Open Access Article
Trent R.
Graham
*a,
Micah P.
Prange
a,
Xin
Zhang
a,
J. David
Bazak
a,
Nancy M.
Washton
a,
Khashayar
Ghandi
b,
Gregory K.
Schenter
a and
Carolyn I.
Pearce
ac
aPacific Northwest National Laboratory, Richland, 99354, USA. E-mail: trent.graham@pnnl.gov
bUniversity of Guelph, Guelph, ON N1G 2 W1, Canada
cDepartment of Crop and Soil Sciences, Washington State University, Pullman, 99163, USA
First published on 29th October 2025
The enhanced radiolytic stability of gibbsite (α-Al(OH)3) containing trace nitrate (NO3−) is a phenomenon in nuclear waste management, but its structural origins remain unresolved. Motivated by the detection of minority tetrahedral aluminum (Td) defects in synthetic gibbsite, we hypothesized that these sites may participate in NO3− retention or mediate H2 suppression. To evaluate this, we combined orthogonal techniques comprised of spatially selective solid-state 27Al MAS NMR, comparative spectroscopy, and density functional theory (DFT) modeling. Paramagnetic editing and dynamic nuclear polarization (DNP) MAS NMR confirm that Td defects are confined to the particle interior. DFT calculations reveal no energetic stabilization of NO3− near Td sites. Comparative NMR analysis shows that Td is also present in chloride-bearing gibbsite, which exhibits high radiolytic hydrogen yields. These three independent disqualifications rule out Td as a structural contributor to nitrate-mediated suppression and narrow the scope of defect-driven explanations. The findings redirect mechanistic attention away from coordination defects and toward redox-active impurity pathways, providing a refined foundation for understanding radiation tolerance in Al(OH)3.
Minor (<1% of 27Al magic angle spinning nuclear magnetic resonance (MAS NMR) signal) populations of tetrahedral aluminum (Td) have been observed in synthetic gibbsite under specific formation conditions, particularly at lower synthesis temperatures.6 Motivated by this structural signature, we hypothesized that Td defects might play a mechanistic role in the anomalous radiolytic suppression observed in nitrate-bearing gibbsite. Specifically, we considered the possibility that Td formation could reflect or enable structural accommodation of retained NO3−, for example via local charge compensation or defect–impurity coupling. To evaluate this, we designed a combined experimental-computational strategy to assess the spatial accessibility, energetic relevance, and correlative behavior of Td in relation to impurity content. Determining whether Td sites reside at the surface or in the particle interior was therefore the first step toward assessing their potential for chemical interaction with NO3−. This hypothesis also intersects with broader questions about local heterogeneity in gibbsite, which is known to host structurally disordered domains including entrained clusters of octahedral Al.7 While the present study addresses structural explanations directly, it forms part of a larger effort to resolve the mechanisms of radiological suppression of H2 in NO3-gibbsite.
To evaluate the spatial accessibility of Td defects, we applied two complementary solid-state, MAS-NMR spectroscopy techniques with orthogonal surface sensitivity. Paramagnetic spectral editing was implemented using post-synthesis adsorption of trivalent chromium (Cr3+), which quenches signals from surface-accessible sites through rapid transverse (T2) relaxation.8 This method has been successfully applied to resolve surface from interior sites in materials ranging from inorganic solids9 to biological macromolecules.10,11 Our method leverages the strong adsorption of Cr3+ ions to render the chemically-defined near-surface region NMR-silent. Recent spectroscopic and microscopic characterization of this system has confirmed that when introduced post-synthesis, Cr3+ adsorbs strongly to the gibbsite surface, forming clusters with minimal penetration into the bulk lattice.12 Dynamic nuclear polarization (DNP), in contrast, selectively enhances surface-localized signals via polarization transfer from an exogenous radical under microwave irradiation.13,14 Together, these methods provide cross-validation of convergent constraints on the location of Td defects. This spatial constraint, combined with comparative evidence from chloride-bearing samples and direct energetic evaluation via DFT, provided a framework to evaluate Td defect-impurity coupling in gibbsite.
