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. 2023 Jun 5;62(24):9350–9359. doi: 10.1021/acs.inorgchem.3c00251

Synthesis, Characterization, and Stability of Two Americium Vanadates, AmVO3 and AmVO4

Jean-François Vigier †,*, Thierry Wiss , Natalia Palina , Tonya Vitova , Jean-Yves Colle , Daniel Bouëxière , Daniel Freis , Rudy J M Konings , Karin Popa †,*
PMCID: PMC10283022  PMID: 37277115

Abstract

graphic file with name ic3c00251_0010.jpg

In search for chemically stable americium compounds with high power densities for radioisotope sources for space applications, AmVO3 and AmVO4 were prepared by a solid-state reaction. We present here their crystal structure at room temperature solved by powder X-ray diffraction combined with Rietveld refinement. Their thermal and self-irradiation stabilities have been studied. The oxidation states of americium were confirmed by the Am M5 edge high-resolution X-ray absorption near-edge structure (HR-XANES) technique. Such ceramics are investigated as potential power sources for space applications like radioisotope thermoelectric generators, and they have to endure extreme conditions including vacuum, high or low temperatures, and internal irradiation. Thus, their stability under self-irradiation and heat treatment in inert and oxidizing atmospheres was tested and discussed relative to other compounds with a high content of americium.

Short abstract

AmVO3 and AmVO4 were prepared by a solid-state reaction and characterized in terms of crystal structure, americium and vanadium oxidation states, thermal behavior, and self-irradiation stability. With a fast amorphization behavior, large volume variation, and interchangeable structure as a function of the presence of the oxygen atmosphere and temperature, americium vanadates do not appear to be good candidates as Am forms for radioisotope power systems.

1. Introduction

The americium isotope 241Am is formed during storage of plutonium via β-decay of 241Pu with a half-life of 14.33 years. Due to 241Am accumulation in existing stocks of civil-separated plutonium in Europe, and its relatively high specific power of 0.114 W/g, 241Am has been proposed for use in radioisotope power systems (RPSs)1 and is under consideration by the European Space Agency (ESA) as an energy source for future European space missions.2 The requirements for a stable solid form are very diverse, ranging from storage on earth and operation in space to safe performance in case of accidents and post-accident scenarios. Our group studied several ceramic forms containing significant specific Am amounts,35 the present study being in line with the past efforts.

The synthesis and crystal structure of AmVO3 were reported for the first time by Keller and co-workers.6,7 In their work, AmVO4 was prepared by dissolving AmO2 and V2O3 as hydroxides, mixed, dried, and reacted at 1250 °C under an oxidizing atmosphere. The produced AmVO4 was subsequently reduced to obtain AmVO3. The authors proposed the crystal structure for the two compounds (perovskite-type for AmVO3 and zircon-like for AmVO4) and gave the lattice parameters.

According to the Inorganic Crystal Structure Database (ICSD), there are no compounds of americium and vanadium with a fully characterized crystal structure. We present here the complete crystal structure refinement of the two vanadates by Rietveld analysis at room temperature. Spectroscopic and microscopic studies were carried out to check the purity of the samples. The high-resolution X-ray absorption near-edge structure (HR-XANES) technique was applied at the Am M5 edge to characterize the Am oxidation states. The stability of AmVO3 and AmVO4 under self-irradiation and heat treatment in an inert and oxidizing atmosphere was tested and discussed relative to other americium-containing compounds.

2. Experimental Section

Caution: 241Am is a highly radioactive isotope (t1/2 = 432.8 years, specific activity of 126.8 GBq/g). All work presented in this paper were carried out in glove boxes in radiological laboratories licensed for handling actinides. When appropriate, shielding and remote handling tools were used to protect the workers in these experiments.

2.1. Sample Preparation

2.1.1. AmVO3

Stoichiometric amounts of 241AmO2 (158 mg of aged material containing about 7% 237Np as the decay product and 2% 239Pu) and V2O5 (48 mg, Merck, 99.95%) were mixed in an agate mortar and pressed into a pellet. The thermal treatment was performed for 10 h at 1250 °C under Ar/H2 (5%) with heating and cooling ramps of 200 °C/h.

2.1.2. AmVO4

A chip of 78 mg of the previous AmVO3 pellet was oxidized for 2 h up to 1000 °C under oxygen by using a Netzsch STA 449C thermogravimetric analysis instrument. Oxidation started at about 400 °C with a maximum oxidation rate at 450 °C, as discussed in the Materials Characterization section. This synthesis was done independently from the thermogravimetric analysis described below during in which higher temperatures were reached.

2.2. Thermogravimetric Analysis

The thermal behaviors of AmVO3 and AmVO4 were assessed under an argon/hydrogen and oxygen atmosphere, respectively (to preserve the oxidation state of the respective compounds) using a Netzsch STA 449C thermogravimetric analysis instrument. The temperature was controlled by a Pt-PtRh (10%) thermocouple. The measurements were conducted on pellet fragments (11–78 mg) up to 1500 °C in alumina crucibles, and the applied heating and cooling rates were 10 °C/min.

2.3. XRD

Room temperature XRD analyses were performed on about 10 mg of powdered material loaded in a bicomponent epoxy resin using a Bruker D8 Advance diffractometer (Cu Kα radiation, 40 kV, 40 mA) mounted in a Bragg–Brentano configuration. The diffractometer was equipped with a curved Ge(1,1,1) Kα1 monochromator, a ceramic copper tube, and a LinxEye position sensitive detector. The XRD patterns were recorded using a step size of 0.01° across the 10° ≤ 2θ ≤ 120° angular range. Structural analysis was performed by the Rietveld method using the Jana2006 software.8

Since all the crystallographic parameters could not be independently refined, some structural constrains were applied. For the atomic displacement parameter, isotropic displacement parameters Uiso were used, and the following equation has been considered:9

2.3. 1

The V–O distances were constrained to 2 Å for the perovskite structure AmVO310 and to 1.71 Å for the zircon structure AmVO4.11

2.4. Raman Spectroscopy

Raman spectroscopy measurements were performed on fragment of pellets (2–3 mg) at room temperature and ambient pressure on a polycrystalline specimen using a Horiba Jobin-Yvon T64000 spectrometer. For technical reasons, two lasers at different wavelengths were used; a 647 nm Kr+ laser and a 660 nm solid state laser excitation source. A 50× long focal objective was used to irradiate the sample and collect the back-scattered light. Great care was taken to avoid sample damage or laser-induced heating. Measurements were performed with few tenths of a milliwatt incident power.

