Abstract
The development of a recycling process for rare-earth-containing waste is important for improving the resource conservation and resource security of rare-earth metals. Phase equilibria between the molten fluoride and rare-earth oxide were investigated to develop a novel recycling process for neodymium magnets based on the flux-remelting method. LiF—rare-earth fluoride (REF3, RE = Nd, Dy) mixtures and rare-earth oxides (RE2O3, RE = Nd, Dy) were selected, and the phase equilibria in the Nd2O3−NdF3−Li2O−LiF and Dy2O3−DyF3−Li2O−LiF systems were investigated by differential thermal analysis and chemical equilibrating method. It was revealed that compounds NdOF, Nd4O3F6, DyOF, and Dy4O3F6 were stable as an equilibrium phase at 1473 K. In the dissolution of Nd2O3 in molten LiF–NdF3, Nd4O3F6 formed when the mixing ratio exceeds the solubility limit of the melt and the compound coexists with the melt. In the same manner, Dy4O3F6 formed when the mixing ratio exceeds the solubility limit of molten LiF-DyF3 and the compound coexists with the melt. At 1473 K, the solubilities of Nd2O3 in molten LiF—50 mol% NdF3 and Dy2O3 in molten LiF—50 mol% DyF3 were determined as 7.4 mass% and 7.6 mass%, respectively. An enhancement device for the dissolution rate of oxyfluorides is required for practical applications owing to the slow dissolution rate. The recycling process can be used to regenerate neodymium magnet waste by adding a small amount of virgin rare-earth metals.
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Introduction
Rare earths (RE: Sc, Y, La–Lu) are indispensable for high-performance industrial products, including permanent magnets such as neodymium (Nd) magnets [1, 2]. A rare-earth-sintered magnet, Nd−iron (Fe)−boron (B)-sintered magnet (Nd magnet), was developed in Japan [1], which is currently one of the largest producers. However, all the raw materials (rare-earth oxides and rare-earth metals) are imported overseas to Japan [3]. In 2010, the import prices of rare-earth metals drastically increased because of a shortage in resource supply [4]. Particularly, the raise of dysprosium (Dy), which is an important additive for increasing coercivity of Nd magnet, was extremely high. Thus, the supply of rare-earth resources is uncertain, and therefore, recycling of rare-earth-containing waste, such as Nd magnet waste, is required to improve resource conservation and resource security of these metals [5,6,7].
The hydrometallurgical method is the major recycling process for Nd magnet waste [8, 9]. In this process, Nd magnet waste is dissolved in an acid and subjected to solvent extraction for primary resource processing. The hydrometallurgical method has advantages, such as the removal of much impurities and mutual separation of rare-earth elements. However, a large amount of waste solution is generated because, in addition to rare-earth metals, iron, as a major component of the magnet, is dissolved. Furthermore, large amounts of energy are consumed because RE is regenerated to metals via molten salt electrolysis along with raw materials derived from natural ore. Plants with recycling facilities are also few in countries where rare-earth smelters are located, such as China.
Based on the background, novel recycling processes have been developed to recycle Nd magnet waste in Japan. Chemical processes at elevated temperatures (pyrometallurgical recycling processes) developed on a laboratory scale are shown in Fig. 1. Recycling technologies for Nd magnet wastes are classified as (1) “material recycling methods” in which scrap materials are charged into smelting processes as raw material, (2) “alloy recycling methods” in which the materials are regenerated into master alloys for magnet production, and (3) “magnet recycling methods” in which magnet alloys are reused in their current form. For material recycling methods, Murase et al. applied the chemical vapor transport method to extract and separate rare-earth elements from magnet waste by forming complexes of aluminum chloride and rare-earth chlorides (Fig. 1a) [10]. Uda et al. studied the mutual separation of rare-earth halides by utilizing the difference in vapor pressure between rare-earth dihalides and trihalides (Fig. 1b) [11]. The extraction of rare-earth elements from magnet waste was also attempted using a chlorination agent or iodization agent (Fig. 1c, d) [12, 13]. Other roasting methods for rare-earth magnet such as sulfidation [14] and sulfation [15, 16] are also recently explored as other oxidative type methods. In contrast, the extraction of rare-earth metals without oxidation (halogenation) was extensively investigated using molten metals as collector metals (Fig. 1e) [17,18,19,20,21,22,23,24]. The removal of carbon and oxygen in magnet alloy wastes by roasting and calciothermic reduction/deoxidation was studied as alloy recycling methods (Fig. 1f) [25].
