Yuting Huoabc,
Yan Luobc,
Zhongqi Zhaobc,
Junxia Geng
bc,
Qiang Dou*bc and
Jie Ma
*a
aSchool of Materials and Chemistry, University of Shanghai for Science and Technology, Shanghai 200093, China. E-mail: majie@usst.edu.cn
bShanghai Institute of Applied Physics, Chinese Academy of Sciences, Shanghai 201800, China. E-mail: douqiang@sinap.ac.cn
cCentre of Excellence TMSR Energy System, Chinese Academy of Sciences, Shanghai 201800, China
First published on 1st March 2022
In thorium molten salt reactors (TMSR), 233Pa is an important intermediate nuclide in the conversion chain of 232Th to 233U, its timely separation from the fuel salt is critically important for both the thorium–uranium (Th–U) fuel cycle and the neutron economy of the reactor. In this study, the evaporation behavior of 233Pa in the FLiBeZr molten salt was investigated during a vacuum distillation process. The separation characteristics between 233Pa and the major components of the fuel (salt and fission products) were evaluated in a calculation of the separation factors between these components. It was found that 233Pa5+ evaporated more readily than 233Pa4+ and the other components of the fuel, the relatively low temperature and medium pressure were much more beneficial to the separation of 233Pa5+ from FLiBeZr salt in the evaporation process, with the maximum value of the separation factor achieving more than 102. Results of distillation experiments also show that increasing the temperature and decreasing the ambient pressure enhances the separation between 233Pa5+ and most of the fission product nuclides due to the 233Pa5+ volatility more strongly depending on the process conditions. These results will be utilized to design a concept for a process for 233Pa separation from the fuel of a molten salt reactor.
In TMSR liquid fuel, 232Th captures neutrons, which undergo the following nuclear reactions and nuclear decay, transforming into a new fissile nuclide 233U.9 The 232Th–233U fuel cycle process is shown in eqn (1):
![]() | (1) |
Especially important is 233Pa (half-life of 27 day), the intermediate nuclide of the 232Th–233U fuel cycle.10 As the thermal neutron capture cross-section of 233Pa is 5 times higher than that of 232Th, 233Pa gradually accumulated in TMSR fuel would capture considerable neutrons. This will bring dual negative effects: not only consumes important precursor of 233U, but also reduces the neutron economy of TMSR.11 In order to maintain efficient operation of the reactor and ensure high breeding of 232Th, 233Pa must be separated from TMSR fuel in time, then could successfully decay into 233U before being reused.12 The efficient separation of 233Pa has received extensive concern and increasing research interest, in line with the strategies of the main countries developing molten salt reactor.
Since 1960s, Oak Ridge National Laboratory (ORNL) had developed the Molten Salt Reactor Experiment (MSRE), and carried out systematic research on fuel treatment of MSR.13,14 In their fuel reprocessing scenario, 233Pa would be separated from fuel salt by reductive extraction method, and metal thorium was used as reductant for reductive extraction.15 233PaF4 in salt phase was reduced to metal state by metal thorium, and then extracted in liquid metal bismuth.16 Finally, the experimental result clearly shows that the separation coefficient of between 232Th and 233Pa can be more than 1500.17 However, some inherent shortcomings of the reductive extraction method, such as rigorous process requirements and complex equipment system, have presented a formidable challenge for the engineering applications of this method. At the same time, ORNL also investigated the isolation of 233Pa from fuel salt by oxidation precipitation and had proved in the laboratory scale that 233Pa could be effectively separated by adding BeO, ThO2, UO2, and other precipitators to LiF–BeF2–ThF4 melt.17,18 As these above-mentioned precipitators were added to salt phase, UO2–ThO2 solid solution would be formed. 