Water-containing layered materials have found various applications such as water purification and energy storage. The highly structured water molecules around ions under the confinement between the layers determine the ion storage ability. Yet, the relationship between the configuration of interlayer ions and water structure in high ion storage layered materials is elusive. Herein, using layered double hydroxides, we demonstrate that the water structure is sensitive to the filling density of ions in the interlayer space and governs the ion storage. For ion storage of dilute nitrate ions, a 24% decrease in the filling density increases the nitrate storage capacity by 300%. Quartz crystal microbalance with dissipation monitoring studies, combined with multimodal ex situ experiments and theoretical calculations, reveal that the decreasing filling density effectively facilitates the 2D hydrogen-bond networking structure in water around interlayer nitrate ions along with minimal change in the layered structure, leading to the high storage capacity.
Water molecules structured around ions are ubiquitous not only in bulk solution1 and at solid/liquid interfaces2 but also in nanostructures3,4,5. Ions and structured water confined in such nanostructures have found various ion storage applications such as water purification and energy storage6,7,8,9. Recently, structured water has been claimed to play an important role in endowing layered materials with high ion storage capacities that are governed by the flexibility of the host layers9,10. In the interlayer space, water molecules are incorporated into the pores that are not filled with ions, thereby stabilising the layered structure. Therefore, the water structure and content are sensitive to the configuration of the interlayer ions. Although the ion configuration in various crystal structures and reaction intermediates controls the ion storage ability11,12,13,14, it has rarely been systematically investigated.
To study the interplay between structured water and ion configuration, the filling density of ions in the interlayer space is considered. A careful observation of the interlayer structure of layered metal oxides/hydroxides suggests an inverse correlation between the stability of the water and layered structure (Fig. 1)15. Considering that the large unfilled pores are enough to form a hydrogen-bond network in interlayer water, water is assumed to structure around ions in the interlayer space16,17. In contrast, progressive water structuration involves the expansion of the interlayer space, thereby possibly destabilising the structure. This is expected to be profound in high-filling regimes because of the small original pore. Therefore, an understanding of the water structure at different interlayer filling densities provides an essential basis for the rational design of ion storage materials.
The high tunability of the host charge density and the rigid layer-stacking structure in layered double hydroxides (LDHs) can be effectively utilised for this purpose. LDHs are a conventional anionic clay with the general formula [M2+1−xM3+x(OH)2]x+(An−)x/n·mH2O, where M2+ and M3+ are divalent and trivalent metal cations, respectively, An− is the charge-compensating anion, and x is the molar fraction of the trivalent cation [M3+/(M2+ + M3+) = 0.166–0.33]18,19,20,21. The number and distribution of the positive charges associated with the host layers are controlled by x. Therefore, the interlayer filling density of the charge-compensating counter-anions is precisely determined by x. On this basis, we considered the separation of nitrate (NO3−) ions through the ion-exchange reaction with chloride ions in LDHs. The poor ion storage ability (compared to other anions) for nitrate ion in dilute conditions is the major unsolved issue in the study of LDHs because of the low charge density and nucleophilicity22, which necessitates a precise control of the binding force between interlayer nitrate ions, water molecules, and the host layers. More importantly, although nitrate and chloride ions have a monovalent negative charge and low nucleophilicity, they possess different molecular structures, resulting in similar interactions between the ions and adsorption site but different hydration behaviours; chloride ions have a high hydration enthalpy23 and the ability to structure water, as suggested by the Hofmeister series24. Thus, the ion-exchange reaction system between nitrate and chloride is a suitable model system for studying the concerted structuring behaviour of water and ions in the two-dimensional confinement of the layered materials. In this study, using two LDHs with different host charge densities (x), we firstly demonstrate that the nitrate ion storage capacity is significantly enhanced in a low interlayer filling density. Next, quartz crystal microbalance with dissipation monitoring (QCM-D) measurements were performed to prove the dynamic structural change of the LDHs upon nitrate ion storage. Finally, these results were combined with the multimodal ex situ experimental results and theoretical calculations to clarify the critical role of the water structure on the high ion storage capacity.
Results and discussion
We prepared two Mg/Al LDHs with different x values by a co-precipitation method followed by chloride ion-exchange treatment to form Cl−-form LDHs25,26,27. The chemical compositions of the LDHs are [Mg0.72Al0.28(OH)2](Cl)0.28·0.41H2O and [Mg0.78Al0.22(OH)2](Cl)0.22·0.41H2O (determined using the ICP-OES, FT-IR, and TG-DTA techniques; Supplementary Figs. 1, 6a, and 7a), indicating that the interlayer filling densities of ions in the weakly charged latter LDHs are 24% lower than those of the highly charged former LDHs. XRD patterns (Fig. 2a) and field emission scanning electron microscopy (FE-SEM) images (Fig. 2b) of the as-prepared LDHs indicate that both samples have similar crystallinity and particle size, although the interlayer distance (d003) of the highly charged LDHs is smaller by ~0.1 Å than those of the weakly charged LDHs.
