Abstract
The present study focuses on the processing of a poly-mineralized concentrate attained from a physical beneficiation of process applied to high grade pegmatitic rock sample of Gabal El- Aurf area. The concentrate contains significant amounts of niobium (Nb), tantalum (Ta), titanium (Ti) and rare earth elements (REE) plus yttrium (Y) assaying 19.5, 2.5, 14.2 and 21.2%, respectively. The economic minerals within the concentrate include euxenite, tant-euxenite, samrsakite, allanite, and anatase.
The processing procedures involve an alkaline potassium hydroxide fusion applied to the poly- concentrate. This is followed by water leaching to extract dissolved Nb and Ta as water-soluble potassium niobate and tantalate. The remaining hydrous cake undergoes leaching process using 1.2M oxalic acid for selective extraction of titanium as soluble potassium-oxalatotitanat. The residue obtained after oxalic acid leaching is then utilized for the recovery of insoluble REE- oxalate. Subsequently, yttrium is individually separated from a nitrate solution using 2M tri-butyl phosphate (TBP) at pH 1.5. The final proposed technical flowsheet outlines the recovery of pure oxides of Nb–Ta, Ti, and Y.
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1 Introduction
Gabal (G.) El-Aurf area in the Central Eastern Desert of Egypt is characterized by pegmatitic bodies containing rare metals and radioactive minerals. Positioned between latitudes 26°37 and 26°45S and longitudes 33°20 and 33°26W, the area is geologically classified into South and North pegmatitic bodies [1]. The younger granite of South G. El-Aurf forms a rugged mountain extending about 14 km in the southwest direction, with a triangulation point at 989m above sea level.
The pegmatitic rocks that intrude the monzogranites of G. El-Aurf exhibit poly-phased mineralization, including minerals such as tant-euxenite, euxenite, monazite, bastnasite, anatase, and zircon [2]. These minerals host various rare metals, predominantly REE, Nb, Ta, Ti, and Zr. Two phases of mineralization have been identified: an earlier phase characterized by colorful mineralization with the presence of radioactive minerals like thorite, xenotime, and zircon, and a latter phase characterized by additional accessory minerals (fluorapatite, cassiterite, atacamite, sulfides, and Nb minerals), alongside REE-bearing minerals like pyrochlore and bastnasite, as well as iron oxides minerals [1, 3,4,5].
Given the significant importance of Nb, Ta, Ti, and REE in modern electronics and nuclear industries, a physical beneficiation process is crucial for extracting these metals from their natural resources [6]. The objectives of physical beneficiation include increasing the metal grade of ore, reducing the amount of associated gangue minerals (quartz, feldspar, hematite, and goethite), lowering leaching plant costs, and enhancing productivity. The beneficiation process typically involves a combination of unit operations such as gravity concentration, magnetic separation, and froth flotation [7,8,9,10,11].
In general, hydrometallurgical processing of Nb–Ta minerals involves acidic and/or alkaline leaching, followed by solvent extraction techniques [12]. The leaching process often employs concentrated acidic solutions, such as HCl/HNO3/H2SO4/H3PO4/HCl + HNO3, due to the lower solubility of Nb–Ta minerals under mild aqueous conditions [13, 14]. Single HF or a mixture of HF and HNO3/H2SO4 solutions is also effective in dissolving these minerals [15,16,17]. Alternatively, leaching agents like NH4.HF2, NaF, and KF can be used, although fluoride leaching systems may face challenges like HF loss through volatilization and wastewater contamination, necessitating treatment [9, 18, 19].
To address these challenges, alternative approaches such as alkaline fusion, roasting followed by water leaching, or a mixture of mineral acid solutions have been employed for the leaching of Ta and Nb from their minerals [20,21,22,23,24,25,26]. In the context of titanium leaching, sulfuric acid or hydrochloric acid is commonly employed for extracting titanium from minerals like ilmenite and rutile under optimal leaching conditions, as outlined in studies by Xiong et al.; Haverkamp et al.; Li et al.; Zhao et al.; Nguyen and Lee & Ahn and Lee [12, 27,28,29,30,31]. Organic acids, such as oxalic acid and citric acid, have shown superior leaching efficiencies for extracting metals from inert minerals when compared to mineral acids. The chelation of metal ions by organic ligands contributes to this improved efficiency, as noted by Panda et al.; Miao et al.; & Li et al., [32,33,34]. Notably, the decomposition of Ti using concentrated KOH followed by organic acids, particularly citric acid and oxalic acid, has been reported to enhance the leaching efficiencies of titanium from potassium titanate roasted material [35,36,37,38].
