1. Introduction
The increasing global demand for lithium, driven by its essential role in the production of lithium-ion batteries used in electric vehicles, energy storage systems, and portable electronics, has stimulated intensive research into sustainable and economically viable extraction methods. According to projections of international analytical agencies, global lithium demand by 2030 may increase by a factor of 5–6 compared to 2020 levels, largely due to the worldwide transition toward decarbonization and renewable energy sources [
1,
2].
Traditional lithium resources—high-grade ores (spodumene, lepidolite, petalite) and brines—are concentrated mainly in China, Australia, Chile, Bolivia, and Argentina. However, the development of such deposits faces several ecological and technological challenges, including the high energy intensity of pyrometallurgical processing, the need for complex multi-stage pretreatment, and the generation of substantial volumes of waste [
3,
4]. In light of the depletion of easily extractable resources and the tightening of environmental regulations, growing attention is being directed toward the processing of low-grade and anthropogenic feedstocks [
5,
6,
7,
8,
9,
10].
Among the most promising alternative sources of lithium are mine tailings generated during the processing of rare-metal ores. These tailings often contain residual lithium associated with muscovite, feldspar, albite, and other aluminosilicates, which are resistant to direct leaching [
11,
12]. Their utilization not only enables the recovery of valuable components but also contributes to land reclamation and the mitigation of environmental impact [
13].
Currently, several approaches are employed for lithium recovery from such materials, including acid leaching, alkaline treatment, sulfate and chloride roasting, as well as high-temperature salt and alkaline roasting [
14,
15,
16,
17,
18,
19]. Sulfate-based technology, first proposed by Ellestad and Leute [
20], has gained the widest application. The process involves decrepitation of spodumene concentrate, with transformation of α-spodumene into the β-phase, subsequent treatment with concentrated H
2SO
4 at 250 °C, and water leaching of the roasted product; after purification, lithium is precipitated as carbonate. The main advantage of this method lies in its applicability to both rich and lean ores. Previous studies have explored ways to improve its efficiency and to activate various lithium-bearing minerals [
21,
22].
It has been established that the efficiency of lithium recovery is strongly influenced by the temperature of sulfuric acid treatment, residence time, the type and dosage of the reagent, particle size of the feed, and the parameters of subsequent leaching [
23,
24,
25]. However, the relationship between the phase transformations of the aluminosilicate matrix and the degree of lithium recovery remains insufficiently investigated. Against this background, the application of statistical tools such as analysis of variance (ANOVA) and response surface methodology (RSM) becomes particularly relevant, as these approaches enable process optimization while reducing the number of experimental trials [
26].
The scientific literature shows that most studies focus either on primary ores (mainly spodumene) or spent lithium-ion batteries, whereas lithium extraction from aluminosilicate-rich anthropogenic tailings remains comparatively underexplored. Moreover, in several works, a comprehensive approach is lacking, particularly one that combines experimental determination of key factors with the development of a robust regression model for predicting lithium recovery [
27].
Kazakhstan possesses a number of large-scale storage facilities of anthropogenic waste that are potentially suitable for integrated processing. One such site is the Maralushinskoe tailings storage facility, formed during the long-term operation of the Ognevskaya beneficiation plant. Mineralogical analysis revealed that lithium in these tailings is predominantly hosted in stable aluminosilicate phases [
28], which necessitates thermochemical pretreatment prior to leaching. Of particular interest is the potential adaptation of sulfate roasting to the specific mineralogical and chemical composition of these tailings.
Therefore, the objective of the present study is to investigate the influence of sulfation parameters and subsequent acid leaching conditions on the efficiency of lithium extraction from the Maralushinskoe tailings. An additional goal was to construct a mathematical model using response surface methodology (RSM) to optimize the leaching parameters of lithium from the sulfate clinker. The factors considered include temperature, process duration, and liquid-to-solid ratio. All experiments were designed using factorial analysis, and the data were statistically evaluated through analysis of variance and multivariate regression, allowing identification of the most significant parameters and construction of a reliable regression model.
The obtained results can be applied to determine the optimal processing conditions for aluminosilicate lithium-bearing tailings and to design efficient technological schemes suitable for industrial application.