233Pa can be precipitated by effective contact between salt phase and solid solution. Nevertheless, the fuel salt treated by the oxide precipitation method must be deoxidized and purified before reusing in the reactor, it will greatly increase the workload of fuel treatment of MSR. Consequently, it is still urgent to develop a more effective and convenient method to isolate 233Pa from the fuel salt. Previous experiments have shown that a certain amount of 233PaF4 will be produced after 232ThF4 is irradiated by neutrons. Brookhaven National Laboratory heated the neutron-irradiated 232ThF4 powder in fluorine gas or chlorine trifluoride gas stream, and found that protactinium compounds evaporated from the powder at 500 °C. In our preliminary experiment, we also found that 233Pa had certain volatility at high temperature after the fuel salt treated with fluorine gas. So we speculated that 233Pa4+ in fuel salt might be oxidized to pentavalent state by fluorine gas, forming a high volatile protactinium compound. Furthermore, previous study also indicated that pentavalent protactinium was more volatile than 233Pa4+ and sublimed under vacuum above 500 °C.19,20
In order to further investigate the feasibility of separation of pentavalent 233Pa from the fuel salt, the evaporation experiments of fuel salt containing 233Pa was carried out over a wide temperature and pressure range in this work. This paper would be first to provide the direct comparison of the evaporation behaviours between 233Pa and molten salt, and address the effect of process conditions on the evaporations of these two substances. Furthermore, in order to investigate the separation between protactinium and the impurity elements in the evaporation process, we systematically detect and compare the radioactivity of 233Pa and some critical fission product nuclides in the fuel salt before and after evaporation, and the condensed salt. The results in this study are useful and important for both the advance of basic knowledge in the high temperature chemistry of pentavalent protactinium and their potential applications in the efficient separation of 233Pa from the fuel salt.
The experimental equipment used in this work is a self-designed thermogravimetric evaporation furnace, shown in Fig. 1. In order to prevent molten salt from absorbing water and leak radioactive substances, the furnace should be placed in a glove box filled with argon gas (oxygen content ≤10 ppm, water content ≤100 ppm). A quartz tube (height = 250 mm, inner diameter = 18 mm, outer diameter 20 mm) is installed in the customized basket. A nickel foil is placed on the quartz tube to collect the vaporized gaseous products, as shown in Fig. 2. Finally, a nickel crucible with height of 25 mm, inner diameter of 14 mm and outer diameter of 16 mm, which is placed at the bottom of the quartz tube.
Vacuum distillation experiment was carried out in FLiBeZr salt. About 1 g of molten salt above was placed in a nickel crucible, which was weighted to record the mass before the experiment and then the radioactivity of the interest nuclides in the molten salt was measured. The crucible is placed at the bottom of a quartz tube with a ring of nickel foil. Then put the quartz tube in the basket and heat the basket in the thermogravimetric furnace, so that the bottom of the basket is heated at the highest temperature zone of the furnace.
The volatility of 233Pa before and after fluoridation was compared. The molten salt before and after the fluorination reaction is heated for 1 h at 700, 800, 900 °C respectively and 8 Pa. The evaporation rate of 233Pa in FLiBeZr molten salt before and after injected fluorine gas was compared. The effect of temperature on 233Pa5+ volatility was studied. The temperature was heated to the experimental temperature (700, 750, 800, 850, 900 °C, respectively) and kept 1 h at 8 Pa. After the evaporation experiment is completed, the mass of the molten salt is weighted, and the activity of the interest nuclides in the remaining molten salt and the molten salt collected by the nickel foil is detected. Next the effect of pressure on 233Pa volatility was studied. According to the above temperature procedure to keep 850 °C for 1 h and change the pressure into 8, 35, 200, 500, 103, 104, 105 Pa, respectively. The experimental operation was described above, and then the mass of molten salt and the activity of 233Pa before and after the experiment were recorded. In this paper, the change of molten salt is calculated with mass. Because of the small amount of 233Pa and some nuclides in salt, the change of nuclides is calculated with radioactivity. Therefore, in order to make a unified comparison between these two substances, the evaporation percentage per hour is used for comparison.
