3.1. Effect of Calcination Temperature
X-ray diffraction (XRD) characterization analysis was conducted on the pristine fly ash, with the mineral composition analysis presented in
Figure 1. The mineral constituents of the fly ash are predominantly mullite (3Al
2O
3·2SiO
2), quartz (
α-SiO
2), hematite (Fe
2O
3), and aluminosilicate glass phases. Notably, aluminum oxide is primarily present in the form of mullite (3Al
2O
3 2SiO
2) and aluminosilicate glass phases (M
2(SiO
3)
n).
To elucidate the phase transformation mechanism of mullite under the influence of sodium carbonate, this study employed X-ray diffraction (XRD) technology to identify the phases of the fused samples of fly ash mixed with sodium carbonate under various reaction temperature conditions.
Figure 2 illustrates the phase changes obtained from the analysis.
The evolution of XRD diffraction peak intensities constitutes a composite manifestation of crystallographic integrity, phase composition, lattice defects, and chemical modifications. This intensity modulation is directly governed by structural reorganization within crystalline domains and/or surface functionalization processes. Three primary mechanisms govern this correlation: (i) crystallinity variation, (ii) phase transformations, and (iii) emergence of neoformed phases. As evidenced by the phase evolution diagram in
Figure 2, a characteristic amorphous-to-crystalline transition occurs, after high-temperature roasting of fly ash; mullite (2, 3Al
2O
3·2SiO
2, orthorhombic) precipitates from the glassy phase, with its crystal plane diffraction peak intensity increasing with higher crystallinity.
Upon comparing the results of
Figure 1 with
Figure 2, it is evident that as the calcination temperature gradually increases, the XRD diffraction peak intensities of both mullite (3Al
2O
3·2SiO
2) and sodium carbonate (1, Na
2CO
3, orthorhombic) exhibit a declining trend. This phenomenon manifests directly in XRD diffraction patterns, where crystalline phase diffraction arises from the long-range ordering of lattice periodicity. In contrast, amorphization disrupts this structural coherence, resulting in progressive attenuation of long-range order parameters (LRO). Consequently, the corresponding diffraction peak intensity decreases significantly or disappears. Specifically, the diffraction peaks of sodium carbonate (Na
2CO
3) almost completely vanish above 700 °C. This phenomenon emerges in the 700–800 °C range, contrasting with the intrinsic decomposition threshold of pure sodium carbonate (>850 °C). The depressed decomposition temperature originates from four synergistic mechanisms: (i) Reactive interfacial coupling between Na
2CO
3 and aluminosilicate oxides (e.g., SiO
2/Al
2O
3 in fly ash) generates intermediate sodium aluminosilicate (3, NaAlSiO
4, orthorhombic), as evidenced by XRD peak evolution at 2θ = 42.6°; (ii) Eutectic melting induced by low-melting-point impurities (Fe
2O
3, CaO) creates localized liquid phases, accelerating intermediate formation via enhanced ionic mobility; (iii) Kinetic competition shows that sodium carbonate is not fully decomposed, but released CO
2 and Na
+ modify the silicoaluminate network, forming reactive new phases; (iv) Thermodynamically, intermediate phase formation (ΔG < 0) is spontaneous but must overcome the sodium carbonate decomposition energy barrier. These characteristics are used in low-temperature activation processes for aluminum recovery. Precise temperature control (700 °C) boosts acid leaching efficiency and avoids excessive high-temperature consumption. This demonstrates the environment-dependent thermal stability of Na
2CO
3 in complex systems, where actual decomposition pathways are governed by the chemo-geometric synergy between reactant activity and co-existing phases, while those of mullite (3Al
2O
3·2SiO
2) become nearly invisible above 900 °C. This phenomenon is synergistically driven by three mechanistic dimensions: (i) Pyrolysis–chemical erosion coupling. Residual sodium carbonate or impurities (e.g., Na
+) form low–melting liquid phases. These disrupt the aluminum–oxygen octahedra and silicon–oxygen tetrahedra structures, causing decomposition into corundum (α–Al
2O
3) and quartz (SiO
2). (ii) Thermodynamically, corundum (α–Al
2O
3) and quartz have lower Gibbs free energy than mullite, making them more stable at high temperatures; (iii) In terms of kinetics, ionic diffusion in the liquid phase controls the decomposition rate. The disappearance of mullite reveals its relative thermal stability. Despite a melting point of 1890 °C, its structure is vulnerable to low–temperature attack in alkaline environments or when liquid phases are present. Industrially, temperature (e.g., below 900 °C) must be strictly controlled, or inhibitors added (e.g., pre–desilication to reduce SiO
2 content) to prevent decomposition that increases aluminum recovery difficulty. Also, the metastable nature of mullite indicates that its behavior in high–temperature chemical processing requires considering both thermodynamic stability and kinetic conditions.