Oxalic acid is distinguished as a more effective leaching agent relative to other organic acids like citric, malonic, and acetic acids. This distinction is based on oxalic acid's unique characteristics, which encompass a higher level of acidity, superior complexing capabilities, and enhanced reduction potential [39, 40]. Studies by Jonglertjunya et al. [41] on the dissolution of ilmenite by oxalic acid reported that 86.4% of Ti was leached under conditions of 4M oxalic acid concentration, 1/20 solid/liquid ratio, and a temperature of 90˚C. In contrast, using the same conditions with 4M sulfuric acid resulted in only 16.1% dissolution of Ti. Also, Nayl and Aly [42] reported on the solubility of Ti and Fe in potassium hydroxide-treated ilmenite using eighty percent oxalic acid. Their findings indicated that the dissolution of titanium (93%) remained unchanged after 180 min., while that of iron (73%) had increased slightly. The extreme dissolution of Ti and Fe was observed with 80% oxalic acid within the studied acid concentration between 20 and 80%. The influence of temperature on the dissolution of ilmenite in oxalic acid was also investigated, revealing a decrease in the percentage of Ti extracted at temperatures higher than 150 °C as result of the hydrolysis of Ti, while the recovery of iron improved with rising temperature.
The significant demand for purified Y compounds in industrial development has led to increased market demand. Solvent extraction (SX) emerges as a widely used commercial technology for Y separation due to its ease of use, scalability, and the ability to achieve high purity in the final product [43]. Various solvents have been employed for the individual separation of Y from other rare earth elements, including Primene JM-T (ω-trimethylalkylamine), di(2-ethylhexyl)phosphoric acid (D2EHPA), and Tri-butyl phosphate (TBP) [44,45,46]. Additionally, Cyanex has been utilized for separating Y from light lanthanides [47]. Tri-butyl phosphate has been successfully developed for preparing pure Y2O3 from a nitrate solution, as documented in studies by Jorjani and Shahbazi; Li; and Khalil et al. [48,49,50]
2 Experimental Work
In the investigation of G. El-Aurf area, the raw sample underwent a comprehensive characterization involving mineralogical and chemical specifications, as well as physical beneficiation processes. Subsequent chemical processing steps were applied to the obtained concentrate to recover Nb–Ta oxide, TiO2, and achieve individual separation of Y2O3 from the prepared REE-cake.
2.1 Chemical Characterization
Chemical analyses, encompassing major oxides of both the raw host rock and the concentrated sample, were conducted using Axios advanced WDXRF-PANalytical (Netherlands). The chemical determination of Nb, Ta, and Ti was carried out using the Microwave Plasma Atomic Emission Spectrometer (4200 MP-AES, Agilent Technologies) throughout the entire workflow. Quantitative analysis of REE was performed by UV spectroscopy using Arsenazo III, with Y serving as a reference [51]. The scanning electron microscope (ESEM) equipped with an EDAX microanalysis unit played a crucial role in identifying the final Nb, and REE products, along with some selected mineral grains. Also, Inductively Coupled Plasma (Prism ICP) High Dispersion (Teledyne Leeman Labs. USA) was used for chemical analysis of the final products.
2.2 Mineralogical Characterization
The mineralogical composition of the representative G. El-Aurf rock sample was investigated by initially grinding and sieving it into the grain size range of 1 to + 0.063 mm. Subsequently, the light and heavy fractions were separated using bromoform (sp. gr. 2.84 gm/cm3). Heavy mineral particles were meticulously picked under a binocular microscope, and selected mineral grains were identified using the X-ray diffraction technique (XRD). A PHILIPS X-ray generator model PW1140/90 fitted with a diffractometer model PW1050/80 was employed. The X-ray tube used was a Cu-target model PW2233/30 fitted with a Ni-filter, operating at 40 kV and 20mA.