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| Fig. 1 Experimental strategy for localizing Td defects in gibbsite. (A) Crystallographic17 visualization18 of gibbsite alongside a scanning electron micrograph showing the euhedral, hexagonal nanoplatelet morphology of the synthesized gibbsite. (B) Schematic of the paramagnetic editing experiment, where surface-adsorbed Cr3+ renders the near-surface region NMR-silent, leaving subsurface signals unperturbed. (C) Schematic of the DNP-NMR experiment, where an exogenous radical solution selectively enhances NMR signals originating from the particle surface. | ||
We first applied a paramagnetic spectral editing approach (Fig. 1B) using Cr3+ ions as surface-selective NMR resonance quenchers to evaluate the spatial accessibility of Td defects. Cr3+ adsorbs strongly to the NO3-gibbsite surface and induces rapid transverse (T2) relaxation in nearby nuclei, rendering surface and near-surface environments (∼5 Å) NMR-silent.19 Upon treatment with Cr3+ at concentrations up to 100 ppm, no attenuation of the Td resonance was observed relative to the dominant octahedral Al signal (Fig. 2). The persistence of the Td signal under these conditions indicates that these sites are not surface-accessible and must reside within the interior of the nanoplatelet. This spatial assignment does not in itself preclude interaction with retained NO3−, but it establishes that any such coupling would have to occur in the bulk, not at the surface. The Td resonance corresponds to <1% of the total 27Al signal, yet its persistence after Cr3+ editing demonstrates that it is an interior feature not associated with the surface. Although minor in intensity, its reproducibility across samples and insensitivity to surface quenching confirm that this resonance reflects a real structural population rather than a spectral artifact.
Further evidence for the subsurface assignment of Td defects was acquired with dynamic nuclear polarization (DNP) experiments, which selectively enhance NMR signals originating from surface-accessible sites through microwave-driven polarization transfer from exogenous radicals (Fig. 1C). In NO3-gibbsite, DNP resulted in enhancement of the surface octahedral Al signal (ε ≈ 18), consistent with surface-initiated polarization relay through the hydroxyl network (Fig. 3). However, the Td resonance showed no preferential enhancement under DNP conditions, indicating that these sites do not reside near the particle surface.
To validate the surface sensitivity of the DNP experiment, we applied the same measurement protocol to a nano-α-Al2O3 control material with well-characterized surface chemistry. This system is known to exhibit a high concentration of distinct Td, pentahedral, and octahedral Al sites located at particle surfaces and grain boundaries.15 This material showed strong and preferential enhancement of surface-associated resonances, in contrast to the lack of an enhancement for Td signal in NO3-gibbsite (Fig. 4). This control supports the interpretation that the lack of enhancement for the Td signal in gibbsite reflects its spatial isolation, rather than complications in polarization transfer or instrumental sensitivity which are potential confounds given the evolving capabilities of high-field DNP NMR. Taken together with the Cr3+ editing data, the DNP results establish that Td defects in NO3-gibbsite are structurally real, spatially resolved, and confined to the particle interior.
With Td defects localized to the interior of the NO3-gibbsite nanoplatelets, we next evaluated whether these sites might structurally interact with NO3− impurities. Although NO3− is not directly observable in these NMR experiments, its retention following extensive aqueous washing suggests that any incorporated NO3− resides within the bulk rather than on the surface. The potential for spatial co-localization between Td and NO3− makes a structural interaction plausible in principle. To assess whether such a coupling is energetically favorable, we performed density functional theory (DFT) simulations to test whether interstitial NO3− can induce or stabilize nearby tetrahedral coordination environments in the gibbsite lattice.
Whether interstitial NO3− incorporation stabilizes nearby Td was evaluated using DFT simulations on NO3− bearing gibbsite (Fig. 5). Initial configurations were constructed by embedding gas-phase-optimized nitrate–aluminate complexes into the gibbsite lattice, followed by structural relaxation under periodic boundary conditions using the RPBE-D3 functional. Across all configurations examined (∼10), lattice relaxation did not produce conversion of neighboring octahedral Al into tetrahedral geometry, nor did it yield energetically favored coupling between NO3− and existing Td motifs. Most relaxations resulting in NO3− substituting an OH− group and extending into the interlayer (Fig. 5B). All aluminum centers remained sixfold coordinated following optimization, with some evidence for fivefold coordination. These results are inconsistent with the hypothesis that NO3− and Td form a structurally coupled defect-impurity pair within the bulk lattice. Representative visualizations of attempted nitrate substitutions and a comparison of relative energies are provided in the SI (Fig. S1).
