Abstract
During the last decades, the growing demand for rare earth elements (REEs) has led to numerous recent studies to recover these elements from various bearing ores and wastes. Therefore, the recovery of REEs from Ras Baroud polymetallic concentrate has been investigated in the current study. Physical beneficiation for the Ras Baroud pegmatite sample was carried out, yielding a concentrate for euxenite (Y), fergusonite (Y), xenotime (Y), monazite (Ce), allanite, thorite, uranothorite, and Hf-zircon, which resulted in raising the concentrations of rare earth elements, Th, Zr, U, and Ti in the sample. Fusion digestion processes with sodium hydroxide were studied using the Conceived Predictive Diagonal (CPD) technique. The three experimental digestion groups proved the dissolution of 99.9, 95.6, 99.9, 52.5, and 0.47% for REEs, Th, U, Ti, and Zr, respectively, under fusion conditions of 723 K, 120 min, 1/1.5 ore/alkali ratio, and − 100-μm particle sizes. Fusion kinetics, isotherms, and thermodynamics were investigated using several suggested models, namely, pseudo reversible first order, uptake general model, and shrinking core model which matched well with the experimental digestion results. Selective recovery of actinide content from REE content of the digested concentrate chloride solutions was accomplished using solvent extraction with di-2-ethyl hexyl phosphoric acid. About 99.9, 99.9, and 4.2% extraction efficiencies for Th, U, and REEs were performed, respectively, using 0.3 mol/L solvent concentration in kerosene as a diluent, 1/2 organic to aqueous ratio, an aqueous pH of 0.2, and 15-min contact time. Thorium and uranium ions were stripped with sulfuric acid solution 2.5 mol/L with 94 and 98% stripping efficiency, respectively. A highly purified REE precipitate was obtained from the raffinate solutions. Zircon mineralization tailings were obtained as a by-product through the alkaline digestion process.
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1 Introduction
Many studies worldwide have revealed the presence of granite-pegmatite-hosted rare-metal mineralizations, including Nb–Ta-REE mineralization as well as Zr-Hf and U-Th mineralization [1,2,3,4,5,6]. Nb–Ta-REE mineralization has been recorded in the pegmatite bodies of Gabal Ras Baroud granite as well as in the granite itself and the surrounding stream sediments [7,8,9,10,11].
Ras Baroud area is considered one of the most promising areas due to the presence of several strategic and economic rare-metal and REE-bearing minerals, is located in the Central Eastern Desert of Egypt, with an area of about 106 km2, extending along Qena-Safaga road between latitudes 26°43′21″ and 26°48′50″ N and longitudes 33°32′50″ and 33°40′08″ E. The exposed granitoid in the area under investigation is classified into two dissimilar rock units, namely, the older granitoid and the younger granites. Ras Baroud pegmatites are hosted by both older and younger granitoid, but they are often concentrated at the contact between the younger and older granites [11]. Previous beneficiation studies were performed on the rare-metal bearing minerals through gravitational concentration followed by a combination of magnetic and electrostatic separation. Froth flotation can also be used as a later or supplemental stage to achieve a cleaner product [12,13,14,15,16,17].
Great efforts have been conducted to recover rare earth elements from uranium and thorium radioactive contents from various ores. The hydrometallurgical recovery processes of the chosen elements are carried out using different techniques, with either an acidic dissolution or an alkaline dissolution. This depends on the ore nature, the element type, and the mineral type. Fusion digestion techniques for REEs and actinides as refractory minerals have been investigated successfully using alkali hydroxides. Alkali hydroxide fluxes proved effective in the digestion process of the desirable elements presented in several ores [18,19,20,21].
Using a very small number of experiments, the inventive technique “Conceived Predictive Diagonal” (CPD) was utilized in the analysis of the experimental results; this methodology resulted in workable and accurate consequences. In contrast to other methods such as the Design of Experiment (DOE) and Taguchi techniques, the CPD technique does not depend on the matrix diagonally dominant techniques or the eigenvalue principle. This technique depended on studying the parameters in a binary manner or by studying two factors simultaneously [22, 23]. By applying the CPD technique, the binary groups of experiments covered the task range skillfully, the response homogeneity was achieved, and all the alkaline digestion process factors were fully represented. The time of the digestion study was saved by employing a few steps, and the other points would not be performed. Using skills in matrices, nonlinear regression modeling, and MATLAB, the kinetics-thermodynamics relation for the alkaline digestion processes for the studied mineralization was investigated [24].
