Matthew S.
Chambers
*a,
Tianyu
Li
b,
Zhilin
Liang
c,
Jong
Keum
de,
Kevin H.
Stone
c,
Raphaële J.
Clément
b,
Beth L.
Armstrong
*f and
Ethan C.
Self
*a
aChemical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA. E-mail: mschambers298@gmail.com; selfec@ornl.gov
bMaterials Department and Materials Research Laboratory, University of California Santa Barbara, Santa Barbara, CA 93106, USA
cStanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, Menlo Park, California 94025, USA
dCenter for Nanophase Materials Sciences, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA
eNeutron Scattering Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA
fMaterials Science and Technology Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA. E-mail: armstrongbl@ornl.gov
First published on 23rd April 2025
Lithium-excess disordered rock salt (DRX) materials are promising candidates for Co/Ni-free Li-ion cathodes due to their high specific energy (800+ W h kg−1) and compositional flexibility. DRX cathodes are typically synthesized using solid-state reactions, which are difficult to scale and provide little-to-no control over particle morphology. To address this bottleneck, the present study reports a two-step, solution-based reaction route to prepare Mn/Ti-based DRX oxyfluoride cathodes with nominal compositions of Li1.25Mn0.5Ti0.3O1.95F0.05 and Li1.35Mn0.7Ti0.1O1.85F0.15. More specifically, a glycine–nitrate combustion reaction is used to produce a lithiated transition metal oxide, which is further reacted with LiF to produce high-purity DRX powders. Remarkably, this route yields 80–90% pure DRX after annealing for 1 h at 800–1000 °C, and 19F solid-state nuclear magnetic resonance (ssNMR) spectra demonstrate that F− anions are successfully incorporated into the DRX structure. Cathodes prepared using this approach exhibit promising electrochemical performance, with Li1.35Mn0.7Ti0.1O1.85F0.15 attaining reversible capacities ∼210 mA h g−1 and moderate cycling stability in half cells (65% capacity retention over 150 cycles). Overall, these results demonstrate that utilizing novel metal oxide precursors presents a viable and largely unexplored method to produce high-performance Co/Ni-free DRX cathodes.
Li-excess disordered rock salt (DRX) oxides represent a promising class of next-generation Li-ion cathodes.7–15 DRX materials adopt the cubic Fm
m rock salt structure, where Li+ and transition metals occupy the cation site, and O2− anions occupy the anion site. Typically, these materials contain both redox-active transition metal(s) (e.g., Mn and Ni) and d0 transition metal(s) (e.g., Ti4+, Zr4+, and Nb5+),7,8,16 where the latter stabilizes the DRX structure.17 Compared to conventional Li-ion cathodes, DRX materials exhibit broad compositional flexibility, and their disordered nature may provide other advantages, including smaller volume changes during cycling.9 DRX cathodes reported in the literature have shown impressive performance including specific capacities ≥300 mA h g−1 and specific energies ∼1000 W h kg−1.18,19 Their electrochemical performance can be further improved by partially substituting O2− with F−, which has been widely investigated for Mn/Ti-based compositions (e.g., Li1+xMnyTi1−x−yO2−zFz).10,13,18,20–26 In addition to improving oxidative stability, F− substitution has been shown to increase Li+ mobility via formation of percolating 0-TM channels in Li1.2Ti0.35Ni0.35Nb0.1O1.8F0.2.27 Ouyang et al.28 showed that fluorination levels <10% (i.e. 0.2 mol F per DRX formula unit) hinder Li+ percolation compared to the pure oxide DRX, but Li+ mobility increases at higher fluorination levels (>15%). Recent work by Wu et al. demonstrated that the performance of Mn-rich DRX cathodes (Li1+xMnyTi1−x−yO2−zFz, y ≥ 0.5) primarily depends on the Mn content, while fluorination plays a secondary role.26
