3.1. Method and Conditions for Separating Lanthanum and Cerium from Ca and Mg by Ammonium Bicarbonate Precipitation
Simulated solution of RECl
3 with concentrations of Mg (1.30 g/L), Ca (2.0 g/L) and REs (72.62 g/L) were used to investigate the effect of pH and aging time on the precipitation percentage and the RE
2O
3 purity of obtained products by fractional precipitation with ABC as well as the contents of Ca, and Mg. The precipitation percentages of REs, Ca, and Mg under different addition conditions of ammonium bicarbonate solution, pH and aging time were determined and compared in
Figure 1. It was found that as the dosage of ammonium bicarbonate increased, the pH value of the solution increased. At the beginning, the increase rate was slow. When the pH is higher than 5, the increase rate increased sharply.
Figure 1 (b, c) respectively show the precipitation percentages of Ca and Mg in the solution and the content of Ca and Mg in the products under different aging times when the dosage of ammonium bicarbonate is controlled for different precipitation percentages of REs. It was found that when the rare earth precipitation percentage was higher than 94%, Ca can be precipitated and entered the products with a small amount of Mg. Meanwhile, it decreased as the aging time increasing. Therefore, as long as the rare earth precipitation percentage is controlled to be less than 94% or the pH is less than 6, neither Ca nor Mg will enter the precipitation, and the precipitation separation from REs can be achieved, with the product purity approaching 100%. When the rare earth precipitation percentage is higher than 94%, Ca and Mg will enter the rare earth precipitation and affect the purity of the products. However, by extending the aging time, the co-precipitation of Ca and Mg can be reduced and the purity of the products can be improved.
3.2. The Effect of Al and Fe on the Precipitation Separation of Lanthanum and Cerium from Ca and Mg by abc
The pH of the initial feed solution was 3, and the concentrations of Ca, Mg, Al, Fe and REs were 1.82 g/L, 1.17 g/L, 2.04 g/L, 0.16 g/L and 65.79 g/L respectively. Gradually add 2% ammonium bicarbonate solution to this solution, measure the content of each ion in the supernatant at different pH values, and calculate the precipitation percentage of each ion.
As the results we reported previously that with the increase of pH from 3 to 4.4, the precipitation percentages of Al and Fe increased significantly. And when pH exceeds 3.8, Ca and Mg in the solution begin to precipitate in advance, and the precipitation percentage increased with the increase of the precipitation percentages of Fe and Al. Furthermore, Fe has been completely precipitated at pH=4.12, but the precipitation percentage of Al is only about 60%. Further increased the pH to 4.4, the removal effect of Al was not improvement obviously. At pH=4.6, the precipitation percentage of Al was 69%, and that of REs was 6.67%.
Figure 2(a) shows the variation of the precipitation percentages of REs, Al and Ca Mg with pH when further precipitated with ammonium bicarbonate after Fe was completely precipitated (pH=4.12) and filtered out. At pH=4.6, the Al precipitation percentage was 85% and the rare earth loss percentage was 5.71%. Therefore, by filtering out the Fe slag and then sedimentation, the removal percentage of Al can be increased, and the loss of REs is small. However, the removal percentage of Al is still not high, less than 90%. Compared with the rare earth solutions containing only Ca and Mg impurities, as the pH increases, Ca and Mg will enter the precipitate in advance via co-precipitation due to the presence of a small amount of Al, resulting in an increase in the impurity content in the final product.
Therefore, it is considered to filter the Al slag at pH=4.6, and then precipitate the filtrate with ammonium bicarbonate until pH=6.1. The ion concentrations in the supernatant were Mg=0.28 g/L, Ca=0.65 g/L and RE=0.067 g/L respectively. The pH was further increased to 6.43, 6.68, 6.78 and 6.92 respectively. After aging at room temperature for 2 hours and filtering by suction, the contents of each ion in the supernatant were determined and the precipitation percentages was calculated. The precipitate was washed several times, dried and calcined at 950 ℃ to obtain rare earth oxides. After dissolution, the contents of rare earth and non-rare earth impurities were determined. The results shown in
Figure 2(b) demonstrated that when the pH value is above 6, REs can almost be precipitated completely with a small amount of Al in the solution. Ca began to precipitate at pH=6.68, while the changes of other impurities were not obvious. Through the product analysis results in
Figure 2(c), it was found that with the increase of pH, the content of impurity Ca in the precipitate gradually increased along with the content of Al, and the purity of rare earth decreased. The purity of the obtained product was the highest when pH=6.43, reaching 97.83%. The contents of Al and Mg were 1.05% and 0.21% respectively, and the contents of Ca and Fe were lower than the detection limits. Because the solubility product constant K
sp of Ca carbonate is much smaller than that of Mg carbonate, Ca is more likely to precipitate than Mg, and impurities such as Mg mainly enter the product as co-precipitates. The results indicated that the presence of Fe will affect the precipitation of Al, and Al will affect the precipitation of Ca and Mg.
To increase the purity of RE
2O
3, the effect of aging time and aging temperature on it at pH=6.43 after filtered Fe and Al was studied. The results in
Figure 3. show that an appropriate aging time was conducive to the stability and growth of the precipitated particles, dissolving the impurity ions carried due to excessive precipitation rate, and reducing the residue of impurities in the precipitates. However, an excessively long aging time may cause the impurity ions adsorbed on the surface of the precipitated particles to re-enter the solution, thereby reducing the purity of RE
2O
3. Meanwhile, appropriately increasing the aging temperature can reduce impurity ions such as Mg entering the precipitates. But excessively high temperatures may cause the impurity ions adsorbed on the surface of the precipitated particles to re-enter the solution, thereby reducing the purity of RE
2O
3. So, the purity of RE
2O
3 was the highest at 6 hours aging time and 50 ℃ aging temperature with proportion of RE 98.51%, Al 0.9%, Mg 0.13%, without Ca and Fe.