Several methods have been studied to separate rare earth elements from the content of radioactive actinides, which are usually associated together as monazite, euxenite, etc., or found together in separate minerals [25]. Separation of U and Th from REEs by precipitation was one of the most applicable separation methods; direct precipitation of U and Th using precipitating agents was widely investigated, such as sodium hydroxide, lime, hydrogen peroxide, and magnesium oxide [26,27,28,29]. Solvent extraction (SX) was the other most applicable method in the actinide separation from REEs. Acidic organophosphorus extractants, neutral organophosphorus extractants, amide extractants, amine extractants, and carboxylic acid extractants were the famous solvent extractants utilized in the differentiation between radioactive actinides and REEs [30,31,32,33,34,35,36]. Adsorption trials of REEs, Th, or U separately were also studied using inorganic adsorbents, organic adsorbents, and biosorbents [37,38,39].
The main goals of this paper were summarized in studying the optimal physical upgrading processes to attain a concentrate of high REEs, Th, U, Ti, and Zr contents. Secondly, the fusion digestion of the polymetallic concentrate using sodium hydroxide as a fluxing agent was investigated using the CPD technique. The alkaline fusion was oriented in the selective dissolution processes for the REEs, Th, and U contents leaving the Ti and Zr mineralization as a by-product for further treatment later. The optimal fluxing temperature was defined as the point at which desirable element content was selectively recovered with minimum Zr and Ti dissolution. MATLAB mathematical analyses were performed to define the activation energy, kinetics, and thermodynamics of the alkaline digestion process. Thirdly, the removal of actinides Th, and U from the REE content was studied using the solvent extraction technique with di-2-ethyl hexyl phosphoric acid in kerosene as a diluent. The solvent extraction of Th and U with D2EHPA from chloride solutions was controlled to produce raffinate solutions containing the highest REE content and without the actinides. In addition, studying the scalability of the process and environmental impact has been taken into account. Finally, the production of high-purity sediments from REEs oxide was accomplished, which achieved the main aim of this study.
2 Experimental
2.1 Materials, Reagents, and Instrumentations
Ras Baroud polymetallic concentrate resulting from physical beneficiation was used as the starting material for this study. The concentrate was analyzed mineralogically and chemically to determine its desirable elements contents (REEs, Th, U, Ti, and Zr). All chemicals and reagents were used as received without further purification. Double-distilled water (DDW) was used in all experiments in this study. The pHs of the chloride solutions were adopted using HAANA pH meter and adjusted with the concentrated HCl and NaOH solution (50%). The SEM–EDX analysis for Ras Baroud polymetallic concentrate and the outcome products was performed using scanning electron micrograph model JEOL-JSM-5600LV.
Total rare earths were instrumentally analyzed with Arsenazo III indicator at 650 nm using a single beam UV-spectrophotometer model SP-8001, Metretech Inc. Thorium was determined spectrophotometrically with Thoron indicator at 655 nm. Uranium concentration was also determined spectrophotometrically using Arsenazo III at 654 nm. On the other hand, titanium and zirconium concentrations were measured spectrophotometrically using tiron and xylenol orange at 430 and 535 nm, respectively [40].
2.2 Physical Beneficiation Stage
Physical beneficiation of the Ras Baroud pegmatite sample was carried out using a low-intensity magnetic separator (for magnetite separation), a high-intensity magnetic separator (for separating paramagnetic minerals), and a Wilfley shaking table (for rejection of associated gangue silicate minerals). After the polymetallic concentrate was obtained, a complete characterization was performed using SEM–EDX analysis to determine the mineral contents.
2.3 Fluxing Digestion Stage
A series of alkaline digestion experiments were performed on the mineral concentrate using sodium hydroxide as a fluxing agent. The polymetallic concentrate was quartered and grounded to the proper grain size before mixing with the sodium hydroxide flux in a platinum crucible and subjected to variable conditions. To treat professional data with fewer numbers of experiments with fewer numbers of experiments, a Conceived Predictive Diagonal (CPD) technique is suggested for this target. By applying the CPD technique, three groups of experiments were carried out using the binary factor study method. Fusion temperature and fusion time, ore particle size and solid-to-alkali (S/A) ratio, and fusion temperature and solid-to-alkali ratio (three binary groups) were performed under fixed conditions as presented in Table 1. Six experiments were performed in each group, which means eighteen digestion experiments with sodium hydroxide under variable and fixed conditions. In the digestion experiments, changing two variables together was carried out while maintaining the other variables at fixed values for a given set of measurements.