Despite their promising attributes, a major limitation of DRX cathodes is the lack of flexible synthesis platforms, which are needed to fine-tune the material's structure and performance. DRX powders are typically prepared using solid-state methods, which utilize ball milling to mix inorganic precursors followed by high-temperature reactions (e.g., 12 h at 1000 °C10 or >9 h at ≥900 °C).7 These methods are difficult to scale and provide little control over particle morphology. For oxyfluoride compositions, this lack of control is compounded by uncertainty in the product's stoichiometry due to LiF evaporation at high temperature (Tm = 848 °C for LiF)29 and/or the presence residual amorphous LiF in the final product, which cannot be detected using standard scattering tools.10 Furthermore, preparing Mn-rich compositions (y ≥ 0.5 in Li1+xMnyTi1−x−yO2−zFz) is challenging due to the high energy of Mn–F bonds compared to Li–F and Ti–F bonds.30 For example, Szymanski et al. reported difficulty in simultaneously incorporating Mn3+ and F− into the DRX lattice when using Li3TiO3F and MnO precursors.10 Considering these challenges, alternative methods have been explored to produce DRX cathodes including mechanochemical,20,21,23 sol–gel,7 molten salt,31 and microwave synthesis routes.15 Intriguingly, some reports have shown that using LiF as a fluorinating agent facilitates DRX phase formation.15,20
Combustion synthesis represents a scalable route that has not yet been explored for DRX cathodes. This approach, which has been widely employed for solid-oxide fuel cell materials32–37 and Li-ion cathodes (e.g., Li2MnO338 Mn-doped LiFePO4,39 and Mn-based spinels40,41), enables the production of powders with precise compositional control and complex chemistries that are not accessible through traditional routes. The method is also used in industrial processes such as production of yttria-stabilized zirconia42 and La1−xSrxMnO3.37 In combustion reactions, an aqueous solution containing metal precursors, oxidizing agents (e.g., nitrate salts32–37,43–45), and a fuel (e.g., malic acid,43 sucrose,44 citric acid,33,36 cellulose,33 ethylene glycol36 or glycine32,35,45) is heated to its autoignition temperature, resulting in the rapid production of nanocrystalline oxide powders. Compared to solid-state and molten-salt synthesis routes which are generally limited to gram-scale quantities, combustion reactions offer several advantages including: (i) atomic mixing of precursors in solutions, which can be readily scaled to yield kg+ batches, (ii) modest reaction temperatures (300–400 °C) to initiate the self-propagating exothermic reactions, and (iii) the ability to produce powders with controlled particle morphology.42 Thus, combustion reactions present an opportunity to address critical synthesis challenges for DRX cathodes.
The present study reports the synthesis and characterization of Mn/Ti-based DRX oxyfluoride cathodes prepared through a two-step route involving: (i) a combustion reaction to prepare a lithiated transition metal oxide precursor, followed by (ii) a high-temperature, solid-state reaction with LiF to produce the final DRX powder. This method is demonstrated for cathodes with two different Mn contents including Li1.25Mn0.5Ti0.3O1.95F0.05 and Li1.35Mn0.7Ti0.1O1.85F0.15. Overall, the approach yields up to ∼90% pure DRX powders which can be prepared at lower temperatures and over shorter timeframes (e.g., 800 °C and 1 h) compared to conventional solid-state processes (e.g., ball milling for 16 h followed by heating at 1100 °C for 2 h16 or ball milling for 6 h followed by heating at 800 °C for 12 h29). Notably, producing pure DRX oxides is difficult with this solution-based route, and adding LiF to the oxide precursor is critical to facilitate DRX phase formation during the second heating step. This work provides a detailed analysis of the reaction pathway and product's structure using in situ and ex situ X-ray diffraction (XRD). These findings are complemented by other characterization methods including: (i) solid-state nuclear magnetic resonance (ssNMR) spectroscopy to probe the distribution of local Li and F environments, (ii) scanning electron microscopy (SEM) to assess particle morphology, and (iii) inductively-coupled plasma optical emission spectroscopy (ICP-OES) and fluoride ion-selective electrode analysis (F-ISE) to determine precise stoichiometries of the fluorinated powders. The reported Mn/Ti-based DRX cathodes exhibit promising electrochemical performance, with Li1.35Mn0.7Ti0.1O1.85F0.15 attaining stable capacities up to ∼210 mA h g−1 in Li metal half cells. Overall, these results illustrate the merits and opportunities for scalable combustion reactions to produce DRX cathodes.