Nuclide | Energy/keV | Intensity/% | Energy/keV | Intensity/% | Energy/keV | Intensity/% |
---|---|---|---|---|---|---|
233Pa | 311.9 | 38.5 | 300.1 | 6.63 | 340.5 | 4.45 |
95Nb | 765.8 | 99.81 | 561.9 | 0.015 | — | — |
103Ru | 497.1 | 91.0 | 610.3 | 5.76 | — | — |
141Ce | 145.4 | 48.29 | — | — | — | — |
140Ba | 537.3 | 24.39 | 162.6 | 6.219 | 304.8 | 4.293 |
95Zr | 756.7 | 54.38 | 724.2 | 44.27 | — | — |
From the beginning of the vacuum distillation experiment to the measurement of radioactivity after the experiment, the influence of the radioactive decay on the accuracy of radioactivity calculation is obvious enough not to be ignored. Therefore, the calculation of radioactivity in this paper used the exponential decay law formula to eliminate the influence of the radioactive decay during this period, so as to ensure the accuracy of the calculation result of the separation factor.22
On studying the separation of 233Pa from fission products, the minimum detectable activity (MDA) in units of Bq for some selected nuclides is calculated as follows eqn (2):23
![]() | (2) |
![]() | (3) |
In order to achieve the efficient separation of 233Pa from the fuel salt, it is necessary to explore the difference in the volatility of 233Pa5+ and FLiBeZr salt over a wide temperature range. Therefore, the concept of separation coefficient was used to evaluate the separation behaviour between 233Pa and FLiBeZr salt in the high-temperature evaporation. The separation coefficient, Φ, was calculated based on the radioactivity of 233Pa and the mass of the molten salt before evaporation and on nickel foil after evaporation, as shown in eqn (4):
![]() | (4) |
From Fig. 6 it is evident that 233Pa is non-volatile at normal pressure (105 Pa), with the evaporation rate of FLiBeZr salt only 0.22%/h. As the ambient pressure decreases continuously, the evaporation rate of 233Pa shows a sharp increase (from 29.43%/h to 99.83%/h) below 1000 Pa. By contrast, the evaporation rate of the salt not show a significant increase until the pressure drops below 100 Pa. A key factor responsible for this difference in their evaporation behaviours may lie in their own volatility. Previous theoretical and experimental studies in high temperature melts have shown that when ambient pressure decreases continuously, the evaporation rate of the melts would not present a sharply increase until the pressure approaches its vapor pressure.25,26 The preceding experimental studies have shown that the vapor pressure of FLiBeZr salt is just around 10–100 Pa,16 which is much close to the transition pressure of this salt shown in Fig. 6. On the basis of the data in Fig. 6, we can also draw a reasonable speculation that the vapor pressure of 233Pa5+ in the melt is near 1000 Pa, which is obviously higher than of the melt.
Hence, in order to further characterize the effect of ambient pressure on the separation between FLiBeZr salt and 233Pa5+, we also calculate the separation coefficient, Φ of these two substances in the pressure range studies, as shown in Fig. 7. Φ increases sharply first and then decreases with decreasing of ambient pressures, and the maximum value (about 43) is observed at 1000 Pa. It is thus evident that the medium pressure, such as about 1000 Pa, can effectively inhibit the evaporation of FLiBeZr salt and is much more beneficial to the separation of 233Pa from the molten salt.