Observations from
Figure 2a reveal that at a temperature of 500 °C, the XRD spectrum primarily displays the diffraction peaks of sodium carbonate (1, Na
2CO
3, orthorhombic) and mullite (2, 3Al
2O
3·2SiO
2, orthorhombic), indicating that no significant chemical reaction has occurred between the two at this temperature. Upon raising the temperature to 600 °C, new diffraction peaks begin to emerge, with the formation of a peak for sodium aluminosilicate (3, NaAlSiO
4, orthorhombic) at 42.6°, representing the initial product of the reaction between sodium carbonate (Na
2CO
3) and mullite (3Al
2O
3·2SiO
2). Sodium aluminosilicate (the intermediate phase mentioned earlier) has a looser structure than the original silicoaluminate oxides (e.g., mullite or glassy phase). Its aluminum bonding state is more susceptible to disruption, significantly enhancing aluminum’s chemical reactivity and promoting aluminum leaching efficiency in subsequent acid leaching processes. As the temperature reaches between 600 °C and 700 °C, the diffraction peak of sodium aluminosilicate (NaAlSiO
4) gradually intensifies, suggesting that increased temperature favors the phase transformation reaction of mullite (3Al
2O
3·2SiO
2) under the influence of sodium carbonate (Na
2CO
3), that is, mullite becomes more susceptible to erosion by sodium carbonate and transforms into sodium aluminosilicate (NaAlSiO
4). When the temperature rises to 800 °C, multiple new diffraction peaks appear in the XRD spectrum, indicating the formation of additional phases, including the peaks for sodium metaaluminate (4, NaAlO
2, orthorhombic) at 32.7°, disodium disilicate (5, Na
2Si
2O
5, orthorhombic) at 51.2°, and nepheline (6, NaAlSiO
4, hexagonal) at 33.1°. As the temperature continues to increase to 900 °C, the diffraction peaks for sodium metasilicate (7, Na
2SiO
3, hexagonal) at 51.2° and 63.3° begin to manifest. Further raising the temperature to 1000 °C results in a stable diffraction pattern, indicating that the reaction between mullite (3Al
2O
3·2SiO
2) and sodium carbonate (Na
2CO
3) has reached a relatively stable state. Experimental studies by A. Molina [
24] revealed that when the reaction temperature exceeds 900 °C, the activation efficiency of coal fly ash exhibits a paradoxical decrease rather than enhancement, which can be attributed to high-temperature-induced lattice reconstruction of fly ash components—a process predominantly occurring within the 900–1300 °C temperature range. This phenomenon can be attributed to the lattice reconstruction of fly ash components induced by high temperatures. Therefore, it is clear that during the activation process of fly ash, the increase in temperature does not follow a linear enhancement pattern, meaning that higher temperatures do not necessarily yield better activation effects. After the above structural discussion and considering the reduction in energy consumption, combined with spectral information, it is evident that the activation effect of mullite within the calcination temperature range of 800 to 900 °C is optimal. Hence, further detailed research on phase transformation within this temperature range is warranted.
Following the aforementioned discussion, a detailed study of the phase changes in the fused materials at calcination temperatures of 830 °C, 850 °C, and 880 °C was conducted, with the XRD patterns presented in
Figure 2b. Referring to the XRD pattern of the fused material at a calcination temperature of 800 °C, upon further elevation of the temperature, it becomes evident that the peak intensities of sodium metaaluminate (NaAlO
2) and nepheline (NaAlSiO
4) also continuously rise, and the diffraction peaks of sodium metasilicate (Na
2SiO
3) become increasingly distinct. This indicates that the activation reaction between sodium carbonate and fly ash is still underway within the 800–900 °C range, eventually reaching a relatively stable state. The specific manifestations are as follows: when the calcination temperature reaches 830 °C, the diffraction peaks of sodium metasilicate (Na
2SiO
3) begin to emerge, particularly evident at 63.8°; upon further increasing the temperature, it is found that at a calcination temperature of 850 °C, the peak intensity of nepheline (NaAlSiO
4) continues to increase, and the diffraction peaks of sodium metasilicate (Na
2SiO
3) also gradually become apparent; as the temperature rises to 880 °C, the diffraction peak of nepheline (NaAlSiO
4) essentially reaches its peak value, suggesting that this temperature is sufficient for sodium carbonate (Na
2CO
3) to fully activate the fly ash. Upon synthesis of the experimental findings and ensuing deliberations, it has been concluded that a calcination temperature of 880 °C is optimal for conducting XRD analysis to assess the impact of varying material ratios.