To assess whether the presence of Td defects correlates with radiolytic suppression, we analyzed 27Al MAS NMR spectra of gibbsite synthesized in the presence of chloride, a system known to produce high radiolytic H2 yields. These samples exhibited a comparable resonance at ∼65 ppm, consistent with Td, despite their lack of radiolytic stability (Fig. 6). Notably, the figure also shows a 27Al MAS NMR spectra of a second batch of synthesized NO3-gibbsite. This second batch also displayed the same Td feature, confirming its reproducibility. Prior reports observed that Td content decreases as crystallinity improves.6 To ensure that the observed signal was not an artifact of rotor background or packing, spectra of air-filled rotors were acquired under identical conditions immediately before packing the Cl-gibbsite and second batch of NO3-gibbsite. The absence of Td resonances in these controls (Fig. 6) confirmed that the resonance is intrinsic to the samples. This finding demonstrates that the presence of Td is not unique to nitrate-bearing systems and is not predictive of radiolytic behavior. While this result does not exclude the possibility that Td may participate in other structural processes, it disqualifies the defect as a mechanistic signature of radiolytic suppression in these materials.
Taken together, the results of this study disqualify three structurally plausible but mechanistically unsupported hypotheses linking Td defects to nitrate-mediated radiolytic suppression of H2 yield in gibbsite. First, spatially selective NMR techniques establish that Td defects are sequestered within the particle interior, ruling out mechanisms that rely on surface accessibility. Second, DFT modeling reveals no energetic stabilization of NO3− near Td sites, falsifying the proposed defect–impurity coupling pathway. Third, comparative NMR analysis shows that Td defects are also present in chloride-bearing gibbsite, which exhibits high radiolytic H2 yields, eliminating Td as a structural marker for radiolytic suppression. These constraints converge on a shared conclusion that Td is a reproducible, subsurface feature of synthetic gibbsite, but it plays no mechanistic role in nitrate-linked radiolytic stability. The residual explanation for radiolytic stability is therefore chemical, not structural. Given the known redox reactivity of NO3−, its function as an electron scavenger now emerges as the leading candidate mechanism for suppressing radiolytic hydrogen production in these materials.
000 transients were collected with a recycle delay of 0.5 s and an acquisition time of 9.8 ms. A magic-angle spinning (MAS) rate of 20 kHz was used for the data presented. Chemical shifts were externally referenced to a 1.0 M aqueous Al(H2O)63+ solution at 0 ppm. Post-acquisition processing of the 27Al MAS NMR spectra was performed in MestReNova (v. 14.01). The free induction decay was zero-filled to 26 ms, and an exponential line broadening of 20 Hz was applied.
All DNP-enhanced solid-state NMR experiments were performed on a Bruker Avance NEO 800 MHz (18.8 T) spectrometer equipped with a 1.9 mm H/X/Y low-temperature DNP/MAS probe, operating at 1H and 27Al Larmor frequencies of 800.1 MHz and 208.50 MHz, respectively. Dynamic nuclear polarization was achieved by continuous microwave irradiation from a Bruker gyrotron operating at 526.932 GHz, with a power of approximately 8 W for gibbsite and 13 W for α-alumina. For all DNP experiments, the sample temperature was maintained at 100 K, and the magic-angle spinning (MAS) rate was 15 kHz.
For both materials, 27Al {1H} cross-polarization (CP) MAS spectra were acquired with a 1H 90° pulse of 3.0 µs, a recycle delay of 30.0 s, and high-power SPINAL-64 1H decoupling during acquisition. For gibbsite, the CP contact time was 2.0 ms, and 64 scans were averaged for both DNP-on and DNP-off experiments. For α-alumina, the contact time was 1.8 ms (DNP-on, 320 scans) and 1.6 ms (DNP-off, 64 scans). Additionally, a quantitative 27Al direct polarization (DP) MAS spectrum of α-alumina was acquired using a small tip-angle pulse (0.75 µs) with a 2.0 s recycle delay, averaging 32 scans. The DNP signal enhancement factor (ε) was calculated from the ratio of integrated intensities of the DNP-on (Ion) and DNP-off (Ioff) spectra, normalizing for the number of scans (NS) where appropriate with the equation, ε = (Ion/NSon)/(Ioff /NSoff). This resulted in ε = 18 for the gibbsite sample and ε = 24 for the α-alumina. Given the slight change in contact time for α-alumina, the associated ε is approximate.
All NMR data were processed using MestReNova (v.16.0.0-392765). Acquired FIDs (8192 complex points) were processed with an exponential line broadening of 20 Hz and were zero-filled to 16
384 points prior to Fourier transformation. The 27Al chemical shift scale was referenced to the apparent peak maximum of the prominent gibbsite signal in the CP MAS NMR spectrum, which was assigned a chemical shift of 10 ppm, which is an approximation of the isotropic chemical shift of the 2 Al sites in gibbsite (13.6 and 11.3 ppm, respectively).15
Supplementary information (SI) is available. See DOI: https://doi.org/10.1039/d5qi01703c.
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