2.3 Physical Beneficiation Procedure
A five kg bulk sample from G. El-Aurf raw pegmatitic material underwent a physical upgrading process to concentrate economic minerals and separate them from the gangue one. Initially, the raw material was deslimed to generate a heavy minerals concentrate. The deslimed portion was subsequently segregated using screens with mesh sizes ranging from –1 to + 0.063 mm, a range optimal for gravity-based separation techniques. A laboratory-grade wet Wilfley shaking table (No.13, Germany) was utilized under defined operational parameters: a feed rate of 5 kg/h, water flow of 4 L/min, a stroke length of 10 mm, and a table inclination set at 8 degrees. Following this, the Carpco high-intensity lift-type magnetic separator Model MLH (13) III-5 (USA) was employed to perform magnetic separation. This process successfully separated Nb, Ti, and REE minerals as a magnetic fraction at a current setting of 3A, distinctly apart from the lighter silicate gangue minerals.
2.4 Chemical Processing Procedures
Two sequential leaching processes were conducted on the poly-mineralized concentrate sample. The first involved KOH fusion to break down the refractory structure of Nb-Ti and REE minerals, bringing Nb–Ta metal values into a solution. This was followed by atmospheric agitation leaching using oxalic acid to dissolve Ti, leaving the REE as an insoluble oxalate cake. Subsequently, individual separation of yttrium from a nitrate solution was achieved using TBP in kerosene under optimum extraction and stripping conditions.
2.4.1 KOH Fusion of Poly-mineralized Concentrate
A series of experiments were executed, involving the combination of a fixed mass of 5g of finely pulverized concentrate sample (S) with solid KOH (which has a melting point of 360°C) as the fusion reagent (R) in varying proportions (from a 1/1 to a 1/2.5 ratio). This mixture was then subjected to fusion at temperatures ranging from 400 to 600 °C for different time spans (1–2.5 h). Upon cooling, the resultant fused cake (C) was subjected to washing and leaching processes using distilled water at various water to cake (W/C) ratio of 1/10, Leaching time 30 min. The leaching temperature (35–90°C) of the fused cake was also studied to achieve maximum leaching efficiencies of Nb and Ta. After filtration and washing, Nb, Ti, and REE in the prepared alkaline solution were analyzed, and their leaching efficiencies (%) were calculated using the equation:
The working alkaline leach liquor, essential for Nb and Ta recovery, was prepared by mixing 100g of the working concentrate with KOH under optimum leaching conditions. After filtration and washing with distilled H2O, the alkaline leach liquor was directed towards Nb–Ta recovery via hydrolysis process.
2.4.2 Atmospheric Oxalic Acid Agitation Leaching of Spent Residue
The spent residue, containing both Ti and REE along with a small amount of Nb, underwent leaching using an oxalic acid solution. The objective was the selective separation of Ti and Fe from REE, considering various leaching conditions such as oxalic acid concentration (%), solid/liquid (S/L) ratio, leaching time (hour), and leaching temperature (oC). Subsequently, the insoluble REE-oxalate cake, after dissolving Ti, Fe and the remaining Nb, was further processed for individual yttrium separation.
2.4.3 Individual Separation of Yttrium
The insoluble REE-oxalate cake, post dissolution of Ti, Fe, and the remaining Nb, was employed for the individual separation of yttrium, a predominant element in the cake. To enhance purification, the obtained REE-oxalate, which contained impurities of Mg, Na, and K, underwent dissolution in 10M HCl. Subsequent re-precipitation using NH4OH at pH 8.5 resulted pure RE(OH)3. The latter was then re-dissolved in a 6M HNO3 acid solution and directed to a solvent extraction circuit for selective Y extraction. TBP in kerosene, in the presence of a 0.5M ethylenediaminetetraacetic acid (EDTA) solution as a complexing agent, was utilized for this purpose.
3 Results and Discussion
3.1 Mineralogical Characteristics
A crucial objective of this study is to highlight the metallogenic features of the rare metal-bearing pegmatites in G. El-Aurf area. To achieve this, a representative sample, enriched in rare metals like Nb, Ta, Ti, and REE, was selected from extensive sections of the pegmatitic bodies. Mineral grains, representing 3.2% of the heavy fractions, were subjected to XRD and EXD analyses to identify the mineralization.