A noteworthy patent proposed the addition of a small amount of fluoride during the remelting of the magnet alloy for smoothly separating the slag and metal [26]. Deoxidation of pure Nd metal using molten fluoride has also been studied [27]. Based on this background, the authors explored a more realistic recycling process for Nd magnet waste and proposed a recycling process to extract rare-earth-oxide inclusions harmful for reproducing magnet alloys from magnet alloy wastes using molten fluoride [28]. The rare-earth-oxide inclusions are mainly located in the boundaries between the grains of matrix phase (RE2Fe14B, RE = Nd, Pr, Dy) [28]. The matrix has to be decomposed in order to liberate the inclusions. A schematic of the extraction process is presented in Fig. 2. In this process, Nd magnet alloys containing rare-earth oxides are remelted together with fluoride flux. The oxides rise in the molten alloy to dissolve into the molten fluoride. The refined alloys are used as the master alloys for magnet production. The separated oxides are reduced to metals by conventional molten salt electrolysis in molten fluoride. After electrolysis, the fluoride is circulated for the extraction process. The recycling process is highly feasible from an industrial point of view because (1) the reactor is simple; (2) the liquid–liquid separation (molten fluoride/molten alloy) is suitable for large-scale treatment; (3) the energy consumption is low because most of the alloy is regenerated without oxidation; and (4) no waste solution is generated.
The most important property of the fluoride flux in the extraction process is the solubility of rare-earth oxides in the molten fluoride. However, the solubility data at high temperatures are limited. For instance, it was reported that the solubilities of cerium oxide (CeO2) into a molten cerium fluoride (CeF3)—12 mass% barium fluoride (BaF2)—15 mass% lithium fluoride (LiF) were 1.7 and 2.1 mass% at 1073 and 1123 K, respectively [29]. Similarly, the solubility of lanthanum oxide (La2O3) into a molten lanthanum fluoride (LaF3)—27 mass% LiF—13 mass% BaF2 was approximately 2.5 mass% at 1223 K [29]. There are no systematic reports on the solubility of Nd2O3 and Dy2O3 in molten fluoride.
In this study, the phase equilibria between molten fluoride and Nd2O3 and Dy2O3 were investigated to determine their solubilities. A mixture of LiF and REF3 (RE = Nd, Dy) was selected as the fluoride. RE2O3 is known to react with REF3 to form chemically stable oxyfluorides (REOF and RE4O3F6) [30, 31]. However, the phase stabilities of REOF and RE4O3F6 at high temperatures remain unclear. Therefore, phase stabilities were analyzed using differential thermal analysis (DTA). The phase equilibria of the systems containing REOF and RE4O3F6 were studied using the chemical equilibrating method. These results were used to investigate the dissolution process of rare-earth oxides into molten fluoride.
The proposed process [28] requires operating temperatures that are higher than the peritectic point of Nd2Fe14B (1454 K [32]), which is the major phase of the Nd magnet, to efficiently extract rare-earth oxides. Heating the Nd magnet alloy above the peritectic temperature decomposes solid Nd2Fe14B into solid γ-Fe and liquid Nd–Fe–B phases, and the rare-earth oxide present in the alloy is liberated. Therefore, the experimental temperature was set at 1473 K (1200 °C), which is higher than the peritectic point of Nd2Fe14B.
Experimental
Sample Preparation
Reagent powders of Nd2O3 (99.9% purity, Soekawa Chemical Co. Ltd) and Dy2O3 (99.9% purity, Kojundo Chemical Laboratory Co. Ltd.) were pressed at 6 MPa to form pellets. These were stacked on an alumina plate, heated, and maintained at 1773 K for 3 h in air to transform a small amount of rare-earth hydrocarbonates contained in the reagents to rare-earth oxides by roasting. After cooling, the pellets were crushed, pulverized, and subjected to equilibrating experiments and oxyfluoride synthesis. Nd oxyfluorides were synthesized by pressing a mixture of Nd2O3 and NdF3 at 6 MPa to form pellets. The pellets were heated at 1173 K for 10 h under vacuum to synthesize NdOF and Nd4O3F6 according to reactions (1) and (2).