After each experiment, the retained crucible was allowed to cool to ambient temperature and then underwent acid dissolution using a diluted HCl solution (1/1) under 353 K, solid/acid ratio 1/10, and stirring for 30 min. The chloride slurry was filtered, washed, diluted with DDW to the flask mark, and analyzed to identify its constituents. The dissolution efficiencies for REEs, Th, U, Ti, and Zr were determined from Eq. 1:
where ML and Mo were REEs, Th, U, Ti, or Zr leached concentrations (mg/L) and their original concentrations in the solid (mg/g).
2.4 Dissolution Parameter Stage
The optimal digestion conditions were applied on a definite weight of the Ras Baroud polymetallic concentrate. The fused cake was washed several times with hot water to remove all undesirable gangues, namely, the dissolved phosphates, silicates, and excess sodium hydroxide. To optimize the dissolution of the studied metals, the washed cake was dried at 110 for 6 h, and then it was subjected to a series of dissolution experiments using different acids. About 1.0 g of the dried fused cake fractions was mixed with acidic portions of hydrochloric, sulfuric, nitric, and citric acids, each separately. The dissolution processes were performed using an acid concentration of 2 mol/L, solid to the acidic solution of 1/10, dissolution temperature of 253 K, and stirring for 60 min. After each experiment, the slurry was filtered, washed with DDW until it reached a definite volume, and analyzed to identify its constituents, and the dissolution efficiencies of the studied elements were calculated using Eq. 1.
2.5 Solvent Extraction Stage
A chloride feed solution was prepared using optimal fusion digestion and dissolution parameters as follows: 10 g of − 100 μm from the mineral concentrate was fused with 15 g sodium hydroxide in a platinum crucible under 723 K fusion temperature and 120 min fusion time. The fused cake was washed several times with hot water. The washed-wetted cake was spontaneously attacked with a 2 mol/L HCl with a S/A ratio of 1/10 and stirred for 60 min at a 353 K stirring temperature. The filtrated and washed solutions were adjusted with DDW until they reached 1 L. This chloride feed solution was considered the aqueous phase in the further solvent extraction processes.
The D2EHPA dissolved in kerosene was utilized as an organic phase in the subsequent lab extraction experiments. Several parameters which control the separation of actinides from REEs of the chloride feed solutions were studied. D2EHPA concentration, feed solution pH, shaking time, and organic-to-aqueous volume phase ratio were considered the main controlling extraction parameters.
All extraction experiments were performed in a 50-mL beaker at (25 ± 2) °C. The variable and fixed values for each studied parameter are represented in Table 2. After stirring the aqueous organic mixture, the phases were separated using a separating funnel, the aqueous raffinate phase was analyzed to identify the REEs, U, and Th concentrations, and the extraction efficiency was calculated according to the following Eq. 2.
where Co and Ce were the original concentrations for REEs, Th, U, Ti, or Zr (mg/L) in the chloride feed solutions and their concentrations in the raffinate solutions after extraction (mg/L).
The stripping experiments of the loaded D2EHPA solvent were performed in a 50-mL glass beaker using a magnetic stirrer. To optimize the stripping process, several stripping factors were studied namely; the stripping solution type, the stirring time, and the phase ratio (VO/VA). By studying the variable factors under the fixed conditions as presented in Table 2, the mixture was settled down and the aqueous phase was separated using a separating funnel. The stripping efficiencies of the actinides were determined and calculated using Eq. 3.
where CS and CL were the concentrations of REEs, Th, U, Ti, or Zr (mg/L) in the stripping solutions after the stripping process and their original loaded concentrations on the solvent before extraction (mg/L).
2.6 Actinide Sediment Preparation
The stripping solutions containing the Th and U contents were subjected to complete precipitation of their actinide content. The pH of the stripping solutions was augmented to 2.2 using NaOH solution (50%), small portions of hydrogen peroxide (50%) were added, and the final pH was 2.0 [41, 42]. By allowing the slurry to sit for 6 h to attain complete precipitation, the produced precipitate was filtered, washed with H2O2 solution (2%) of the same pH, dried at 283 K for 6 h, and analyzed using SEM–EDX to identify the actinidepurity.