Therefore, to get insight into the evaporation of these nuclides during vacuum distillation, we performed in distillation experiments in this work at temperatures ranging from 700–900 °C with evaluating the γ-activity changes of these critical nuclides in the fuel salt before and after distillation. Fig. 8 represents that the γ-activity of 233Pa and fission product nuclides in the fuel salts before and after distillation. It can be seen that the volatility of 233Pa increases sharply with increasing evaporation temperature. However, 95Nb and 95Zr do not vaporized until the evaporation temperature rises above 800 °C. Under the same conditions, the γ-activity of 141Ce, 140Ba and 103Ru is not influenced by the evaporation process, indicating that these fission products are non-volatile in the temperature range studied. Separation factor is used to defined as the process separability between two components of reference and impurity.27 In order to further characterize the separation behaviour between 233Pa and these critical fission products, the separation factor, β(i/Pa), between these nuclides was calculated based on the activity data of relevant nuclides in fuel salts before evaporation and on nickel foil after evaporation respectively, and list in Table 2. The β(i/Pa) of 233Pa in TMSR fuel salt with respect to a specified nuclide were calculated by the following formula eqn (5):
![]() | (5) |
![]() | ||
Fig. 8 The γ-activity of each element in the remaining FLiBeZr salt, at 8 Pa, as a function of temperature. |
β(Ce/Pa) | β(Ba/Pa) | β(Ru/Pa) | β(Zr/Pa) | β(Nb/Pa) | |
---|---|---|---|---|---|
700 °C | 87 | 13 | 25 | 31 | 19 |
800 °C | 184 | 41 | 63 | 127 | 86 |
900 °C | 323 | 42 | 94 | 102 | 143 |
Next, to get insight into the effect of pressure on the separation distillation experiments were performed under the ambient pressures ranging from 8 Pa to 105 Pa by using the simulated fuel salt. The γ-activity of these nuclides in the molten salt before and after distillation are shown in Fig. 9, and it is found that at normal pressure 95Nb is only nuclides which shows obvious volatility. As the ambient pressure decreases continuously, 233Pa begins to volatilize at 104 Pa, and 95Zr does not show obvious volatility until the pressure drops to 200 Pa. Meanwhile, we also found that 141Ce, 140Ba, 103Ru are almost non-volatile and not influenced by the pressure in these distillation experiments. The β(i/Pa) between 233Pa and these nuclides at different pressure were also calculated by using the γ-activity of relevant nuclides in FLiBeZr salt before distillation and on nickel foil after distillation, listed in Table 3. Since 233Pa, 141Ce, 140Ba, 95Zr, and 103Ru are not volatile at normal pressure, the β values between them is basically 1. But the evaporation rate of 95Nb reaches 18%/h, and β(Nb/Pa) is 0.002, indicating that the separation of 233Pa and 95Nb can be achieved at normal pressure. With the decrease of pressure, the β values between 233Pa and the non-volatile fission products, such as 141Ce, 140Ba and 103Ru, increase sharply, reaching the highest values of 75, 296 and 26 at 8 Pa, respectively. Since 95Zr shows obvious volatility at 200 Pa, the maximum separation factor β(Zr/Pa) (343) is observed at 500 Pa.
![]() | ||
Fig. 9 The γ-activity of each element in the remaining FLiBeZr salt, at 850 °C, as a function of pressure. |
β(Ce/Pa) | β(Ba/Pa) | β(Ru/Pa) | β(Zr/Pa) | β(Nb/Pa) | |
---|---|---|---|---|---|
8 Pa | 75 | 296 | 26 | 6 | 2 |
200 Pa | 57 | 91 | 9 | 38 | 1 |
500 Pa | 39 | 43 | 10 | 343 | 2 |
103 Pa | 3 | 9 | 2 | 10 | 0.18 |
104 Pa | 10 | 17 | 3 | 78 | 0.33 |
Normal pressure | 1 | 1 | 1 | 1 | 0.002 |
Understanding the separation behavior between 233Pa and the critical fission products is an important step towards the recovery and the purification of 233Pa. The experimental results suggest that the difference in the volatility between 233Pa5+ and these fission product nuclides increases with temperature, and lower pressure is more conducive to the separation of 233Pa and the non-volatile fission products (141Ce, 140Ba and 103Ru). In contrast, 95Nb can be well separated from 233Pa at normal pressure. The results in this study would be useful and important for the understanding of the physicochemical property of 233Pa in the molten salt and for the design of a process for 233Pa separation from the TMSR fuel.
This journal is © The Royal Society of Chemistry 2022 |