2.5. Scanning Electron Microscopy

Images of the samples (fragment of pellets of 1–2 mg) were obtained in a Philips/FEI XL40 SEM operated at 25 kV, equipped with a SAMx energy-dispersive X-ray analysis system (EDX). This microscope (high-voltage unit, column, chamber, and turbomolecular pump) was placed inside a glovebox, while the components that are not getting in contact with the active materials (primary vacuum system, the water-cooling circuit, and the acquisition electronic) were outside.12

2.6. XANES and HR-XANES

For AmVO3 and AmVO4 compounds, the Am M5 HR-XANES spectroscopy technique was performed at the ACT station of the beamline for catalysis and actinide research (hereafter CAT-ACT beamline) of the KIT Light Source, Karlsruhe, Germany.13 Spectra acquisitions were done utilizing a Johann type X-ray emission spectrometer. The incident beam was monochromatized by a Si(111) double-crystal monochromator (DCM), focused to 500 × 500 μm, and subsequently narrowed down by slits onto the sample to a spot size of about 200 × 200 μm. The X-ray emission spectrometer consists of four Si(220) crystals with a 1 m bending radius and a single diode VITUS silicon drift detector (Ketek, Germany), which together with the sample were arranged in a Rowland circle geometry.13 AmO2 reference sample was used to calibrate Am M5 HR-XANES spectra. The main absorption maximum was set to 3890 eV for AmO2.14 The maxima of the WLs are located at AmCl63– (3888.4 eV), AmFe2 (3887.5 eV) reported elsewhere.15,16 Both Am M5 edge data cited above were measured in conventional fluorescence mode and were similar to AmVO3 and AmVO4 (3888.5 eV) recorded in this work. The slight divergence of the absorption maximum of AmO2 in the current work (3890 eV) from the data reported by Epifano et al.(17) (about 3891.5 eV) is a result of different experimental energy resolutions (for details cf. Discussion in the Supporting Information and Figure S5). The multi-position sample cell (containing <1 mg powdered material embedded in bicomponent glue) was placed into a double containment, where the inner compartment was sealed by 8 μm and the outer compartment by 13 μm Kapton foil. The HR-XANES spectra were measured with a step size of 0.1 eV from −10 to +25 eV from the white line (WL) of the respective edge and 0.5 eV in all other parts of the spectra. At least two spectra were averaged for each sample. The sample, crystals, and detector were enclosed in a box filled with helium to minimize intensity losses due to scattering and absorption of photons in air. Constant helium flow was maintained to keep the oxygen level below 0.1%.

Additionally, Am L3 edge and V K-edge XANES measurements were performed at the INE-Beamline18 of the KIT Light Source, Karlsruhe, Germany. The radiation protection measures were kept identical to those used at the ACT station.19 Two Ge(422) and two Si(111) crystals were mounted in the double-crystal monochromator (DCM) for Am L3 and V K edge measurements, respectively. The beam was focused on a ∼0.5 mm × 0.5 mm spot on the sample. Zr or V metal foils were used for energy calibration for the Am L3 edge or V K edge XANES, respectively. V2O3 (Sigma-Aldrich, 99.99%) and V2O5 (Merck, 99.95%) powders were mixed with cellulose and pressed into the pellets and used as references for V K edge XANES. The XANES spectra were measured in fluorescence mode with step sizes of 0.25 and 0.8 eV from −10 to +25 eV from the white line (WL) of the respective edges for the V K edge and Am L3 edge and 4 eV steps in the post-edge area of the spectra. At least two spectra were averaged for each sample. Measurements were performed in air, and no radiation damage was observed during the measurements.

2.7. α Self-Irradiation

Due to the high alpha activity of americium, the doses accumulated by the AmVO3 and AmVO4 at the time of different measurements must be considered. Daily doses of about 7.8 × 1015 and 7.4 × 1015 α/g were built up for AmVO3 and AmVO4, respectively. Only TGA and XRD techniques could be applied on freshly prepared material. The calculated doses of the materials at the time of the different measurements are summarized in Table 1. Between measurements, the samples were stored under the atmosphere of the glovebox where the samples were produced (nitrogen with up to 10,000 ppm oxygen).

Table 1. α Dose Accumulated in AmVO3 and AmVO4 at the Time of the Different Measurements, in α Decay Events per Gram of Material.

  AmVO3
AmVO4
  sample age, days cumulated dose, α/g sample age, days cumulated dose, α/g
XRD 1.6 1.2 × 1016 2.7 2.1 × 1016
132 1.0 × 1018 131 1.0 × 1018
212 1.6 × 1018 211 1.6 × 1018
TGA 3.4 2.7 × 1016 2.5 1.9 × 1016
Raman 451 3.5 × 1018 450 3.5 × 1018
890 6.8 × 1018 890 6.8 × 1018
SEM 660 5.1 × 1018 659 5.1 × 1018
Am L3 edge XANES, Am M5 edge HR-XANES 603 4.7 × 1018 607 4.7 × 1018
V XANES 726 5.6 × 1018 727 5.6 × 1018

3. Results and Discussion

3.1. Materials Characterization: Fresh Material

During the synthesis of AmVO4 by oxidation of an AmVO3 specimen, the DTA measurement (Figure S1) performed in oxygen indicated a single exothermic event reaching a maximum energy release at 450 °C with an associated weight gain of 4.5 wt %, which was attributed to the oxidation to the AmVO4 form (expected gain of 4.7 wt %).