3.3. The Effect of Precipitation Percentage of REs on the Purity of RE2O3 and the Contents of Ca, and Mg by Fractional Precipitation of RECl3 with ABC
RE
2O
3 products obtained by above one-step precipitation method still contained a small amount of impurities such as Al and Mg. To study the influence of co-existing ions (Al, Fe, Ca and Mg), fractional precipitation was adopted after filtered out the precipitate of Fe and Al. The results shown in
Figure 4. indicated that the precipitation percentage of Mg increased with that of REs, about 10% when the precipitation percentage of REs between 40% and 75%, and 15% for rare earth precipitation percentage at around 88%. Compared with the fractional precipitation of RECl
3 containing only Ca and Mg, Mg precipitated prematurely due to a small amount of impurities of Al.
Interestingly, the co-precipitation of Ca was occurred when the precipitation percentage of REs is lower that 40% or higher that 90%. No Ca isolated When the precipitation percentage between 60% and 88%. However, when ammonium bicarbonate was excess, Ca entered the precipitate in the form of Ca carbonate prematurely due to the presence of a small amount of Al. Therefore, to separate Mg and Ca from REs, controlling the precipitation percentage of REs is important. In addition, the aging time also show a significant impact. When the REs precipitation percentage was set at 60%, the purity of RE2O3 was the highest with RE purity of 98.83%, Al 0.73%, Mg 0.06%, without Ca and Fe.
3.4. The Effect of Precipitation Percentage of REs on the Purity of RE2O3 and the Contents of Ca, and Mg by Fractional Precipitation of RECl3 with ABC and TAC
The fractional precipitation method could improve the separation effect of REs from Fe and Ca, but the separation of REs from Al and Mg was still not thorough. Therefore, when precipitating Fe and Al, an appropriate amount of TAC was added, then the filtrate was used to precipitate REs with ammonium bicarbonate. The results in
Figure 5 indicated that adding a small amount of TAC significantly improved the precipitation percentage of Al. When the precipitation percentage of REs was controlled below 99%, Ca and Mg can not be precipitated via co-precipitation. When the REs precipitation percentage was controlled at 94%, the purity of RE
2O
3 was the highest, reaching 99.66%, only containing 0.09% of Al, without Ca, Mg and Fe remaining. We reported a method in the previous paper by raising removal percentage of Al by the coordination of Fe, Al with a small amount of TAC. Its dosage ratio and pH control range were very important. TAC could not only be used as a purifying agent to coordinate with Al and Fe ions for lowering the precipitation pH of Al and Fe, but also lower the crystallization rate of REs precipitation and reduce the co-precipitation of Ca, Mg with REs. So the separation selectivity of REs from Al, Fe, Ca, Mg was improved and high-purity of RE
2O
3 products with low impurities content can be obtained.
3.5. Coupling of Continuous Precipitation Crystallization and Coordination Assisted Precipitation Separation of REs from Impurities by ABC and TAC
The above results prove that the control of TAC dosage and precipitation pH in the previous stage is very important in the precipitation separation of REs from Ca, Mg, Fe and Al by ammonium bicarbonate with the coordination of TAC. Meanwhile, the control of precipitating agent dosage, as well as the pH range is also important, which can be achieved by using continuous precipitation crystallization. In a continuous precipitation crystallization technology, the role of seed crystals is fully utilized to accelerate the precipitation and crystallization rate of rare earth carbonate. The method of injecting and discharging simultaneously can effectively reduce the entrainment of impurity ions in the product, and it is also convenient to control the feeding ratio and the pH value of the solution. For this purpose, we compared the continuous crystallization effects in the two cases of impurity removal with and without the addition of TAC. It can be seen from
Figure 6(a) that REs concentration in the supernatant decreased with the increase of aging time, and the rare earth concentration was the lowest at a 6 hours of aging time. During this process, REs concentration in the supernatant for continuous precipitation was 0.599 g/L with TAC added and 0.863 g/L without TAC added, and REs concentrations after impurity removal were 19.66 g/L and 19.43 g/L, with REs loss rate 5% and 7% respectively. REs loss percentage is lower in the continuous precipitation process with the addition of TAC. During the continuous precipitation process, the volume ratio of the precipitating agent (10%NH
4HCO
3) to the feed liquid is approximately 55:100.
Figure 6(b-f) showed the purity of RE
2O
3 obtained after calcination at 950 ℃ for 1 hour under different aging times with or without TAC during the impurity removal process when the rare earth precipitation percentage was controlled at 94%. The results showed that the purity of RE
2O
3 reached 98.93% with 0.41% of Al, 0.03% of Fe, 0.08% of Ca, 0.16% of Mg when the aging time was 6 hours without adding TAC. However, the purity of RE
2O
3 was found to be 99.87%, only with 0.03% of Al, without Fe, Ca and Mg, when the aging time was 6 hours adding TAC. It can be seen that adding TAC during the impurity removal process can effectively reduce the contents of Ca, Mg, Al, Fe in RE
2O
3, improve the purity of products, and the effect of continuous precipitation crystallization is even better.