Fumitaka
Takeiri
ab,
Keiko
Kusumoto
ac,
Kosuke
Kawai
d,
Hiroshi
Yaguchi
a,
Takashi
Saito
e,
Kazuhiro
Mori
e,
Saburo
Hosokawa
f,
Masashi
Okubo
d and
Genki
Kobayashi
*ad
aSolid State Chemistry Laboratory, Cluster for Pioneering Research (CPR), RIKEN, Saitama 351-0198, Japan. E-mail: genki.kobayashi@riken.jp
bDepartment of Chemistry, Kindai University, Osaka 577-8502, Japan
cDepartment of Structural Molecular Science, School of Physical Sciences SOKENDAI (The Graduate University for Advanced Studies), Aichi 444–8585, Japan
dDepartment of Chemistry, Electrical Engineering and Bioscience, Waseda University, Tokyo 169-8555, Japan
eInstitute of Materials Structure Science, High Energy Accelerator Research Organization (KEK), Ibaraki 305-0801, Japan
fFaculty of Materials Science and Engineering, Kyoto Institute of Technology, Kyoto 6068585, Japan
First published on 12th November 2024
Transition-metal oxyhydrides are an emerging class of functional materials; however, the known compounds have mostly been limited to perovskite-type sturctures. Here, we successfully synthesized Li2NbHO2, the first example of a rock-salt-type transition-metal oxyhydride, using mechanochemical methods. Galvanostatic charge/discharge tests revealed that Li2NbHO2 functions as an electrode for lithium secondary batteries.
However, TM oxyhydrides have so far been limited in terms of structural diversity. In fact, reported compounds are mostly categorized as perovskite and related structures. For example, simple cubic-type ATiO3−xHx (A = Ca, Sr, Ba)9 and SrCrO2H,10 hexagonal-type BaMO3−xHx (M = Ti,2 V,11 Cr12), and layered-type LaSrCoO3H0.713 and Srn+1VnO2n+1Hn (n = 1, 2, ∞).14 Here, we focus on the role of non-TM ions. In “hydrides” composed solely of transition-metals, including TiHx, NiHx, and PdHx, hydrogen typically dissolves in the metal or alloy to form an interstitial solid solution, where hydrogen behaves more like atomic hydrogen (H0) rather than as a hydride ion (H−). Given that H− ions occupy the anionic sites in the above-mentioned oxyhydrides, electropositive (i.e. strongly electron donating) alkaline earth or rare-earth cations should play a critical role in stabilizing H− in the lattice. The relatively large ionic radii of those cations, e.g. La3+ (1.36 Å; CN = 12), Sr2+ (1.44 Å; CN = 12), and Ba2+ (1.61 Å; CN = 12),15 may contribute to the formation of perovskite structures; in other words, the Goldschmidt tolerance factor approaches unity. Based on this expectation, the use of smaller electropositive cations like Li+ and Mg2+ could enable the preparation of new TM oxyhydrides with other crystal structures such as rock-salt, ilmenite, and LiNbO3-types. In this communication, we report the successful synthesis of Li2NbHO2 that is the first example of rock-salt-type TM oxyhydride.
A polycrystalline sample of Li2NbHO2 was synthesized using a mechanochemical method that was recently found to be effective for transition-metal oxyhydride synthesis.16 The raw materials LiH (Alfa Aesar, 99.4%), Li2O (KOJUNDO, 99%), NbO (KOJUNDO), NbO2 (KOJUNDO, 99.9%) were weighed in a molar ratio of 2
:
1
:
1
:
1, and the mixture was sealed in a 20 mL zirconia pot with 65 zirconia balls with a diameter of 5 mm. High energy ball milling at 800 rpm was conducted using a planetary ball mill apparatus (PL-7, Fritsch). The black powder obtained after milling for 36 hours can be indexed in X-ray diffraction (XRD) as a cubic unit cell with a lattice constant of approximately 4.2 Å in a single phase (Fig. S1, ESI†). To avoid unexpected moisture contamination, the powder sample was always handled in an Ar-filled glove box.
Structural information, particularly the presence of H− ions in the crystal lattice, was clarified by time-of-flight powder neutron diffraction (ND) experiments. We initially measured the aforementioned product; however, the low signal-to-noise (S/N) ratio due to the incoherent scattering of hydrogen made refinement difficult. Subsequently, we prepared a deuteride product by using LiD instead of LiH as a raw material. Fig. 1 shows the Rietveld refinement profile of ND data for the deuteride product, which also consisted of a single cubic unit cell, collected at room temperature. We refined the profile using a structure model with a disordered rock-salt-type structure (space group Fm
m), where Li/Nb atoms were placed at the Wyckoff position 4b (0, 0, 0) and D/O at 4b (1/2, 1/2, 1/2). Prior to refinement, the Li/Nb ratio of 2.09
:
1, which is close to the nominal ratio of 2
:
1, was confirmed by elemental analyses (AAS for Li and ICP-OES for Nb performed by Toray Research Center, Inc.). The refinement converged reasonably with agreement indices of Rwp = 5.36% and Rp = 4.85%; the parameters are summarized in Table 1.