The data revealed that the principal minerals belong to the Euxenite–Polycrase series. This series is characterized by multiple replacement sites and the presence of Ti, whose content relative to Nb and Ta determines the mineral name. Notably, in euxenite, Nb and Ta are enriched relative to Ti, while in polycrase, Ti is more enriched than Nb and Ta. The identified minerals include:
Euxenite: (Y, Ce, Ca)(Nb, Ta, Ti)2(O)6: widespread niobates resembling columbite-(Fe) and pyrochlore. It exhibits colors ranging from black to greenish or brownish, Fig. 1.
Tant-euxenite: (Y, Ce, Ca)(Ta, Nb, Ti)2(O)6: Named for its similarity to euxenite-(Y) with a higher Ta2O5 content than Nb2O5. Found in granite pegmatites, it appears brownish-black and is associated with anatase (TiO2), hematite (Fe2O3), and quartz (SiO2), Fig. 2.
Samarskite: (Y, Ce, Fe+3)3(Nb, Ta, Ti)5 O16: Dark pitchy to velvety black or dark brown, with irregular massive grains and sub-conchoidal fracture (Fig. 3).
Allanite: Typically black but can be brown or brown-violet. Coated with a yellow–brown alteration product, it comprises various minerals within the allanite group (allanite-(Ce), allanite-(La), allanite-(Nd), and allanite-(Y)), Fig. 4.
This comprehensive mineralogical study of G. El-Aurf raw sample unveiled significant Nb, Ta, Ti, REE, and Zr-bearing minerals alongside gangue minerals like quartz and feldspar. The latter constitutes the main mineral component, emphasizing the need for physical beneficiation before proceeding to recovery processes.
3.2 Gravity Concentration and Magnetic Separation
Depending on the substantial variance in specific gravities of heavy minerals (Sp.gr. 3.9–5.9) in contrast with the associated gangue minerals (primarily quartz and feldspar with Sp. gr. ≈ 2.6), the technique of gravity concentration via a shaking table was harnessed as an effective strategy for the primary separation and concentration of valuable minerals. A 5 kg bulk raw specimen was partitioned into various size fractions (ranging from – 1 to + 0.063 mm), and the Wilfley Shaking Table No. 13 was deployed to procure a preliminary mineral concentrate.
The data in Table 1 revealed variations in specific gravities between heavy minerals and associated gangue minerals. The distribution of heavy minerals among fraction sizes suggested that the crushing operation effectively saved the majority of heavy minerals (86.3%) in fraction sizes ( – 1 mm to + 0.063 mm). Approximately 86% of the heavy mineral content accumulated in about 86% of the total weight of the original sample.
The obtained pure concentrate was primarily composed of euxenite, tant-euxenite, samarskite, and anatase associated with zircon. The evident variations in magnetic susceptibilities between Nb-Ti REE minerals and zircon and remains silicate minerals formed the basis for their final magnetic separation. A magnetite-free feed was prepared and subjected to magnetic separation using a high-intensity lift-type magnetic separator (Carpco Model MLH (13) III-5). The data illustrated that the ultimate non-magnetic concentrate at 3 amps mainly contained zircon and silicate minerals, while the magnetic concentrate contained tant-euxenite, euxenite, samarskite, and anatase, ready for recovery processes.
3.3 Chemical Composition of the Study Sample
Both the bulk raw sample and the working concentrate of G. El-Aurf underwent chemical analysis for their major and trace element composition (Table 2).The results clearly indicate that the raw material contains economic rare metals such as Nb, Ta, Ti, and REE, alongside Zr. Additionally, it contains well-known gangue minerals, namely quartz and feldspar, evidenced by high SiO2 (76.9%) and Al2O3 (9.7%) content, together with K2O (3.53%). These findings underscore the importance of applying a physical beneficiation process before chemical treatment to recover the metals of interest. It is noteworthy that after applying the beneficiation process, Nb, Ta, Ti, and (REE + Y) increased from 0.52, 0.04, 0.27, and 0.3% to 19.5, 2.5, 14.2, and 21.2%, respectively. Conversely, SiO2 content decreased to 4.5% from the original 76.9%, while Al2O3 and K2O decreased to 0.9 and 0.3% from the original 9.7 and 3.53%, respectively.