3. Results and Discussion
3.1. Mineralogy and Thermal Analysis
The rare-metal production tailings represent a technogenic mineral raw material with a high content of aluminosilicate components. According to chemical analysis, the main components are oxides of silicon, aluminum, sodium, and potassium. The overall chemical composition is presented in
Table 3.
According to XRD results (
Figure 1), the phase composition is dominated by aluminosilicates: albite (Na
0.
98Ca
0.
02)(Al
1.
02Si
2.
98O
8), muscovite KAl
2(Si,Al)
4O
10(OH)
2, microcline KAlSi
3O
8, and quartz SiO
2.
Thermal behavior of the tailings was investigated using differential thermal analysis (DTA) and derivative thermogravimetry (DTG). A 425 mg sample was heated up to 1224 °C at a rate of 15 °C/min.
The thermogram (
Figure 2) showed a pronounced endothermic effect with a maximum at 564.5 °C, corresponding to the enantiotropic polymorphic transformation of quartz. In addition, an exothermic effect at 478.7 °C and the corresponding minimum on the DTG curve at 469.5 °C were recorded, which are associated with the oxidation of minor carbonaceous residues formed during the long-term open storage of the tailings. These residues do not host lithium. The endothermic maximum on the dDTA curve at 833.9 °C is interpreted as dehydration of muscovite, whereas the minimum at 272.6 °C likely corresponds to dehydration of iron hydroxide.
Upon cooling, weak exothermic peaks appeared on the DTA curve at 872.2 °C and 979.6 °C, possibly indicating crystallization of sodium silicate (Na2O·2SiO2) and potassium silicate (K2O·SiO2), respectively. An exothermic peak at 1168.6 °C on the dDTA curve is interpreted as the formation of lithium silicate (Li2O·SiO2). An endothermic effect at 554 °C observed during the cooling stage may indicate the reverse transformation of high-temperature β-quartz into its α-modification.
Mineralogical analysis aimed at identifying the forms of lithium occurrence was performed using physicochemical methods, including quantitative grain size and morphological analysis with a binocular microscope at 25–40× magnification. It was established that lithium in the tailings is mainly present as isomorphic substitutions in muscovite and biotite, and partially as the native mineral spodumene. This conclusion is supported by XRD and thermal analysis data, as well as by microscopic and luminescent methods, which confirmed the presence of spodumene and the structural incorporation of lithium into aluminosilicate minerals.
Spodumene was confirmed in the sample (
Figure 3b). The mineral is characterized by perfect cleavage, vitreous luster, translucent white color, hardness of ~6.5, and bright yellow–orange cathodoluminescence. Crystals are small, elongated-prismatic in shape.
In addition, biotite occurs as anhedral grains with typical brown coloration and sizes up to 0.2 mm, whereas muscovite appears as colorless, irregularly shaped grains with diameters up to 0.06 mm (
Figure 4).
Thus, the obtained data on the material composition confirm the feasibility of applying thermochemical opening by sulfation. The presence of lithium as isomorphic substitutions in muscovite and biotite, and partly as spodumene, indicates that these minerals are locked within a stable aluminosilicate matrix. Sulfation decomposes this matrix, transforming lithium into soluble sulfate forms and thereby making it available for subsequent leaching.
3.2. Investigation of Sulfation and Lithium Leaching Parameters
The results of aqueous leaching of the clinkers (90 °C, L/S = 6:1, 1 h), presented in
Table 4, revealed a clear dependence of lithium recovery on the sulfation temperature. At 100 °C, lithium recovery was 34.63%, and it progressively increased with temperature, reaching 67.83% at 300 °C. A similar upward trend was observed for aluminum, where recovery increased from 2.92% at 100 °C to 26.25% at 300 °C, while iron consistently exhibited high recoveries in the range of ~80.56–83.47% across all tested conditions. The maximum lithium recovery of 67.83% was recorded at 300 °C, which is close to the boiling point of 93% H
2SO
4 (278–283 °C at 760 mmHg [
29]). The pronounced increase in recovery within the 250–300 °C range highlights the enhanced reactivity of the system at these conditions. The higher lithium yield at 300 °C, despite the proximity to the boiling point of concentrated sulfuric acid, can be attributed to the specific thermal behavior of the system and the partial decomposition of the aluminosilicate matrix. This transformation likely facilitated the release of lithium from the structures of muscovite and biotite into soluble sulfate forms. Overall, the results demonstrate that the temperature range of 250–300 °C is critical for matrix breakdown and provides the most favorable conditions for efficient lithium extraction.
