Hydrometallurgical Process to Recover Cobalt from Spent Li-Ion Batteries

The growth of the lithium-ion battery industry requires a secure supply of raw materials and appropriate end-of-life management of batteries. In almost five years, global cobalt consumption has increased by nearly 30%, driven mainly by rechargeable batteries. Consequently, several risks have been identified for cobalt, in particular the growing demand for electric vehicles, which could exceed current production. Therefore, research into the recovery of this critical metal, from industrial or urban waste, is particularly important in the years to come. In this study, cobalt is recovered from a lithium-ion battery leachate in hydroxide form. The thermodynamic simulations performed with Visual Minteq showed that it was possible to recover 99.8% of cobalt (II) hydroxide at 25 ◦C. Based on these results, experiments were conducted to validate the hypotheses put forward and to compare the results obtained with the simulations performed. Experimentally, several operating parameters were studied to determine the optimal conditions for cobalt recovery, in terms of yield, filterability, and selectivity. Results obtained in a batch reactor allowed the determination of the temperature conditions to be applied in continuous reactor. The cobalt (II) hydroxide precipitation in continuous reactor was carried out under different pH conditions. It was then possible to determine the optimal conditions for cobalt recovery in terms of yield and filterability. Results showed that working at pH 9 would effectively meet the desired criteria. Indeed, cobalt recovery is close to 100% and filtration flow rate is three times higher. Results obtained allow a better understanding of cobalt (II) hydroxide precipitation.


Introduction
Many high value-added technologies contain an almost unavoidable metal: cobalt. Due to its unique properties, cobalt is used in many industrial applications such as aerospace, superalloys, and in hydrocarbon desulfurization, which is crucial for the clean fuel industry. In only five years, global consumption of cobalt has increased by almost 30%, driven mainly by the rechargeable battery sector. Indeed, the lithium-ion (Li-ion) battery industry has grown exponentially since its creation at the end of the 20th century. As battery materials evolve, Li-ion battery applications are becoming more widespread. The main areas of use for Li-ion batteries include portable consumer electronics and electric/hybrid vehicles. Indeed, since 2010, Li-ion batteries have been used in hybrid and electric vehicles because of a higher power and energy density [1,2]. Approximately 2.72 million HEVs (Hybrid Electric Vehicles)/PHEVs (Plug-in Hybrid Electric Vehicles)/EV (Electric Vehicles) batteries were sold in 2015. The current market for Li-ion batteries in the automotive industry has reached more than USD 5 billion [3]. Based on the global growth of Li-ion batteries used in the automotive sector over the past five years, it is estimated that the global market for electric vehicles will reach 125 million electric vehicles by 2030 [4]. The need to reduce its environmental footprint is driving the growth for electric vehicles demand. However, this strong demand for electric vehicles could exceed current cobalt aluminum are recycled. However, the drawbacks of these processes are their long life cycle. The Table 1 summarizes the main methods and processes for recycling batteries. The Li-ion battery leachate composition remains complex and requires a new recycling processes development to best meet industrial needs. In this study, the leachate studied results from an innovative and more environmentally friendly process of the material battery NMC dissolution [24]. The leachate contains copper, cobalt, nickel, manganese and lithium in sulfate media as presented in Table 2. Table 2. Metals concentration in studied batteries leachates [24].

Metal Lithium (I) Copper (II) Nickel (II) Cobalt (II) Manganese (II)
Concentration (mol L −1 ) 0.442 0.259 0.134 0.131 0.125 The separation of these metals remains a challenge in terms of cost, environmental friendliness, and efficiency. Based on the literature and the thermodynamic study carriedout with Visual Minteq 3.0 (KTH Royal Institute of Technology, Stockholm, Sweden) software, it has been possible to identify the optimum experimental conditions for cobalt (II) hydroxide recovery. Visual Minteq 3.0 is a software for the simulation of thermodynamic equilibria, used in the calculation of metal speciation, solubility, and sorption equilibria. The advantage of using this software is the time saving, the accuracy of the results and especially the prediction of dissolution or precipitation in a complex medium, which is fundamental in this context of study. The thermodynamic database used in this software is thermos.vdb and comp_2008.vdb for inorganic species. The input data of the model are the total concentrations of the different components in solution, presented in Table 2. For all calculations, the system under study is at thermodynamic equilibrium. Thus, kinetic considerations are not taken into account in the simulations. The software then solves the problem in the form of non-linear algebraic equations to calculate thermodynamic chemical equilibria. Thus, Visual Minteq 3.0 evaluates the dissolution or precipitation of solid phases by calculating the supersaturation index [25].