Americium vanadate AmVO3 crystalizes in the perovskite Pbnm structure after sintering under an Ar/H2 atmosphere; meanwhile, after thermal treatment in oxidative conditions, the material converts into AmVO4 showing a zircon-like I41/amd structure (Figure 1 and Table 2). Residual NpO2 can be detected in quantifiable amounts, which indicates that this daughter element of 241Am does not fully integrate the two vanadate compounds and segregates (at least partially) into an oxide phase. The Np L3 edge XANES data are shown in Figure S4, supporting the above statement.

Figure 1.

Figure 1

XRD patterns, Rietveld refinement, and crystal structure of AmVO3 and AmVO4.

Table 2. Unit Cell Parameters and Results of the Rietveld Refinement for AmVO3 and AmVO4a.

formula unit AmVO3 AmVO4 AmVO4 (Keller et al.(7)) AmVO4 (Goubard et al.(20))
space group Pbnm I41/amd I41/amd I41/amd
space group number 62 141 141 141
a, Å 5.4445(3) 7.2938(2) 7.31(1) 7.311(2)
b, Å 5.5914(3) 7.2938(2) 7.31(1) 7.311(2)
c, Å 7.7556(4) 6.4284(2) 6.42(1) 6.422(2)
α, ° 90 90 90 90
β, ° 90 90 90 90
γ, ° 90 90 90 90
V, Å3 236.10(2) 341.992(10) 343 343.26
Z 4 4 4 4
M, g/mol 340.00 356.00 356.00 356.00
crystallographic density, g/cm3 9.565 6.9142 6.89 6.89
GOF 1.57 2.15    
RP 0.0106 0.0154    
Rwp 0.0150 0.0254    
Rexp 0.0068 0.0072    
a

Rp = Σ(i)[|yi(obs) – yi(calc)|]/Σ(i)[yi(obs)]; Rwp = {Σ(i)[wi(yi(obs) – yi(calc))2]/Σ(i)[wi × yi(obs)2]}1/2; GOF = Rp/Rexp; Rexp = {Σ(i)[wi × yi(obs)2]/(np)}1/2.

The crystal structures suggest that americium stays in the oxidation state III in the materials whatever the redox condition, while vanadium can have the oxidation state III or V, which results in ABO3 perovskite or ABO4 zircon structures, respectively. One can notice that during the oxidation process, the density of the material strongly decreases from 9.565 g/cm3 for the close-packed AmVO3 to 6.914 g/cm3 for the oxyanionic AmVO4, which indicates a volume increase of 45% during oxidation. The formation of a zircon-like structure for AmVO4 is in accordance with the works of Keller et al.(6,7) or of Goubard et al.(20) showing slightly lower but similar lattice parameters (Table 2).

TGA analyses, under air and argon/hydrogen for AmVO4 and AmVO3, respectively, revealed no significant weight loss for both materials, indicating a good thermal stability of the compounds at high temperature. However, XRD analysis of AmVO3 after TGA measurement showed the presence of a new unidentified phase, AmVO3 remaining as the main compound, suggesting the beginning of a degradation of the material at this temperature. In contrast, XRD measurement of AmVO4 after TGA showed that the material remains fully unchanged, indicating an excellent thermal stability of this material under oxidative conditions.

The evolution of the unit-cell parameters/volumes of the MVO3 and MVO4 compounds (Figure 2) confirms that the Am-vanadates belong to the corresponding crystallographic families. Only the perovskite phases crystalizing in the orthorhombic Pbnm space group are considered in the MVO3 part of Figure 2. The atomic coordinates and displacement parameters for AmVO3 and AmVO4 compounds are presented in Table 3.

Figure 2.

Figure 2

Evolution of the unit-cell volumes of MVO3 and MVO4 compounds as a function of the cationic radii. The unit-cell volume values are taken from the Inorganic Crystal Structure Database (https://icsd.fiz-karlsruhe.de) and the ionic radii from Shannon.21

Table 3. Atomic Coordinates and Displacement Parameters for AmVO3 and AmVO4 Compounds.

element label oxidation state SOF Wyckoff position x y z Uiso, Å2
AmVO3 (Pbnm, perovskite)
Am Am1 +3 1 4c 0.9888(15) 0.0507(5) 1/4 0.004(1)
V V1 +3 1 4b 1/2 0 0 0.004(1)
O O1 –2 1 4c 0.397(8) –0.010(9) 1/4 0.008(2)
O O2 –2 1 8d 0.745(12) 0.263(11) 0.037(6) 0.008(2)
AmVO4 (I41/amd, zircon)
Am Am1 +3 1 4a 0 3/4 1/8 0.0074(6)
V V1 +5 1 4b 0 1/4 3/8 0.0074(6)
O O1 –2 1 16h 0 0.4377(11) 0.2156(17) 0.0148(12)

3.2. Materials Characterization: α Self-Irradiated Material

Due to the impact of the COVID-19 pandemic, SEM, XANES, and Raman characterization could only be performed about 1–2 years after synthesis. Due to the high alpha activity of 241Am, the effect of self-irradiation must be considered in this condition, the main effect being amorphization of the crystal structure. The amorphization of the two vanadates was followed through XRD analyses, confirming that SEM, XANES, and Raman were performed on amorphous material. However, the results further described below seem to show only a limited impact of this amorphization on the microstructure (SEM) and electronic structure (XANES) of the two vanadates, while Raman spectroscopy showed limited impact of self-irradiation for AmVO4 and a chemical transformation due to Raman laser heating for AmVO3.

The XRD results reveal that the volume of the close-packed AmVO3 perovskite structure increases by about 4.2% after a dose of 1.03 × 1018 α/g, while that of the oxyanionic AmVO4 zircon structure shows a contraction of about 1.8% after a similar dose (Table 4). Therefore, the increased lattice disorder under α self-irradiation in this low-density structure results in a more compact arrangement. One can clearly see the swelling in AmVO3 and the contraction in AmVO4 in Figure 3, with a shift of the diffraction peaks into lower and higher 2Θ values, respectively. After a dose of about 1.65 × 1018 α/g (7 months), the main diffraction peak of AmVO3 is still visible, which indicates that the amorphization process is well advanced but not completed, while at that dose, the amorphization of AmVO4 seems fully completed.