The above conditions for the synthesis of oxyfluorides were set according to the previous study [33]. DyOF and Dy4O3F6 were synthesized in the same manner.
Reagent powders of LiF (98% purity, Kanto Chemical Co., Inc.) and neodymium fluoride (NdF3, 99.9% purity, Nippon Yttrium Co. Ltd.) were mechanically mixed to obtain LiF-x mol% NdF3 (x = 25, 50) as the fluoride flux. Similarly, reagent powders of LiF and dysprosium fluoride (DyF3, 99.9% purity, Nippon Yttrium Co. Ltd.) were mixed to obtain LiF-x mol% DyF3 (x = 25, 50). The mixed salts were placed in an iron crucible (99.7% purity) and hermetically sealed using tungsten inert gas (TIG) welding. The mixed salts were then heated and melted at 1473 K for 3 h. After cooling, the salts were crushed and pulverized for subsequent experiments.
Experimental Procedure
Phase Stability Analysis
DTA experiments were conducted with 10 to 20 mg of synthesized oxyfluorides (NdOF, Nd4O3F6, DyOF, and Dy4O3F6) placed in an alumina pan, using a thermal analysis instrument (SDT Q600, TA instruments, USA). The temperature was increased from 293 to 1523 K (50 K higher than 1473 K as the target temperature) at a heating rate of 5 K·min−1 under an argon flow of 100 mL·min−1. The reference material was alumina powder (99.9% purity).
Determination of Phase Equilibria and Dissolution Investigations
Schematic representations of the vessel containing the samples and of the entire experimental apparatus, including the electric furnace, are shown in Fig. 3. The pre-determined compositions of the mixed samples were plotted as a reciprocal system in a compositional square (Fig. 4).
For Exp. A to J for the Nd system (LiF−NdF3/Nd2O3), and Exp. Q to S for the Dy system (LiF−DyF3/Dy2O3), mixed fluoride powders (0.316−6.859 g) and oxide powders (0.300–0.937 g) were well mixed and placed in an iron crucible to determine phase equilibria. For Exp. K to O for the Nd system (LiF−NdF3/NdOF), and Exp. U to X for the Dy system (LiF−DyF3/DyOF), oxyfluoride pellets were placed in an iron crucible, and the mixed fluoride powders were placed on the pellets to determine the phase equilibria and solubility.
In the neodymium system in the compositional square (Fig. 4a), Exp. A has the highest oxide concentration (lowest fluoride concentration), and Exp. M has the lowest oxide concentration (highest fluoride concentration). In the dysprosium system in the compositional square (Fig. 4b), Exp. Q has the highest oxide concentration, whereas Exp. W exhibits the lowest oxide concentration.
The mixed samples were placed in an iron crucible (99.7% purity, diameter and depth of 10 mm) and sealed using TIG welding. Three to four crucibles containing samples of different compositions were placed in a stainless-steel (SUS 310S in JIS standard) container that was sealed using TIG welding. The container was placed in a high-purity alumina tube in an electric furnace and heated at 1473 K for 86.4−605 ks (24–168 h). After the experiment, the container was removed from the alumina tube and quenched with water (The quench rate was estimated as approximately 130 K·s−1 on average). The recovered crucible was cut into two pieces, and the cross section was visually observed. A piece mounted in a resin was polished using emery papers, and a diamond paste (under 1 μm diameter particle) was observed using a scanning electron microscope with an energy-dispersive X-ray spectrometer (SEM–EDX, XL-30FEG, Philips Co.). The salt sample contained in another piece was mechanically peeled, crushed, and pulverized for X-ray diffraction analysis (XRD, Ultima IV, Rigaku Co.).
Results and Discussion
Phase Stability of Oxyfluorides up to 1473 K
The XRD patterns of synthesized Nd2O3, NdOF, and Nd4O3F6 are shown in Fig. 5. The XRD patterns were consistent with powder diffraction data files edited by International center for diffraction data (ICDD). The color of Nd2O3 was navy, while that of NdOF and Nd4O3F6 was aqua. Nd oxide and oxyfluorides were easily distinguished from the fluoride because the color of the mixed fluoride was white. DyOF and Dy4O3F6 were synthesized in the same manner. It was difficult to visually distinguish Dy2O3, DyOF, and Dy4O3F6 from mixed fluoride because all the compounds were white.