2.7 Rare Earth Sediment Preparation
The raffinate solutions, after removal of actinide contents using solvent extraction with D2EHPA, were collected and subjected to complete precipitation of the REE content using the oxalic acid method [43]. The raffinate solution pH was adjusted to pH 5 using sodium hydroxide solution (50%) additions, then the oxalic acid solution (10%) was added till the solution pH reached 1.0. The slurry was allowed to complete precipitation, settled, filtered, and washed with an oxalic acid solution (1%). The final sediment was dried, ignited at 1123 K, and analyzed using SEM–EDX to identify its constituents.
3 Results and Discussion
3.1 Mineralogical Investigation for Ras Baroud Polymetallic Concentrate
The pegmatite of the Ras Baroud area was previously discussed (Fawzy et al. 2020). The detailed mineralogical investigations of the studied samples revealed that the content of the light gangue silicate minerals (sp. gr. < 2.85) was 91.9% mass of the studied sample and represented as quartz and feldspar. On the other side, heavy minerals represent 7.9% mass which includes the existence of several economic and strategic minerals; Nb–Ta oxide minerals (euxenite (Y) and fergusonite (Y), REE minerals (xenotime (Y), monazite (Ce), allanite (Ce)), and thorium minerals (thorite and uranothorite). Thus, in addition to zircon and iron oxide minerals, muscovite represents about 5.3% mass (Figs. 1 and 2; Table 3).
The polymetallic concentrate was obtained from Ras Baroud pegmatite sample via successive physical beneficiation techniques that began with the comminution process, through crushing and grinding to prepare a feed material of about less than 1 mm, and then the comminuted raw material was subjected to a low-intensity magnetic separator for magnetite separation, followed by a separation of the paramagnetic minerals using a Carpco high-intensity magnetic separator. The non-magnetic fraction was used as a feed for the wet-gravity concentration process using the Wilfley shaking table (No. 13) to obtain a concentrate of zircon and reject the light gangue silicate minerals (quartz and feldspar).
The magnetic separation processes resulted in obtaining three products, which are as follows:
-
Magnetite concentrate
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Paramagnetic mineral concentrate, which was obtained as a result of separating at 3 amperes magnetic field. This concentrate includes euxenite (Y), fergusonite (Y), xenotime (Y), monazite (Ce), allanite (Ce), thorite, uranothorite, iron oxides, and muscovite
-
Quartz, feldspar, and zircon were obtained as a non-magnetic fraction at a magnetic field current of 3 amperes
To attain a clean zircon concentrate, the non-magnetic fractions were fed to the Wilfley shaking table. The obtained heavy fractions were mainly composed of zircon as well as fewer amounts of thorite, while the gangue light silicate minerals (quartz and feldspar) were discarded. Finally, a paramagnetic mineral concentrate with recovery efficiencies of 86.2, 96.6, and 91.2% for REEs, Th, and U elements, respectively, was obtained from the original sample as shown in Fig. 3.
Considerable contents of REEs, Th, U, Ti, and Zr were detected in the paramagnetic polymetallic concentrate using the EDX analysis as presented in Fig. 4. The illustrated SEM–EDX charts proved the presence of valuable minerals. These minerals were Monazite (Ce,La,Th)PO4, Xenotime (Y) (Y(PO4)) Thorite (Th,U)SiO4, Uranothorite (Th,U)SiO4, Allanite (Ce) ((CaCe)(Al2Fe2+)(Si2O7)(SiO4)O(OH)) euxenite (Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6, and Zircon Zr(SiO4). Most of these minerals were refractory minerals and reflected the refractory nature of these polymetallic concentrates. So, aggressive opening conditions were needed to digest the concentrate and liberate the desirable elements from their crystal lattice.
