Democratic People’s Republic of Korea (DPRK) has produced weapon-grade plutonium in a graphite-moderated experimental reactor at the Yongbyon nuclear facilities. The amount of plutonium produced can be estimated using the Graphite Isotope Ratio Method (GIRM), even without considering specific operational histories. However, the result depends to some degree on the operational cycle length. Moreover, an optimal cycle length can maximize the number of nuclear weapons made from the plutonium produced. For conservatism, it should be assumed that the target reactor was operated with an optimal cycle length. This study investigated the optimal cycle length using which the Calder Hall MAGNOX reactor can achieve the maximum annual production of nuclear weapons. The results show that lower enrichment fuel produced a greater number of critical plutonium spheres with a shorter optimal cycle length. Specifically, depleted uranium (0.69wt%) produced 5.561 critical plutonium spheres annually with optimal cycle lengths of 251 effective full power days. This research is crucial for understanding DPRK’s potential for nuclear weapon production and highlights the importance of reactor operational strategy in maximizing the production of weapons-grade plutonium in MAGNOX reactors.

For the safety assessment of the high-level radioactive waste (HLRW) disposal, the thermodynamic data such as solubility products, formation constants of complexes, redox equilibrium constants of radionuclides, and their reaction enthalpy and entropy are required. In order to recommend and summarize the reliable data, thermodynamic databases (TDB) have been persistently developed through the OECD-NEA TDB projects and an updated TDB of actinides has been recently published in 2020. To date, reliable data for Pu reactions are scarce due to the possibility of coexistence of four different oxidation states, Pu(III-VI) by redox equilibria in solutions. To determine the thermodynamic data for the reaction of each Pu oxidation state, it is necessary to precisely control the oxidation state and quantitatively analyze all reactants, products and bi-products by using highly sensitive speciation techniques. Since 2004, the nuclear chemistry research team in KAERI has been focused on developing techniques for the sensitive chemical speciation by using laser-based spectroscopy and determining thermodynamic data of actinides such as U, Pu, Am. In this paper, chemical speciation and thermodynamic studies on Pu in KAERI are reviewed. A combination of a commercial spectrophotometer and a capillary cell was adopted for a sensitive chemical speciation of Pu(III-VI) in solutions. A sensitive detection of trace amount of Pu colloids was carried out with the laser-induced breakdown detection (LIBD) system. Pu(VI) complexation with hydroxide or carbonate ions were investigated under strong oxidation conditions controlled with hypochlorite (NaOCl). The solubility product of Pu(OH)3(am) and formation constant of Pu(III)-OH speices were determined by a combination of wet-chemistry experiments and several analysis methods of spectrophotometry, LIBD, radiometry under a strong reducing condition controlled by electrochemistry. More recently, we reported the reaction enthalpy and entropy data for the formation of Pu(OH)2+ and the dissolution of Pu(OH)3(am). A preliminary data for reaction between Pu(III) and organic matter will be presented.

Radionuclides can be leached into groundwater or soil over a long period of time due to unexpected situations even after being permanently disposed of in a repository. Therefore, it is necessary to investigate the mobility of radionuclides for the safety assessment of radioactive waste disposal. In this study, the effects of organic complexing agents such as ethylenediaminetetraacetic acid (EDTA) and isosaccharinic acid (ISA) on the sorption behavior of 239Pu and 99Tc over cementitious (concrete and grout) and natural rock samples (granite and sedimentary rock) were investigated in batch sorption experiments. For characterization of rock samples, XRD, XRF, FT-IR, FE-SEM, BET, and Zeta-potential analyses were performed. For the evaluation of mobility, the distribution coefficient (Kd) was selected and compared. The adsorption experiment was carried out at two pHs (7 and 13), a temperature of 20°C, and a range of organic complexing agents concentrations (10-7~10-2 M and 10- 5~10-2 M for 239Pu and 99Tc, respectively). The radionuclides concentrations in adsorption samples were analyzed using ICP-MS. The Kd values for 239Pu in all rock samples reduced significantly due to the presence of EDTA, even at low concentrations such as 10-5 M. In the case of ISA, the limiting noeffect concentration was much higher than that of EDTA. On the other hand, 99Tc showed relatively lower Kd values than 239Pu, and the sorption behavior of 99Tc was almost unaffected by the organic complexing agents for all rock samples. Therefore, it is possible to assume that the increased mobility of radionuclides, especially, 239Pu, in groundwater caused by the lowering of sorption at even low concentrations of organic complexing agents may result in the transport of radionuclides to the nearand far-field location of the repository.

Graphite Isotope Ratio Method (GIRM) can be used to estimate plutonium production in a graphite-moderated reactor. This study presents verification results for the GIRM combined with a 3-D polynomial regression function to estimate cumulative plutonium production in a graphite-moderated reactor. Using the 3-D Monte-Carlo method, verification was done by comparing the cumulative plutonium production with the GIRM. The GIRM can estimate plutonium production for specific sampling points using a function that is based on an isotope ratio of impurity elements. In this study, the 10B/11B isotope ratio was chosen and calculated for sampling points. Then, 3-D polynomial regression was used to derive a function that represents a whole core cumulative plutonium production map. To verify the accuracy of the GIRM with polynomial regression, the reference value of plutonium production was calculated using a Monte-Carlo code, MCS, up to 4250 days of depletion. Moreover, the amount of plutonium produced in certain axial layers and fuel pins at 1250, 2250, and 3250 days of depletion was obtained and used for additional verification. As a result, the difference in the total cumulative plutonium production based on the MCS and GIRM results was found below 3.1% with regard to the root mean square (RMS) error.

Electrochemical reduction has previously been reported for uranium oxide and mixed oxide nuclear fuel (uranium oxide, plutonium oxide). The laboratory scale electrochemical reduction of plutonium oxide powder is demonstrated in CaCl2- 1wt%CaO. The plutonium oxide contained within a permeable steel basket cathode is sacrificed during the process. A graphite anode is also employed during the reduction, leading to a significant contamination of the product.