Using these two LDHs, the effect of host charge density on the nitrate ion storage capacity was examined. To evaluate the maximum storage capacity (qm), adsorption isotherms were collected at room temperature and fit to appropriate models (Fig. 2c). Two different models were required for valid fitting in the entire range of nitrate concentrations, indicating that nitrate ion-exchange adsorption is driven by different mechanisms based on the extent of reaction. For both LDHs, Langmuir-Freundlich and Langmuir models28,29 were employed in the dilute (–5.0 mM) and concentrated (–200 mM) regions, respectively (see Supplementary Fig. 2 and Supplementary Table 1). The basic assumptions underlying the Langmuir-Freundlich (energetically heterogeneous adsorption sites) and Langmuir (energetically homogeneous adsorption sites) models imply that nitrate intercalation is accompanied by several metastable interlayer structures and interactions in the early storage regime, and by slight structural changes in the later storage regime. According to the fitting results, the equilibrium constants for the weakly charged LDHs are consistently higher by one order of magnitude than those for the highly charged LDHs in both concentration regions. Moreover, the weakly charged LDHs yield approximately 300% higher nitrate storage capacity in the dilute region compared to the highly charged LDHs, although the nitrate storage capacity decreases in the concentrated region (Fig. 2d). The remarkable difference in the nitrate ion storage ability is attributed to the different intermediate interlayer structures and interactions, which depend on the interlayer filling density.
To further elucidate the mechanism underlying the high nitrate ion storage capacity, we conducted a comparative QCM-D study for the two LDHs (Fig. 3a). QCM-D is powerful in situ measurement tool for understanding ion dynamics of matter. Based on the change in frequency, mass transfer upon intercalation/deintercalation of ion and water has been studied30,31,32. Importantly, dissipation monitoring has been long utilised for studying the dynamic deformation behaviours accompanying viscoelastic changes in water-containing soft matter33,34. The viscoelasticity of LDHs represents the overall interlayer interactions. Therefore, by simultaneously monitoring dissipation values and frequencies, the dynamic change in the interlayer interactions along with mass transfer of LDHs upon nitrate intercalation is studied (Fig. 3b). The experiments were carried out with a flow system. The prepared Mg/Al LDHs were deposited on a SiO2-coated Au electrode (Supplementary Fig. 3) and examined by QCM-D. The medium was changed from an aqueous NaCl solution to an aqueous NaNO3 solution, and the changes in frequency and dissipation upon ion exchange were monitored. Prior to the analysis of LDHs, we confirmed that the surface reaction on the SiO2-coated Au electrode has a negligible effect on the QCM-D profiles for the results of the experiments described below (Supplementary Fig. 4).
A distinct difference in the dissipation and frequency changes of the two LDHs is observed in the QCM-D profiles immediately after changing the solution (Fig. 3c; expanded profiles given in Supplementary Fig. 5). Highly charged LDHs show a large decrease in the dissipation and a slight decrease in the frequency, followed by a sudden and large increase in the dissipation and the corresponding large decrease in the frequency. The early change in the dissipation suggests enhanced interlayer interactions triggered by the incorporation of a tiny amount of nitrate in the interlayer space. The slight decrease in the frequency in the early regime may be contributed by the interlayer water (de)intercalation in addition to the mass increase via one-to-one ion exchange between chloride and nitrate. In the later regime, the change in the dissipation and frequency indicates the progressive intercalation of nitrate accompanied by a considerable weakening of the interlayer interactions. The progressive nitrate intercalation across the two regimes drives the transition from strong interlayer interactions to weak interactions in the LDHs, which is energetically unfavourable and results in low nitrate ion storage capacity. This transition accounts for the experimentally observed isotherms. The additional QCM-D measurements at a decreased flow rate, wherein the above-mentioned sudden and large change in the later regime disappeared, support this mechanism (Supplementary Fig. 6). This indicates that the interlayer structures containing excess nitrate observed in the later regime are presumably metastable.
