Understanding the physical and chemical properties of materials arising from nuclear meltdowns, such as the Chernobyl and Fukushima accidents, is critical to supporting decommissioning operations and reducing the hazard to personnel and the environment surrounding the stricken reactors. Relatively few samples of meltdown materials are available for study, and their analysis is made challenging due to the radiation hazard associated with handling them. In this study, small-scale batches of low radioactivity (i.e., containing depleted uranium only) simulants for Chernobyl lava-like fuel-containing materials (LFCMs) have been prepared, and were found to closely approximate the microstructure and mineralogy of real LFCM. The addition of excess of ZrO2 to the composition resulted in the first successful synthesis of high uranium–zircon (chernobylite) by crystallisation from a glass melt. Use of these simulant materials allowed further analysis of the thermal characteristics of LFCM and the corrosion kinetics, giving results that are in good agreement with the limited available literature on real samples. It should, therefore, be possible to use these new simulant materials to support decommissioning operations of nuclear reactors post-accident.
On 26th of April 1986, Reactor 4 of the Chernobyl nuclear power plant underwent a catastrophic failure whilst undergoing an experimental power failure test. The reactor experienced uncontrolled fission and water flashed into steam causing an explosion, which exposed the reactor to the atmosphere and caused ignition of the graphite core. It took several days to eventually quell the fire, in which time, radioactive particles were emitted into the surrounding area and the atmosphere, to be spread across the region (now Ukraine, Belarus and Russia) and parts of Europe. This event, classified as Level 7 on the International Nuclear Event Scale (INES), was arguably the most serious nuclear incident to affect the world to date; it is known to have caused 31 direct deaths and a mass evacuation from a 30-km exclusion zone surrounding the reactor, that remains in place today.
During the meltdown of the reactor core, temperatures reached in excess of 1600 °C, which caused the uranium nuclear fuel to melt with the zirconium cladding.1,2 This molten material interacted with structural reactor building materials, including steel, concrete, serpentine and sand, forming ~100 tons of a glass-like lava that was transported under its own weight to sub-reactor rooms, solidifying in large masses, such as the widely reported “elephants foot”.1,3,4,5 Known as lava-like fuel-containing materials (LFCM), these highly crystalline, radioactive, glass-like slags, were found in two main forms, known as Brown and Black lavas.1 Crystalline phases observed in both types of LFCM include non-stoichiometric UO2 and ZrO2 from fuel and cladding materials, a U–Zr–O mixed oxide phase and high uranium–zircon (Zr1-xUx)SiO4, referred to as “chernobylite”.1,6,7,8,9 The glassy material in which these crystalline phases reside is a Mg-bearing (from serpentine minerals used in the reactor construction) Ca-aluminosilicate glass,1,6 although the actinide and minor fission product content of the glass is not well known. The main differences between Brown and Black lavas are the extent of crystallisation (greater in the Brown LFCM), the presence of a significant proportion of Fe-bearing phases (Brown LFCM only) and the uranium content (higher in the Brown LFCM). Owing to the heterogeneous nature of LFCM, bulk analysis has yielded a range of compositions, as shown in Supplementary Table 1.
While analysis of samples taken from Chernobyl LFCM was performed over 20 years ago,1,2,3,4,5,6,7,10,11,12,13,14,15,16 the highly radioactive nature of the materials limited the types of characterisation performed. Samples of the material are limited due to the difficulties and dangers associated with their collection (unstable building, high radiation levels), and only a few specimens of the lava that were sampled from within the reactor building have been studied. Despite recent studies,9,17,18 little is known about the condition of Chernobyl LFCM, especially now, 33 years after the accident. To overcome this lack of information, past attempts to simulate low-activity LFCMs (i.e., containing no fission products, only depleted uranium) have been made to help understand the conditions within the reactor during the accident, however, this work was unable to accurately approximate the microstructure, morphology and mineralogy of LFCM.19,20,21,22
One important aspect of LFCM behaviour that has not yet been investigated in detail is its corrosion behaviour within the reactor building. It is known that, due to the condensation of water inside the roof of the original Chernobyl sarcophagus (as a result of the temperature differential within and outside the structure), and the presence of holes in the sarcophagus roof, a significant proportion of water has dripped onto the LFCM causing it to corrode.16,23 This is apparent from the presence of yellow secondary alteration products formed on the surface of LFCM, known to include paulscherrerite (UO2(OH)2); studtite (UO4·4H2O); UO3·2H2O (epiianthinite); rutherfordine (UO2·CO3); schoepite ((UO2)8O2(OH)12·12H2O), Na4(UO2)(CO3)3 and the sodium carbonate phases Na3H(CO3)2·2H2O and Na2CO3·H2O.1,18,24,25 These phases have potential to generate significant amounts of radioactive, uranium-bearing dust when the humidity within the sarcophagus falls below 85%.23,26,27
Understanding the corrosion behaviour of LFCM, and developing a detailed evaluation of the kinetics and mechanisms of dissolution, are vital to support ongoing decommissioning efforts—both at Chernobyl and also at the Fukushima Daiichi Nuclear Power Plant, where LFCM-type materials are thought to have formed, which largely remain submerged in water used to cool the melted core. As such, in this study, we present the results of an investigation to synthesise low radioactivity, accurate simulant LFCMs and perform a preliminary evaluation of their corrosion behaviour.