The investigation into high-temperature interactions between sodium carbonate (Na2CO3) and mullite (3Al2O3·2SiO2) has elucidated their synergistic thermokinetic mechanisms, providing critical optimization pathways for industrial and technological applications. This fundamental understanding enables precise control of phase evolution processes while balancing energy efficiency and material performance. In aluminum recovery, precise temperature control (700 °C for reactive intermediate phase formation, avoiding mullite decomposition at 900 °C) boosts efficiency and cuts energy use. In refractory and ceramic industries, mullite stability is maintained by avoiding alkaline conditions, or new functional materials are developed using intermediate phases. In metallurgy, sodium carbonate’s eutectic effect lowers smelting temperatures, and by–product silicate slags are resourcefully used (e.g., in construction materials), promoting circular economy models. These findings, by balancing thermodynamic drives and kinetic constraints, help industries enhance energy efficiency, reduce costs, and achieve environmental goals, advancing resource valorization and sustainable development.
3.2. Effect of Material Ratio
To cleave the silicoaluminate bonds within mullite (3Al
2O
3·2SiO
2), sodium carbonate is selected as an activating agent to react with aluminum oxide and silicon dioxide, thereby generating nepheline (NaAlSiO
4), which is more soluble in acid. This process aims to enhance aluminum extraction through the activation roasting with sodium carbonate. Studies show that the fly ash–sodium carbonate ratio significantly impacts activation efficiency. At low sodium carbonate ratios (1:0.3 to 1:0.5), insufficient carbonate reacts with Al
2O
3 and SiO
2 in fly ash. This prevents the full conversion of the aluminosilicate glass phase to the reactive intermediate phase (NaAlSiO
4), leaving mullite and resulting in an aluminum–leaching rate of less than 65%. At high ratios (1:0.8 to 1:1.0), excess carbonate creates a high–alkalinity liquid phase, causing excessive sintering of fly ash particles. The resulting dense particles hinder acid penetration and produce by–products like sodium silicate, which are detrimental to leaching. Consequently, thise experiment selected fly ash–sodium carbonate ratios of 1:0.3, 1:0.4, 1:0.5, 1:0.6, 1:0.7, 1:0.8, 1:0.9, and 1:1.0, which were used for the roasting activation. Subsequently, the fused materials with varying ratios of fly ash to sodium carbonate were characterized using XRD analysis, with the results presented in
Figure 3.
By comparing the XRD patterns of pristine fly ash (
Figure 1) with those of the fused materials after calcination activation (
Figure 3), it is evident that the degree of reaction between mullite (3Al
2O
3·2SiO
2) in the fly ash and the activating agent, sodium carbonate, varies as the amount of sodium carbonate (Na
2CO
3) increases, leading to a gradual decrease in mullite (3Al
2O
3·2SiO
2) until it disappears. When the material ratio of FA to Na
2CO
3 is between 1:0.3 and 1:0.5, mullite mineral (3Al
2O
3·2SiO
2) partially transforms into nepheline, yet a portion remains as the mullite mineral (3Al
2O
3·2SiO
2) phase. In this stage, the insufficient amount of sodium carbonate restricts the reaction chemically, resulting in a low aluminum leaching rate of only 32% to 65%. The calcination activation product is reddish-brown, loosely textured, and easily removable, with no sintering occurring. At a material ratio of 1:0.6, mullite (3Al
2O
3·2SiO
2) is largely converted into nepheline (NaAlSiO
4, hexagonal), as indicated by the increased presence of nepheline in the XRD patterns. When the ratio is 1:0.7, mullite (3Al
2O
3·2SiO
2) is entirely transformed into nepheline (NaAlSiO
4, hexagonal), suggesting that the amount of sodium carbonate (Na
2CO
3) is sufficient to fully activate the mullite (3Al
2O
3·2SiO
2) in the fly ash. At this ratio (Na
2CO
3/FA ≈ 1:0.6 to 1:0.7), sodium reacts fully with silicoaluminate components, achieving an aluminum leaching rate of 66% to 85%. The calcination activation product is grayish-yellow, soft in texture, and easily removable, with no sintering. At a ratio of 1:0.8, mullite (3Al
2O
3·2SiO
2) disappears entirely, giving rise to nepheline (NaAlSiO
4, hexagonal) and sodium aluminosilicate (NaAlSiO
4), with the calcination activation product being predominantly yellow with some green areas, denser in texture, more difficult to remove, and exhibiting sintering. When the material ratio reaches 1:0.9 and 1:1.0, the XRD pattern peaks are essentially the same as at the 1:0.8 ratio, indicating that the reaction has reached a stable state. The calcination activation product is yellow-green, compact in texture, difficult to remove, and sintered. Excess sodium carbonate creates a high-alkalinity liquid phase that encapsulates particles, triggers side reactions (e.g., sodium silicate formation), and increases acid leaching difficulty, decreasing the leaching rate to 70–75%.