3.4 Results of KOH Atmospheric Fusion Processes
The mineralogical composition of the working concentrate necessitated the application of alkaline KOH breakdown for the selective leaching of Nb and Ta, separating them from Ti and REE contents. In this process, Nb and Ta were transformed into water-soluble K-niobates and tantalates, while Ti and REE formed an insoluble potassium-hydrous cake. The expected chemical reactions are summarized as follows [20, 52]:
The relevant factors affecting the leaching efficiencies of the metals of interest were studied as follows:
3.4.1 Effect of Concentrate Sample/KOH Weight Ratio
The effect of varying the weight ratio of concentrate sample to KOH was meticulously analyzed, spanning a range from 1/1 to 1/2.5, while maintaining a consistent set of fusion conditions: a fusion duration of 2 h and a temperature setting of 450°C. Post-fusion, the solidified matrix underwent leaching with distilled water at ambient temperature for a duration of 30 min, adhering to a water to cake (W/C) ratio of 1/10. The findings, depicted in (Fig. 5A), revealed a notable enhancement in the Nb and Ta leaching efficiencies, which escalated from 30.6 and 21.3% to 79.9 and 66.7%, respectively as the weight ratio of concentrate sample to KOH (S/R) was adjusted from 1/1 down to 1/1.75. Nonetheless, a further diminution of the weight ratio beyond 1/1.75 resulted in a marginal increase in Nb and Ta leaching efficiencies. This marginal enhancement may be ascribed to the consumption of KOH for the leaching of interfering metal ions like Si, as discussed by [20].
In contrast, the leaching efficiencies of other economic metal values, namely Ti and REE, remained low, recording values of 1.5 and 3.6%, respectively, at the S/R ratio of 1/1.75.
3.4.2 Effect of Fusion Temperature
The data summarized in Fig. 5B highlighted that the maximum Nb (87.4%) and Ta (78.5%) leaching efficiencies were achieved at 550°C, with an S/R weight ratio of 1/1.75 and a fusion time of 2 h, under fixed leaching conditions (W/C 1/10, 30 min leaching time at room temperature). However, a further increase in fusion temperature up to 600°C resulted in decreased Nb and Ta leaching efficiencies. This decline could be attributed to the fact that the reaction between Nb–Ta and KOH occurred more readily at a temperature of 550°C [20, 25].
3.4.3 Effect of Fusion Time
The impact of fusion time was examined in the range of 1 to 3 h, with the other parameters held constant at a fusion temperature of 550ºC and an S/R weight ratio of 1/1.75, along with W/C 1/10, and a 30 min leaching time at room temperature. The data presented in Fig. 5C revealed that the leaching efficiencies of both of Nb and Ta did not exhibit any improvement beyond 2 h of fusion time. Regarding Ti and REE, their leaching efficiencies remained at very limited values across all fusion time intervals.
3.4.4 Effect of Water Leaching Temperature
Different water leaching temperatures (ranging from 35 ± 5 to 90°C) for the fused cake were investigated under optimal fusion conditions: S/R weight ratio of 1/1.75, fusion time of 2 h, fusion temperature of 550°C, W/C of 1/10, and leaching time of 30 min. The results indicated that the maximum Nb and Ta leaching efficiencies were achieved at a leaching temperature of 80°C, reaching 91.1 and 83.5%, respectively (Fig. 5D). Conversely, the leaching efficiencies for Ti and REE were limited, recording values of 1.2 and 3.1%, respectively.
3.4.5 Recovery of Nb and Ta
Accordingly, an alkaline pregnant leach liquor of Nb andTa was then prepared by fusing of 100g of the concentrate sample with a solid KOH at the obtained optimum fusion and leaching conditions. The chemical composition of the pregnant solution (1000mL) of pH value 13.2 was found to assay in g/L: 17.8 Nb, 2.1 Ta, 1.3 Si, 0.45 Y and 0.1 Ti. Almost complete precipitation of Nb associated with Ta was achieved via hydrolysis and acidification of the leach liquor (using nitric acid) to pH 2.5 with continuous stirring for 30 min at room temperature to avoid precipitation of the associated impurities e.g. Si and K which remain soluble in the solution. After filtration, washing, drying and ignition at 650°C, the pure Nb–Ta oxide was then identified using EDX analysis (Fig. 6).
3.5 Results of Oxalic Acid Agitation Leaching of Ti-REEs Hydrous Cake
The hydrous cake, left behind after dissolving almost of Nb (91.1%) and 83.5% of Ta, was subjected to XRF analysis to identify its components (Table 3). It was found that the hydrous cake contains significant amounts of the economic elements Ti and REE, accounting for 14.3 and 21.1%, respectively, in addition to the remaining Nb. The concentration of K was notably high at 32.1%, likely due to the formation of potassium titantate, hydrous K-REE, and potassium niobate.