3.2 Fusion Digestion Results
Three experimental groups were investigated using the CPD technique to study the dissolution behavior of REEs, Th, U, Ti, or Zr elements with alkaline digestion using sodium hydroxide as a flux. The essential target was to maximize the dissolution of REEs, U, and Th from their barren minerals (xenotime, monazite and allanite, thorite, and uranothorite minerals) while minimizing the dissolution of Zr and Ti contents (zircon and titanite). Eighteen fusion experiments were performed by varying the temperature versus fusion time, ore particle size versus solid-to-alkali (S/A) ratio, and fusion temperature versus solid to alkali ratio. The three binary groups and six experiments for each group were performed under certain fixed conditions as shown in Table 1.
From the dissolution results for REEs, Th, U, Ti, and Zr illustrated in Fig. 5, the following were noticed:
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From group 1 experiments, maximum dissolution for REEs, Th, and U was carried out using dissolution temperatures ranging from 673 to 723 K and dissolution times ranging from 105 to 120 min under a solid ore/alkali ratio of 1/1.5 and solid ore particle size of − 100 μm.
-
From group 2 experiments, the solid ore/alkali ratio ranged from 1/1.5 and 1/2.25 with a solid ore particle size of − 74 μm could achieve maximum dissolution for desirable elements.
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From group 3 experiments, by varying the temperature and solid ore/alkali ratio together under fixing the time and the ore particle size (120 min, − 74 μm), from 623 to 723 K dissolution temperature with solid ore/alkali ratio ranging from 1/1.75 to 1/2.25 would achieve the maximum dissolution efficiencies for REEs, Th, and U.
-
Using the maximum dissolution parameters of REEs, Th, and U elements, dissolution efficiency for Ti ranged from 40 to 60%. This may be attributed to the easy dissolution of allanite minerals with the difficult dissolution of titanite which contains the remaining Ti content under these conditions [43]. The dissolution results were paired with a minimum dissolution for Zr content under these moderate alkaline fusion digestions. Zircon and titanite minerals needed aggressive fusion digestion conditions with fusion temperatures over 923 K [23].
-
From the results of the three groups, a significant increase in the digestion of the REEs, Th, U, Ti, and Zr elements was observed by studying the time versus temperature and S/A ratios versus the temperature, while by studying the S/A ratios versus the particle size, the change percentages in the REEs, Th, U, Ti, and Zr digestion were relatively small. So, the digestion parameters could be arranged according to their effect on the dissolution process as follows: digestion temperature > digestion time > S/A ratios > particle size.
3.3 Digestion Kinetics Results
A suggested model was utilized to explain the digestion chemical reactions of the mineral concentrate using sodium hydroxide as a fusing agent. The model namely shrinking core model was previously proved using mathematical treatments [23].
Shrinking Core Model Equation (Eq. 4)
where the terms r and R represent the solid-to-alkali (S/A) ratios and the molar gas constant. The terms Xf, kD, and kC represent the resistances to the fractional conversion external mass transfer, product layer diffusion, and chemical reaction, respectively.
By applying the suggested model equation to the results obtained from the three digestion groups, the resulting kinetic parameters for the digestion processes of REEs, Th, U, Ti, and Zr elements were graphed using the MATLAB program in three-dimensional 3D curves, as shown in Figs. 6 and 7. The R2, Xf, kD, and kC values for the digestion processes using NaOH were illustrated in Table 4.
The shrinking core model assumes the particles are uniform non-porous grains. Initially, the reaction occurs on the grain surface, and then the reaction zone moves into the solid leaving a product layer behind. The total radius of the particle remains constant, while the radius of the unreacted core and the layer of products vary over time as a function of conversion. The approximate solution of the shrinking core model applied in this work was a combination of the resistances that can simultaneously occur in a particle under reaction: alkali diffusion in the layer surrounding the particle, alkali diffusion through the product layer around the unreacted core, and chemical reaction on the unreacted core surface. Introducing Arrhenius relation in the graphical simulation that relates the conversion as a function of solid ore to alkali ratio for a spherical particle is given by Eq. 5.
From the experimental results graphed in Figs. 6 and 7 and illustrated in Table 4, the shrinking core results using group 1 and 3 experiments indicated that the interaction between the alkali and the ore was carried out through a mix of solid diffusion and chemical control. On the other side, from group 2 results for the digestion processes of REEs, Th, U, Ti, and Zr elements, which have the minimum value for KD (kD < kC < Xf), the interaction between the alkali and the ore was performed through a solid diffusion control.