Notably, sodium carbonate loss (e.g., high-temperature volatilization, reactions with Fe
2O
3/CaO impurities) further impacts efficiency. For instance, a 1% increase in CaO content raises sodium loss by about 3%, necessitating a 20–30% excess addition of sodium carbonate to compensate for increasing costs. Thus, an experimental fly ash–sodium carbonate ratio of 1:0.7 achieves the highest aluminum leaching rate (
Figure 4). Higher ratios, though completing mullite conversion, reduce efficiency due to side reactions of by-products (e.g., sodium aluminosilicate does not react with acid; nepheline is acid-soluble), their accumulation, and sintering. To enhance cost-effectiveness, pre-desilication (reducing SiO₂ content) or mineralizers (e.g., CaF₂) can be introduced, lowering the calcination temperature from 750 °C to 650 °C in order to reduce sodium loss.
XRD analysis shows that the fly ash–sodium carbonate ratio affects the product phase composition. At a 1:1 ratio and 880 °C calcination, nepheline forms, boosting aluminum extraction. Excess or insufficient sodium carbonate generates by-products like sodium silicoaluminate or leaves unreacted minerals. Optimizing the material ratio to 1:1 and keeping the calcination temperature around 700 °C reduces by-products and environmental impact. Precise control of the material ratio and impurity management are key to balancing aluminum recovery and process costs. As the ratio of coal fly ash to sodium carbonate increases, the extraction yield of alumina exhibits an initial increase followed by a subsequent decrease. The leaching efficiency of alumina reaches its zenith when the material ratio of coal fly ash to sodium carbonate is 1:0.8, which is in substantial agreement with the phase transformation patterns of the coal fly ash depicted in
Figure 3.
3.3. Effect of Roasting Time
Pursuant to this experiment conducted at a calcination temperature of 880 °C, as established in
Section 3.1, the calcination durations were selected to be 0.5 h, 1.0 h, 1.5 h, and 2.0 h. Upon completion of the reactions, the molten products were allowed to cool naturally and then retrieved. Subsequently, the extraction yield of alumina was measured and calculated following the acid leaching, stirring, and solid–liquid separation procedures outlined in the experimental methods of
Section 2.2. To eliminate experimental anomalies and ensure result reliability, multiple experimental controls and repetitions, shown in
Figure 5, were set up. These considered calcination temperature, time, and material ratio. Three parallel experiment groups were obtained. For example, at a material ratio of 1:0.8 and 830 °C calcination temperature, the extraction rate after 1.5 h (54%) was significantly higher than after 1 h (45%).
As depicted in
Figure 5, the calcination duration exerts a significant influence on the activity of alumina within coal fly ash. At excessively high temperatures (e.g., 2 h), the aluminum extraction rate decreases. This is due to the sintering of particle surfaces from prolonged high-temperature exposure, causing densification. Also, excess sodium salts (Na
+) react with free SiO
2 to form by-products (sodium aluminosilicates), which do not react with acid. Overall, the key mechanism for the decrease in reactivity is a cascade effect of “kinetic hindrance (sintering) → by-product formation → thermodynamic reverse reaction”, resulting in a trend where the extraction yield of aluminum first increases and then decreases. Within the range of 0.5 h to 1.5 h of calcination, the gradient of the extraction rate curve is in the steeply ascending segment; there is a direct correlation between the extended duration and the increased reactivity of alumina, which corresponds to a notable improvement in the extraction yield of aluminum, a pattern especially pronounced between 0.5 h and 1.0 h. Within this interval, the curve shows high increments and a steep slope. The aluminum extraction rate increases rapidly from 57% to 79% at a calcination temperature of 880 °C and a material ratio of 1:0.7. This indicates that increasing the calcination time significantly promotes aluminum extraction, with a substantial increase in extraction rate. The data align with a first-order reaction kinetics model, suggesting that the reaction rate is dominated by interfacial chemical reactions. The solid-solid reaction between sodium carbonate and mullite rapidly forms nepheline. With the augmentation of calcination time up to 1.2 h, the curve maintains an upward trend (Plateau stage), yet the gradient is less steep than in the 0.5 h to 1.0 h range; this process conforms to the Ginstling–Brounshtein diffusion model, indicating that the reaction becomes limited by the diffusion rate of Al
3+/Na
+ through the product layer; Upon reaching a calcination time of 1.5 h, the extraction yield essentially attains its maximum value, observable in the figure by a markedly diminished increment in the curve and an approximate leveling of the slope. Based on the above discussion and considering extraction efficiency, energy consumption, and environmental impact, 1.5 h was chosen as the optimal calcination time. Experimental data shows that at 1 h, the aluminum leaching rate peaks at 83% (at 880 °C). At 1.5 h, it marginally increases to 89%. However, the latter ensures complete mullite–to–nepheline conversion (XRD residual peak intensity < 1%), preventing unreacted cores from interfering with subsequent acid leaching. Additionally, a longer calcination time reduces acid–leaching effluent and by–products (e.g., silica gel), enhancing net environmental benefits. Thus, 1.5 h achieves the best balance among extraction rate, cost, and sustainability.
