3.3. Nickel Matte Smelting with CaS Sulfurizing Agent and Carbon
An investigation was conducted to find out how increasing the CaS addition affected matte formation during the matte smelting process, and, as part of this, the CaS dosage was optimized across a range of conditions, specifically M1–M7, which are provided in
Table 2. According to the findings of the Equilib modelling, it appears that the simulations conducted under conditions M6 and M7 are expected to be the most successful in creating matte that has a high nickel grade.
Table 7 shows a comprehensive overview of the chemical composition of the slag, which resulted from the smelting experiments that involved CaS additions, and were conducted under conditions labelled M1–M7. Slag is primarily composed of the following oxide components: SiO
2, Fe
2O
3, MgO, and Al
2O
3. The CaO content increased from 2.10% in condition M1 to 7.68% in condition M7 as the addition of CaS was increased. Consequently, the slag basicity increased from 0.41 to 0.66. For conditions M1–M5, the slag’s nickel content showed an average variance between 3.5% and 4.0%; however, the nickel dropped to less than 3% when conditions M6 and M7 were applied.
XRD was used to conduct a mineralogical analysis of the slag. The results of the mineralogical analysis for samples M1–M7 are presented in
Figure 6, correlated with varying amounts of CaS sulfurizing agent. The mineralogical structure of the slag produced during the M1 condition experiment was found to be a multi-component system, including magnesium–aluminum–iron oxide (MgAlFeO
4) as evidenced by the PDF number 01–071–1233, and Enstatite, Mg
2FeSi
2O
6, with the PDF number 01–084–2029. With the addition of a relatively small amount of 1.46 wt.% CaS (M1 test), there were no instances of detecting any phases that included CaO. On the other hand, the M2 slag sample exhibited a prevalent formation of the forsterite phase MgFeCaSiAlO
4, according to the PDF number 01–079–1202, which implies that the CaO derived from the CaS addition had been incorporated into the multi–component slag system. Both the M3 and M4 samples showed forsterite as the primary phase, which indicates the increased activity of CaO within the slag. Upon examination of the M5 sample, the presence of the clinopyroxene phase AlCaFeSi
2O
6, which corresponds to the PDF number 01–085–1740, was identified, and this discovery suggests that CaO played a significant role in the creation of new multi-component phases. In the M6 sample, forsterite and ringwoodite (MgFeSiO
4), as indicated by PDF number 01–021–1258, were found, representing a phase originating from the slag’s main constituents. The M7 sample showed that forsterite was still the primary phase and the observation of Diopside, CaMgSi
2O
6, PDF number 01–075–1092, supported the conclusion that the slag contained a higher amount of CaO. Through a synthesis of mineralogical analysis results and XRF measurements, the conclusion was drawn that the multi-component system finds stability in the oxides of primary constituents such as Mg, Fe, Si, and Al, while the role of CaO is notably active in both the creation and stabilization of these phases.
In the smelting experiments that involved varying CaS additions conducted under the M1–M7 conditions, there was no visually observable distinct separation of matte from the slag. However, during the melts from M4 to M7, a dense, thin layer, easily distinguishable from the bulk slag, was observed forming at the slag’s bottom side. The thickness of the layer, which was already dense, grew as the amount of CaS added increased, and in the M6 and M7 trials, the layers that were formed looked similar and had about the same thickness. Using SEM–EDS, the M4, M5, and M6 samples were analyzed for the morphology of the dense bottom layer, and the results can be seen in
Figure 7. Morphological imaging, the mapping of elemental distribution, and the identification of localized phases were all provided through the use of SEM–EDS analysis. As illustrated in the SEM image shown in
Figure 7a, the M4 sample’s bottom layer contained small, matte droplets that had a rounded morphology. Due to their size, the droplets were unable to coalesce and remained within the slag. According to the mapping analysis in
Figure 7b, the areas corresponding to the rounded matte droplets reveal high concentrations of Ni and S, unlike the surrounding dark regions which show an elevated Fe distribution, thus suggesting the formation of small matte droplets. According to the findings of our prior study [
11], we determined that dark iron–magnesium silicates are generated at the base of the slag during the ferronickel extraction from nickel concentrate. The transformation of iron oxide into this zone takes place through a reduction process, wherein iron oxide relinquishes its oxygen, which is subsequently transferred to calcium. The lighter phases, by comparison, demonstrate heightened distributions of Al, Ca, Si, and Mg, which suggests slag components. The results of the elemental distribution mapping for samples M4, M5, and M6 are presented in
Table 8. The presence of matte droplet was confirmed by the detection of 7.73% nickel and 3.65% sulfur in the dense lower layer of the M4 slag. As a result of the accumulation of exceedingly small matte droplets and a phase abundant in Fe, it was established that the thick, bottom layer of the slag was created. Upon morphological analysis of the M5 sample, as illustrated in
Figure 7c,d, it was observed that the matte droplets not only had increased in size, but also that a higher concentration of droplets developed. The mapping analysis showed a clearer distinction in the matte’s separation droplets, with the elemental distributions showing 8.73% nickel and 6.32% sulfur, and these percentages were higher than the corresponding values observed in the M4 sample. The morphological analysis of the M6 sample, as depicted in
Figure 7e,f, revealed that the initially separate matte droplets had, in fact, combined to create considerably larger groupings. While a few minor droplets persisted, they were significantly fewer. The dark areas rich in iron that usually surround the droplets of matte were not something that was seen. The elemental distribution map revealed that the concentrations of nickel and sulfur were 10.95% and 10.22%, respectively, suggesting an increased level of matte accumulation in the lower layer.