Lava-like fuel-containing material microstructure and phase analysis
Analysis of Brown and Black LFCMs revealed a microstructure and mineralogy consistent with real Chernobyl LFCM materials, e.g., ref. 1 A glass-like material containing crystallites was confirmed for both materials by XRD (Fig. 1), with a region of diffuse scattering present between 15° < 2θ < 35° and Bragg reflections indexed as: UO2 [PDF 71–0258]; monoclinic ZrO2 [PDF 78–1807]; cubic ZrO2 [PDF 81–1550]; ZrSiO4 [PDF 72–0402] and albite (NaAlSi3O8) [PDF 41–1480]. The expanded unit-cell parameter of the cubic ZrO2 phase, a = 5.150(4) Å, compared with the reference data, a = 5.135(9) Å, is consistent with the formation of cubic (Zr1-xUx)O2. The reflections indexed as ZrSiO4 appeared to be more intense in the Black LFCM. The presence of these phases was confirmed by SEM/EDS analysis of each material, as shown in Fig. 2 and Supplementary Fig. 1. Phases containing Zr and U (i.e. (Zr1-xUx)O2) had a cubo-octahedral, fused, or dendritic morphology, consistent with textures observed in real LFCM.1,11,17 Furthermore, spherical inclusions containing Fe, Cr, Ni and Mo were observed, arising from the addition of stainless steel to the samples prior to thermal treatment (Supplementary Fig. 1).
Previous studies that aimed to simulate LFCM were unable to promote the formation of U-rich zircon, often referred to as chernobylite [(Zr1−xUx)SiO4], which is present in real LFCM.19,20,21 Since most of the Zr present in the LFCM partitions into crystalline phases, and the reported Zr concentrations of real LFCM (Supplementary Table 1) are averaged electron probe microanalysis or EDS measurements across the whole sample (including lower Zr-content glass), it is possible that previous attempts to force crystallisation of chernobylite were unsuccessful due to an under-estimation of the Zr content. In this study, through the addition of excess ZrO2 it was possible to promote crystallisation of high uranium–zircon, as shown in Fig. 3. The U-containing zircon had a characteristic bi-pyramidal shape with distinct growth zonation; EDS data averaged over several U-bearing zircon crystallites gave an approximate composition of (Zr0.95U0.05)SiO4 for the Black LFCM and approximately (Zr0.90U0.10)SiO4 for Brown LFCM. The incorporation of ~5 wt% and 10 wt% U in zircon from simulated Black and Brown lavas is in good agreement with literature values (5.6 wt% and 11.3 wt%, respectively).17 At the centre of several of the zircon crystals, small Zr-bearing inclusions were observed (e.g., Fig. 3c). Such inclusions were observed in real Brown LFCM, thought to be relict ZrO2 inclusions from the crystallisation of Zr–U–O phases into high uranium–zircon.1,7 The presence of monoclinic ZrO2, in the form of baddeleyite, is rare in the previous analysis of real LFCM;1,7 its relative abundance in this study (Fig. 1; Supplementary Fig. 1) may be due to the addition of more ZrO2 than was required to form the zircon phase. The presence of albite (NaAlSi3O8), as large dendrites within the glassy matrix, is in accordance with previous observations of pyroxene-like minerals with a composition of (Ca0.08Fe0.02Cr0.02Zr0.02)Al0.18Mg1.86Si1.82O5.97, in particles of real LFCM.17
Thermal analysis of simulant LFCM, as determined by DTA, gave values for Tg of 722 ± 5 °C and 732 ± 5 °C for the Brown and Black compositions, respectively (Table 1; Supplementary Fig. 2). This is somewhat lower than previously estimated values for LFCM.28 Two distinct crystallisation peaks were observed in both materials, the first occurring between 1006 ± 5 °C and 1020 ± 5 °C, and the second at ~1245 ± 5 °C. By application of Ti-thermometry, Poml et al.9 estimated the temperature of high-uranium–zircon crystallisation in LFCM to be ~1250 °C, suggesting that the Tc of ~1245 ± 5 °C observed in this work may be related with crystallisation of zircon. This is consistent with zircon crystallisation in geological formations, where zircon is known to form at temperatures between 1300 and 1600 °C.29,30 The lower crystallisation temperature should therefore be associated with the formation of Zr–U–O-containing phases. The samples became liquid at temperatures of >1213 ± 5 °C, and heating to 1280 ± 5 °C and 1359 ± 5 °C was required to obtain a crystal-free melt for simulant Brown and Black LFCM, respectively. This is somewhat lower than the estimations of the melt temperature of LFCM within the Chernobyl reactor, which range between 1400 °C and 1550 °C,2,17 and may be explained by the compositional heterogeneity of LFCM. Other than the exclusion of fission products, the primary difference in composition between the real LFCM and the simulant materials analysed here is the source of Zr. During the accident, it is thought that the first portion of liquid phases formed at ~1400 °C as a result of melting of U and Zr into a U,Zr alloy,2 after which the melt contacted construction materials forming LFCM; in this study, this stage of melting is not observed, due to the addition of Zr in oxide form. Furthermore, during the accident, there was a long period of melting prior to breakthrough of the lava to the under-reactor compartments, which may differ from the double-stage (but single composition) melting process used to generate the simulant LFCM. Thermogravimetric data obtained simultaneously with thermal analysis showed no appreciable mass change upon heating.
Analysis of the U LIII edge XANES spectra acquired from bulk simulant Brown and Black LFCM samples and oxidation state standards are shown in Fig. 4. The position of the absorption edge (E0), and the similarity in the post-edge features with those of UO2, suggest that the average uranium oxidation state in both lava samples is close to four. This is confirmed by comparison of the extracted edge position of the lava samples to those of known oxidation state (Fig. 4; Supplementary Table 2). The mean U oxidation state was determined to be 4.1 ± 0.2 for the Black LFCM and 4.3 ± 0.2 for the Brown LFCM, which is in agreement with previous analysis of real LFCM particles by XANES.17
Lava-like fuel-containing material corrosion behaviour
The extent of corrosion of each of the LFCM samples in UHQ water at 50 °C was found to be comparable, as shown in Fig. 5 and Supplementary Fig. 3. For both samples, the pH averaged at approximately pH 5 throughout the experiment (Supplementary Fig. 3), which is ~1 pH unit lower than in the corresponding blank solutions. The normalised mass loss of Na (NLNa), typically used as a tracer in the dissolution of glass materials, of the Black LFCM was greater than the Brown LFCM (Fig. 5). The normalised mass loss of U (NLU) was also higher in the Black LFCM (Fig. 5c), consistent with the marginally higher oxidation state of uranium in this material. There were, however, clear differences in the trend of NLU for each of the samples after 1 day of corrosion, with the Black LFCM NLU reaching a plateau, while that of the Brown LFCM continued to increase throughout the experiment. This indicates that U may be incorporated in secondary phases within the Black LFCM to a greater extent than the Brown LFCM. Given that there was a plateau in NLSi for the Black LFCM at the same time point as the plateau in NLU (not observed for the Brown LFCM), and a Si-rich layer was observed to form on the surface of LFCM particles (Fig. 6; Supplementary Figs. 5, 6), an alternative explanation could be that further corrosion of the Black LFCM was passivated by a silica gel layer, as commonly observed for silicate glass corrosion. Zirconium was highly resistant to leaching in both materials.