The DTA curves for analyzing the phase stability of the rare-earth oxyfluorides are shown in Fig. 6. NdOF undergoes an endothermic phase transformation at 797 K, which is attributed to the transformation from rhombohedral to cubic crystals [30]. The transformation temperature was close to that reported in the literature (788 K [30] and 800 K [34]). No transformation was observed between the transformation temperature and 1473 K, indicating the stability of solid NdOF at 1473 K. This agrees with the report by Niihara and Yajima [30].
Nd4O3F6 exhibited no phase transformation from 293 to 1473 K, which is consistent with some previous reports [30, 35]. Nd4O3F6 was also stable as a solid at 1473 K.
DyOF underwent an endothermic phase transformation at 831 K (transformation from rhombohedral to cubic crystals [30]). The transformation temperature was slightly lower than those reported in the literature (852 K [30], 842 K [34]). No further transformation was observed above the transformation temperature, which indicates that DyOF is stable as a solid at 1473 K.
Dy4O3F6 exhibited a phase transformation at 843 K, which exhibits a considerable discrepancy with the results obtained by Niihara and Yajima [30], who observed a transformation from tetragonal to unknown crystals at 1322 K. Kozak et al. [36] reported the decomposition of Dy4O3F6 to DyOF and Dy1+xO3xF3(1−x) at 1348 K; however, evidence of decomposition was not observed in the present study. Because an endotherm corresponding to melting was not detected during the DTA experiment and no change in the morphology of the Dy4O3F6 sample by melting was observed after the DTA experiment, it was concluded that Dy4O3F6 is stable as a solid at 1473 K.
Phase Equilibria Determination of the RE2O3-REF3-LiF system (RE = Nd, Dy)
The XRD patterns of the samples containing Nd2O3 mixed with LiF—50 mol% NdF3 and Nd2O3 mixed with LiF—25 mol% NdF3 are shown in Figs. 7 and 8, respectively. Nd2O3 disappeared, and NdOF was formed with decreasing oxide concentration (Exps. A to F/Exp. G to J). Then, NdOF disappeared and Nd4O3F6 was formed as the oxide concentration decreased further. It has been reported that Nd4O3F6 forms a solid solution, as indicated by the formula NdO1-xF1+2x (x = 0.15–0.34) [31], but the difference in composition could not be identified in the present study because analytical precision of SEM–EDX on gas elements such as oxygen and fluorine are very low. Nd oxide was found to be converted in the order of NdOF and Nd4O3F6. It was estimated that Nd4O3F6 dissolved into the molten fluoride to form ionic species.
Pure Nd2O3 and pure LiF were mixed in Exp. P. Nd2O3 and pure LiF were observed after the experiment. It was confirmed that the following reaction did not occur, and Nd2O3 equilibrated with LiF.
It is reasonable to investigate the equilibria in the composition triangle comprising Nd2O3, NdF3, and LiF corners in this study.
The XRD patterns of the sample containing Dy2O3 mixed with LiF—50 mol% DyF3 are shown in Fig. 9. The oxide concentration decreases from Exp. Q to R. The compound LiDyF4, identified in Exp. T, is by a peritectic reaction (peritectic point: 1137 K) during the cooling of the sample after the experiment. Dy2O3 disappeared, and DyOF was formed by decreasing the oxide concentration. Subsequently, DyOF disappeared, and Dy4O3F6 was formed as the oxide concentration decreased further. Thus, dysprosium oxide was converted in the order of DyOF and Dy4O3F6. It was considered that Dy4O3F6 dissolved into the molten fluoride to form ionic species. Based on the above results, it was considered that rare-earth oxides dissolve into molten fluoride by forming several rare-earth oxyfluorides.