Safety note: due to the release of NOx species, the combustion reaction should be performed inside a fume hood. This reaction produces nanocrystalline powders, which may be present as nanoparticles. Therefore, the fume hood should also be suitable for nanomaterials.
| Li1.2Mn0.5Ti0.3O1.95 + 0.025Li2O → Li1.25Mn0.5Ti0.3O1.975. | (1) |
DRX oxyfluorides with nominal compositions of Li1.25Mn0.5Ti0.3O1.95F0.05 and Li1.35Mn0.7Ti0.1O1.85F0.15 were synthesized by grinding the oxide precursors with stoichiometric amounts of LiF (Alfa Aesar, 99.8%) and heating to 800–1000 °C under flowing Ar for 1–4 h (heating/cooling rates of ±5 °C min−1) to yield ∼0.6 g of final product. During the initial set of reactions, precursors were ground with LiF in air. However, as the precursors are hygroscopic, a second set of reactions was performed by grinding the precursors (dried at 90 °C under vacuum for 24 h) with LiF in an Ar-filled glove box with low H2O content (<10 ppm). Both approaches yielded similar cathode phase purity, morphology, and electrochemical performance. A summary of all reaction conditions investigated in this study is provided in Table S2 (ESI†). The compositions of select samples were determined using ICP-OES and F-ISE measurements performed by Galbraith Laboratories Inc.
:
1 Kα1
:
Kα2; λ1 = 0.70930 Å; λ2 = 0.71359 Å) were collected with a θ/2θ range of 5–65° and a scan rate of 1.5° min−1. Measurements with the Cu source (2
:
1 Kα1
:
Kα2; λ1 = 1.54056 Å; λ2 = 1.54439 Å) were collected with a θ/2θ range of 10–90° and a scan rate of 1.5° min−1. The dried Li1.2Mn0.5Ti0.3O1.95 and Li1.2Mn0.7Ti0.1O1.85 precursors were measured using an air-tight sample holder which was loaded inside an Ar-filled glove box. All other powders were loaded in air onto glass sample holders. Ex situ XRD data for Li3TiO3F were acquired on a Panalytical Empyrean with a Cu radiation source (2
:
1 Kα1
:
Kα2) using a θ/2θ range of 10–90° and a scan rate of 0.2° min−1.
In situ XRD data were collected using a Panalytical Xpert with a Cu radiation source (2
:
1 Kα1
:
Kα2) with a θ/2θ range of 10–90° and a scan rate of 1.5° min−1 at each temperature. For these measurements, Li1.2Mn0.5Ti0.3O1.95 was ground with LiF in an Ar-filled glove box, and the sample was heated under flowing Ar using an Anton Paar XRK-900 furnace. The powder was loaded onto the sample holder in air. Data were collected at 27 °C, and incrementally every 100 °C from 100–800 °C at a ramp rate of 10 °C min−1. The sample was left to equilibrate for 3 minutes before each measurement.
:
22 w
:
w mixture containing DRX and graphite (MSE Supplies, TIMCAL KS-6) powders was milled in a Spex® 8000M using a stainless steel jar with 5 mm stainless steel media (mass ratio of 10
:
1 media
:
powder) for 1 h following the procedure described elsewhere.7 The DRX/graphite mixture was then blended with N-methyl-2-pyrrolidone (NMP; Sigma, 99.5%) and a polyvinylidene fluoride (PVDF, Kynar) binder solution (10 wt% in NMP) in a polypropylene vial on a Turbula T2F mixer for 1 h. The slurry was cast onto a C-coated aluminum current collector using a doctor blade (wet gap 200 μm). The electrode laminates were dried in air on a hot plate at 100 °C for 2 hours. Cathode disks (7/16′′ diameter) were punched and dried under vacuum at 90 °C overnight and transferred to an Ar-filled glove box. The final electrodes contained DRX/graphite/PVDF in a 70/20/10 weight ratio and had areal loadings of approximately 2 mgDRX cm−2. Flooded R2032 cells containing the DRX cathode, Celgard 2325 separator, liquid electrolyte [1.2 M LiPF6 in 3
:
7 w
:
w ethylene carbonate
:
ethyl methyl carbonate (SoulBrain MI)], and Li metal auxiliary/reference electrode (0.75 mm thick disc) were prepared in the glovebox. Electrochemical performance was evaluated on a Maccor 4000 battery cycler by polarizing the cathodes between 2.0–4.8 V vs. Li/Li+ at specific currents of 10 mA g−1 for the first 5 cycles followed by 20 mA g−1 for subsequent cycles. All specific capacities reported herein are normalized to the active material's mass.