The normalised mass loss of all elements from the Black LFCM (except Na) reached a plateau, but those of the Brown LFCM did not. A plateau is indicative of a change in the degree of saturation of the solution with respect to these elements; such saturation phenomena are related to the formation of secondary phases on the surface of the material. Geochemical modelling of the elemental solution concentrations at 28 days predicted that smectite clay (beidellite with a general formula of (Ca,Na,K,Mg0.5)xAl4+xSi8-xO20(OH)4.nH2O), the phyllosilicate, kaolinite (Al2Si2O5(OH)4) and haematite (Fe2O3) were saturated in solution for both LFCM materials, while the uranium-bearing phase, soddyite [(UO2)2SiO4·2H2O] was predicted to be in equilibrium (Supplementary Table 3). XRD analysis of the LFCM samples after 28 days of corrosion in UHQ water at 50 °C (Supplementary Fig. 4) showed no change in the crystalline phase assemblage when compared with the pre-leached samples, suggesting that any secondary phases formed were non-crystalline or present only in small (<3 wt%) quantities. Analysis of samples subject to corrosion under the conditions utilised in this study (UHQ water, 50 °C or 200 °C) gave evidence for the formation of Na-, Si- and Al-bearing alteration products for both LFCM materials (Fig. 6; Supplementary Figs. 5, 6), consistent with geochemical modelling predictions. The alteration layer was found to range from ~1 µm to 10 µm in thickness for both LFCM compositions. No uranium-bearing alteration products were observed in either type of corrosion experiment.
The data presented in this study confirm that the synthesis of realistic low-activity (i.e., containing depleted uranium as the only radioactive isotope) simulants for Chernobyl LFCM is achievable at a small, batch scale, in the laboratory. The microstructure and mineralogy of the resulting materials were the same as found in real Brown and Black LFCMs, containing the same range of phases, including the high uranium–zircon, chernobylite, which previous studies of simulants have been unable to form.19,20,21 It was previously proven possible to synthesise this phase through high-temperature heat treatment of U–Zr–Si–O gels,31 however, to our knowledge, this study is the first to successfully crystallise this phase from a glass melt. The LFCM simulants synthesised here additionally contained Zr–U–O phases, UO2, ZrO2 and Fe-, Ni-, Cr- and Mo-bearing metallic inclusions, also found in real LFCM. The identification of small inclusions of ZrO2 at the centre of chernobylite grains confirms previous hypotheses that this phase is the product of reaction between Zr–U–O and the silicate melt.1,7
One advantage of being able to create low-activity simulants is the ability to perform measurements that are otherwise difficult to conduct within a hot-cell environment. In this study, we have been able to further elucidate the thermal characteristics of LFCM, determining the glass-phase transition, liquidus temperature and the crystallisation temperatures of zircon and Zr–U–O-containing phases. The latter values are consistent with those measured for natural minerals, and the former may differ slightly from real LFCM due to the use of ZrO2 as a precursor rather than zircaloy cladding. The preparation of low-activity samples is also advantageous for analysis at user facilities, for example, synchrotron beamlines. This study confirmed, by XANES, that the oxidation state of uranium in the simulant samples, which was initially added to the batch as UO3, was U(IV), as observed in real LFCM.17 In the absence of zircaloy cladding, the melting of which is thought to have partially reduced UO2 during the accident, our study required the application of a reducing atmosphere during synthesis to create the desired oxidation state.
There is a further benefit of being able to synthesise small (25 g) batches of realistic simulant LFCM. The use of large-scale demonstrators, where experiments are conducted to understand the interaction of molten fuel and cladding with structural building materials, such as the VULCANO facility in France,32 are expensive and hazardous to operate. Having a reliable, small-scale synthesis procedure may be helpful in screening compositions and experimental matrices so that the use of the large-scale demonstrator can be reduced to only those most important experiments; this may prove highly useful in the ongoing assessment of molten corium–concrete interaction (MCCI) products at the Fukushima Daiichi Nuclear Power Plant in Japan, ahead of fuel retrieval operations.