For weakly charged LDHs, a slight decrease in the dissipation is observed (corresponding to slightly enhanced interlayer interactions) along with a large decrease in the frequency (corresponding to the inclusion of a large amount of nitrate into the LDHs) in the early storage regime. In the later regime, a small increase in the dissipation (corresponding to a weakening of the interlayer interactions) and in the frequency value (corresponding to decreasing mass) are observed. This indicates that further intercalation in the latter regime is suppressed due to the weakening of the interlayer interactions and is accompanied by slight dehydration. These comparative QCM-D studies, in combination with the isotherm analysis, reveal that a lower interlayer filling density causes minimal changes in the interlayer interactions, resulting in high nitrate storage capacities under dilute conditions.
To validate the proposed reaction mechanism, structural changes under the ion storage mechanism were analysed. The equilibrated LDHs used in the isotherm measurements (Fig. 2c) were analysed by ex situ synchrotron powder XRD (SPXRD). The re-posted isotherms are given with the Y-axis replaced by the xB value [= NO3−/(Cl− + NO3−)] to facilitate discussion (Fig. 4A). Ex situ SPXRD measurements were conducted using slurry-form samples packed in glass capillary, consisting of the LDH powder and the aqueous solution. The obtained pattern consists of the reflections attributed to the LDHs, amorphous water, and the capillary (representative result shown in Fig. 4B-a). A closer inspection of the obtained ex situ SPXRD results for the 003 reflections revealed that highly charged LDHs show contraction and expansion of the interlayer space depending on the xB value, implying the transition of the orientation of the interlayer nitrate from parallel to tilted toward the ab-plane of the host layer. The weakly charged LDHs show a gradual decrease in the interlayer distance. These results reveal that the contracted (expanded) interlayer space is attributed to the enhanced (weakened) interlayer interactions identified in the QCM-D analysis.
To identify the nature of the interlayer water binding affecting the interlayer interactions, we carried out TG-DTA analysis of the equilibrated LDHs used in the ex situ SPXRD measurements. The typical TG-DTA profiles of the LDHs are shown in Fig. 4C-a (see Supplementary Figs. 7 and 8 for data for other samples). A large loss and two small losses are observed in the TG profile in the temperature range of 50–180 °C and at 180 and 220 °C, respectively, along with the corresponding endothermic peaks in the DTA profile. The former large weight loss is attributed to the content of water physically adsorbed on the particle surface and between particles, and in the interlayer space35,36,37. The latter two peaks are attributed to the structured water strongly bound in the interlayer space with different binding energies. The former and latter structured water are referred to as SW-I and SW-II, respectively. For both LDHs, the total water content of these three features decreased with nitrate intercalation. The structured water emerged only after nitrate intercalation (Figs. 4C-b and 4C-c), indicating that it is established around interlayer nitrates. A remarkable difference is found for the content of structured water. For highly charged LDHs, a large amount of SW-I appeared in the early regime and then the SW-1 amount decreased in the later regime, while for weakly charged LDHs, the amount of SW-1 gradually increased with nitrate intercalation. SW-II appeared only in highly charged LDHs. These results account for the interlayer interactions and structures elucidated by QCM-D and ex situ SPXRD experiments. For highly charged LDHs, the enhanced interlayer interactions in the contracted interlayer space in the early storage regime arise from the presence of strongly bound structured water (SW-I and -II). The weakened interactions in the expanded interlayer space in the latter regime arise from the disappearance of SW-I. For weakly charged LDHs, a gradual increase in SW-I content facilitates moderate interlayer interactions in the nitrate-incorporated interlayer space, along with minimal structural changes.
Finally, to better understand the role of interlayer water, the variation in energy and the possible interlayer water structures were investigated by DFT calculations. First, we prepared two model LDH structures with highly charged [Mg0.66Al0.33(OH)2] layers and weakly charged [Mg0.833Al0.166(OH)2] layers to analyse the above-described experimental results. Second, the interlayer binding energies, the hydrogen-bonding structure associated with the orientation of interlayer anions and water molecules, and the interlayer distance38 for both LDHs with various interlayer anion compositions (xB) were calculated as a function of the interlayer water content (m). The structure with xB = 0.125 in highly charged LDHs and the structure with xB = 0.25 in weakly charged LDHs were employed to investigate the intermediate interlayer structures during the nitrate ion storage. Using the total energy of the optimised structures (Etotal), the binding energy was estimated per interlayer anion (Ebind.) as:
Finally, to investigate the favourable direction of the ion-exchange system described by Cl−(s) + NO3−(l) ⇌ Cl−(l) + NO3−(s), we calculated the binding energy of such system (Esys.) using the total energy of the anions and the experimentally obtained hydration enthalpy23 as defined by,
The computational details are described in detail in the Methods section together with supplementary data (Supplementary Figs. 9 and 10). The calculated binding energy of the optimised LDHs with xB value and the corresponding interlayer distance are given as a function of m in Supplementary Fig. 11. The results revealed that for both LDHs, the interlayer binding energy gradually increased with m and decreased with xB. The interlayer distance shows a gradual increase with m and xB. Interestingly, a drastic increase in the interlayer space is observed for m = 0.3–0.5 in highly charged LDHs with xB = 0 and 0.125 (Supplementary Fig. 11b), corresponding to the offset in the binding energy (Supplementary Fig. 11a). A similar behaviour is observed in the weakly charged LDHs with xB = 1.0 (Supplementary Figs. 11c and 11d). These results indicate that such interlayer expansion involves destabilisation of the layered structure.