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| Fig. 1 (left) Powder ND data of Li2NbDO2 collected at room temperature using the SPICA diffractometer at J-PARC. Refinement was performed by the Rietveld method using the Z-Rietveld program.17 The red crosses and green solid curves represent observed and calculated intensities, respectively. The blue solid lines at the bottom indicate residual curves. The green ticks indicate the peak positions of Li2NbDO2. (right) The crystal structure of Li2NbDO2, illustrated using the VESTA program.18 Green, black, blue, and red balls represent Li, Nb, D, and O atoms, respectively. | ||
| Atom | Site | g | x | y | z | B iso (Å2) |
|---|---|---|---|---|---|---|
Space group: Fm m(225); a = 4.21998(16) Å; Rwp = 5.36%, Rp = 4.85%, RB = 8.24%, RF = 3.42%. |
||||||
| Li | 4a | 0.6081(9) | 0 | 0 | 0 | 0.499(12) |
| Nb | 4a | 0.3919(9) | 0 | 0 | 0 | 0.499(12) |
| D | 4b | 0.33 | 0.5 | 0.5 | 0.5 | 0.499(12) |
| O | 4b | 0.67 | 0.5 | 0.5 | 0.5 | 0.499(12) |
Fig. 2a shows room-temperature Nb K-edge XANES spectra for the product (black line), along with commercially available NbIIO (blue), NbIVO2 (green), and NbV2O5 (red) as references. The absorption edge is located between those of NbO and NbO2, suggesting the presence of trivalent Nb in our compound. The absence of protons (hydroxyl groups) in the product was confirmed by Fourier-transform infrared (FT-IR) measurement, as shown in Fig. 2b. No sharp peak was observed around 3700 cm−1, which contrasts with the stretching vibrations of O–H bonds in the reference LiOH. Based on these results, along with the electrical neutrality condition, we conclude that the product is a disordered (simple) rock-salt-type oxyhydride, close to the nominal composition of Li2NbHO2, although the Li/Nb O/D ratios may contain errors of less than 10%. In addition, thermogravimetric measurements and subsequent XRD results revealed that the compound is stable in Ar and dry O2 atmosphere up to 400 °C and 125 °C, respectively (Fig. S2 and S3, ESI†).
The newly obtained Li2NbHO2 is the first example of a rock-salt-type TM oxyhydride. The discovery of a new class of compounds with such a fundamental crystal structure is notable and somewhat surprising. We believe that many more rock-salt-type oxyhydrides of (Li,TM)(H,O) with various Li/TM and H/O ratios, will be found in the future. Moreover, rock-salt type structure has a rich variety of related including layered ones (e.g. α-NaFeO2-type), CdCl2-type, and spinel-type. Those structures are expected to appear also in oxyhydrides, potentially providing new functions. Note that the synthetic process using high-energy ball-milling could contribute to the successful preparation of Li2NbHO2. Chemical reactions driven by mechanical energy rather than thermal energy sometimes result in metastable phase.19 The feature that solid-state reaction proceeds at around room temperature is particularly advantageous for synthesizing hydride-based compounds, that tend to release hydrogen gas (H2) when heated.
The discovery of disordered rock-salt-type oxyhydrides is also interesting in terms of electrode material for lithium secondary batteries, especially in relation to lithium-rich oxides and oxyfluorides represented by Li3NbO420 and Li2Mn2/3Nb1/3O2F21 for cathode, and by Li3V2O522 for anode. Here, we performed galvanostatic charge/discharge tests over the voltage range from 1.0 to 4.0 V (vs. Li/Li+) at 25 °C using 2032-type coin cells to evaluate the electrode performance of Li2NbHO2. The current density was set as 38.3 mA g−1, that corresponds to C/10 rate, where the theoretical capacity is calculated based on two Li+ removal per formula unit (383 mA h g−1).
Fig. 3 shows the charge/discharge curves of Li2NbHO2. Although an irreversible capacity loss of approximately 50 mA h g−1 was detected in the initial cycle, after the second cycle, the charge/discharge behavior stabilized, and even after 80 cycles, a discharge capacity of 105 mA h g−1 was maintained. The capacity value indicates that x in Li2−xNbHO2 reaches up to approximately 0.55 based on Nb4+/Nb3+ redox reaction during charge/discharge. This result means that Li2NbHO2 has sufficient Li+ intercalation ability, and it may be possible to achieve higher voltage and capacity by partial substitution of Nb with 3d transition-metals such as Ni, Co, Mn, and Fe, which are effective as redox species for cathode materials.
In summary, we successfully synthesized Li2NbIIIHO2, the first transition-metal (TM) oxyhydride with a rock-salt-type structure, using mechanochemical methods. The discovery of a new compound with one of the most common crystal structures opens up opportunities for further development in solid-state hydride chemistry. Given that there are many examples of synthesizing H− conductors that do not contain TM elements using lithium hydride (LiH) as a raw material,4,5,23 direct synthesis involving TM elements with LiH may have the potential to create an even more diverse group of materials. Moreover, the observed Li+ intercalation ability suggests that H− species could function as a new dopant to enhance electrode performance, such as improving electrical conductivity and tuning voltage.
This work was supported by JSPS, KAKENHI (JP24H00390, JP24H02204, JP22H04514, JP24H02205, and JP22K14755), JST, PRESTO (JPMJPR20T2) and FOREST (JPMJFR213H). The synchrotron radiation experiments were performed at BL01B1 of SPring-8 (2023B2008), with the approval of the Japan Synchrotron Radiation Research Institute (JASRI). The neutron experiments were conducted at J-PARC (2019S10 and 2024S10). F. T. acknowledges grants from the UBE Industries Foundation, the Kato Foundation for Promotion of Science, the Foundation for The Promotion of Ion Engineering, and the Izumi Science and Technology Foundation.
Footnote |
| † Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4cc05503a |
| This journal is © The Royal Society of Chemistry 2024 |