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| Fig. 1 Rietveld plots (Mo radiation) for products obtained by: (a) heating the Li1.2Mn0.5Ti0.3O1.95 precursor alone (Scheme 1, path A), Rwp = 10.644%, χ2 = 3.615 and (b) heating Li1.2Mn0.5Ti0.3O1.95 + 0.025Li2O (Scheme 1, path B), Rwp = 13.465%, χ2 = 3.967. Blue curves = observed data; red curves = calculated patterns; grey curves = difference between observed and calculated data. Tick marks correspond to reflections arising from each phase. m-Rock Salt and o-Rock Salt refer to monoclinic and orthorhombic rock salt phases, respectively. | ||
| Li1.2Mn0.5Ti0.3O1.95 + 0.05LiF → Li1.25Mn0.5Ti0.3O1.95F0.05 | (2) |
Heating this mixture to 1000 °C for 1 h yielded a product with 94.1(2)% DRX, 3.25(18)% monoclinic rock salt, and 2.70(13)% LiMn2O4 spinel (Fig. 2(a)). Comparing these results with Fig. 1(a) demonstrates that adding LiF to the precursor greatly facilitates DRX phase formation. Similarly, heating at 800 °C for 1 h yielded 86.4(3)% DRX, 12.1(6)% monoclinic rock salt, and 1.56(16)% orthorhombic rock salt (o-Rock Salt, see Fig. 2(b)). The beneficial impact of a small amount of LiF on the final product's purity has also been reported for mechanochemical20 and microwave15 synthesis routes. Two plausible mechanisms for the improved phase conversion of DRX oxyfluorides include: (i) LiF serving as a sintering agent and/or (ii) F− substitution in the DRX lattice altering the reaction pathway and energy landscape. While quantifying the relative importance of each mechanism is difficult, the present dataset suggests the latter may dominate. More specifically, NMR and F-ISE measurements (discussed below) demonstrate that F− is successfully doped into the DRX structure rather than precipitating out as a secondary phase (e.g., LiF) at grain boundaries. More detailed investigations on the role of LiF would require in situ neutron and X-ray total scattering methods combined with computational modeling to probe how the Li+ and F− environments evolve during the reaction. Such measurements are outside the focus of the present work but are recommended for future studies on DRX oxyfluorides.
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| Fig. 2 (a) and (b) Rietveld plots (Mo radiation) for Li1.25Mn0.5Ti0.3O1.95F0.05 synthesized at (a) 1000 °C for 1 h, Rwp = 9.779%, χ2 = 2.835 and (b) 800 °C for 1 h, Rwp = 9.349%, χ2 = 2.760. Blue curves = observed data, red curves = calculated pattern, grey curves = difference between observed and calculated. Tick marks correspond to reflections arising from each phase. m-Rock Salt and o-Rock Salt refer to monoclinic and orthorhombic rock salt phases, respectively. (c) and (d) ssNMR results for Li1.25Mn0.5Ti0.3O1.95F0.05 heated at 800 °C for 1 h including (c) 7Li (D1 = 20 s) and (d) 19F (D1 = 20 ms) spectra. The inset in (c) highlights shoulders at 36 ppm and 240 ppm. The peak deconvolution in (d) shows a sharp component at −196 ppm, which is similar to that of Li3TiO3F (see Fig. Sc, ESI†), and the broad signal is fit with two arbitrary DRX components. Sidebands are denoted with asterisks (*). Side bands were not plotted in (d) as they do not appear in the given chemical shift range. NMR spectra were taken under 100 MHz field at 40 kHz magic angle spinning (MAS). | ||
To further probe the reaction between the Li1.2Mn0.5Ti0.3O1.95 precursor and LiF, in situ XRD experiments were performed (Fig. 3). The starting precursor contains nanocrystalline Mn2O3 and LiMn2O4, with sharp Bragg reflections arising from unreacted LiNO3 (see Fig. S1a, ESI†). Rietveld refinements were performed for data acquired between 300 and 800 °C (Fig. 4). At 300 °C (Fig. 4(a)), peaks associated with LiNO3 disappear due to melting of this phase, and the sample contains primarily LiMn2O4 (43.4(16)%) and Mn2O3 (24.6(12)%). At 500 °C (Fig. 4(b)), the dominant phase is a monoclinic rock salt, which accounts for 45(3)% of the sample. The DRX phase may also begin forming at this stage, as the weight percentage obtained from Rietveld refinement is 30(2)%. However, it should be noted that the peaks are very broad at this temperature, resulting in significant overlap between reflections associated with the DRX, monoclinic rock salt, and LiMn2O4 phases. At 700 °C (Fig. 4(c)), the DRX phase is clearly present, with a weight percentage of 38(2)%. At 800 °C (Fig. 4(d)), the dominant phase is DRX (76.8(13)%), which is in good agreement with the ex situ results shown in Fig. 2(b).