To describe the stability of the prospective structures more clearly, Esys. values are presented as a function of the interlayer distance (d) for highly charged LDHs (Fig. 5a) and for weakly charged LDHs (Fig. 5b). Compared to the weakly charged LDHs, the highly charged LDHs show small negative slopes for all xB values. This is because the unfilled pores occupied by ions in the interlayer spaces are of different sizes (the Connolly surface of the dehydrated LDHs is shown in Supplementary Fig. 12). For highly charged LDHs, the energy gain upon filling of the unfilled pores by water molecules is lower than that for the weakly charged LDHs. Remarkably, several points at which two lines intersect are observed. For xB = 0 in highly and weakly charged LDHs, the interlayer distances reproduce the experiments (Supplementary Fig. 10). This implies that the crystal structures obtained at the other specific points can be employed to account for the experimental results (the corresponding interlayer structures are presented in Figs. 5c and 5d). Based on this, the interlayer contraction behaviour in the early nitrate storage regime confirmed experimentally (for both highly and weakly charged LDHs) was reproduced in these calculations. The remarkable contraction-expansion behaviour, along with the transformation of the orientation of the interlayer nitrate from parallel to tilted, was also reproduced in the highly charged LDHs. In this regard, the energetic hierarchy (Fig. 5a) reveals that the energy decreased between xB = 0.0 and 0.125 and increased between xB = 0.125 and 1.0 in the highly charged LDHs. On the other hand, in the weakly charged LDHs, the energy decreased between xB = 0.0 and 0.25 while it remained nearly the same between xB = 0.25 and 1.0.
Careful inspection of the hydrogen-bonded network structure of water reveals that the water structure determines the specific points (that is, the water content) and hence, the structural stability of the possible structures. For highly charged LDHs, the progressive formation of three-dimensional structured water is confirmed in the high-m region over the above specific points, defining interlayer water connected tetrahedrally to interlayer water molecules, anions, and hydroxide ions in the host layers via hydrogen bonding; its representative structure with xB = 0.0 (m = 0.58) is illustrated in Fig. 5e; other structures are shown in Supplementary Figs. 13–18. For weakly charged LDHs, the development of two-dimensional structured water is confirmed in the high-m region; its representative structure with xB = 0.0 (m = 0.58) is illustrated in Fig. 5f, confirming the presence of hexagonal, pentagonal, and quadrangular hydrogen-bonding networks. Notably, quadrangular water clusters known as square ice are rarely found in other materials3. The different structural features of the hydrogen-bonded network are attributed to the differently sized pores that are not filled by the interlayer ions – a high (low) filling density tends to facilitate the small (large) pore, which, in turn, leads to the formation of a three (two)-dimensional network along with interlayer ions. Importantly, the advanced water structuring in the high-m region decreases the system entropy considerably and therefore, such structures are hardly obtained experimentally. Furthermore, in the highly charged LDHs, the large energy decreases for xB < 0.125 is due to the formation of a stable quasi-two-dimensional hydrogen-bonded network of water (two-dimensional structure without hexagonal, pentagonal, and quadrangular features) and the interlayer contraction. For xB > 0.125, the large increase is due to the subsequent structural transformation to a three-dimensional hydrogen-bonded network along with tilted nitrate ions, accompanied by interlayer expansion that is facilitated at high interlayer filling densities of ions (Fig. 6); this energetically unfavourable transformation precludes nitrate intercalation. Notably, these two- and three-dimensional water structures possibly correspond to SW-I and -II, respectively, as concluded from the TG-DTA analysis. On the other hand, the weakly charged LDHs show structural transformation from a slightly quasi-two-dimensional to a two-dimensional hydrogen-bonded network of water, while maintaining a parallel orientation of the nitrate ions, involving minimal changes in the interlayer distance; this facilitates progressive nitrate intercalation (Fig. 6). This concerted interplay between the interlayer ion configuration, especially the filling density of ions, and structural change of the hydrogen-bonding network of interlayer water governs the nitrate ion storage mechanism and can be precisely tuned by varying the host charge density.