Figure 6 presents a comparison of scanning electron microscope (SEM) images of pristine fly ash and those under specific calcination activation conditions. As shown in
Figure 6a, the microparticles of pristine fly ash predominantly exhibit spherical, elliptical, and irregular cubic shapes with surfaces that are approximately smooth.
Figure 6b, in contrast, displays the SEM image obtained under experimental conditions of a calcination temperature of 880 °C, a material ratio of 1:0.7, and a calcination time of 1.5 h. Compared to
Figure 6a, the calcined fly ash particles exhibit a marked increase in porosity, a more fluffy surface structure, and a significant transformation in crystal structure. These observations suggest that during the calcination activation process, the aluminate octahedral crystal structure in fly ash underwent the cleavage of Al-O bonds, subsequently transforming into an silicon (aluminum) oxygen tetrahedron crystal structure (as depicted in
Figure 7). The structural transition from octahedral to tetrahedral coordination in aluminates induces the formation of six-membered rings (
Figure 8), where interconnected AlO
4 and SiO
4 tetrahedra construct [Si
4O
10]
4− rectangular units, significantly enhancing acid susceptibility. In the octahedral configurations, aluminum ions are surrounded by six oxygen atoms, forming a stable coordination environment. This structure is relatively dense and resistant to acid attack. In the tetrahedral structure, aluminum ions are surrounded by four oxygen atoms, reducing the coordination number and stability. This transformation enhances the chemical reactivity of aluminum salts in acidic environments, making them more susceptible to acid attack. These ring structures serve as basic units for constructing aluminosilicate materials, such as nepheline (acid-soluble).
3.4. Effect of Hydrochloric Acid Concentration
The concentration of hydrochloric acid is crucial in the acid–leaching process, which directly impacts the leaching kinetics and reaction pathways of aluminum. In the low-concentration range (1–3 mol/L), insufficient H+ concentration leads to inefficient disruption of the Al-O bonds in nepheline (NaAlSiO4). The reaction is controlled by surface chemical reactions, with the reaction rate linearly related to the acid concentration. At medium–high concentrations (4–6 mol/L), the synergistic effects of H+ and Cl− become significant. H+ attacks the nepheline structure to release Al3+, while Cl− promotes aluminum ion dissolution through complexation (forming AlCl4−). Leaching efficiency can reach 80–90%, and the reaction shifts to diffusion control, with the rate limited by ion migration. When the concentration exceeds 6 mol/L (7–8 mol/L), high acidity triggers a surge in side reactions. These include the competitive dissolution of impurity ions like Fe3+ and Ca2+ and the rapid formation of silica gel (SiO2·nH2O). The silica gel encapsulates unreacted particles, creating a diffusion barrier and reducing the aluminum leaching rate to below 85%, and higher concentrations of hydrochloric acid not only have strong volatility but may also lead to overly vigorous reactions, resulting in significant losses of volatile chemicals. This not only increases costs but also has adverse effects on the leaching operation and the environment. Particularly during acid leaching at high concentrations of hydrochloric acid, a substantial amount of aluminum silicate sol is produced, which makes the solid-liquid separation process extremely difficult. However, should the hydrochloric acid’s concentration fall below the optimal level, it can result in insufficient acid leaching reactions, thereby affecting the extraction rate of aluminum.
To determine the optimal hydrochloric acid concentration, a systematic concentration variation experiment was conducted within the range of 1–8 mol/L under precisely controlled thermal conditions (100 °C); the lower limit of 1 mol/L ensures the minimum effective H
+ concentration to initiate the acidolysis of aluminosilicates, avoiding ineffective leaching due to insufficient acid. The upper limit of 8 mol/L balances diminishing returns and operational risks. Beyond 8 mol/L, aluminum–leaching efficiency plateaus occur, while acid consumption and waste liquid treatment costs (e.g., neutralization and recovery) rise. High-concentration acid also significantly accelerates the corrosion rate of reactor materials like titanium alloys. Moreover, this range encompasses the entire kinetics of aluminum leaching: low concentrations (1–3 mol/L) correspond to chemically-controlled reactions, medium concentrations (4–6 mol/L) to diffusion-controlled reactions, and high concentrations (7–8 mol/L) reveal extreme conditions dominated by side reactions (e.g., silica gel formation), providing comprehensive data for process optimization. Other experimental conditions included a material ratio of FA to Na
2CO
3 of 1:0.7, a calcination temperature of 880 °C and a calcination time of 1.5 h (obtained from
Section 3.3); the hydrochloric acid solution was maintained at 100 °C, a solid-liquid ratio at 1:5, and a leaching time at 1 h. Under these established conditions, a series of experiments were executed to explore the influence of varying hydrochloric acid concentrations on the aluminum extraction rate. The findings of these experiments are delineated in
Figure 9.