The corrosion behaviour of LFCM is of concern with regards to decommissioning of the Chernobyl reactor. This is due to the large amounts of radioactive dust generated from the secondary alteration products when the humidity within the sarcophagus falls; the removal of water from the LFCM surfaces can significantly intensify UO2 oxidation and dehydrate hydrous uranium-containing oxidation products, forming dust.27 Some estimates suggest that the maximum rate of dust formation in the last 33 years was on the order of 1–10 kg y−1.27 Several studies have been performed to elucidate the corrosion rate of LFCM and to ascertain the nature of the secondary alteration phases that are formed during corrosion. Many of these have been concerned specifically with the leaching rate of various fission products (e.g., 106Ru, 137Cs, etc.)12,16,18, however, relatively few have focused on the corrosion rate of other elements in the LFCM, including uranium—the source of the radioactive dust hazard. Furthermore, the release of uranium and other radionuclides to the ground surrounding and below the reactor, may have resulted in the generation of a significant quantity of contaminated soil that will require eventual remediation, in addition to the contamination of groundwater.
The only reported corrosion rate of uranium from real LFCM pertains to monoliths of Brown material.12 A dissolution rate of 1.8 × 10−3 g m−2 d−1 was calculated by a simple extrapolation of the normalised mass loss over a 22-day period, with samples leached in a solution of 0.4 mol L−1 NaCl (initial pH 6.5), at room temperature.12 Using the same method (between 3 and 28 days, to avoid the possible influence of dissolved fines on the corrosion rate) for simulant Brown LFCM, we obtain a uranium corrosion rate of 1.05 ± 0.06 × 10−4 g m−2 d−1 (Supplementary Fig. 7). This is somewhat lower than the real LFCM. Similarly, the corrosion rate of uranium for simulant Black LFCM was found to be 3.42 ± 0.20 × 10−5 g m−2 d−1. Other studies of fission product (e.g., Pu, Am, Cs and Eu) leaching from real LFCM have shown no real difference in the corrosion rate between the two compositions.18 These crudely obtained uranium release rates should be treated with caution and no extrapolations to longer durations should be made, however, it is clear that the values obtained are approximately one order of magnitude greater than those for uranium leached from spent nuclear fuel under oxidative conditions,33 but are comparable with those for U3O8-doped borosilicate glass.34 The normalised mass loss values of Na and Si from the simulant LFCM compositions are also of the same order of magnitude as borosilicate high-level nuclear waste glass compositions such as MW2535 or the non-radioactive simplified surrogate of French high-level waste glass, the International Simple Glass.36 The presence of a silicate alteration layer observed after corrosion (Supplementary Fig. 6) suggests that the mechanism of corrosion of LFCMs is, at least in part, similar to that of silicate glasses.
Comparing the corrosion of simulant LFCM with available data in the literature for real LFCM, the pH of the solutions of both were observed to decrease by 1–2 pH units, relative to the blank, over the 28-day duration of leaching. This is somewhat unusual behaviour for alkali–aluminosilicate glasses (where the release of alkali elements to solution from the corroding glass and subsequent complexation with alkali elements raises the pH to alkaline values), and points to the formation of pH-influencing secondary alteration phases, such as those that incorporate hydroxide ions (removal of which may lower pH), or those that complex with carbonate ions. Within the Chernobyl sarcophagus, the carbonate concentration was found to vary between 370–2900 mg L−1, and uranyl carbonate mineral phases were observed to form,1,16,18,24,25 which may effectively lower the pH. However, the present experiments contained significantly less carbonate (only that in equilibrium with CO2 in the air), and such phases were neither observed, nor predicted by geochemical modelling. It is possible that colloidal complexes containing carbonate may have formed, which were not detectable using the analytical techniques applied here, however, it seems that the removal of OH− ions into secondary phases is the most plausible explanation for the observed pH decrease in this study.
Further work is required to fully understand, and quantify, the corrosion behaviour of LFCM simulants; in particular, the corrosion kinetics of the simulant materials were somewhat slower than real LFCM (albeit comparing with only one study, using a simplified corrosion rate calculation) and uranium-bearing secondary precipitates, as seen on real LFCM, were apparently absent from the simulant samples. In this work, three key factors may contribute to these differences: (1) the pH may be too low to promote the formation of Na-uranyl carbonate phases—the pH of the water within the sarcophagus16 was measured as pH 8.5–10, higher than in this study; (2) as mentioned above, the carbonate concentration within these experiments is significantly lower than within the sarcophagus and (3) most significantly, the simulant samples do not contain any alpha-emitting isotopes. Radiolysis of water by alpha particles is known to promote the formation of hydrogen peroxide (in addition to other radical species), which is known to have a significant influence on the oxidative dissolution of UO2, significantly enhancing the corrosion rate.37 Furthermore, studtite (UO4·4H2O), which has been observed on real LFCM samples, is a peroxide-containing mineral that forms by incorporating hydrogen peroxide created by alpha-radiolysis, thus requires radiation for its formation.38 Further studies are currently being performed to explore these factors, and to develop further understanding of the corrosion, and dust generation capacity of LFCMs and other fuel debris.