To date, understanding the water structure has been of great importance not only for ion storage layered metal oxides/hydroxides, but also for van der Waals materials, MXenes, and conventional clays. Our results demonstrate that the ion configuration in the interlayer confinement enables precise control of the dynamic structural change in water, considerably improving the ion storage ability of the material. We expect that further tuning of the host materials will offer a new framework for the optimisation of ion storage-related functionalities.
Reagent-grade Mg(NO3)2·6H2O, Al(NO3)3·9H2O, Na2CO3, NaOH, HCl, and NaCl (Wako Pure Chemical Industries, Ltd.) were used. Highly and weakly charged Mg/Al LDHs with x = 0.28 and 0.22, respectively, were synthesised by the conventional co-precipitation method using an aqueous solution containing Mg2+ and Al3+ ions as a precursor solution and NaOH/Na2CO3 aqueous solution as a precipitation agent, followed by hydrothermal treatment at 140 °C for 22 h24,25,26. After drying at 60 °C in air, the samples were subjected to the Cl-exchange treatment method using an acidic chloride aqueous solution to eliminate carbonate contamination (immersed overnight in aqueous HCl (33.0 mM) and NaCl (4.0 M) solutions at room temperature).
The crystal structures of the obtained LDHs were studied by powder XRD analysis (Miniflex II, Rigaku) performed using a Cu Kα radiation (λ = 1.5418 Å) source operated at 30 kV and 20 mA; the scans were performed for 2θ values ranging from 5° to 80°. The peak positions were calibrated with respect to the external standard (Si powder, Standard Reference Material 640 f, NIST). Ex situ synchrotron powder XRD patterns for analysing the crystal structure of water-soaked LDHs were recorded at beamline BL5S2 at the Aichi Synchrotron Radiation Centre at a beam energy of 12 keV (λ = 0.7 Å). All samples were dispersed in ultra-pure water and placed in 0.4-mm-diameter Lindemann glass capillaries. The capillaries were rotated during the data collection to obtain uniform diffraction intensities. All samples were measured using the transmission geometry. The X-ray wavelength was calibrated with CeO2 (Standard Reference Material 674b, NIST). The chemical composition of the as-prepared samples was analysed using the ICP-OES (SPS5510, SII NanoTechnology, Hitachi High-Tech Science Corporation, Japan) technique. The TG-DTA (Thermo Plus EVOII TG8120, Rigaku) technique was used to analyse the water content in the as-prepared samples at a heating rate of 10 °C min−1. The IR spectra of the as-prepared samples were recorded using a Fourier-transform infrared FT-IR spectrometry system (FT/IR-6100, Jasco) equipped with a smart-endurance single-bounce diamond attenuated total reflection cell (ATR PRO450-S, Jasco). The spectral profiles in the range of 4000–450 cm−1 were obtained by adding the results of 100 scans performed at a resolution of 4.0 cm−1. Spectral manipulations, such as baseline correction, smoothing, and normalisation, were performed using the Jasco Spectra Manager (version 2) software package. The morphologies and compositional distribution of the as-prepared samples were observed using the FE-SEM (JSM-7400F, JEOL) technique. The SEM instrument was operated at an acceleration voltage in the range of 2−15 kV. Energy-dispersive X-ray spectroscopy (EDX JSM-7000F, JEOL) was also used to analyse the samples.
Nitrate ion storage performance
To generate the ion-exchange adsorption isotherms for the as-prepared LDHs, the initial concentrations of the nitrate ions were set in the range of 0.2–5.0 mM for the experiments in dilute conditions and to 1.0–200.0 mM for the experiments in concentrated conditions using reagent-grade NaNO3 (Wako Pure Chemical Industries, Ltd.). The powder was mixed with an aqueous solution of nitrate in a capped bottle, and the mixture was subsequently subjected to conditions of automatic shaking (SRR-2, AS ONE, Japan; 150 rpm; overnight). For the dilute condition experiments, the resultant supernatant solution was collected and analysed by ion chromatography (HIS-20A SUPER, Shimadzu, Shimpack IC-SA2 analytical column, Shimpack ICGSA2 guard column, and a hydrogen carbonate/carbonate eluent) to determine the residual concentration of the nitrate ions. For the concentrated conditions experiments, the powder was collected from the resultant solution and subjected to EDX analysis to determine the adsorbed amount of nitrate ions from the Cl/Al ratio in the LDHs. We confirmed that the pH levels of the testing solution were maintained at ~7.0 before and after the ion-exchange adsorption experiment, ensuring minimal inclusion of carbonate ions. The AEC was defined as the number of moles of adsorbed nitrate per mole of LDH formula unit, [M2+1−xM3+x(OH)2]x+(Cl−)x·mH2O.