Based on the trend line in
Figure 9, it has been noted that the rate of aluminum extraction exhibits an upward trend followed by a decline as the concentration of hydrochloric acid escalates. This reveals the nonlinear relationship between acid concentration and aluminum leaching rate, as well as the critical point for by-product formation: (i) The leaching rate peaks at 83–86% in the 4–6 mol/L range, indicating optimal diffusion-controlled conditions where the reaction rate is limited by the diffusion of Al
3+ from the particle surface to the liquid phase. (ii) After the concentration exceeds 6 mol/L, the leaching rate decreases (86% → 82%), signaling by-product formation (silica gel). The accumulation of silica gel is the main cause of the efficiency drop. Therefore, 6 mol/L hydrochloric acid was chosen for subsequent experiments.
3.6. Effect of Leaching Time
The efficacy of the acid-leaching process is predominantly shaped by the extent of the leaching duration. If the leaching time is too short, the acid leaching reaction will not be sufficiently carried out; conversely, if the leaching time is too long, it may lead to a decrease in leaching efficiency. The underlying mechanism involves a dual process: (i) kinetics of leaching regime transition from chemical reaction control to diffusion control, and (ii) cumulative side reactions. This transition can be delineated into two distinct phases: Initial phase: Rapid chemical dissolution dominates, where active aluminum-bearing phases (e.g., NaAlSiO
4, γ-Al
2O
3) react exergonically with HCl, resulting in time-dependent leaching efficiency enhancement (dC/dt > 0.85 min
−1). Terminal phase: Progressive accumulation of reaction byproducts (e.g., residual silicates, neoformed sulfates) generates a diffusion-limiting passivation layer, transitioning the rate-limiting step to solid-state diffusion. Concurrently, prolonged leaching induces competitive dissolution of ancillary minerals (e.g., hematite Fe
2O
3, lime CaO), releasing Fe
3+ and Ca
2+ ions that either (a) compete with Al
3+ for complexation sites or (b) precipitate as colloidal hydroxides (e.g., Fe(OH)
3), thereby reducing aluminum recovery efficiency by 12–18%. Furthermore, selective dissolution occurs during acid treatment, where activated aluminum phases (e.g., nepheline NaAlSiO
4) are preferentially leached, leaving refractory phases (e.g., mullite 3Al
2O
3·2SiO
2, quartz SiO
2) with enhanced structural stability. Based on this mechanistic understanding, a time-dependent leaching profile was established through systematic experiments at 0.5 h intervals across the 0.5–3.0 h range. These trials were conducted under a set of controlled conditions: a precise material ratio of fly ash to sodium carbonate at 1:0.7, calcination at a consistent temperature of 880 °C for a duration of 1.5 h, a hydrochloric acid solution was maintained at 100 °C and had a concentration of 6 mol/L; a solid-liquid ratio optimized to 1:6. The impact of different leaching times on the aluminum extraction rate was investigated, with the results presented in
Figure 11.
As shown in
Figure 11, the extraction rate of aluminum increases with the extension of the acid leaching time, reaching a peak when the leaching time is 2.0 h. However, a continued increase in leaching time results in a decline in the extraction rate, which may be attributed to the re-precipitation of dissolved aluminum due to excessive leaching times, thereby reducing the leaching efficiency. Upon examining the figure, it becomes apparent that a substantial surge in the extraction rate of aluminum is observed. when the leaching time is between 0.5 to 1.0 h and 1.0 to 1.5 h. This indicates that an appropriate leaching time can ensure a complete reaction of aluminum in FA, thereby enhancing the leaching rate of aluminum.