Laser Granulometry
Particle size analysis is performed using a laser diffraction granulometer, the Malvern Mastersizer 2000 (Malvern Panalytical, Malvern, UK). This instrument allows the measurement of particle size distribution of precipitate. This technique uses a laser beam, where the particles are beforehand dispersed in water using dispersion module, to pass through this laser. Then, particles diffract the light at an angle that depends on their size. Indeed, the smaller the particle size, the larger the diffraction angle. Once a sufficient amount of sample has passed through, a particle size distribution can be plotted [26].

Inductively Coupled Plasma Atomic Emission Spectrometry ICP-AES
Inductively Coupled Plasma Spectrometry is a physical method of chemical analysis that allows the determination of different elements in solution. This technique consists of ionizing a sample using an argon plasma. Plasma is generated and maintained by a magnetic field, induced by a coil and heated to a temperature from 6000 • K to 8000 • K. The spectrometer analyses the light emitted by elements contained in the sample. The liquid solution to be analyzed is brought by a peristaltic pump into a nebulizer through which a stream of argon is passed, where it is transformed into an aerosol and then filtered in the nebulization chamber [27]. The experimental set-up is composed of: a double-jacketed reactor of one liter, a thermostatic bath (Julabo F32-EH, Julabo, Seelbach, Germany) a pH meter (Mettler Toledo, Columbus, OH, USA) a stirring motor (IKA Eurostar 60 control, IKA, Staufen, Germany) a Büchner filtration system with 0.45 or 0.22 µm porosity, laser diffraction particle size analyzer (Hydro MS 2000 Malvern) Experiments were performed at different temperatures: 25 • C, 40 • C, 50 • C, 60 • C and 70 • C. The thermostatic bath regulates the experimental media at the desired temperature. To precipitate 3.2 × 10 −2 mol of Co 2+ , 6.55 × 10 −2 mol of OH − are needed, which corresponds to a volume of 65.5 mL of soda (1 mol L −1 ). Experiment begins with the introduction of the complete volume, promptly, into the cobalt solution. Every 10 min, for three hours, pH is measured, and a sample of the solution is taken, filtered, and acidified with HNO 3 for ICP analyses.

Methods
Precipitation of Co(OH) 2 in Continuous Reactor at 25 • C Reagents and material used for the precipitation of cobalt hydroxide in continuous reactor are the same as Section 2.2.1 The experimental set-up is identical to Section 2.2.1 the additional elements to the set-up are as follows: 3 peristaltic pumps The cobalt solution (0.131 mol L −1 ) is introduced into the perfectly stirred doublejacket reactor using a peristaltic pump. The flow rate varies according to the desired pH in the reactor. The sodium hydroxide solution (2 mol L −1 ) is introduced at a flow rate of 3.5 mL min −1 . It has a concentration twice as high as that used in batch tests to reduce the dilution effect. Once the reactor volume (500 mL) has been reached, the withdrawal pump is witched on, thus maintaining a constant level throughout the experiment. Outlet samples are taken every 10 min for subsequent ICP analyses. The different flow rates are shown in the Table 3 below: These experiments allow the determination of the cobalt evolution of the concentration as a function of time and therefore cobalt hydroxide precipitation kinetic. Concerning particle size analyses, samples are analyzed at the end of the experiment in the same day.

Simulations Results on Batteries Leachate at Different Temperatures
Simulations on the precipitation of metal hydroxides were carried out at different temperatures: from 25 • C to 70 • C. The aim of these simulations is to determine the optimal temperature for total and selective cobalt recovery. The thermodynamic calculations were established based on the concentration of metals in leachate ( Table 2). As a function of the temperature of the medium and the supersaturation, Visual Minteq calculates the concentrations of the precipitates formed as a function of pH. Based on the solubility products of the different metal hydroxides at 25 • C and on the concentrations of the metals, copper hydroxide is the most insoluble and precipitates at the lowest pH. This is followed by the successive precipitation of nickel (II), cobalt (II) and manganese (II) hydroxides.