QCM-D analyses were conducted with a QCM-D instrument (Bioline Scientific) using Au/SiO2 quartz sensors. Prior to the measurements, the Au/SiO2 quartz sensors were cleaned by UV/O3 treatment for 10 min followed by immersion in a 2.0 wt% sodium dodecyl sulfate solution. After 30 min, the sensors were rinsed with ultra-pure water and dried, and then the surface of the sensors was activated to facilitate the fabrication of thin films of LDHs. Subsequently, the LDH thin film was deposited on the sensors by immersing in an aqueous suspension (4.8 mg LDHs per mL) for 1.0 min, followed by drying for 10 min to obtain a mass loading of ~8.5 µg cm−2. The high rigidity of the coating was confirmed by the small frequency changes measured in air and water (less than two units of dissipation for all measured overtones). The measurements were performed using 200 mM NaCl and NaNO3 aqueous solution with a flow rate of 300 μL min−1 at 25.0 °C. For the investigation of high-viscoelastic materials, the overtone order should be considered for the QCM-D measurement39. Therefore, we examined the overtone orders of 1 and 3, and the data were subsequently collected with an overtone order of 3 due to the large noise in the overtone order of 1.
The Vienna ab initio simulation package (VASP) was used with the Perdew-Burke-Ernzerhof formulation of the generalised gradient approximation for the exchange-correlation functional and with the projector-augmented wave method for all calculations40,41,42,43. An energy cut-off of 500 eV was used (based on the data presented in previous reports)44,45,46,47. The relaxation of the crystal structure was allowed for the stoichiometric models, and the final energies of the optimised structural geometries were recalculated to correct for the changes in the plane-wave basis during relaxation. For all calculations, a k-point mesh was chosen so that the product of the number of k-points and the number of atoms in the unit cell was greater than 1000. The convergence criteria were set to 10−4 eV for electronic self-consistent field calculations and to 10−3 eV for ionic relaxation. For an appropriate treatment of the long-range van der Waals interactions, the Grimme D2 approach was employed48,49. The structural model of LDHs with a 6 × 6 × 1 supercell and 1H stacking sequences was employed in this work, which is analogous to the one-layer hexagonal polytype manasseite, the 1H polytype (Supplementary Fig. 9). In addition, interlayer anions are located beneath the Al3+ ions within host layers and water molecules are located in the empty space between interlayer anions. The lattice parameters of the optimised geometries were in good agreement with the experimental observations, with a relative error of <1.5% (Supplementary Fig. 10). For the total energy (Etotal) in Eq. (1), the total energies of Cl− and NO3− were obtained by studying the isolated system with a cubic cell (a = 20 Å; for only the gamma point). The energy of the hydrated anions was calculated as the sum of the total energy of (Cl− and NO3−) and the hydration enthalpy obtained by experiments in the previous work (−381 and −314 kJ mol−1, respectively)23. The total energy of [Mg1−xAlx(OH)2] was obtained by setting the interlayer distance to 20 Å to minimise the interlayer interactions.
The experimental data generated in this study are provided in the Supplementary Information/Source Data file. Source data are provided with this paper.
Gurney, R. W. Ionic Processes in Solution (McGraw-Hill, New York, 1953).
Gileadi, E. Electrode Kinetics for Chemists, Chemical Engineers, and Materials Scientists (VCH, 1993).
Algara-Siller, G. et al. Square ice in graphene nanocapillaries. Nature 519, 443–445 (2015).
Pitman, M. C. & van Duin, A. C. T. Dynamics of confined reactive water in smectite clay–zeolite composites. J. Am. Chem. Soc. 134, 3042–3053 (2012).
Hack, J. H. et al. Structural characterization of protonated water clusters confined in HZSM-5 zeolites. J. Am. Chem. Soc. 143, 10203–10213 (2021).
Norrish, K. The swelling of montmorillonite. Nature 1, 120–134 (1954).
Conway, B. E. Electrochemical Supercapacitors: Scientific Fundamentals and Technological Applications (Kluwer-Academic, 1999).
Srimuk, P., Su, X., Yoon, J., Aurbach, D. & Presser, V. Charge-transfer materials for electrochemical water desalination, ion separation and the recovery of elements. Nat. Rev. Mater. 5, 517–538 (2020).
Boyd, S. et al. Effects of interlayer confinement and hydration on capacitive charge storage in birnessite. Nat. Mater. 20, 1689–1694 (2021).