3.4 Digestion Thermodynamics Results
By applying the fusion digestion results obtained from group 3 using the CPD technique, a binary study between varied temperatures and solid ore to alkali ratios was performed to determine the thermodynamics of REEs, Th, U, Ti, and Zr. Temperatures from 473 to 723 K and ratios from 1/1 to 1/2.25 S/A were performed under fixed conditions. The thermodynamic parameters of the digestion process using NaOH were determined using two models’ equations, namely Equilibrium Constant-Van’t Hoff model equation (Eq. 5) and Floatotherm including Van’t Hoff model equation (Eq. 6). The two equations were previously proven [22, 23]. Two types of equations were utilized in the determination of the thermodynamic parameters, the distribution coefficient kd and the uptake qm, respectively.
where qe and qm were the maximum uptake that can be liberated by these matrices (system conditions) and the maximum uptake that ore can give, respectively. Practically, n, m, and g were the powers to be estimated that indicate the effect of their variables at which the highest value indicated the greatest effect on the reaction. Kd (ml/g), ΔH (KJ/mol), ΔS (J/mol·K), t (min), T (Kelvin), and R (KJ/K·mol) were the distribution coefficient, the enthalpy, the entropy, the digestion time, the temperature in Kelvin, and the molar gas constant, respectively. The Gibbs free energy, ΔG (KJ/mol), was calculated from the following equation (Eq. 7).
The two suggested models were represented in 3D using MATLAB as shown in Figs. 8, 9, 10, and 11. The thermodynamic parameters, namely, enthalpy, entropy, Gibbs free energy, and the correlation coefficient for REEs, Th, U, Ti, and Zr using the two models are collected in Table 5. It was indicated from the results of the thermodynamic parameters that the endothermic nature of the digestion processes of REEs, Th, U, Ti, and Zr using sodium hydroxides was proven from the positive value of ΔH. Therefore, all reactions were temperature-dependent. The positive values of ΔS for all digestion reactions were confirmed which indicates an increase in the randomness at the solid/solution interface during the attack of fused alkali on the ore particles. All digestion reactions have a feasible and spontaneous nature due to the negative value of ΔG.
3.5 Solvent Extraction Results
3.5.1 Feed Solution Preparation
By applying the optimal digestion parameters to Ras Baroud polymetallic concentrates and washing the fused cake several times with DDW, several acids, namely, hydrochloric, sulfuric, nitric, and citric acids, were examined to determine the optimal acid that has maximum leaching efficiency for REEs, Th, and U contents. From the obtained data illustrated in Fig. 12, the hydrochloric acid of 2 mol/L has a maximum leaching efficiency for the REEs, Th, and U desirable elements under experimental conditions of solid to the acid solution of 1/10, dissolution temperature of 253 K, and stirring for 60 min. Approximately, all REEs, Th, and U contents were dissolved in the hydrochloric acid solution forming a chloride feed solution which has been used in the subsequent separation stages.
3.5.2 Batch Extraction Results
A series of recovery experiments were performed using varied conditions values, namely, from 0.075 to 0.45 mol/L D2EHPA solvent concentrations, from 0.2 to 0.8 pH of the feed solution, from 1 to 15 min stirring time, and from 1:6 to 2:1 O/A ratios. These variations were performed under fixed conditions as mentioned in Table 2. Kerosene was the preferred choice to be used as diluent which was considered economical and had other advantages during the extraction process as previously mentioned [43]. The chloride feed solutions containing REEs, Th, and U ions were subjected to a solvent extraction stage to separate and remove the radioactive actinide content from the REEs and produce a pure REEs oxide cake from the Ras Baroud polymetallic concentrate.
From the recovery results illustrated in Fig. 13a, the solvent concentration of 0.3 mol/L of D2EHPA dissolved in kerosene as a diluent was the optimal solvent concentration. About 97.5 and 92.6% extraction efficiencies for Th and U were achieved; this was combined with about 4.8% extraction efficiency for REEs which was considered the lowest REE extraction efficiency. By increasing the solvent concentration, the recovery efficiency of REEs was sharply increased with simple enhancements in Th and U cases. So, 0.3 mol/L D2EHPA was considered the best choice to perform the next parameter steps.
A wide range for the chloride feed solution was examined to determine the optimal pH as shown in Fig. 13b. To increase the extraction of Th and U and retain the raffinate-contained REE content after the extraction process, low values of pH (0.2–0.4) were preferred that succeeded in a complete recovery for actinide contents and remaining a raffinate solution contained about 95% of REE content. So, the pH of 0.2 was considered the best feed solution pH to perform the recovery processes.