Figure 12 illustrates the changes in the surface microstructure of FA after acid leaching, as observed through scanning electron microscopy (SEM). Compared with the SEM image of pristine FA in
Figure 6a, it is evident that after hydrochloric acid treatment, the spherical particles exhibit distinct signs of erosion, with etched pits forming and the surface becoming rough. These alterations indicate that the acid leaching process disrupts the mullite structure within the fly ash, thereby releasing the aluminum elements contained within. The reaction mechanism is as follows: Calcination activation of fly ash under alkaline conditions provided by sodium carbonate leads to the cleavage of Al-O bonds in the aluminate octahedral crystal structure, which are then rearranged to form an aluminate tetrahedral crystal structure. Under the above alkaline pretreatment conditions, the reaction forms soluble aluminate phases. This creates more active sites on the mineral surface, providing additional reaction points for subsequent acid leaching and enhancing the etching efficiency. The pretreatment under alkaline conditions can partially dissolve inert phases on the mineral surface, such as mullite. This increases the mineral’s porosity and specific surface area, allowing acid to infiltrate deeper into the mineral and boosting the etching depth. Under the influence of hydrochloric acid (H
+), it chemically reacts with the aluminosilicate minerals in fly ash. Specifically, hydrochloric acid reacts with the alumina and silicate components in these minerals to form soluble aluminum and silicate salts. This disrupts the original structure of the fly ash, causing its dense glassy surface to be etched and leading to the breakage of Al-O bonds and the release of aluminum ions. As the Al-O bonds cleave, etching pits gradually form on the fly ash surface. These pits increase the specific surface area of the solid particles and expose more active sites, further promoting the reaction between the acid and the minerals and accelerating the dissolution of fly ash and the extraction of aluminum.
In summary, the microstructural changes in fly ash after treatment affect its overall properties and potential applications as follows: (i) The formation of etching pits and an increased specific surface area enhance the chemical reactivity of fly ash, making it more responsive to subsequent chemical treatments and improving the extraction rate of aluminum and other valuable elements. (ii) Microstructural alterations can influence the physical properties of fly ash, such as particle morphology, size, and porosity, which may affect its performance as a filler, adsorbent, or other functional materials. (iii) Microstructural changes can also impact the environmental effects of fly ash. For example, an increased specific surface area and porosity may enhance its adsorption capacity for pollutants, offering potential applications in environmental remediation.
3.7. Reproducibility and Statistical Validation of Alumina Extraction from Fly Ash Using Alkali
To accurately assess the interactions between factors, an orthogonal experimental design is used: (i) The orthogonal table is designed based on six factors affecting aluminum extraction from fly ash: calcination temperature, material ratio, calcination time, hydrochloric acid concentration, solid-liquid ratio, and acid–leaching time. These factors have significant interactions. (ii) The L18 (36) orthogonal array is chosen for quantitative analysis. Range analysis evaluates interaction effects, and significant interactions are further analyzed. (iii) Model validation shows R2 = 0.959, indicating that the six main factors and their potential interactions explain 95.9% of the variation. Columns are assigned to interaction terms in the orthogonal table, and their R and F values are calculated. (iv) Statistical tests verify the significance of Kavg differences using ANOVA and post-hoc tests to confirm significant differences at different levels.
The principle of factor and level selection: (i) Factor selection, six parameters significantly affecting aluminum extraction rate were chosen: calcination temperature (A: 830 °C, 850 °C, 880 °C), material ratio (B: 1:0.7, 1:0.8, 1:0.9), calcination time (C: 1 h, 1.5 h, 2 h), hydrochloric acid concentration (D: 5 mol/L, 6 mol/L, 7 mol/L), solid-liquid ratio (E: 1:6, 1:7, 1:8), acid-leaching temperature (E: Maintain at 100 °C) and acid-leaching time (G: 1.5 h, 2 h, 2.5 h), with effective ranges determined by preliminary experiments; (ii) Level setting, levels cover the operable interval (three levels); for example, the calcination time spans 0.5 h to ensure the experimental design can capture parameter effects; (iii) Orthogonal table matching; the appropriate orthogonal array (L
183
6) was chosen as the control parameter design for quantitative analysis, and repeat experiments were conducted.
Table 2 shows the controlled factors and levels for the (L
183
6) orthogonal array, with the extraction rate as the orthogonal experiment response.
Table 3 uses the Tukey HSD test to compare differences between levels. For instance, the extraction rate at 880 °C calcination temperature is significantly higher than at 830 °C (97% in experiment 13 vs. 83.16% in experiment 1). As indicated by the results in
Table 3, an alumina extraction efficiency of up to 97% can be achieved when the fly ash-to-sodium carbonate mass ratio is 1:0.7, after calcination at 880 °C for 1.5 h, this pretreatment was followed by leaching with 6 mol/L hydrochloric acid at 100 °C under controlled solid-liquid phase conditions (1:6 ratio) for 2 h. Under the aforementioned experimental conditions, the extraction efficiency of alumina can reach 97%.