The application of a stepwise heating regime was therefore introduced to trace the sequence of phase transformations of the aluminosilicate matrix and to capture the behavior of concentrated sulfuric acid at different temperature intervals. This methodological choice allowed us to reliably identify the critical window of 250–300 °C and to directly relate it to the enhanced lithium recovery observed in the experiments.
The two-stage sulfation process (first stage: 250 °C, L/S = 1:10, 2 h; second stage: 350–750 °C, 1 h) proved to be less effective (
Table 5). The maximum lithium recovery reached 51.52% at 750 °C, which was lower than the 67.83% achieved during single-stage sulfation at 300 °C. Recovery of aluminum and iron sharply decreased at temperatures above 600 °C (0% and 0.22% at 750 °C, respectively), due to decomposition of their sulfates into insoluble oxides with the release of sulfur gases. The decline in lithium recovery is likely related to the formation of new phases or partial sintering of the clinker, limiting solvent accessibility.
The effect of sulfation duration was studied at 300 °C and L/S = 1:10 for 1–4 h. The maximum lithium recovery (~71.2%) was achieved at 1 h (
Figure 5). Prolonging the duration to 3–4 h reduced recovery, likely due to loss of the acid reagent during extended thermal treatment. Investigation of the effect of L/S ratio (1:10, 1:8, 1:6, 1:4) at 300 °C for 2 h demonstrated that L/S = 1:6 was optimal, providing 80.23% lithium recovery (
Figure 6). Further increases in acid (L/S = 1:4) did not improve efficiency, suggesting saturation of the reaction system.
Hydrochloric acid leaching (0.5 M HCl, 80 °C, L/S = 6:1, 1 h) proved to be less effective than aqueous leaching (
Table 6). The maximum lithium recovery of 48.31% was achieved after single-stage sulfation (300 °C, 2 h), whereas two-stage variants (250 °C + 750 °C; 300 °C + 750 °C) yielded lower recoveries of 41.04% and 39.58%, respectively. This indicates reduced lithium availability due to phase transformations at high-temperature sulfation and the lack of advantages from using HCl.
Considering the identified optimal sulfation conditions (300 °C, L/S = 1:6, duration 1 h, H2SO4) and aqueous leaching parameters (90 °C, L/S = 6:1, 1 h), lithium recovery of 82.3% was achieved. However, results indicated that even under these conditions, extraction efficiency remained limited. Comparison with hydrochloric acid leaching confirmed the superiority of aqueous leaching, highlighting the need for in-depth investigation of this process.
The use of concentrated sulfuric acid at elevated temperatures requires strict safety precautions due to its corrosive and volatile nature. For industrial applications, gas scrubbing systems and effluent neutralization are necessary to minimize environmental impact.
To quantitatively assess the influence of process parameters on lithium recovery, mathematical modeling of aqueous leaching was carried out using response surface methodology.
3.3. Statistical Analysis and Model Selection
The results of analysis of variance (ANOVA) for the response surface methodology (RSM) model of the lithium leaching process are presented in
Table 7.
The F-value of 15.01 indicates high statistical significance of the developed model. The probability that such a high F-value is due to random error is less than 0.01% (p < 0.0001), which is well below the conventional significance threshold of 0.05. This confirms the reliability of the model for interpretation within the established experimental range.
Values of p < 0.0001 highlight the statistical significance of the corresponding model terms. In this case, the significant factors are A (L/S), B (temperature), and the interaction AB (p = 0.0158).
The coefficient of determination R2 = 0.8738, indicating that the model explains 87.38% of the variance in the response. The adjusted R2 = 0.8156 is also high, confirming minimal influence of insignificant terms. However, the predicted R2 (Pred R2) equals 0.4515, which is noticeably lower than the adjusted R2. This discrepancy may point to block error, outliers, or overfitting of the model. Model reduction or transformation of the response variable is recommended to improve predictive performance.
Nevertheless, the Adequate Precision ratio of 14.117 greatly exceeds the minimum acceptable threshold of 4. This demonstrates an excellent signal-to-noise ratio and confirms the suitability of the model for navigating the design space.