Simulation results of metal hydroxide precipitation at 25 • C and 70 • C are shown in Figure 1. At room temperature, 25 • C, nickel (II) hydroxide begins its precipitation at pH 6 and reaches 99% at pH 7. It is followed by cobalt (II) hydroxide precipitation at pH 7 and reaches 99% at pH 8. Manganese (II) precipitates at a higher pH than the preceding metals. In fact, manganese (II) hydroxide precipitation begins at pH 8.4 and reaches 99% at pH 10. It is useful to note that copper (II) hydroxide starts its precipitation from pH 4, as predicted by the precipitation diagram. Nevertheless, copper (II) hydroxide is highly insoluble and tends to transform into its most thermodynamically stable form, which is copper oxide [28]. According to free enthalpy values: ∆G formation (Cu(OH) 2 ) = −28,610 cal mol −1 and ∆G formation (CuO) = −30,400 cal mol −1 . According to various studies [24], copper oxide precipitates in a pH range between 4 and 7, which is in perfect agreement with the results obtained. gins at pH 8.4 and reaches 99% at pH 10. It is useful to note that copper (II) hydroxide starts its precipitation from pH 4, as predicted by the precipitation diagram. Nevertheless, copper (II) hydroxide is highly insoluble and tends to transform into its most thermodynamically stable form, which is copper oxide [28]. According to free enthalpy values: ΔG formation (Cu(OH)2) = −28,610 cal mol −1 and ΔG formation (CuO) = −30,400 cal mol −1 . According to various studies [24], copper oxide precipitates in a pH range between 4 and 7, which is in perfect agreement with the results obtained. Temperature does not significantly affect the pH formation of Ni(OH)2 or Co(OH)2. Indeed, at 25 °C or 70 °C, cobalt (II) and nickel (II) begin to precipitate at pH 6 and pH 7 respectively, regardless the temperature of the solution. Nevertheless, the temperature influence is particularly important for manganese. Indeed, Mn(OH)2 formation starts at pH of 8.4 at 25 °C, compared to pH 7.4 at 70 °C, which is very close to Co(OH)2 precipitation. As a result, it is important, according to these simulations, to not exceed the pH of Mn(OH)2 precipitation formation, if cobalt/manganese separation is based on precipitation. In addition, the most significant temperature influence is found in cobalt (II) hydroxide oxidation. Indeed, cobalt (II) precipitation at temperature higher than 40 °C has a significant impact on the thermodynamic stability of cobalt (II) hydroxide. The increase in temperature leads to a reduction in the stability range of cobalt (II) hydroxide. Cobalt hydroxide will tend to switch more rapidly to a more stable oxidized form (Co(OH)3). The higher the temperature, the more the range is reduced. The cobalt will remain as Co(OH)2 much longer at 25 °C than at higher temperature [30].
Thus, working at 25 °C would allow selective cobalt recovery and theoretically slow down cobalt (II) hydroxide oxidation. Thus, according to simulations results, a hydrometallurgical process has been designed from a Li-ion battery leachate. The hydrometallurgical process is essentially and purposefully based on precipitation operations, where our process consists of recovering each element individually. This process is adaptable to the various Li-ion battery technologies, and more precisely to the chemistry of the electrodes to recover the high valued metals as well as possible. Temperature does not significantly affect the pH formation of Ni(OH) 2 or Co(OH) 2 . Indeed, at 25 • C or 70 • C, cobalt (II) and nickel (II) begin to precipitate at pH 6 and pH 7 respectively, regardless the temperature of the solution. Nevertheless, the temperature influence is particularly important for manganese. Indeed, Mn(OH) 2 formation starts at pH of 8.4 at 25 • C, compared to pH 7.4 at 70 • C, which is very close to Co(OH) 2 precipitation. As a result, it is important, according to these simulations, to not exceed the pH of Mn(OH) 2 precipitation formation, if cobalt/manganese separation is based on precipitation. In addition, the most significant temperature influence is found in cobalt (II) hydroxide oxidation. Indeed, cobalt (II) precipitation at temperature higher than 40 • C has a significant impact on the thermodynamic stability of cobalt (II) hydroxide. The increase in temperature leads to a reduction in the stability range of cobalt (II) hydroxide. Cobalt hydroxide will tend to switch more rapidly to a more stable oxidized form (Co(OH) 3 ). The higher the temperature, the more the range is reduced. The cobalt will remain as Co(OH) 2 much longer at 25 • C than at higher temperature [30].
Thus, working at 25 • C would allow selective cobalt recovery and theoretically slow down cobalt (II) hydroxide oxidation. Thus, according to simulations results, a hydrometallurgical process has been designed from a Li-ion battery leachate. The hydrometallurgical process is essentially and purposefully based on precipitation operations, where our process consists of recovering each element individually. This process is adaptable to the various Li-ion battery technologies, and more precisely to the chemistry of the electrodes to recover the high valued metals as well as possible.