Table 4. Lattice Parameter Variation of AmVO3 and AmVO4 under Self-Irradiation.

a, Å b, Å c, Å V, Å3 volume variation, % dose (α/g) dpaa
AmVO3 (Pbnm, perovskite)  
5.444 5.590 7.755 235.982   0.01 × 1018 0.0016
5.513 5.661 7.882 245.994 4.2 1.03 × 1018 0.158
AmVO4 (I41/amd, zircon)  
7.294 7.294 6.428 341.952   0.02 × 1018 0.0027
7.243 7.243 6.405 335.964 –1.8 1.02 × 1018 0.134
a

Estimated from the SRIM2013 simulation of displacements produced by an 241Am alpha-decay (i.e., an alpha-particle of 5.486 MeV and a 237Np recoil nucleus of 92 keV) in AmVO3 and AmVO4 yielding dose multiplication factors, d, from dose to displacement per atom of 1700 and 1800, respectively.

Figure 3.

Figure 3

Evolution of the XRD pattern of AmVO3 and AmVO4 over time showing the progressive amorphization of the material.

The SE micrographs presented in Figure 4 were recorded about 2 years after the synthesis. Even if the specimens had a relatively high level of self-irradiation at the time of the measurements, it can be observed that the microstructures are typical for solid state reactions, confirming the self-homogenization of the reaction mixture during heat treatment.

Figure 4.

Figure 4

SE images of the microstructure of AmVO3 (left) and AmVO4 (right) recorded at 660 days after synthesis (5.1 × 1018 α decay events/g).

To assess the oxidation state of both americium and vanadium in the AmVO3 and AmVO4, XANES spectroscopy characterization was performed. Am M5 edge HR-XANES, Am L3 edge XANES, and V K edge XANES spectra were collected. The HR-XANES data at the Am M5 edge reveals that Am atoms have an AmIII oxidation state for both AmVO3 and AmVO4 compounds. The energy position of the main absorption resonance (white line, WL) maximum in the AmVO3 and AmVO4 spectra (Figure 5, blue and red solid lines) is located at about 3888.5 eV that is characteristic of the main absorption intensity of AmIII, consistent with previously reported data.14,15 Note that a very limited number of Am M5 data are published to date. To be able to compare to published spectroscopic data on compounds containing AmIII, Am L3 edge XANES experiments were also performed prior to collecting the V K-edge data. The AmVO3, AmVO4, and AmO2 XANES spectra were obtained following background subtraction by fitting a linear polynomial to the pre-edge region of the absorption spectrum and normalized at the maximum (WL) intensity for Am M5 (Figure 5) and at the high energy range for Am L3 and V K edge data (Figures 6 and 7). The maxima of the WLs located at AmIIIVO3 (18,521 eV eV), AmIIIVO4 (18,521 eV), and AmIVO2 (18,525 eV) are similar to AmIII2O3 and AmIVO2 reported elsewhere.22 The difference in the tail feature around 18,533 eV as well as smearing of the shape-resonance located at about 18,556 eV for AmVO3 as compared to AmVO4 suggests a different level of amorphization. Therefore, even though at this level of self-irradiation, both AmVO3 and AmVO4 are lacking a long-range order as observed by XRD, the degree of amorphization is somewhat different as revealed by Raman data (see below) and suggests that amorphization affects less the local structure in AmVO4 as compared to AmVO3.

Figure 5.

Figure 5

HR-XANES spectra acquired at the Am M5 edge for AmO2 (green, dash-dotted), AmVO3 (red, solid, 4.7 × 1018 α/g), and AmVO4 (blue, solid, 4.7 × 1018 α/g) materials. The maximum of the white line position is indicated for AmIII and Am IV compounds, recorded at 3888.5 and 3890 eV, respectively.

Figure 6.

Figure 6

XANES spectra acquired at the Am L3 edge for AmO2 (green, dash-dotted), AmVO3 (red, solid, 4.7 × 1018 α/g), and AmVO4 (blue, solid, 4.7 × 1018 α/g) materials. The shift of the WL maximum of 4 eV is consistent with the chemical shift between AmIII and AmIV.

Figure 7.

Figure 7

XANES spectra acquired at the V K edge for AmVO3 (red, solid, 5.6 × 1018 α/g) and AmVO4 (blue, solid, 5.6 × 1018 α/g) along with VIII (orange, dotted) and VV (black, dashed) references.

To directly compare the electronic structure of vanadium, the background-subtracted and normalized V K-edge XANES spectra for AmVO3 and AmVO4 (blue and red solid lines, respectively) as well as reference V2O3 and V2O5 compounds (orange dotted and black dashed lines, respectively) are shown in Figure 7. As expected, for AmVO3, vanadium has a VIII oxidation state since all spectral features (A–D) match the spectral features of the V2O3 reference spectrum. The reduced intensity of the pre-edge feature A in AmVO3 compared to V2O3 may indicate changes in the electronic structure of vanadium as a result of AmVO3 amorphization due to self-irradiation effects as well as the influence of Am-presence in the resulting AmVO3 after reaction of AmO2 and V2O5 at 1250 °C, which differs from the pure V2O5 structure. The V K-edge XANES spectrum of AmVO4 exhibits a strong pre-edge feature (A) characteristic to VV that is well known to be due to a formally forbidden (very weak) 1s → 3d electronic transition, which is dipole-allowed when the local Oh symmetry is distorted.2325 Features B and B′ seem to be smeared out for AmVO4, indicating a change of the VO5 square-pyramidal polyhedral configuration in V2O5 to tetrahedral in AmVO4. The findings are consistent with previously reported data by Benzi et al.(26) for V2O5 and palenzonaite (natural VV) compounds. In that study, feature C′ in the tetrahedral geometry is located at about 5510 eV, matching the position of the shape-resonance C′ observed for AmVO4.

In conclusion, all the oxidation states probed through XANES and HR-XANES measurement are in perfect agreement with the expectations based on the initial crystallographic structure of the two materials. The effect of self-irradiation and amorphization has therefore no impact on their oxidation states.