Thus, the developed quadratic model demonstrates high statistical significance, good approximation, and acceptable predictive accuracy, providing a robust foundation for further modeling and optimization of lithium extraction conditions.
The regression equation obtained from this analysis is expressed as
Diagnostic plots (
Figure 7) were used to comprehensively assess the adequacy of the constructed quadratic model describing lithium recovery. The normal probability plot of residuals (
Figure 7a) shows that standardized residuals are distributed along the diagonal line of the normal distribution, indicating the absence of significant deviations from normality and confirming the validity of the normal error assumption. The color scale reflecting lithium recovery values (65–95%) demonstrates no dependence of residuals on the level of recovery.
The residuals versus predicted values plot (
Figure 7b) reveals a random distribution of residuals relative to the zero line. The absence of visible trends or systematic deviations confirms that the model is free of autocorrelation and demonstrates satisfactory accuracy within the prediction range (64.5–94.3%). The residuals versus run order plot (
Figure 7c) illustrates the temporal stability of the model: no systematic trends were detected, and residuals remained within ±3, confirming uniform random error and the reliability of the experimental results across all 20 trials. Finally, the predicted versus actual values plot (
Figure 7d) demonstrates a high degree of agreement: most points are grouped along the ideal fit line. Predicted values ranged from 64.5% to 94.3%, while actual recoveries ranged from 64.5% to 95.0%, confirming the high accuracy of the model and its applicability for predicting lithium recovery within the studied factor space.
Author Contributions
Conceptualization, A.Y. (Azamat Yessengaziyev) and Z.K.; methodology, A.Y. (Azamat Yessengaziyev), A.Y. (Albina Yersaiynova) and A.T.; software, K.S., A.M. and A.T.; validation, A.Y. (Azamat Yessengaziyev), Z.K. and B.O.; formal analysis, Z.K.; investigation, A.Y. (Azamat Yessengaziyev), A.Y. (Albina Yersaiynova) and A.T.; resources, K.S., A.M. and B.O.; data curation, Z.K., A.Y. (Albina Yersaiynova) and A.Y. (Azamat Yessengaziyev); writing—original draft preparation, Z.K. and A.Y. (Azamat Yessengaziyev); writing—review and editing, A.Y. (Azamat Yessengaziyev) and Z.K.; visualization, A.M., B.O. and K.S.; supervision, Z.K.; project administration, Z.K.; funding acquisition, Z.K. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by the Science Committee of the Ministry of Science and Higher Education of the Republic of Kazakhstan (Grant No. AP23488932).
Data Availability Statement
The original contributions presented in this study are included in the article. Further inquiries can be directed to the corresponding author.
Conflicts of Interest
The authors declare no conflicts of interest.
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Figure 1.
X-ray diffraction pattern of tailings.
Figure 2.
Thermogram of the tailings obtained during cooling.
Figure 3.
Tailings concentrate under binocular microscope: (a) non-electromagnetic fraction (×25); (b) spodumene in concentrate (×40).
Figure 4.
Muscovite (1) and biotite (2) in tailings sample under binocular microscope.
Figure 5.
Effect of sulfation duration (300 °C, L/S = 1:10) on lithium recovery.
Figure 6.
Effect of L/S ratio during sulfation (300 °C, 2 h) on lithium recovery.
Figure 7.
Diagnostic plots for the quadratic model of lithium leaching: (a) normal probability of residuals, (b) residuals vs. predicted values, (c) residuals vs. run order, (d) predicted vs. actual values.
Figure 8.
Three-dimensional response surface plots of factor interactions (with the third factor fixed) on lithium recovery: (a) A and C, (b) A and B, (c) B and C.
Table 1.
Levels and codes of factors for CCD.
Factor | Symbol | Coding Level |
---|
−1 | 0 | 1 |
---|
Liquid-to-solid ratio (mL) | A | 4 | 7 | 10 |
Time (min) | C | 30 | 75 | 120 |
Temperature (°C) | B | 25 | 57.5 | 90 |
Table 2.
Leaching parameters and ranges applied in the experiments.