The reaction time was considered one of the most important factors to study at which the equilibrium time of the chemical reaction could be determined. The stirring time range was studied from 1 to 15 min under fixed conditions, namely, 0.3 mol/L D2EHPA concentration, 0.2 feed solution pH, and 1/2 O/A ratio. From the illustrated Fig. 13c, the optimal stirring time between the chloride solution and the D2EHPA solvent was 15 min at which a complete removal of the actinidecontent from the chloride solution and keeping all REE content in the raffinate solution was achieved. This was considered the solvent extraction main target.
The actinide (Th and U) recovery from the chloride solution using D2EHPA solvent was investigated using various O/A ratios ranging from 1/6 to 2/1. As shown in Fig. 13d, complete removal of actinides was carried out in one contact using O/A ratios of 2/1, 1/1, and 1/2. However, using a high aqueous to solvent of 1/6 O/A ratio resulted in enhancing the actinide uptake and producing a raffinate containing all the REE content with small portions from Th and U which needed further treatments to be removed.
3.5.3 Stripping Results
To back-extract Th and U ions from the D2EHPA loaded organic phase, stripping tests were investigated to determine the confident stripping agent and the other relevant stripping parameters namely acid concentration, stirring time, and A/O ratio. All the stripping processes were performed using a 400-rpm stirring rate and at room temperature (25 ± 2).
To recover the loaded Th and U from the loaded D2EHPA, hydrochloric, nitric, sulfuric, and citric acids were tested as stripping agents for the loaded actinides in the studied solvent. Each acid of 4 mol/L concentration was contacted with the loaded organic phase with an aqueous-to-organic ratio of 2/1 and stirred for 15 min. The plotted figure (Fig. 14a) indicated that sulfuric acid was the optimal stripping acid compared with the other acids. The other studied acids failed in the re-extraction of the Th and U contents from the loaded solvent. So, the subsequent stripping processes were carried out using sulfuric acid as a stripping agent.
Different concentrations of sulfuric acid were tested to determine the optimal acid concentration causing maximum recovery for the actinide contents. From 1 to 5 mol/L, sulfuric acid concentrations as an aqueous phase were studied under fixed conditions of 2/1 A/O ratio and 15 min of stirring. From the results plotted in Fig. 14b, 2.5 mol/L sulfuric acid concentration was the preferable aqueous acid concentration resulting in maximum stripping for both Th and U from the loaded solvent. By increasing the acid concentration over 2.5, sharp decreases in the U stripping efficiencies were detected. So, 2.5 mol/L sulfuric acid was the choice to perform the stripping processes.
The influence of stirring time on the stripping efficiency of actinides was investigated using a 2.5 mol/L sulfuric acid concentration aqueous solution and a 2/1 A/O ratio. Varied stirring times from 1 to 20 min were studied to determine the equilibrium time. Maximum stripping efficiency for both Th and U was achieved after prolonging the stirring time for the stripping process by 20 min. So, as shown in Fig. 14c, the stirring time of 20 min was the optimum stripping time for both Th and U.
The effect of phase ratio was studied using different phase ratios ranging from 1/4 to 3/1 A/O. The fixed conditions were 20 min of stirring time and 2.5 mol/L sulfuric acid concentration aqueous solutions. From the obtained results plotted in Fig. 14d, a sharp increase in the Th and U recovery was carried out using ratios of higher organic than aqueous phase as 1/3 and 1/4 A/O, this was combined with small decreases in the stripping efficiencies of Th and U, and this was attributed to the dilution factor. So, the stripping processes were preferably performed using equivolume from the organic and aqueous phases (A/O of 1/1) at which all the actinides were extracted from the loaded solvent in one stage.
3.6 Rare Earths and Actinide Sediment Preparation Results
A series of recovery experiments were performed to precipitate the REEs, Th, and U contents. Previously, the Th and U contents were separated together using D2EHPA organic solvent from the chloride feed solution of the Ras Baroud mineralization. The actinide contents were successfully re-extracted using sulfuric acid. The precipitation of the Th and U contents was investigated by enhancing the pH to 2.0 using a sodium hydroxide solution of 50%. The prepared precipitate was dried and analyzed to identify its constituents. From the resulting EDX chart plotted in Fig. 15a, a produced cake with significant Th and U contents was attained from the studied mineralization.