Solubility and Dissolution Process of Oxyfluoride in Molten Fluoride
Figure 10 shows the photographic and SEM images of the iron crucible's cross section after the experiment in which the NdOF pellet was mixed with molten LiF—50 mol% NdF3 at 1473 K. The mixing ratio (RM) is defined as follows:
where nLiF-NdF3 and nNdOF represent the number of moles of fluoride (based on the average formula weight) and NdOF, respectively. The RM for the experiments shown in Fig. 10 was 20. A residue was visually observed at the bottom of the crucible after 24 h of holding. SEM–EDX revealed that the bulky particles in the residue were undissolved oxyfluoride (NdOxFy). Fine particles of oxyfluoride (NdOxFy) precipitated in the supernatant (flux region) during quenching were also observed. No residue was observed at the bottom of the crucible over 72 h, either visually or microscopically.
The experimental results obtained by mixing NdOF to LiF—50 mol% NdF3 are summarized in Fig. 11. The horizontal and vertical axes indicate the holding time and mixing ratio RM, respectively. When RM was 10, residues were observed after 24, 72, and 168 h. Therefore, the fluoride was saturated by neodymium oxyfluoride. When the values of RM were 20 and 30, the residue disappeared after 72 h of holding. Thus, the concentrations of oxyfluoride in the fluorides were lower than the solubility.
Based on the results, it was determined that the solubility of NdOF in molten LiF—50 mol% NdF3 at 1473 K was 7.9 mass%. The solubility of Nd2O3 in the molten salt was converted 7.4 mass%. Similarly, it was determined that the solubility of DyOF in molten LiF—50 mol% DyF3 at 1473 K was 8.0 mass%. The solubility of Dy2O3 in the molten salt was converted 7.6 mass%. Therefore, both the solubilities were similar.
The SEM images of the residue and precipitates after the dissolution of NdOF into molten LiF—50 mol% NdF3 and molten LiF—25 mol% NdF3 are shown in Fig. 12. For molten LiF—50 mol% NdF3, many fine particles of oxyfluoride precipitated during solidification were observed in the flux region, whereas particles of oxyfluoride were hardly observed in the flux region for molten LiF—25 mol% NdF3.
From the viewpoint of kinetics, it took a time over 24 h for complete dissolution of NdOF into molten fluoride. This means that dissolution rate of oxyfluoride into molten fluoride is very slow because the experiments were carried out without stirring. Therefore, an enhancement device for the dissolution rate, such as agitation of the melt, is required for practical applications to perform the extraction process efficiently.
Phase Diagram for the RE2O3–REF3–LiF System (RE = Nd, Dy)
The partial phase diagram for the Nd2O3–NdF3–Li2O–LiF system at 1473 K, constructed based on the above discussion, is shown in Fig. 13a. The horizontal and vertical axes indicate equivalent concentrations of lithium and oxygen, respectively. The composition regions surrounded by Nd2O3 (s)/LiF (l)/Li2O (s) and Nd4O3F6 (s)/NdF3 (s)/NdF3–LiF (l) were not investigated. Ternary phase equilibrium of Nd2O3 (s)/NdOF (s)/LiF (l) in the Nd2O3-rich region, and another ternary phase equilibrium of NdOF (s)/Nd4O3F6 (s)/LiF (l) is established by lowering the Nd2O3 concentration. The binary phase equilibria of Nd4O3F6 (s)/NdF3–LiF (l) appear with a further decrease in the Nd2O3 concentration. Solubility width of Nd4O3F6 was drawn along the literature [31]. Tie lines (dashed line) were drawn by an estimation along the phase rule. At a high temperature of 1473 K, any components in the system studied must have mutual solubilities to some extent. For instance, LiF must have a certain level of solubility of Nd2O3. However, the mutual solubilities are ignored in the present study because of lack of solubility data. In order to construct more accurate phase diagram, the solubility data have to be obtained. For example, it may be effective that molten LiF saturated with Nd2O3 at 1473 K is sampled and Nd and O concentrations in the LiF are measured. We will continue to work on the task to construct more accurate phase diagram. The hatched region in the diagram exhibits a homogeneous liquid phase. A homogeneous liquid phase should be formed during the practical extraction process by adding sufficient fluoride flux.