Sugahara, A. et al. Negative dielectric constant of water confined in nanosheets. Nat. Commun. 10, 850 (2019).
Wang, P.-F. et al. Na+/vacancy disordering promises high-rate Na-ion batteries. Sci. Adv. 4, eaar6018 (2018).
Kubota, K. et al. Understanding the structural evolution and redox mechanism of a NaFeO2 –NaCoO2 solid solution for sodium-ion batteries. Adv. Funct. Mater. 26, 6047–6059 (2016).
Whittaker, M. L. Ion exchange selectivity in clay is controlled by nanoscale chemical–mechanical coupling. Proc. Natl Acad. Sci. USA 116, 22052–22057 (2019).
Liu, X.-D. & Lu, X.-C. A. Thermodynamic understanding of clay-swelling inhibition by potassium ions. Angew. Chem. Int. Ed. 45, 6300–6303 (2006).
Momma, K. & Izumi, F. VESTA 3 for three-dimensional visualization of crystal, volumetric and morphology data. J. Appl. Crystallogr. 44, 1272–1276 (2011).
Meleshyn, A. & Bunnenberg, C. Swelling of Na/Mg-montmorillonites and hydration of interlayer cations: a Monte Carlo study. J. Chem. Phys. 123, 074706 (2005).
Penga, C. et al. Molecular dynamics simulation of NH4-montmorillonite interlayer hydration: structure, energetics, and dynamics. Appl. Clay Sci. 195, 105657 (2020).
Krivovichev, S. V., Yokovenchuk, V. N. & Zhitova, E. S. Natural double layered hydroxides: structure, chemistry, and information storage capacity in Minerals as Advanced Materials (Springer, Berlin, ed. 2, 2012), pp. 87.
Wang, Q. & O’Hare, D. Recent advances in the synthesis and application of layered double hydroxide (LDH) nanosheets. Chem. Rev. 112, 4124–4155 (2012).
Khan, A. I. & O’Hare, D. Intercalation chemistry of layered double hydroxides: recent developments and applications. J. Mater. Chem. 12, 3191–3198 (2002).
Cavani, F., Trifiro, F. & Vaccari, A. Hydrotalcite-type anionic clays: preparation, properties and applications. Catal. Today 11, 173–301 (1991).
Miyata, S. Anion-exchange properties of hydrotalcite-like compounds. Clays Clay Miner. 31, 305–311 (1983).
Smith, D. W. Ionic hydration enthalpies. J. Chem. Educ. 54, 540–542 (1977).
Hofmeister, F. About the science of the effects of salts: about the water withdrawing effect of the salts. Arch. Exp. Pathol. Pharmacol. 24, 247–260 (1888).
Hibino, T. Anion selectivity of layered double hydroxides: effects of crystallinity and charge density. Eur. J. Inorg. Chem. 6, 722–730 (2018).
Sideris, P. J., Blanc, F., Gan, Z. & Grey, C. P. Identification of cation clustering in Mg–Al layered double hydroxides using multinuclear solid state nuclear magnetic resonance spectroscopy. Chem. Mater. 23, 2449–2461 (2012).
Roussel, H. et al. Study of the formation of the layered double hydroxide [Zn−Cr−Cl]. Chem. Mater. 13, 329–337 (2001).
Giles, C. H., MacEwan, T. H., Nakhwa, S. N. & Smith, D. Studies in adsorption. Part XI. A system of classification of solution adsorption isotherms, and its use in diagnosis of adsorption mechanisms and in measurement of specific surface areas of solids. J. Chem. Soc. 846, 3973–3993 (1960).
Rouquerol, F., Rouquerol, J., Sing, K. S. W., Llewellyn, P. & Maurin, G. Adsorption by Powders and Porous Solids: Principles, Methodology and Applications (Academic Press, Oxford, 1998).
Griffin, J. et al. In situ NMR and electrochemical quartz crystal microbalance techniques reveal the structure of the electrical double layer in supercapacitors. Nat. Mater. 14, 812–819 (2015).
Wu, Y.-C. et al. Electrochemical characterization of single layer graphene/electrolyte interface: effect of solvent on the interfacial capacitance. Angew. Chem. Int. Ed. 60, 13317–13322 (2021).
Shpigel, N. et al. Can anions be inserted into MXene? J. Am. Chem. Soc. 143, 12552–12559 (2021).
Reviakine, I., Johannsmann, D. & Richter, R. P. Hearing what you cannot see and visualizing what you hear: interpreting quartz crystal microbalance data from solvated interfaces. Anal. Chem. 83, 8838–8848 (2011).