Parameter | Values |
---|
Liquid-to-solid ratio (mL) | 4, 5.5, 7 *, 8.5, 10 |
Time (min) | 30, 52.5, 75 *, 97.5, 120 |
Temperature (°C) | 25, 41.25, 57.5 *, 73.75, 90 |
Table 3.
Chemical composition of rare-metal production tailings (wt.%).
Element | Li | Si | Al | Fe | K | Na | Ca | Mg | O | Others |
---|
Content | 0.038 | 35.89 | 6.59 | 0.74 | 2.55 | 3.07 | 0.44 | 0.15 | 49.10 | - |
Table 4.
Effect of sulfation temperature on lithium and associated element recovery into aqueous solution.
Process | Content in Solid Product, % | Recovery into Solution, % |
---|
Li | Al | Fe | Li | Al | Fe |
---|
100 °C |
Sulfation | 0.031 | 4.943 | 0.684 | - | - | - |
Leaching | 0.022 | 6.344 | 0.274 | 34.63 | 2.92 | 81.64 |
150 °C |
Sulfation | 0.029 | 4.617 | 0.655 | - | - | - |
Leaching | 0.023 | 6.772 | 0.319 | 36.17 | 6.19 | 80.83 |
200 °C |
Sulfation | 0.027 | 5.079 | 0.637 | - | - | - |
Leaching | 0.023 | 6.174 | 0.311 | 39.79 | 10.25 | 80.56 |
250 °C |
Sulfation | 0.032 | 5.420 | 0.704 | - | - | - |
Leaching | 0.015 | 5.339 | 0.270 | 60.64 | 25.63 | 83.47 |
300 °C |
Sulfation | 0.029 | 5.234 | 0.660 | - | - | - |
Leaching | 0.017 | 5.168 | 0.275 | 67.83 | 26.25 | 82.29 |
Table 5.
Recovery of lithium, aluminum, and iron during two-stage sulfation.
Process | Content in Solid Product, % | Recovery into Solution, % |
---|
Li | Al | Fe | Li | Al | Fe |
---|
350 °C |
Sulfation | 0.035 | 4.986 | 0.593 | - | - | - |
Leaching | 0.026 | 5.297 | 0.572 | 41.74 | 9.86 | 23.24 |
450 °C |
Sulfation | 0.032 | 5.284 | 0.623 | - | - | - |
Leaching | 0.024 | 5.111 | 0.651 | 44.07 | 12.83 | 11.08 |
550 °C |
Sulfation | 0.033 | 5.262 | 0.570 | - | - | - |
Leaching | 0.024 | 5.140 | 0.677 | 40.86 | 14.81 | 11.34 |
650 °C |
Sulfation | 0.036 | 5.459 | 0.619 | - | - | - |
Leaching | 0.036 | 4.992 | 0.572 | 16.88 | 18.21 | 19.12 |
750 °C |
Sulfation | 0.038 | 5.93 | 0.727 | - | - | - |
Leaching | 0.024 | 6.758 | 0.759 | 51.52 | 0 | 0.22 |
Table 6.
Effect of hydrochloric acid leaching on lithium recovery.
Process | Temperature (°C) | Duration (h) | Li Recovery into Solution (%) |
---|
Experiment 1 |
Sulfation | 300 | 2 | 48.31 |
Experiment 2 |
Sulfation | Mode 1 | 250 | 2 | 41.04 |
Mode 2 | 750 | 1 |
Experiment 3 |
Sulfation | Mode 1 | 300 | 2 | 39.58 |
Mode 2 | 750 | 1 |
Table 7.
ANOVA for the quadratic response surface model.
Source | Sum of Squares | df | Mean Square | F Value | p-Value Prob > F | Standard Error | 95% CI (Lower–Upper) |
---|
Model | 1146.30 | 6 | 191.05 | 15.01 | <0.0001 | – | – |
A-l | 656.10 | 1 | 656.10 | 51.54 | <0.0001 | 2.83 | 635.0–677.2 |
B-C | 348.10 | 1 | 348.10 | 27.34 | 0.0002 | 2.92 | 330.1–366.1 |
AB | 98.00 | 1 | 98.00 | 7.70 | 0.0158 | 3.11 | 90.1–105.9 |
Residual | 165.50 | 13 | 12.73 | – | – | – | – |
Cor Total | 1311.80 | 19 | – | – | – | – | – |
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