The Raman spectrum of the aged AmVO4 (Figure 8) suggests that the VO4 tetrahedra in the zircon-like structure are intact despite the amorphization of AmVO4 at this level of self-irradiation found by XRD. The five clearly identifiable internal modes of the [V–O4] tetrahedron, ν1(A1g), ν3(B1g,Eg), ν4 (B1g), ν2(A1g), and ν2 (B2g), were found at very similar wavenumbers as for the lanthanide LnVO4 zircon compounds,27 as shown in Table 5, though somewhat lower than the orthovanadate of neodymium, whose ionic radius is closest to trivalent AmIII. The two clearly identifiable low-frequency external modes, which reflect the motion between the [V–O4] tetrahedron and the AmIII ion, were observed, of which the lowest is the T(B1g) and the highest is assigned to the R(Eg). The spectrum also shows a very weak mode at the position of one of the T(Eg) modes. The T(B1g) mode is substantially lower than that found for the lanthanide LnVO4 compounds.27 This can be explained by the observation by Moura et al.(28) that the T(B1g) mode in the Tb(V1–xPx)O4 solid solution shows a different broadening, indicating that it is related primarily to the Tb motion on the [Tb–O8] sublattice. The strong shift observed here thus supports that it is due to the mass effect between the actinide and lanthanide series.

Figure 8.

Figure 8

Room-temperature Raman spectrum of AmVO4 recorded at 450 days after synthesis (3.3 × 1018 α decay events/g).

Table 5. Raman Modes of AmVO4 (in cm–1) Compared to Some Lanthanide Analoguesa.

  AmVO4 LaVO4 CeVO4 NdVO4 SmVO4
  this work Cheng et al.(31) Panchal et al.(30) Nguyen et al.(32) Santos et al.(27)
ν1(A1g) 850 859.0 864.3 871 877
ν3(Eg) 785 796.7 801.3 795 816
ν3(B1g) 785 783.3 789.1 808 816
ν4 (B1g) 457 462.3 468.9 472 477
ν2(A1g)       381 380
ν4 (Eg) 370 376.6 381.1    
ν2 (B2g) 255 262.9 261.9 375  
T(B1g)         261
R(Eg) 225 228.7 234.1 237 240
T(Eg) [140] 141.8      
T(B1g) 95 119.7 124.4 123 123
T(Eg)   109.5   113 112
a

We follow the band assignment for CeVO4 by Panchal et al.(30) that was supported by density functional theory (DFT) calculations.

The shifts of the modes in AmVO4 compared to the LnVO4 series are very similar to AmPO45 and LnPO4.29 However, the strong broadening of the modes after aging that was observed for AmPO4 did not occur. This may be explained by recrystallization of the amorphous AmVO4 phase resulting from heating by the incident Raman laser. This would suggest relatively low critical amorphization temperatures, in line with the observations for the monazite and zircon LnPO4 analogues.29

Surprisingly, the Raman spectrum of the aged AmVO3 sample was identical to that of AmVO4, suggesting that oxidation took place. We exclude that the oxidation is related to the damage build-up since it is not observed in the XRD and XANES results at similar dose. We therefore conclude that it is triggered by heating the laser during the Raman measurement.

3.3. Closer Look at the α Self-Irradiation Mechanism in AmVO4

Our results for AmVO4 amorphization derived from XRD analysis differ significantly from the observations in the study of Goubard et al.,20 who studied the radiation damage build-up in AmVO4 during a much longer period of 5 years (14 × 1018 α/g). They reported that the structure remained at least partially crystalline during this period and became predominantly amorphous after 5 years, which is about 10 times slower than in our work. Moreover, Goubard et al.(20) did not observe a volume contraction under α self-irradiation like in the present study, but a moderate lattice expansion with a volume increase to a maximum of about ΔV/V0 = 1.2%. At a comparable dose to our study (1 × 1018 α/g), they found ΔV/V0 = 0.15%.

The reasons for the discrepancies with the work of Goubard et al.(20) remain unclear, and one can only hypothesize the following:

  • A different content of neptunium (daughter element of americium) in the initial material. Note that Goubard et al.(20) did not give details about the purity of the used Am. The exact quantity of Np that could be incorporated in AmVO4 is not known, but we observed NpO2 as the separate phase in this work. Moreover, uptake of NpIV in the structure would require charge compensation, for example, by VIII, which was not observed by XANES in our work.

  • The higher synthesis temperature in the current work (1000 °C vs 600 °C), which could have resulted in a more crystalline material and thus less initial disorder. As a result, a potential time span of contraction could have been absent or short in the study by Goubard et al.(20) It should be noted that their first data point at 0.7 × 1018 α/g is anomalous in their ΔV/V0 vs dose curve and indicates a minimal expansion (ΔV/V0 = 0.03%) after approximately 90 days.

  • The difference in production scale (hundreds of milligrams here versus 1 mg by Goubard et al.(20)) and more probable methods (synthesis temperature and duration) could have resulted in substantially different crystallite sizes, powder morphologies, and densities, thus potentially affecting the impact of the alpha decay through annihilation of defects, in particular via diffusion to sinks (grain boundaries).33

  • Radiogenic helium can interact with defects (vacancies), but the effect of this will depend on the microstructure and crystallinity. The larger the grain size, the larger the helium fraction retained in the lattice, affecting the defect recombination kinetics. Similarly, the initial disorder (crystallinity) will affect the helium retention. Unfortunately, information on the microstructure of the material synthesized by Goubard et al.(20) is missing.

The first three hypotheses could explain the slight difference of the initial lattice parameters (see Table 2), but not the different kinetics. Although the damage kinetics could be affected by size and geometry of samples analyzed in the XRD instruments, the discrepancy is huge. The last two hypotheses could explain the different recombination kinetics, but remain speculative, in the absence of comparative microstructural data.