Janshoff, A., Galla, H.-J. & Steinem, C. Piezoelectric mass-sensing devices as biosensors-an alternative to optical biosensors? Angew. Chem. Int. Ed. 39, 4004–4032 (2000).
Xu, Z. P. & Zeng, H. C. Decomposition pathways of hydrotalcite-like compounds Mg1-xAlx(OH)2(NO3)x·nH2O as a continuous function of nitrate anions. Chem. Mater. 13, 4564–4572 (2001).
Zhang, J. et al. Reinvestigation of dehydration and dehydroxylation of hydrotalcite-like compounds through combined TG-DTA-MS analyses. J. Phys. Chem. C. 114, 10768–10774 (2010).
Thomas, G. S., Radha, A. V., Vishnu Kamath, P. & Kannan, S. Thermally induced polytype transformations among the layered double hydroxides (LDHs) of Mg and Zn with Al. J. Phys. Chem. B 110, 12365–12371 (2006).
Li, X. et al. Atomistic insight into the hydration states of layered double hydroxides. ACS Omega 7, 12412–12423 (2022).
Ju, M. et al. Conductive polymer intercalation tunes charge transfer and sorption–desorption properties of LDH enabling efficient alkaline water oxidation. ACS Appl. Mater. Interfaces 13, 37063–37070 (2021).
Kresse, G. & Furthmuller, J. Efficient iterative schemes for ab initio total-energy calculations using a plane-wave basis set. Phys. Rev. B 54, 11169–11186 (1996).
Kresse, G. & Furthmuller, J. Efficiency of ab-initio total energy calculations for metals and semiconductors using a plane-wave basis set. Comput. Mater. Sci. 6, 15–50 (1996).
Perdew, J. P. et al. Restoring the density-gradient expansion for exchange in solids and surfaces. Phys. Rev. Lett. 100, 136406 (2008).
Bloch, P. E. Projector augmented-wave method. Phys. Rev. B 50, 17953 (1994).
He, Y. et al. Synthesis of Co(II)-Fe(III) hydroxide nanocones with mixed octahedral/tetrahedral coordination toward efficient electrocatalysis. Chem. Mater. 32, 4232–4240 (2020).
Sene, S. et al. Intercalation of benzoxaborolate anions in layered double hydroxides: toward hybrid formulations for benzoxaborole drugs. Chem. Mater. 27, 1242–1254 (2015).
Parvin, S., Hazra, V., Francis, A. G., Pati, S. K. & Bhattacharyya, S. In situ cation intercalation in the interlayer of tungsten sulfide with overlaying layered double hydroxide in a 2D heterostructure for facile electrochemical redox activity. Inorg. Chem. 60, 6911–6921 (2021).
Kim, N. et al. Engineering to simultaneously control the defect/stacking structures of layered double hydroxide nanosheets to optimize their energy functionalities. ACS Nano 15, 8306–8318 (2021).
Grimme, S., Antony, J., Ehrlich, S. & Krieg, H. A consistent and accurate ab initio parametrization of density functional dispersion correction (DFT-D) for the 94 elements H-Pu. J. Chem. Phys. 132, 154104 (2010).
Grimme, S., Ehrlich, S. & Goerigk, L. Effect of the damping function in dispersion corrected density functional theory. J. Comput. Chem. 32, 1456–1465 (2011).
Marcus, Y. Ionic radii in aqueous solutions. Chem. Rev. 88, 1475–1498 (1988).
Wu, G., Freure, C, J. & Verdurand, E. Proton chemical shift tensors and hydrogen bond geometry: a 1H−2H dipolar NMR study of the water molecule in crystalline hydrates. J. Am. Chem. Soc. 120, 13187–13193 (1998).
This work was supported by the Environment Research and Technology Development Fund 5RF-1902 of the Environmental Restoration and Conservation Agency of Japan, JSPS KAKENHI Grant Numbers 22H00568, 22H04533, 21K14404, and 20H05214, and MEXT Programme for Building Regional Innovation Ecosystem. The SPXRD experiments were conducted at the BL5S2 and BL5S1 beamlines of the Aichi Synchrotron Radiation Centre, Aichi Science & Technology Foundation, Aichi, Japan (Proposal Nos. 2020D6009 and 2020D6008).
The authors declare no competing interests.
Peer review information
Nature Communications thanks Xia Long, Mikhail Zheludkevich and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Peer reviewer reports are available.
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
About this article
Cite this article
Sudare, T., Yamaguchi, T., Ueda, M. et al. Critical role of water structure around interlayer ions for ion storage in layered double hydroxides. Nat Commun 13, 6448 (2022). https://doi.org/10.1038/s41467-022-34124-9
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.