The partial phase diagram for the Dy2O3–DyF3–Li2O–LiF system at 1473 K is shown in Fig. 13b. The composition regions surrounded by Dy2O3 (s)/LiF (l)/Li2O (s) were excluded for the same reason as in the case of the neodymium system. A ternary phase equilibrium of Dy2O3 (s)/DyOF (s)/LiF (l) is observed in the Dy2O3-rich region, and another ternary phase equilibrium of DyOF (s)/Dy4O3F6 (s)/LiF (l) is established by decreasing the Dy2O3 concentration. The binary phase equilibria of D4O3F6 (s)/DyF3–LiF (l) appear with a further decrease in the Dy2O3 concentration. Solubility width of Dy4O3F6 was drawn along the literature [36]. Tie lines (dashed line) were drawn by an estimation along the phase rule. In the same manner with the system containing neodymium, the mutual solubilities between involved components are ignored in the system containing dysprosium because of lack of solubility data. In order to construct more accurate phase diagram, we will continue to work on the solubility measurement at high temperatures. It is estimated that Dy4O3F6 (s) equilibrates with molten fluorides containing oxyfluoride ions. The homogeneous liquid phase shown in the hatched region should be produced during a practical extraction process by adding sufficient fluoride flux in the same manner as the neodymium system.
Future Prospects for Practical Application
Figure 14 shows a schematic illustration of the extraction process of rare-earth oxides from a magnet alloy using molten fluoride. Nd2O3 in the alloy reacts with NdF3 in molten fluoride to form NdOF, which successively reacts with NdF3 to form Nd4O3F6. Nd4O3F6 finally dissolves in molten fluoride to form an oxyfluoride ion.
A Nd-sintered magnet generally contains approximately 31 mass% of rare-earth metals (Nd + Pr + Dy) and approximately 0.5 mass% of oxygen [25]; for instance, 100 kg of magnet alloy contains 31 kg of rare-earth metals and 0.5 kg of oxygen. If oxygen exists as Nd2O3, 100 kg of magnet alloy contains approximately 3.5 kg of Nd2O3. Based on the solubility of Nd2O3 (7.4 mass%) in LiF—50 mol% NdF3 at 1473 K, approximately 47 kg of flux is required to completely dissolve Nd2O3. Therefore, a considerable amount of flux is required. However, the flux can be reused several times after regenerating rare-earth metals using molten salt electrolysis. The loss of rare-earth metals from magnet alloys after refining is approximately 10%. Virgin metals corresponding to the lost rare-earth metals must be added for regenerating magnet alloys. In other words, magnetic waste can be regenerated with a small amount of virgin metals. The materials and energy required for recycling are extremely low compared to the current recycling process based on hydrometallurgical method.
Conclusions
The phase equilibria between molten fluoride and rare-earth oxide were investigated to develop a recycling process for Nd magnets using molten fluoride. LiF–REF3 and RE2O3 (RE = Nd, Dy) were selected as the fluoride and oxide, respectively. In the dissolution of Nd2O3 in molten LiF-NdF3, Nd4O3F6 formed when the mixing ratio exceeds the solubility limit of the melt and the compound coexists with the melt. In the same manner, Dy4O3F6 formed when the mixing ratio exceeds the solubility limit of molten LiF-DyF3 and the compound coexists with the melt. At 1473 K, the solubility of Nd2O3 in LiF—50 mol% NdF3 was determined as 7.4 mass%, while that of Dy2O3 in LiF—50 mol% DyF3 was determined as 7.6 mass%. An enhancement device for the dissolution rate, such as agitation of the melt, is required for practical applications. Partial phase diagrams in Nd2O3–NdF3–Li2O–LiF and Dy2O3–DyF3–Li2O–LiF systems were constructed, and a homogeneous liquid region suitable for efficient extraction was revealed. The recycling process developed in this study can be used to regenerate Nd magnet waste by adding a small amount of virgin metals.
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Acknowledgements
This work was financially supported by a Grant-in-Aid for Young Scientists (Start-up) (Project ID No. 19860015) and by a Scientific Research (S) (Project ID No. 19H05623) from the Ministry of Education, Culture, Sports, Science, and Technology (MEXT), Japan, and Research Grant from the Arai Science and Technology Foundation.
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Takeda, O., Nakano, K., Kobayashi, F. et al. Solubilities of RE2O3 in REF3-LiF (RE = Nd, Dy) at 1473 K. J. Sustain. Metall. 8, 1498–1508 (2022). https://doi.org/10.1007/s40831-022-00617-6
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DOI: https://doi.org/10.1007/s40831-022-00617-6