The first step is to recover copper by adding NaOH, under conditions of pH < 6 as it is presented in Figure 2. Then, cobalt and manganese are separated from nickel and lithium by liquid/liquid extraction. As an example, Cyanex 272-(organophosphinic acid) is the most widely used solvent extraction for the cobalt and nickel separation [31]. It has a very high selectivity allowing the efficient treatment of solutions with high nickel sulfate content and low cobalt content [32]. Subsequently, according to simulations, it is possible to separate cobalt/manganese by precipitation. However, it will be complicated to consider it experimentally. In fact, locally in the reactor, at the place where the NaOH is introduced, the pH is very high. As a result, cobalt and manganese co-precipitate, despite the homogenization of pH throughout the reactor. Then, an alternative solution to cobalt/manganese separation consists of an oxidative precipitation of manganese by NaOCl. Oxidative precipitation is an interesting alternative to a conventional precipitation, provided that it is within a specific pH and potential range to the selective precipitation of manganese oxide. For a potential range between 1.0 and 1.2 V (vs Standard hydrogen electrode) and a pH between 1 and 3, cobalt remains in the soluble Co 2+ state while the stable form of manganese is solid MnO 2 . Indeed, in the pH range between 3 and 4 and in the same potential range, cobalt predominates as Co(OH) 3 or Co 2 O 3 , 3H 2 O [33]. After that, cobalt is recovered by adding NaOH solution, pH range will be related to the polymorph aimed to precipitate: α-Co(OH) 2 or β-Co(OH) 2 . As for nickel, it is precipitated in the same way at a pH between 6 and 7. Lithium is recovered by the addition of sodium carbonate as mentioned in the literature [34], until saturation and crystallization of lithium carbonate.
vided that it is within a specific pH and potential range to the selective precipitation of manganese oxide. For a potential range between 1.0 and 1.2 V (vs Standard hydrogen electrode) and a pH between 1 and 3, cobalt remains in the soluble Co 2+ state while the stable form of manganese is solid MnO2. Indeed, in the pH range between 3 and 4 and in the same potential range, cobalt predominates as Co(OH)3 or Co2O3, 3H2O [33]. After that, cobalt is recovered by adding NaOH solution, pH range will be related to the polymorph aimed to precipitate: α-Co(OH)2 or β-Co(OH)2. As for nickel, it is precipitated in the same way at a pH between 6 and 7. Lithium is recovered by the addition of sodium carbonate as mentioned in the literature [34], until saturation and crystallization of lithium carbonate. The simulation results showed that it was possible to recover 99.8% of cobalt, in the hydroxide form. Indeed, at pH 8, [Co(OH)2] = 0.1307 mol L −1 . Based on these simulations results, experiments were conducted to validate the hypotheses put forward and to compare the results obtained with the simulations performed. Experimentally, several parameters were studied to determine the best conditions for cobalt recovery, in terms of yield, filterability, and selectivity. The selected polymorph should allow the obtaining of the highest yields and the lowest filtration times, thus growing closer to the real conditions of Li-ion battery leachates, and appearing on the proposed process scheme. The simulation results showed that it was possible to recover 99.8% of cobalt, in the hydroxide form. Indeed, at pH 8, [Co(OH) 2 ] = 0.1307 mol L −1 . Based on these simulations results, experiments were conducted to validate the hypotheses put forward and to compare the results obtained with the simulations performed. Experimentally, several parameters were studied to determine the best conditions for cobalt recovery, in terms of yield, filterability, and selectivity. The selected polymorph should allow the obtaining of the highest yields and the lowest filtration times, thus growing closer to the real conditions of Li-ion battery leachates, and appearing on the proposed process scheme. The temperature increase accelerates the phase transition from α-Co(OH) 2 to β-Co(OH) 2 and cobalt recovery is optimal at 25 • C with a yield close to 100% (Figure 3) [29]. Indeed, at 25 • C, after 28 min, 99.98% ± 0.02% of the cobalt is in β-Co(OH) 2 form. In comparison, at 70 • C, in only 4 min, 99.8% ± 0.02% of the cobalt has precipitated. In addition, a slight decrease in cobalt yield can be observed over time. This could be explained by Co(OH) 2 oxidation with oxygen from the air. When supersaturation, which is the driving force of precipitation, is sufficiently high, cobalt precipitates as β-Co(OH) 2 . It is useful to note that α-Co(OH) 2 is the less stable polymorph in a thermodynamical point of view and tends to transform into the most stable polymorphic form: β-Co(OH) 2 [35]. In Figure 3, the cobalt recovery is