To selectively dissolve Ti, an oxalic acid solution was chosen, forming water-soluble potassium-oxalatotitanate (IV) K8[TiO(C2O4)2]4 [53] and Fe as iron oxalate Fe(C2O4)33−; Fe(C2O4)22− [54], along with the remaining Nb as niobium oxalates [Nb(C2O4)2]−; [Nb(C2O4)3]3− [55]. The obtained residue after the oxalic acid leaching process was then utilized for the recovery of insoluble REE- oxalate [REE2(C2O4)3]. Various factors affecting the dissolution of metal values, namely Ti, Fe, and Nb, were studied. These factors include oxalic acid concentration, solid/liquid (S/L) ratio, leaching time, and leaching temperature.
3.5.1 Effect of Oxalic Acid Concentration
Different oxalic acid concentrations (ranging from 0.5 to 1.5M) were employed to investigate their impact on the leaching efficiencies of the studied metal values, including Ti, Fe, and Nb, from the potassium hydrous cake. The other leaching conditions were kept constant at room temperature, a leaching time of 1 h, and S/L ratio of 1/5. The results (Fig. 7A) revealed that the leaching efficiencies of all metals of interest increased with the rise in acid concentration, reaching maximum efficiencies of 50.4, 67.9, and 58.4% for Ti, Fe, and Nb, respectively, at 1.2M. Beyond this concentration, a negligible effect on the leaching efficiencies of the metal values was observed.
3.5.2 Effect of Solid/Liquid Ratio
The impact of the S/L ratio was examined at different ratios ranging from 1/5 to 1/12, using a 1.2M oxalic acid concentration at room temperature and stirring for 1 h. The data (Fig. 7B) demonstrated that the leaching efficiencies of Ti, Fe, and Nb increased with an increasing S/L ratio up to 1/10. However, an S/L ratio higher than 1/10 had no significant effect on the leaching efficiencies of all metal values.
3.5.3 Effect of Leaching Time
Various leaching times, ranging from 1 to 3 h, were considered under the conditions of 1.2M oxalic acid, an S/L ratio of 1/10, and room temperature. The corresponding leaching efficiencies (Fig. 7C) indicated that after 1.5 h, efficiencies of 83.9, 86.2, and 84.1% for Ti, Fe, and Nb, respectively, were achieved. Beyond this time, a slight decrease in the leaching efficiencies of Ti and Nb was observed, possibly due to hydrolysis.
3.5.4 Effect of Leaching Temperature
The influence of leaching temperature on the dissolution efficiencies of various metals was studied across a range from ambient temperature to 90°C, while other leaching parameters were held constant: an acid concentration of 1.2 M oxalic acid, a S/L ratio of 1/10, and a leaching duration of 1.5 h. The collated data (Fig. 7D) underscored that a near-complete dissolution of all target metals was achieved at 80°C. Specifically, at this temperature, dissolution rates of 99.6% for Fe, 99.9% for Nb, and 99.1% for Ti were observed.
Conclusively, based on the oxalic acid agitation leaching experiments conducted on the potassium-Ti, Nb, and REE hydrous cake, it is evident that Ti, Fe, and Nb were predominantly dissolved by oxalic acid, forming water-soluble metal ion oxalates. This process left the REE as an insoluble residue. The following conditions were determined to be optimal: a 1.2M concentration of oxalic acid, a 1/10 S/L ratio, a leaching duration of 1.5 h, and a temperature of 80°C.
3.5.5 Recovery of Titanium
To recover both titanium (Ti) and niobium (Nb), the prepared oxalate leach solution (pH 1.8), containing 29 g/L Ti, 1.1 g/L Nb, 5.2 g/L Fe, and 0.05 g/L Ta, underwent direct precipitation through a hydrolysis process at elevated temperature. Nearly complete precipitation of Ti and Nb was achieved by boiling the oxalate solution, followed by addition to boiled distilled water with stirring for 2 h at 120°C. The Ti-Nb hydrated oxide precipitated and was separated from the soluble Fe-oxalate solution by filtration. The obtained precipitate underwent several washes with water, was dried, ignited at 700°C to produce TiO2 pigment, and analyzed using XRD (Fig. 8). The ICP chemical analysis of the final product indicated a TiO2 purity of 97.9% with associated Nb.