A survey of the literature was used to ascertain the composition of Black and Brown lavas from Chernobyl; an average of all analysed samples in the literature (Supplementary Table 1) was used to produce the batched compositions shown in Table 2. When compared with the literature values, excess ZrO2 was added to the batch. Stoichiometric amounts of the reagents for each of the elements present within the LFCM samples were used (SiO2 (Lochaline Quartz Sand 99.6%), CaCO3 (Fisher 98%), ZrO2 (Aldrich 99%), Na2CO3 (Alfa Aesar 98%), BaCO3 (Alfa Aesar 99%), Al(OH)3 (Acros 95%), Mn2O3 (Aldrich 99%), Fe/Cr18/Ni10/Mo3 (Goodfellow), Mg(OH)2 (Sigma-Aldrich 99.9%) and UO2 (BDH)). Batches were intimately mixed for at least 1 min. Thermal synthesis of the loose batched powders was performed in alumina boat crucibles under a reducing atmosphere (H2(5%)–N2(95%) gas) at 1500 °C for 4 h and subsequently 720 °C for 72 h. The ramp rate was 3 °C min−1 at the beginning and end of the synthesis, and 1 °C min−1 between 1500 °C and 720 °C steps. The second heating step was necessary to prevent shattering of the alumina crucible and to facilitate crystallite growth. The composition of the resulting materials was determined by ICP-OES (Spectro Ciros Vision) after digestion in aqua regia, as shown in Table 2. The elevated concentration of Al2O3 is due to corrosion of the alumina crucible during thermal treatment.
The crystalline-phase assemblage was determined by powder X-ray diffraction (XRD) using a Bruker D2 Phaser X-ray diffractometer in reflectance mode over the range 10° ≤ 2θ ≤ 70° with Cu Kα radiation (30 kV, 10 mA). Representative cross-sections were prepared by mounting monolith samples in resin and polishing to a 1 µm finish using successive SiC grit papers and diamond suspension polishing solution. The morphology of the crystalline-phase assemblage was imaged using a Hitachi TM3030 Scanning Electron Microscope (SEM) with semi-quantitative analysis of mineral composition using a built-in Bruker XFlash 430 H Energy Dispersive X-ray Spectroscopy (EDS) system. Thermal characterisation of the LFCMs was performed using Differential Thermal Analysis (DTA) of representative powdered samples using a Netzsch TG 449 F3 simultaneous thermal analyser. The glass transition (Tg), crystallisation (Tc) and liquidus (Tl) temperatures were determined, with the annealing temperature of the samples taken to within 50 °C of the Tg observed. Helium pycnometry analysis gave densities of 3.054 ± 0.004 g cm−3 and 2.998 ± 0.003 g cm−3 for Brown and Black simulant LFCM, respectively.