stabilized from 16 to 30 min, because of α-Co(OH) 2 dissolution is compensated with β-Co(OH) 2 particles growth. In fact, as β-Co(OH) 2 particles gradually form, their growth consumes the solute. From 36 min onwards, the cobalt concentration slowly decreases at 25 • C compared to temperatures higher [29]. This can be explained by the progressive oxidation of β-Co(OH) 2 to cobalt oxyhydroxide CoOOH, which is in line with various studies results [36,37]. Indeed, at high temperatures, oxidation occurs more rapidly, in less than 8 min and more importantly. The increase in temperature has the effect of reducing supersaturation, due to the increase in solubility products, and thus, of promoting the progressive dissolution of Co(OH) 2 particles. Previous work has shown that oxidation also occurs by a dissolution-precipitation mechanism [38,39]. The quantity of cobalt in solution will thus increase with temperature, the yield of the precipitated cobalt (II) will thus slightly decrease. decreases at 25 °C compared to temperatures higher [29]. This can be explained by the progressive oxidation of β-Co(OH)2 to cobalt oxyhydroxide CoOOH, which is in line with various studies results [36], [37]. Indeed, at high temperatures, oxidation occurs more rapidly, in less than 8 min and more importantly. The increase in temperature has the effect of reducing supersaturation, due to the increase in solubility products, and thus, of promoting the progressive dissolution of Co(OH)2 particles. Previous work has shown that oxidation also occurs by a dissolution-precipitation mechanism [38], [39]. The quantity of cobalt in solution will thus increase with temperature, the yield of the precipitated cobalt (II) will thus slightly decrease. Experimental results show that the temperature increase leads to a faster decrease in pH over time as displayed in Figure 4, which could be explained by the Co (II) hydroxide oxidation. Indeed, according to various research studies, the cobalt (II) hydroxide oxidation may be explained by proton diffusion, which corresponds to a decrease in pH [38]. Therefore, the rapid decrease in pH at high temperature is related to the oxidation reaction acceleration. Experiments conducted at 50 °C have confirmed this observation, where cobalt (II) hydroxide precipitation were conducted under nitrogen conditions [29]. Several simulations of precipitation of metal hydroxides contained in battery leachates show that care must be taken at the chosen temperature, whether manganese/cobalt separation is conducted by precipitation with hydroxides. Thus, Mn(OH)2 precipitates at pH close to the Co(OH)2 precipitation. To avoid manganese co-precipitation and according to the results of the simulations, it is advisable to work at temperatures close to room temperature, 25 °C. Moreover, this temperature's choice is in perfect agreement with literature. Indeed, Experimental results show that the temperature increase leads to a faster decrease in pH over time as displayed in Figure 4, which could be explained by the Co (II) hydroxide oxidation. Indeed, according to various research studies, the cobalt (II) hydroxide oxidation may be explained by proton diffusion, which corresponds to a decrease in pH [38]. Therefore, the rapid decrease in pH at high temperature is related to the oxidation reaction acceleration. Experiments conducted at 50 • C have confirmed this observation, where cobalt (II) hydroxide precipitation were conducted under nitrogen conditions [29]. Several simulations of precipitation of metal hydroxides contained in battery leachates show that care must be taken at the chosen temperature, whether manganese/cobalt separation is conducted by precipitation with hydroxides. Thus, Mn(OH) 2 precipitates at pH close to the Co(OH) 2 precipitation. To avoid manganese co-precipitation and according to the results of the simulations, it is advisable to work at temperatures close to room temperature, 25 • C. Moreover, this temperature's choice is in perfect agreement with literature. Indeed, working at temperatures higher than 25 • C promotes considerably the cobalt (II) hydroxide oxidation, which is not interesting in terms of yield and precipitates evolution. working at temperatures higher than 25 °C promotes considerably the cobalt (II) hydroxide oxidation, which is not interesting in terms of yield and precipitates evolution.

Temperature's Influence on Cobalt (II) Hydroxide Granulometry
Concerning temperature's influence on particle size distribution, experimental results show that increasing the temperature results in smaller particles of β-Co(OH)2 as shown in Figure 5. Indeed, at 25 °C, the cut-off diameter (d50) of Co(OH)2 particles is about 30 µm. In comparison, this diameter decreases by 55% at 70 °C, as d50 = 13 µm. However, this decrease varies slightly between 40 °C and 70 °C, with a particle cut-off diameter of about 16 µm.

