numbers (1)–(5) represent the Reactions (1)–(5).
Figure 9. Proposed schematic diagram of enhancing chalcopyrite bioleaching under the induction of Triton X-100. The numbers (1)–(5) represent the Reactions (1)–(5).
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Zhang, R.; Sun, C.; Kou, J.; Zhao, H.; Wei, D.; Xing, Y. Enhancing the Leaching of Chalcopyrite Using Acidithiobacillus ferrooxidans under the Induction of Surfactant Triton X-100. Minerals 2019, 9, 11. https://doi.org/10.3390/min9010011

AMA Style

Zhang R, Sun C, Kou J, Zhao H, Wei D, Xing Y. Enhancing the Leaching of Chalcopyrite Using Acidithiobacillus ferrooxidans under the Induction of Surfactant Triton X-100. Minerals. 2019; 9(1):11. https://doi.org/10.3390/min9010011

Chicago/Turabian Style

Zhang, Ruiyang, Chunbao Sun, Jue Kou, Hongyu Zhao, Dezhou Wei, and Yi Xing. 2019. "Enhancing the Leaching of Chalcopyrite Using Acidithiobacillus ferrooxidans under the Induction of Surfactant Triton X-100" Minerals 9, no. 1: 11. https://doi.org/10.3390/min9010011

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