X-ray absorption near edge spectroscopy (XANES) analysis of the U LIII edge was performed on Black and Brown lava samples, on beamline BL-27 at the Photon Factory synchrotron facility (Tsukuba, Japan),39 to evaluate the bulk uranium oxidation state. XANES spectra were collected between 16865 and 18265 eV with an accumulation time of 1 s step−1 and energy steps of 4 eV (16865–17115), 1 eV (17115–17665), 4 eV (17665–17965) and 1 eV (17965–18265). Multiple spectra were averaged to improve the signal-to-noise ratio, and a fluorescence spectrum of a Zr foil was acquired simultaneously with each sample to ensure accurate energy calibration. Three crystalline standards were also measured using the same conditions. All samples were prepared by mixing finely ground powders with PEG and pressing into cylindrical disks of 13 mm diameter. The PEG to powder ratio was optimised to give a suitable edge step over the U LIII absorption edge. Data reduction and analysis performed using the Athena software package.40 Linear regression of the U LIII edge energy position (defined as the energy where the edge step is equal to 0.5) with respect to standards of known oxidation state (UO2, Yb0.5U0.5Ti2O6 and CaUO4) confirmed the uranium oxidation state within the sample.41
Two ASTM standard methods were used as the basis of corrosion experiments. Firstly, a modified ASTM Product Consistency Test B (PCT-B) protocol (ASTM C1205–14),42 utilising a surface area to volume ratio of 120 m−1, was performed to give insight to dissolution kinetics. LFCM materials were crushed and sieved to a powder of 75 to 150 µm in size. Washed powders were placed in Teflon vessels, and 10 mL of UHQ water (in equilibrium with CO2 in the air) was added. Vessels were tightened and placed inside an oven at 50 ± 1 °C for 28 days. At several time intervals, vessels were sacrificed, and aliquots of solution were taken for elemental analysis using inductively coupled plasma-mass spectroscopy (Agilent 4500) and the pH was measured. Experiments were performed in triplicate, with duplicate blanks and all errors reported refer to the standard deviation of triplicate measurements.
The normalised mass loss of elements within the LFCMs was determined according the following equation:
where NLi is the normalised mass loss (g m−2) of element i, Ci is the elementary concentration (g cm−3) in the solution, fi is the mass fraction of element i, and SA/V is the ratio (m−1) between the surface area of the glass (m2) and the volume of solution used (m3). The normalised dissolution rate, RLi (g m−2 d−1), is defined as the time derivative of the normalised mass loss, and was calculated using the normalised mass loss obtained from triplicate samples between 3 and 28 days, according to Eq. (2). The errors represent the uncertainty in the determination of the linear chi-square fit gradient, taking into account triplicate NLi values.
Analysis of the experimental data from the 28-day solutions was performed using the geochemical speciation software PHREEQC, using the Lawrence Livermore National Laboratory thermodynamic database, LLNL-TDB. Data used in the LLNL-TDB are valid for temperatures ranging from 0 to 300 °C. The corroded samples were further characterised by XRD.
The second method of corrosion analysis was Vapour Hydration Testing (VHT), performed by using a modified ASTM C1663,43 to develop insight into the secondary phases formed on LFCMs during corrosion. Monolith coupons, 10 × 5 × 1 mm in size, were polished to an optical finish with successive SiC grit papers. Samples were suspended within stainless steel pressure vessels using stainless steel wire, such that all surfaces of the coupons were in contact with water vapour during the experiment. Vessels were tightly sealed and placed within a temperature controlled oven at 200 °C for 28 days. At the end of the experiment, samples were mounted in cross section in epoxy resin for SEM/EDS analysis, as described above.
The data that support the findings of this study are available from the corresponding author upon reasonable request.
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The authors wish to acknowledge funding for this research from EPSRC through grant agreement numbers EP/L015390/1, EP/R01924X/1, EP/M026566/1 and EP/P013600/1 and the European Commission Horizon 2020 Research and Training Programme, Theramin, of the European Atomic Energy Community (EURATOM), under grant agreement number 755480. C.L.C. is grateful to EPSRC for the award of an Early Career Research Fellowship (EP/N017374/1), and N.C.H. is grateful for support from the University of Sheffield Global Challenges Research Fund. This research was performed in part at the MIDAS Facility, at the University of Sheffield, established with support from the Department of Energy and Climate Change. Collection of the XAS data was performed under the approval of the Photon Factory Advisory Committee (Proposal No. 2017G187); the support of Yoshihiro Okamoto (JAEA) and Noriko Usami (KEK) during the experiment is gratefully acknowledged. We thank Dr. Boris Burakov and Dr. Sergei Shiryaev for useful discussions throughout these experiments, the International Atomic Energy Agency for financial support to attend meetings on the Coordinated Research Project on the Management of Severely Damaged Spent Fuel and Corium, and also Julia Wallenius and Alexander and Elina Corkhill for assistance with Russian to English translation.
The authors declare no competing interests.
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Barlow, S.T., Bailey, D.J., Fisher, A.J. et al. Synthesis, characterisation and corrosion behaviour of simulant Chernobyl nuclear meltdown materials. npj Mater Degrad 4, 3 (2020). https://doi.org/10.1038/s41529-020-0108-z