Temperature's Influence on Cobalt (II) Hydroxide Granulometry
Concerning temperature's influence on particle size distribution, experimental results show that increasing the temperature results in smaller particles of β-Co(OH) 2 as shown in Figure 5. Indeed, at 25 • C, the cut-off diameter (d 50 ) of Co(OH) 2 particles is about 30 µm. In comparison, this diameter decreases by 55% at 70 • C, as d 50 = 13 µm. However, this  Temperature's Influence on Cobalt (II) Hydroxide Granulometry Concerning temperature's influence on particle size distribution, experimental results show that increasing the temperature results in smaller particles of β-Co(OH)2 as shown in Figure 5. Indeed, at 25 °C, the cut-off diameter (d50) of Co(OH)2 particles is about 30 µm. In comparison, this diameter decreases by 55% at 70 °C, as d50 = 13 µm. However, this decrease varies slightly between 40 °C and 70 °C, with a particle cut-off diameter of about 16 µm. The particle size decrease depends significantly on the temperature increase. These conditions may therefore not be favorable to the agglomeration mechanism. To highlight this transformation, the particle number size distribution at 25 °C and 70 °C is displayed in Figure 6. The shift from a volume size distribution g(L) ( Figure 5) to a number size distribution n(L) is done using a constant. Starting from the mass concentration expression (Cc) of the crystals in suspension, it is then possible to determine this constant which makes it possible to link the size distributions. The particle size decrease depends significantly on the temperature increase. These conditions may therefore not be favorable to the agglomeration mechanism. To highlight this transformation, the particle number size distribution at 25 • C and 70 • C is displayed in Figure 6. The shift from a volume size distribution g(L) ( Figure 5) to a number size distribution n(L) is done using a constant. Starting from the mass concentration expression (Cc) of the crystals in suspension, it is then possible to determine this constant which makes it possible to link the size distributions.
Considering that for a volume of suspension given: Then: Considering that for a volume of suspension given: Then: By combining Equation (1) in Equation (4), g(L) expression form is the following: Then: With: ϕ v : Volume form factor n (L): Number size distribution (m −4 ) C c : Mass concentration of crystals (kg·m −3 ) m c : Mass of crystalline particle (kg) ρ c : Density of crystalline particle (kg·m −3 ) L: Average particle size (µm) m t : Total sample mass of the precipitate (kg) As displayed in Figure 6, the fine particles number is significantly higher at 70 • C than at 25 • C, which has an impact on the precipitate filterability. At 70 • C, the filtration of the precipitate is very difficult, with a strong increase in pressure drop and a long filtration time. It should be remembered that the solubility of Co(OH) 2 increases as a function of temperature, as do the reaction kinetics. Thus, supersaturation decreases more rapidly over time at 70 • C than at 25 • C, which is detrimental to particle agglomeration. On the other hand, an increase in temperature favors the Co(OH) 2 particles oxidation. The oxidation mechanism takes place in two stages, dissolution and precipitation. The cobalt (II) hydroxide particles dissolve and then precipitate as smaller particles. Thus, these conditions are unfavorable both from a kinetic and particle size point of view.
It is, therefore, recommended to work at temperatures close to room temperature to limit oxidation, maintain a very good cobalt (II) yield and control the particle size, which is a fundamental parameter for the filtration and washing stages. It should be noted that operating at room temperature allows the proposal of a low-energy-consuming process, without thermal risks and with lower implementation and operating costs. In addition, working at 40 • C or higher would generate the formation of particles with a cut-off diameter of about 17 µm versus 34 µm at 25 • C. Consequently, working at low temperature allows validation of all the criteria sought: selectivity, yield, and filterability.

Precipitation of Co(OH) 2 in Continuous Reactor at 25 • C
The Co(OH) 2 precipitation was first studied in a discontinuous regime to determine the operating parameters to achieve the established objectives. Indeed, it was concluded to work at 25 • C to slow down the Co(OH) 2 oxidation. Moreover, this temperature was also chosen based on the different unit operations that take place with the recovery of cobalt (II) in the hydrometallurgical process, the liquid/liquid extraction and the cobalt/manganese separation. The second parameter that has been studied is the reaction time: it only takes a few minutes for the cobalt to precipitate at more than 99.9%. However, the polymorphic transition is slightly longer (about 20 min). Nevertheless, the product obtained is stable and does not evolve over time. Since filtration takes place during the day, oxidation is not a problem for the cobalt yield or even for the stability of the powder obtained. The particle size quality obtained is essential for the subsequent use of the cobalt. Thus, the study was carried out over a pH range from 8.2 to 9.4 to avoid Co(OH) 2 oxidation and to determine the optimal pH, whose control is essential to meet the best recovery and filterability.
The experiments were conducted in a pH range between 8.2 and 9.4, corresponding to a molar ratio n OH − /n Co 2+ < 2. The experiments showed that for a molar ratio lower than 2, cobalt (II) hydroxide of type α-Co(OH) 2 is formed. Indeed, supersaturation is not sufficient for the rapid polymorphic transition from α-Co(OH) 2 to β-Co(OH) 2 [40]. Studies have shown that for a molar ratio n OH − /n Co 2+ between 1 and 1.8, the polymorph α-Co(OH) 2 remained stable, its conversion to the β-Co(OH) 2 form is very long. Experimentally, the cobalt (II) hydroxide precipitation under these conditions leads to a polymorphic transition of up to 70 h. On the other hand, for a molar ratio greater than or equal to 2, α-Co(OH) 2 transforms quite rapidly into β-Co(OH) 2 [36], a transition time of about two hours has been observed. Thus, it is interesting to study the behavior of α-Co(OH) 2 in a continuous regime and in a varied pH range, which depends mainly on the molar ratio n OH − /n Co 2+ < 2. This study will allow the determination of the optimal pH that will meet the criteria of yield and filterability. The results in terms of cobalt recovery yield as a function of pH are shown in Figure 7.
oxidation and to determine the optimal pH, whose control is essential to meet the best recovery and filterability.