Our observations for zircon-type AmVO4 are different from our results for the monazite-type AmPO4.5 The zircon structure is closely related to the monazite LnMO4 structure, both made of isolated tetrahedra of V or P, connected by trivalent metal ions in eight or nine coordinations, respectively. Under the influence of temperature and/or pressure, a transition can take place.30,31 For AmPO4, a significant expansion of the unit cell was observed (ΔV/V0 = 1.8% at 0.6 × 1018 α/g), whereas the AmVO4 cell contracts with irradiation time. However, the dose at which the transition to a fully amorphous phase takes place is close in both studies, slightly higher for AmVO4 compared to AmPO4, which is in line with the observation of Meldrum et al.(29) that the critical amorphization temperature is slightly higher for zircon-type LnPO4 compounds as well.

These contrasting observations are not easy to combine. Volume contraction due to α self-irradiation is known for Am2Zr2O7 pyrochlore34 and was attributed to the stability of the [Zr–O6] octahedra and their rotation in response to the increase in disorder around americium. Although Am2Zr2O7 has a close-packed pyrochlore structure, which is very different from the open oxyanionic structures of zircon and monazite, this explanation may help understand. The volume in the LnVO4 series is discontinuous, with the zircon (xenotime) structure (eight-coordinated MIII) being larger than the monazite (nine coordination),35 similar to the LnPO4 series.36 So, in case the radiation damage in zircon-type AmVO4 affects predominantly the americium coordination sphere leading to a higher coordination with a concomitant rotation of the [V–O4] tetrahedra, the volume will decrease, as we observed here. In AmPO4, the Am ions are already nine-fold coordinated, resulting in prompt expansion of the lattice with increasing dose. Of course, also differences in the radiation resistance of the [V–O4] and [P–O4] tetrahedral entities may play a role.

4. Conclusions

Two americium vanadates were produced and characterized in terms of crystal structure, cation oxidation states, and chemical, thermal, and radiation stability. The XRD and XANES measurements demonstrate that americium stays in the oxidation state III in the material whatever the redox condition, while vanadium shows the oxidation state III in the perovskite-like AmVO3 or V in the zircon-like AmVO4.

After an accumulation of a dose of 1018 α/g, the close-packed AmVO3 shows a volume expansion of 4.2% while the low density oxyanionic AmVO4 contracts with 1.8% in volume (in contrast with other literature reports20). With a fast amorphization behavior, large volume variation, and interchangeable structure as a function of the presence of the oxygen atmosphere and temperature, americium vanadates do not appear to be good candidates as Am forms for radioisotope power systems. Moreover, 237Np (the decay product of 241Am) tends to segregate as a fluorite fcc secondary phase, creating interfaces and inducing stress in the material. Comparing the existing data on Am-containing ceramics with fluorite,3 pyrochlore,34 zircon, monazite,5 and perovskite4 structures, the (Am,U)O22,3 fluorite solid solution seems currently to be the most suitable form for space applications.

Acknowledgments

The technical assistance and analytical support of Bert Cremer, Kathy Dardenne, Herwin Hein, Tim Prüßmann, Jörg Rothe, and Octavian Vălu are highly appreciated. N.P. and T.V. gratefully acknowledge funding from the European Research Council (ERC) Consolidator Grant 2020 under the European Union’s Horizon 2020 research and innovation programme (grant agreement no. 101003292). We acknowledge the KIT Light Source for provision of beamtime at the ACT- and INE-Beamline station operated by the Institute for Nuclear Waste Disposal and the Institute for Beam Physics and Technology (IBPT) for the operation of the storage ring, the Karlsruhe Research Accelerator (KARA). We acknowledge Kristina Aleksandrova for the design of the cover art.

Supporting Information Available

The Supporting Information is available free of charge at https://pubs.acs.org/doi/10.1021/acs.inorgchem.3c00251.

  • Thermogravimetric behavior of AmVO3 and AmVO4; overview of the AmVO3 and AmVO4 specimens measured by SEM and EDX; XRD diffraction pattern of AmVO3 after TGA measurement; Np L3 XANES spectra of the AmVO3 and AmVO4; discussion on the difference in the experimental energy resolution leading to an energy shift of the main maxima of the An M4,5 edge HR-XANES spectra; discussion on the neptunium dioxide residual phase from XRD data (PDF)

The authors declare no competing financial interest.

Notes

J.-F.V.: Conceptualization, formal analysis, investigation, methodology, validation, and writing (original draft; review and editing); T.W.: Investigation and writing (review and editing); N.P.: Formal analysis, investigation, methodology, validation, and writing (original draft; review and editing); T.V.: Formal analysis, funding acquisition, project administration, validation, and writing (review and editing); J.-Y.C. and D.B.: Investigation; D.F.: Project administration, resources, and writing (review and editing); R.J.M.K.: Project administration, resources, supervision, and writing (review and editing); K.P.: Conceptualization, investigation, methodology, supervision, and writing (original draft; review and editing).

Supplementary Material

ic3c00251_si_001.pdf (1.2MB, pdf)