On the other side, the raffinate solution after the solvent extraction stage was recycled to recover the REE content. Small portions of 10% oxalic acid were added to the raffinate solution after adjusting its pH to 5 using 50% sodium hydroxide solution; then the oxalic acid solution (10%) was added till the solution pH reached 1.0. After settling and filtration, the filtrated cake was washed with 1% oxalic acid solution several times to remove the undesirable gangues, dried at 383 K for 6 h, ignited at 1123 K, and finally analyzed to identify its constituents. From the resulting EDX chart plotted in Fig. 15b, a finally produced REE cake was obtained with about 90% REE concentrations. There was not any appearance for Th and U in the EDX-chart of the REE cake, which proved the successful recovery of the REEs from the radioactive actinides using D2EHPA solvent. However, more studies on the separation of individual REEs will be conducted in the future as the obtained REE cake deserves further individual processing. As shown in Fig. 16, a proposed flow sheet was drawn to collect all the recovery stages performed in this study.
4 Conclusion
Several strategic and economic rare-metal and REE-bearing minerals were recorded in the Ras Baroud pegmatite sample, and they were as follows: euxenite (Y), fergusonite (Y), yttrocolumbite, xenotime (Y), monazite (Ce), allanite, thorite, uranothorite, titanite, and Hf-zircon. The recovery of these target minerals from the head sample was performed via a low-intensity magnetic separator, followed by a high-intensity magnetic separator, and finally wet-gravity concentration via the Wilfley shaking table. Applying the optimum conditions for both separation techniques, it is possible to attain a good concentrate containing considerable contents of REE, Th, Zr, Ti, and U.
Three experimental digestion groups REEs, Th, U, Ti, and Zr were investigated using the Conceived Predictive Diagonal (CPD) technique, namely, time versus temperature, solid ore to alkali ratio versus ore particle size, and solid ore to alkali ratio versus temperature. Optimal digestion efficiencies of 99.9, 95.6, 99.9, 52.5, and 0.47% for groups REEs, Th, U, Ti, and Zr, respectively, were attained using fusion conditions of 723 K, 120 min, 1/1.5 ore/Alkali ratio, and − 100-μm ore particle size. Fusion kinetics, isotherms, and thermodynamics were investigated using several suggested models namely pseudo reversible first order, uptake general model, and shrinking core model which matched well with the experimental digestion results. The studied models indicated that the digestion reactions for all elements were carried out through a mix of solid diffusion and chemical control.
Total actinide content was separated from the REE content using solvent extraction with di-2-ethyl hexyl phosphoric acid. About 99.9, 99.9, and 4.2% extraction efficiency for Th, U, and REEs were performed, respectively using 0.3 mol/L solvent concentration in kerosene as a diluent, 1/2 organic to aqueous ratio, aqueous pH of 0.2, and 15-min contact time. Thorium and uranium ions were stripped with a sulfuric acid solution of 2.5 mol/L, stirring time of 20 min, and A/O of 1/1 achieving 98.5 and 94.5% stripping efficiencies, respectively.
A highly purified REE precipitate was obtained from the raffinate solutions using an oxalic acid precipitation process. Th/U cake was also attained from the precipitation of stripping solutions. Solid waste from zircon-titanite mineralization has been produced by alkaline digestion.
Data Availability
Data will be made available on request.
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Ahmed A. Eliwa: project administration, methodology, validation, formal analysis, data curation, and writing—original draft. Amal E. Mubark: methodology, formal analysis, validation, data curation, and writing—original draft. Ebrahim A. Gawad: validation, formal analysis, data curation, and writing—original draft. Ahmed H. Orabi: validation, formal analysis, visualization, writing—review and editing, and supervision. Mona M. Fawzy: methodology, validation, writing—review and editing, and project administration.
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Eliwa, A.A., Mubark, A.E., Gawad, E.A. et al. Maximizing the Processing of Polymetallic Concentrates via Actinide Separation and Rare Earth Retrieval. Mining, Metallurgy & Exploration 41, 1379–1400 (2024). https://doi.org/10.1007/s42461-024-00985-5
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DOI: https://doi.org/10.1007/s42461-024-00985-5