The elemental composition of the spectrums in
Figure 7, as determined by EDS point analysis, is shown in
Table 9. As shown in
Figure 7a, an analysis of the M4 sample revealed three distinct matte droplets correlated with spectrum 1, 2, and 3, and each of these droplets presented Fe, Ni, and S elemental distributions. Spectrum 1 showed 51.54% Ni and 48.46% S. Spectrum 2 showed 11.26% Fe, 60.72% Ni, and 28.02% S. Spectrum 3 showed 15.07% Fe, 52.04% Ni, and 32.89% S. The outcomes confirm the creation of matte with a comparatively high nickel composition. Conversely, spectrums 4 and 5 exhibited distributions of Fe, Mg, Al, Si, and Ca—elements indicative of slag-forming constituents—suggesting that those areas correlate with slag. The presence of Ni, Fe, and S was also confirmed by the elemental distributions that were gained from spectrum analyzes 6 and 7 of sample M5, as shown in
Figure 7c, and from spectrum 10 of sample M6, shown in
Figure 7e, which shows that high-nickel matte had formed. In contrast, the principal slag-forming elements were observed in spectra 8 and 9 for sample M5 (
Figure 7c) and spectrum 10, 11, and 12 for sample M6 (
Figure 7e). Spectrum EDS analysis of matte droplets in samples M4–M6 revealed nickel concentrations ranging from 40% to 50%, iron concentrations from 10% to 25%, and sulfur concentrations from 28% to 39%. These values are in close agreement with the matrix composition predicted by Equilib modelling for 4–6 wt.% CaS addition (
Table 3), showing strong agreement between experimental and modelling results.
According to calculations based on stoichiometry, the reduction in both iron and nickel is intensified by increasing the required amount of carbon, which is described in Equation (5). Following the reduction in metal phases, they then merge into the matte, resulting in an increase in the production of matte. With the goal of conducting nickel smelting experiments, the amount of carbon added was adjusted to both two and three times the baseline stoichiometric requirements for the conditions where the concentration of CaS was measured at 5 and 6 wt.%. The experiments were identified using the labels M8, M9, M10, and M11. Increasing carbon addition significantly improved metal separation, confirmed by solid mass formation. The products of slag and matte, as they appeared under condition M9, are illustrated in
Figure 8. The slag had a zoned structure; the bottom side area looked dark and porous, whereas the upper area was notable for its dark, glassy fracturing. Two solid metal bulks with dissimilar sizes were created at the bottom of the crucible.
The chemical compositions of the matte, which resulted from the experiments M8–M11 that were performed with CaS and carbon additions, are shown in
Table 10. The composition of the matte produced in experiment M8 was as follows, 37.17% Fe, 35.62% Ni, and 24.4% S, with a Ni/Fe ratio of 0.96, a result that achieves nearly within the intended target range. Elements like Si, Mg, and Cr were found in small quantities, indicating minor impurities. In experiment M9, the iron content in the matte increased to 45.55% when the carbon addition was increased by 0.35 wt.%, whilst the nickel and sulfur contents saw a decline to 33.2% and 20.48%, respectively. As the experiments M10 and M11 were performed, the iron content continued to rise. According to these findings, the direct addition of carbon does indeed impact the composition of the matte, which is in corresponding with the Equilib modelling results shown in
Table 5.
In the smelting experiments conducted under conditions M8–M11, the morphology and chemical composition of the resultant matte were examined using the analysis of SEM–EDS lining.