The experiments were conducted in a pH range between 8.2 and 9.4, corresponding to a molar ratio n OH − /n Co 2+ < 2. The experiments showed that for a molar ratio lower than 2, cobalt (II) hydroxide of type α-Co(OH)2 is formed. Indeed, supersaturation is not sufficient for the rapid polymorphic transition from α-Co(OH)2 to β-Co(OH)2 [40]. Studies have shown that for a molar ratio n OH − /n Co 2+ between 1 and 1.8, the polymorph α-Co(OH)2 remained stable, its conversion to the β-Co(OH)2 form is very long. Experimentally, the cobalt (II) hydroxide precipitation under these conditions leads to a polymorphic transition of up to 70 h. On the other hand, for a molar ratio greater than or equal to 2, α-Co(OH)2 transforms quite rapidly into β-Co(OH)2 [36], a transition time of about two hours has been observed. Thus, it is interesting to study the behavior of α-Co(OH)2 in a continuous regime and in a varied pH range, which depends mainly on the molar ratio n OH − /n Co 2+ < 2. This study will allow the determination of the optimal pH that will meet the criteria of yield and filterability. The results in terms of cobalt recovery yield as a function of pH are shown in Figure 7.  It appears that the cobalt recovery yield at pH 8.3 is around 90%. The recovery is not total because this pH corresponds to a molar ratio n OH − /n Co 2+ of 1.1, which is not enough to recover all cobalt in solution. Thus, the total precipitation of cobalt starts from pH 8.6 where 98% of cobalt is in α-Co(OH) 2 form. Cobalt is recovered totally in a pH range between 8.6 and 9.4. It should be noted that in this range, the molar ratio n OH − /n Co 2+ is between 1.3 and 1.6. It is useful to note that the solid formed under this pH condition could correspond to a Co(OH)x; 1.3 < x < 1.6 form, due to the α-Co(OH) 2 hydrotalcite structure, which mean the quantity of soda used is reduced, which is quite promising in economic point of view. From a particle size point of view (Figure 8), it appears that the pH increase causes a decrease in the median particle diameter of the Co(OH) 2 particles. Indeed, for a pH of 8.2 the median diameter is 42 µm ± 1.5 µm and it increases to 23 µm ± 0.04 µm for a pH of 9.4.
x FOR PEER REVIEW 12 of 15 It appears that the cobalt recovery yield at pH 8.3 is around 90%. The recovery is not total because this pH corresponds to a molar ratio n OH − /n Co 2+ of 1.1, which is not enough to recover all cobalt in solution. Thus, the total precipitation of cobalt starts from pH 8.6 where 98% of cobalt is in α-Co(OH)2 form. Cobalt is recovered totally in a pH range between 8.6 and 9.4. It should be noted that in this range, the molar ratio n OH − /n Co 2+ is between 1.3 and 1.6. It is useful to note that the solid formed under this pH condition could correspond to a Co(OH)x; 1.3 < x < 1.6 form, due to the α-Co(OH)2 hydrotalcite structure, which mean the quantity of soda used is reduced, which is quite promising in economic point of view. From a particle size point of view (Figure 8), it appears that the pH increase causes a decrease in the median particle diameter of the Co(OH)2 particles. Indeed, for a pH of 8.2 the median diameter is 42 µm ± 1.5 µm and it increases to 23 µm ± 0.04 µm for a pH of 9.4. In terms of filterability, at pH = 9.4, filtration takes place at a flow rate of 100 mL.min −1 compared to 33 mL min −1 at any other pH. The filtration rate is three times higher. In addition, the polymorph control is a major issue. Comparing the different nucleation rates, it appears that in a range of pH < 9.4, nucleation rates increase, as shown in Figure  9.  In terms of filterability, at pH = 9.4, filtration takes place at a flow rate of 100 mL.min −1 compared to 33 mL min −1 at any other pH. The filtration rate is three times higher. In addition, the polymorph control is a major issue. Comparing the different nucleation rates, it appears that in a range of pH < 9.4, nucleation rates increase, as shown in Figure 9.