3.5.6 Individual Separation of Yttrium
In this procedure, the isolated REE-oxalate cake was retrieved post-filtration, followed by washing and drying at 110°C. It underwent SEM–EDX analysis (Fig. 9A), revealing the presence of trace impurities of K, Mg, and Na within the REE. For enhanced purification, the resultant cake was dissolved in a 10M HCl solution at 85°C and stirred for an hour. Subsequently, re-precipitation was executed using NH4OH at a pH of 8.5, yielding a highly pure RE(OH)3, as depicted in Fig. 9B [56].
Given yttrium’s significant industrial relevance, notably in nuclear energy, metallurgy, ceramics, and luminescence, a dedicated separation process for pure yttrium was initiated. The process commenced with dissolving the REE-hydroxide cake, which assays 53.2% of Y, in a 6M HNO3 solution to liberate the REE content. The resultant nitrate solution, with a Y concentration of 5.45 g/L, was subjected to a selective extraction process utilizing 2MTBP in kerosene. The process was facilitated by 0.5M EDTA, serving as a complexing agent to sequester various impurities. The incorporation of 0.5M EDTA into the aqueous phase significantly bolstered the selectivity of yttrium separation from other REE. Approximately 90% of Y was extracted from the aqueous phase under specific conditions: using 2M TBP, pH 1.5, and with an O/A ratio of 1/1 over a shaking duration of 10 min. Subsequent water scrubbing (1/1) of the loaded solvent was performed to eliminate any co-extracted REE.
Eventually, around 97% of Y was regenerated from the loaded solvent using 3M H2SO4, maintaining an A/O ratio of 2/1 and a shaking time of 20 min. The resultant strip sulfate solution, containing 2.4 g/L of Y, was processed for yttrium precipitation using ammonia solution. This step resulted in the formation of insoluble Y(OH)3 and soluble ammonium sulfate, in accordance with the reaction:
Yttrium precipitation was nearly complete at pH of 8.5, with stirring for 20 min at ambient temperature. The yielded Y precipitate was filtered, rinsed with distilled water, dried, and dehydrated to Y2O3 at 450°C, as verified through XRD analysis (Fig. 10). ICP chemical analysis of the final product indicated a Y purity of 98.4%, with minor impurities comprising 0.9% Dy and 0.6% Er.
4 Conclusion
The processing methodology for the raw material from G. El-Aurf area is a well-structured and comprehensive approach that involves multiple stages of beneficiation and chemical processing to recover various economic minerals. Initially, the identification of minerals such as tant-euxenite, euxenite, samrsakite, allanite, and anatase sets the foundation. Subsequent concentration techniques, including gravity separation and magnetic separation, efficiently concentrate these economic minerals. The application of an alkaline fusion with KOH, followed by water leaching, proves highly effective in selectively leaching niobium and tantalum as water-soluble potassium niobates and tantalates, achieving remarkable efficiencies of 91.1% and 83.5%, respectively. Furthermore, the use of oxalic acid under optimized conditions enables the dissolution of Ti and Fe from the spent residue. The recovery of hydrated titanium oxide through a hydrolysis process yields a final TiO2 product with a purity of 97.9%. Additionally, individual separation of Y from the recovered REE oxalate is accomplished using a solvent extraction process with 2M TBP in kerosene and 0.5M EDTA as a chelating agent. The proposed technical flowsheet outlines a systematic approach for the recovery of pure oxides of Nb–Ta, Ti, and Y, highlighting the efficiency and optimization achieved at each step in the complex processing sequence (Fig. 11).
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Deep appreciation and thankful to Prof. T. E. Amer for providing the working sample, critical reading and revising the manuscript. Also, the author is greatly indebted to Prof. Dr. Hanaa Abu Khozeim and Prof. Dr. Mona Fawzy, for their continuous help in accomplishing this work.
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Abdellah, W.M. Recovery of Niobium, Titanium and Yttrium from Poly-mineralized Concentrate of Gabal El- Aurf Pegmatitic Rocks, Central Eastern Desert, Egypt. Chemistry Africa (2024). https://doi.org/10.1007/s42250-024-01051-9
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DOI: https://doi.org/10.1007/s42250-024-01051-9