Analysis of range (range analysis) of orthogonal experimental results is an important method for evaluating the experimental index values at each level of the factors, examining the interactions between factors, determining the significance of different factors on the experimental outcomes, and ultimately identifying the optimal combination of factor levels that maximizes the experimental index.
Table 4 presents the range analysis table, which includes the sum of the experimental index values at the ith level of a factor (K
i), the number of replicates per level (r), the number of levels for a factor (m), the average experimental index at the same level (K
avg), and the optimal level (range) R. R denotes the range value of a factor, which is calculated as the difference between the maximum and minimum values of Kavg for that factor. The range values can be used to compare the relative importance of different factors. It reflects the degree of impact on experimental results when factor levels change. (i) Factors can be ranked by R-value size; those with larger R-values significantly affect results and are main factors, while those with smaller R-values have less impact and are secondary factors. (ii) Numerical-difference analysis quantitatively determines factor importance by reflecting the relative intensity of different factors’ impacts on results. For example, the sum of the experimental index values (K
1) and the corresponding average experimental index (K
avg) at the first level of factor C are calculated in Equations (2) and (3), where L
i represents the response in the ith row of the orthogonal experimental table.
For managing and assessing intra–replicate variability, take factor C as an example: (i) Calculate variability metrics using Formulas (2) and (3) to quantify intra-replicate variability, which usually involves calculating statistical measures like standard deviation or variance to numerically represent data dispersion; (ii) Manage variability by multiple replicates (e.g., repeating experiment 13 three times) to reduce random errors and enhance data stability. Repeating experiments improves estimation and control of variability, making results more representative and reliable; (iii) Discuss the impact on the optimal combination. High variability may mask true effects, making it difficult to accurately identify interactions and main effects between factors in experiments. However, orthogonal experiments can effectively reduce the impact of variability through repeated design (e.g., six repeats per level) and mean calculation, ensuring the reliability of the optimal parameter combination. For instance, in
Table 3, experiment 13 achieves an extraction rate of 97% under the following conditions: a material ratio of 1:0.7, a calcination temperature of 880 °C, a calcination time of 1 h, a solid–liquid ratio of 1:7, a hydrochloric acid concentration of 7 mol/L, an acid-leaching temperature of 100 °C, and an acid–leaching time of 2 h. This indicates that proper experimental design and data processing can overcome the interference of intra-replicate variability in identifying the optimal combination and finding the best experimental conditions.
Based on the range values (
R) of each factor in
Table 4 and the corresponding range chart of average values at different levels (
Figure 13) presenting the results of the multi-factor ANOVA and revealing the significant effects of each factor on the experimental outcomes., the following conclusions can be drawn: The factors are ranked in descending order of importance as follows: calcination temperature, material ratio, calcination time, hydrochloric acid concentration, solid-to-liquid ratio, and leaching time. To demonstrate the relationship between importance and differences, statistical methods were employed to verify the reliability of these differences. Using the extraction amount of aluminum ions as the response variable, a multi-factor ANOVA was conducted with six factors-material ratio, calcination temperature, calcination time, hydrochloric acid concentration, acid leaching time, and solid-to-liquid ratio-as independent variables.
The ANOVA was used to determine whether these factors and their interactions have significant effects on the extraction of aluminum ions. The results of the sum of squares, mean squares (MS), degrees of freedom (df), F-values, and
p-values for each factor are presented in
Table 5. These F-values were compared with the critical F-values at the given significance level (
p = 0.05).
If the F-value of a factor is greater than the critical F-value, it indicates that the factor has a statistically significant effect on the extraction amount of aluminum ions, suggesting that changes in the levels of this factor will significantly affect the extraction efficiency of aluminum ions. For example, the F-critical value (α = 0.05, numerator degrees of freedom 2, denominator degrees of freedom 4) is 6.94. The F-values and p-values are as follows: calcination temperature F = 48.737 (p = 0.001), material ratio F = 34.150 (p = 0.012), calcination time F = 26.963 (p = 0.016), hydrochloric acid concentration F = 22.187 (p = 0.019), solid–liquid ratio F = 13.66 (p = 0.031), and acid–leaching time F = 9.35 (p = 0.043). All passed the significance test (p < 0.05), and the F–values of the six factors are greater than 6.94, indicating significant effects.
As shown in
Table 5, a multi-factor ANOVA was conducted to investigate the differences in outcomes associated with six factors: calcination temperature, material ratio, calcination time, hydrochloric acid concentration, solid-to-liquid ratio, and leaching time. The model R-squared value was 0.959, indicating that these six controlled factors collectively explained 95.92% of the variation in the results. The analysis revealed that all six factors significantly affected the results (
p < 0.05). Among them, calcination temperature had the most pronounced effect (
p = 0.001), while leaching time also had an impact but with a less significant difference compared to the other factors.