References

  1. Campbell C.; Carrigan C.; Carrott M.; Maher C.; McLuckie B.; Mason C.; Gregson C.; Griffiths T.; Holt J.; Sarsfield M.; Taylor R.; Tinsley T.; Stephenson K. The separation of 241Am from aged plutonium dioxide for use in radioisotope power systems. Procedia Chem. 2016, 21, 140–147. 10.1016/j.proche.2016.10.020. [DOI] [Google Scholar]
  2. Ambrosi R. M.; Williams H.; Watkinson E. J.; Barco A.; Mesalam R.; Crawford T.; Bicknell C.; Samara-Ratna P.; Vernon D.; Bannister N.; Ross D.; Sykes J.; Perkinson M.-C.; Burgess C.; Stroud C.; Gibson S.; Godfrey A.; Slater R. G.; Reece M. J.; Chen K.; Simpson K.; Tuley R.; Sarsfield M.; Tinsley T. P.; Stephenson K.; Freis D.; Vigier J.-F.; Konings R. J. M.; Fongarland C.; Liberssart M.; Merrifield J.; Kramer D. P.; Byrne J.; Foxcroft B. European Radioisotope Thermoelectric Generators (RTGs) and Radioisotope Heater Units (RHUs) for space science and exploration. Space Sci. Rev. 2019, 215, 1–41. 10.1007/s11214-019-0623-9. [DOI] [Google Scholar]
  3. Vigier J.-F.; Freis D.; Pöml P.; Prieur D.; Lajarge P.; Gardeur S.; Guiot A.; Bouëxière D.; Konings R. J. M. Optimization of uranium-doped americium oxide synthesis for space applications. Inorg. Chem. 2018, 57, 4317–4327. 10.1021/acs.inorgchem.7b03148. [DOI] [PubMed] [Google Scholar]
  4. Vigier J.-F.; Popa K.; Martel L.; Manara D.; Dieste Blanco O.; Freis D.; Konings R. J. M. Plutonium and americium aluminate perovskites. Inorg. Chem. 2019, 58, 9118–9126. 10.1021/acs.inorgchem.9b00679. [DOI] [PubMed] [Google Scholar]
  5. Popa K.; Vigier J.-F.; Martel L.; Manara D.; Colle J.-Y.; Dieste Blanco O.; Wiss T.; Freis D.; Konings R. J. M. Synthesis, characterization and stability of americium phosphate, AmPO4. Inorg. Chem. 2020, 59, 6595–6602. 10.1021/acs.inorgchem.0c00697. [DOI] [PubMed] [Google Scholar]
  6. Keller C.Über die Festkörperchemie der Aktiniden-Oxide; Institut für Radiochemie, Kernforschungzentrum Karlsruhe, Gesellschaft für Kernforschung m.b.H, KFK-225, Karlsruhe, 1964. [Google Scholar]
  7. Keller C.; Walter K. H. Darstellung, gitterkonstanten und chemishe eigenschaften einiger ternärer oxide des plutoniums, americiums und curiums von typ MIIIXVO4. J. Inorg. Nucl. Chem. 1965, 27, 1253–1260. 10.1016/0022-1902(65)80087-2. [DOI] [Google Scholar]
  8. Petříček V.; Dušek M.; Palatinus L. Crystallographic computing system JANA2006: General features. Z. Kristallogr. 2014, 229, 345–352. 10.1515/zkri-2014-1737. [DOI] [Google Scholar]
  9. Oka Y.; Yao T.; Yamamoto N. Hydrothermal synthesis of lanthanum vanadates: Synthesis and crystal structures of zircon-type LaVO4 and new compound LaV3O9. J. Solid State Chem. 2000, 152, 486–491. 10.1006/jssc.2000.8717. [DOI] [Google Scholar]
  10. Pickardt J.; Schendler T.; Kolm M. Röntgenuntersuchung von einkristallen ternärer lanthanoid-vanadium(III)-oxide LnVO3 (Ln = Gd, Dy, Er). Z. Anorg. Allg. Chem. 1988, 560, 153–157. 10.1002/zaac.19885600118. [DOI] [Google Scholar]
  11. Chakoumakos B. C.; Abraham M. M.; Boatner L. A. Crystal structure refinements of zircon-type MVO4 (M = Sc, Y, Ce, Pr, Nd, Tb, Ho, Er, Tm, Yb, Lu). J. Solid State Chem. 1994, 109, 197–202. 10.1006/jssc.1994.1091. [DOI] [Google Scholar]
  12. Wiss T.; Thiele H.; Janssen A.; Papaiannou D.; Rondinella V. V.; Konings R. J. M. Recent results of microstructural characterization of irradiated light water reactor fuels using scanning and transmission electron microscopy. JOM 2012, 64, 1390–1395. 10.1007/s11837-012-0483-1. [DOI] [Google Scholar]
  13. Zimina A.; Dardenne K.; Denecke M. A.; Doronkin D. E.; Huttel E.; Lichtenberg H.; Mangold S.; Pruessmann T.; Rothe J.; Spangenberg T.; Steininger S.; Vitova T.; Geckeis H.; Grunwaldt J.-D. CAT-ACT- A new highly versatile x-ray spectroscopy beamline for catalysis and radionuclide science at the KIT synchrotron light facility KARA. Rev. Sci. Instrum. 2017, 88, 113113 10.1063/1.4999928. [DOI] [PubMed] [Google Scholar]
  14. Vigier J.-F.; Freis D.; Walter O.; Dieste Blanco O.; Bouëxière D.; Zuleger E.; Palina N.; Vitova T.; Konings R. J. M.; Popa K. Synthesis and characterization of homogeneous (U,Am)O2 and (U,Pu,Am)O2 nanopowders. CrystEngComm 2022, 24, 6338–6348. 10.1039/D2CE00527A. [DOI] [PMC free article] [PubMed] [Google Scholar]
  15. Cross J. N.; Su J.; Batista E. R.; Cary S. K.; Evans W. J.; Cozimor S. A.; Mocko V.; Scott B. L.; Stein B. W.; Windorff C. J.; Yang P. Covalency in americium(III) hexachloride. J. Am. Chem. Soc. 2017, 139, 8667–8677. 10.1021/jacs.7b03755. [DOI] [PubMed] [Google Scholar]
  16. Magnani N.; Caciuffo R.; Wilhelm F.; Colineau E.; Eloirdi R.; Griveau J.-C.; Rusz J.; Oppeneer P. M.; Rogalev A.; Lander G. H. Magnetic polarization of the americium J=0 ground state in AmFe2. Phys. Rev. Lett. 2015, 114, 097203 10.1103/PhysRevLett.114.097203. [DOI] [PubMed] [Google Scholar]