Figure 9 provides a visual representation using SEM images showing the morphology of matte samples M8, M9, M10, and M11, additionally displaying the EDS line–scan X-ray intensity pulses. Upon analysis, it was observed that the nickel matte was composed of layered crystals of [Fe,Ni]S
X sulfides, and there was no metallic matrix present. It was observed that the addition of CaS and carbon did not cause any major changes in the matte morphology. Through EDS line-scan analysis, it was found that Fe, Ni, and S were present in all the matte samples from M8 to M11, but the concentrations of these elements differed, which was shown by the X-ray intensity curves. Furthermore, the elemental intensities that were highly fluctuating along the scan lines provided evidence that the matte was not made up of a single, uniform [Fe,Ni]S
X phase.
The elemental distributions for the M8–M11 matte samples, as determined by the EDS line-scan, are shown in
Table 11. The M8–M11 samples all have iron, nickel, and sulfur in them; however, there are compositional distinctions between them. More carbon enhances iron reduction, increasing iron transfer to the matte phase. As shown in
Table 10, the XRF results and these discoveries show a pattern of consistency.
Table 12 shows the analysis of the slag’s composition under experimental conditions M8–M11. The FeO–SiO
2–MgO basic system is where the slag is formed, as its major components show. When the carbon additive was increased three times in the M9 and M11 experiments, the Fe
2O
3 content in the resulting slag decreased to 32.25% and 32.17%, respectively, which suggests that iron reduction occurred. When the CaS additive was 7.30 wt.% and 8.76 wt.%, the CaO content in the slag increased to approximately 7% and 8%. During experiments from M8 to M11, the nickel content dropped from 1.25% to 0.22%, and the M11 experiment, which featured three times increase in the carbon additive, showed a substantial decrease in nickel content, showing a strong correlation between nickel reduction and the carbon additive quantity.
The morphology structure of the slag formed during the matte smelting experiments performed under conditions ranging from M8 to M11, along with the distribution of chemical elements found within the slag, are shown in
Figure 10. The SEM image in
Figure 10a provides a view of the morphology analysis results that were obtained from the M8 slag sample. Differing from the morphological structure of the M4–M6 slags, which was influenced by the CaS additive amount, as presented in
Figure 7, this slag is mainly composed of the slag matrix and irregularly shaped white crystals that have sharp edges embedded within the matrix, and there was no considerable distribution of matte droplets to be seen. Based on the elemental distribution obtained through EDS mapping analysis (
Figure 10b), the slag composition primarily comprises oxides of Fe, Si, Mg, Al, and Ca, with a prominent sulfur distribution, stated in pink. Upon conducting an EDS point analysis within this specific region, the results show a matte droplet with the following elemental composition: 34.02% sulfur, 33.80% iron, and 32.18% nickel, as shown in Spectrum 1 of
Figure 10a. The slag samples from M9, as shown in
Figure 10c, and M10, which is shown in
Figure 10e, did not contain any detectable matte droplets. The structure of their morphology is composed of hard crystals, which are embedded within the matrix, a characteristic that resembles the M8 slag sample. Based on the EDS mapping analysis displayed in
Figure 10d,f, the slag is composed of various oxides, including those of elements like Mg, Fe, Si, Al, and Ca. The M11 slag sample’s morphology stood in contrast to that of the other samples, featuring an arrangement of large, rigid crystals, as depicted in
Figure 10g. Through detection, the distribution of elements including Mg, Fe, Si, Al, and Ca was observed, and it was also determined that the dark-coloured slag matrix resulted from compounds based on Al, Ca and Si, as shown in
Figure 10h.
Table 13 shows the results of the element distribution analysis conducted on the slag samples produced during the M8–M11 condition. The slags, which are part of the FeO–SiO
2–MgO system, have been confirmed as such by analyzing the distribution of Fe, Si, and Mg elements. The M8 sample uniquely exhibited a sulfur detection at 2.22%, and this finding corresponds directly with the matte sections displayed in
Figure 10a, as stated in Spectrum 1. It was found that Al and Ca were present as elements that were not part of the primary composition, showing that they were impurities.
Figure 11 displays the results of the mineralogical analysis of the slag from experiments M8–M11. As was previously stated in
Figure 6, the CaS changes the slag structure into primarily composed of forsterite MgFeCaSiAlO
4. The slags that resulted from the M8–M11 experiments exhibited a structure that was largely characterized by forsterite. When examining the M11 slag, despite the emergence of Augite (MgFe),(CaMg)(SiAl)
2O
6 phases (PDF number 01–076–0544), there were no other remarkably different alterations observed.