In terms of filterability, at pH = 9.4, filtration takes place at a flow rate of 100 mL.min −1 compared to 33 mL min −1 at any other pH. The filtration rate is three times higher. In addition, the polymorph control is a major issue. Comparing the different nucleation rates, it appears that in a range of pH < 9.4, nucleation rates increase, as shown in Figure  9. This is supported by the fact that as the pH rises, the amount of OH − increases, which promotes nucleation. However, depending on the available supersaturation, nucleation may be limited, and growth promoted. This range corresponds well to the molar ratio n OH − /n Co 2+ < 2, where the α-Co(OH)2 form predominates. Nevertheless, at pH 9.4 the trend is more pronounced, the nucleation rate increases sharply in contrast to the growth rate which decreases. This can be explained by α-Co(OH)2 which will tend to transform into its β-Co(OH)2 form when precipitation conditions are close. It could be that for a pH of 9, α-Co(OH)2 is in the transformation phase, so it acquires the properties of both polymorphs.  This is supported by the fact that as the pH rises, the amount of OH − increases, which promotes nucleation. However, depending on the available supersaturation, nucleation may be limited, and growth promoted. This range corresponds well to the molar ratio n OH − /n Co 2+ < 2, where the α-Co(OH) 2 form predominates. Nevertheless, at pH 9.4 the trend is more pronounced, the nucleation rate increases sharply in contrast to the growth rate which decreases. This can be explained by α-Co(OH) 2 which will tend to transform into its β-Co(OH) 2 form when precipitation conditions are close. It could be that for a pH of 9, α-Co(OH) 2 is in the transformation phase, so it acquires the properties of both polymorphs.
Consequently, the solid α-Co(OH) 2 filtration takes place relatively quickly, the β-Co(OH) 2 transition does not occur under these conditions. In addition, the polymorph α-Co(OH) 2 has several advantages such as its hydrotalcite crystal structure. Indeed, it has a larger interlayer space, which gives it much better electrochemical capabilities [41]. Consequently, it is necessary to work at pH 9.4 to recover all cobalt in solution and to filter optimally. In addition, working at pH 9 limits the quantities of soda added, the molar ratio between soda and cobalt is 1.6 against 2 theoretically, which remains interesting from an economic point of view.

Conclusions
In this study, it was possible to determine the most favorable conditions for the cobalt (II) hydroxide precipitation, based on simulations and experimental results. The temperature increase accelerates the phase transition from α-Co(OH) 2 to β-Co(OH) 2 and the cobalt recovery is optimal at 25 • C with a yield close to 100%. Experimental results show that the temperature increase leads to a faster decrease in pH over time, which could be explained by the Co (II) hydroxide oxidation. According to various research studies, the cobalt (II) hydroxide oxidation is accompanied by proton diffusion, which corresponds to a decrease in pH. Therefore, the rapid decrease in pH at high temperature is probably related to the acceleration of the oxidation reaction. Various simulations for battery leachates show that care must be taken at the chosen temperature, because at high temperature, Mn (II) hydroxide precipitates at pH levels close to the precipitation of Co (II) hydroxide, in the case of cobalt/manganese separation by precipitation. According to the simulations results, it is advisable to work at temperatures close to room temperature, to avoid manganese co-precipitation. Moreover, this temperature is in perfect agreement with the best cobalt precipitation yields and with the results of the particle size distribution, which is favorable to a better filterability. Working at 40 • C and above would generate the formation of particles with a median diameter of about 17 µm versus 34 µm at 25 • C. Consequently, working at low temperature allows validation of all the criteria sought: selectivity, yield, and filterability.
Subsequently, the cobalt (II) hydroxide precipitation was studied in a continuous reactor. The optimal operating conditions determined in batch mode constituted the starting point for the continuous precipitation and for the rest of the work. The continuous precipitation of cobalt (II) hydroxide was carried out under different pH conditions to determine the optimal pH to best meet the desired criteria (yield and filterability). Working at pH = 9 allows the recovery of all the cobalt in the form α-Co(OH) 2 , to filter quickly and to limit the quantities of soda added. Indeed, the molar ratio between soda ash and cobalt is 1.6 against 2 for β-Co(OH) 2 , which is interesting from an economic point of view. These cobalt (II) recovery conditions allow the determination of the optimal cobalt (II) hydroxide precipitation conditions in terms of yield, filterability, and polymorphism. This promising result allows the consideration of cobalt (II) hydroxide precipitation on a larger scale as fluidized bed reactor for example. Indeed, the fluidized bed reactor should guarantee a larger granulometry and thus a better filterability, which represents one of the main conditions of this study. Then, it will be possible to extend this study in an industrial scale for different type of Li-ion battery leachate.