  17. Epifano E.; Naji M.; Manara D.; Scheinost A. C.; Hennig C.; Lechelle J.; Konings R. J. M.; Guéneau C.; Prieur D.; Vitova T.; Dardenne K.; Rothe J.; Martin P. M. Extreme multi-valence states in mixed actinide oxides. Commun. Chem. 2019, 2, 59. 10.1038/s42004-019-0161-0. [DOI] [Google Scholar]
  18. Rothe J.; Butorin S.; Dardenne K.; Denecke M. A.; Kienzler B.; Löble M.; Metz V.; Seibert A.; Steppert M.; Vitova T.; Walther O.; Geckeis H. The INE-Beamline for actinide science at ANKA. Rev. Sci. Instrum. 2012, 83, 043105 10.1063/1.3700813. [DOI] [PubMed] [Google Scholar]
  19. Schacherl B.; Prüssmann T.; Dardenne K.; Hardock K.; Krepper V.; Rothe J.; Vitova T.; Geckeis H. Implementation of cryogenic tender X-ray HR-XANES spectroscopy at the ACT station of the CAT-ACT beamline at the KIT Light Source. J. Synchrotron Radiat. 2022, 29, 80–88. 10.1107/S1600577521012650. [DOI] [PMC free article] [PubMed] [Google Scholar]
  20. Goubard F.; Griesmar P.; Tabuteau A. Alpha self-irradiation effects in ternary oxides of actinides elements: The zircon-like phases AmIIIVO4 and AIINpIV(VO4)2 (A = Sr, Pb). J. Solid State Chem. 2005, 178, 1898–1902. 10.1016/j.jssc.2005.03.039. [DOI] [Google Scholar]
  21. Shannon R. D. Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides. Acta Crystallogr., Sect. A: Cryst. Phys., Diffr., Theor. Gen. Crystallogr. 1976, A32, 751–767. 10.1107/S0567739476001551. [DOI] [Google Scholar]
  22. Nishi T.; Nakada M.; Suzuki C.; Shibata H.; Itoh A.; Akabori M.; Hirata M. Local and electronic structure of Am2O3 and AmO2 with XAFS spectroscopy. J. Nucl. Mater. 2010, 401, 138–142. 10.1016/j.jnucmat.2010.04.011. [DOI] [Google Scholar]
  23. Giorgetti M.; Berrettoni M.; Passerini S.; Smyrl W. H. Absorption of polarized X-rays by V2O5-based cathodes for lithium batteries: an application. Electrochim. Acta 2002, 47, 3163–3169. 10.1016/S0013-4686(02)00235-9. [DOI] [Google Scholar]
  24. Horrocks G. A.; Braham E. J.; Liang Y.; De Jesus L. R.; Jude J.; Velázquez J. M.; Prendergast D.; Banerjee S. Vanadium K-Edge X-ray Absorption spectroscopy as a probe of the heterogeneous lithiation of V2O5: First-principles modelling and principal component analysis. J. Phys. Chem. C 2016, 120, 23922–23932. 10.1021/acs.jpcc.6b06499. [DOI] [Google Scholar]
  25. Deng S.; Yuan Z.; Tie Z.; Wang C.; Song L.; Niu Z. Electrochemically induced metal–organic-framework-derived amorphous V2O5 for superior rate aqueous zinc-ion batteries. Angew. Chem., Int. Ed. 2020, 59, 22002–22006. 10.1002/anie.202010287. [DOI] [PubMed] [Google Scholar]
  26. Benzi F.; Giuli G.; Della Longa S.; Paris E. Vanadium K-edge XANES in vanadium-bearing model compounds: a full multiple scattering study. J. Synchrotron Radiat. 2016, 23, 947–952. 10.1107/S1600577516008134. [DOI] [PubMed] [Google Scholar]
  27. Santos C. C.; Silva E. N.; Ayala A. P.; Guedes I.; Pizani P. S.; Loong C. K.; Boatner L. A. Raman investigations of rare earth orthovanadates. J. Appl. Phys. 2007, 101, 053511 10.1063/1.2437676. [DOI] [Google Scholar]
  28. Moura M. R.; Ayala A. P.; Guedes I.; Grimsditch M.; Loong C. K.; Boatner L. A. Raman scattering study of Tb(V1-xPx)O4 single crystals. J. Appl. Phys. 2004, 95, 1148. 10.1063/1.1640461. [DOI] [Google Scholar]
  29. Meldrum A.; Boatner L. A.; Ewing R. C. Displacive radiation effects in the monazite- and zircon-structure orthophosphates. Phys. Rev. B 1997, 56, 13805. 10.1103/PhysRevB.56.13805. [DOI] [Google Scholar]
  30. Panchal V.; Lopez-Moreno S.; Santamaría-Pérez D.; Errandonea D.; Manjón F. J.; Rodríguez-Hernandez P.; Muñoz A.; Achary S. N.; Tyagi A. K. Zircon to monazite phase transition in CeVO4. Phys. Rev. B 2011, 84, 024111 10.1103/PhysRevB.84.024111. [DOI] [Google Scholar]
  31. Cheng X.; Guo D.; Feng S.; Yang K.; Wang Y.; Ren Y.; Song Y. Structure and stability of monazite- and zircon-type LaVO4 under hydrostatic pressure. Opt. Mater. 2015, 49, 32–38. 10.1016/j.optmat.2015.08.011. [DOI] [Google Scholar]
  32. Nguyen A.-D.; Murdoch K.; Edelstein N.; Boatner L. A.; Abraham M. M. Polarization dependence of phonon and electronic Raman intensities in PrVO4 and NdVO4. Phys. Rev. B 1997, 56, 9794. 10.1103/PhysRevB.56.7974. [DOI] [Google Scholar]
  33. Martínez E.; Senninger O.; Caro A.; Soisson F.; Nastar M.; Uberuaga B. P. Role of sink density in nonequilibrium chemical redistribution in alloys. Phys. Rev. Lett. 2018, 120, 106101 10.1103/PhysRevLett.120.106101. [DOI] [PubMed] [Google Scholar]
  34. Belin R. C.; Martin P. M.; Valenza P. J.; Scheinost A. C. Experimental insight into the radiation resistance of zirconia-based americium ceramics. Inorg. Chem. 2009, 48, 5376–5381. 10.1021/ic900369b. [DOI] [PubMed] [Google Scholar]
  35. Baglio J. A.; Sovers O. J. Crystal structures of the rare-earth orthovanadates. J. Solid State Chem. 1971, 3, 458–465. 10.1016/0022-4596(71)90085-5. [DOI] [Google Scholar]
  36. Ni Y.; Hughes J. M.; Mariano A. N. Crystal chemistry of the monazite and xenotime structures. Am. Mineral. 1995, 80, 21–26. 10.2138/am-1995-1-203. [DOI] [Google Scholar]

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