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| Fig. 3 XRD patterns (Cu radiation) of the in situ reaction to produce Li1.25Mn0.5Ti0.3O1.95F0.05 (eqn (2)). (a) 3D plot highlighting notable peaks and corresponding phases and (b) surface plot where peaks arising from unreacted LiNO3 in the precursor are denoted by white boxes. Data were collected at 27 °C, and incrementally every 100 °C from 100–800 °C at a ramp rate of 10 °C min−1. The sample was left to equilibrate for 3 minutes before each measurement. m-Rock Salt refers to a monoclinic rock salt phase. | ||
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| Fig. 4 Rietveld plots of XRD patterns at select temperatures during the in situ synthesis of Li1.25Mn0.5Ti0.3O1.95F0.05 (eqn (2)). These plots show the observed data, overall calculated pattern, and the patterns arising from each phase (excluding the background). (a) 300 °C, Rwp = 10.382%; (b) 500 °C, Rwp = 9.268%; (c) 700 °C, Rwp = 15.345%; (d) 800 °C, Rwp = 11.265%. m-Rock salt and o-Rock salt refer to monoclinic and orthorhombic rock salt phases, respectively. | ||
While the XRD patterns indicate that blending the oxide precursor with LiF is critical to increase DRX phase conversion, these results do not reveal whether F− anions are successfully incorporated into the DRX lattice, as F− and O2− possess similar X-ray form factors. To further probe the distribution of local Li and F environments in the final product, the Li1.25Mn0.5Ti0.3O1.95F0.05 sample (annealed at 800 °C) was analyzed using 7Li and 19F solid-state nuclear magnetic resonance (ssNMR) spectroscopy. The 7Li ssNMR spectrum (see Fig. 2(c)) contains two major components: (i) a sharp resonance near 0 ppm arising from Li in diamagnetic environments (e.g., Li in a Ti4+-only rock salt phase, and/or in amorphous impurities such Li2CO3, LiOH, or LiF) and (ii) a broad resonance spanning from −100 to 1000 ppm attributed to Li in the DRX phase.29 A shoulder at ∼320 ppm indicates the presence of an ordered paramagnetic phase (e.g., monoclinic m-Li2Mn1–xTixO3). Similarly, the signal at ∼36 ppm is attributed to orthorhombic LiMnO2 (o-LiMnO2),53 which is consistent with the XRD analysis (Fig. 2(b)). An ordered, monoclinic LiMnO2 phase would have a 7Li resonance at ca. 130–140 ppm,53 which is not observed here, and therefore, this phase is not present.
19F ssNMR spectra were recorded under two conditions using either: (i) a long inter-scan delay (20 s) to obtain quantitative insights into the diamagnetic F environments (Fig. S3a, ESI†), or (ii) a short delay (20 ms) to enhance the intensity of fast-relaxing paramagnetic signals (Fig. 2(d)). Notably, 19F ssNMR underestimates the amount of F incorporated into the bulk DRX structure, as F species directly bonded to paramagnetic Mn yield signals that are too short-lived to be observed by NMR. Previous work describes this effect in more detail.29 A rough fit of the 19F NMR spectrum (Fig. S3a, ESI†) indicates that, while the major component centered at −100 ppm is consistent with F in the DRX phase, a secondary component centered around −200 ppm indicates the presence of a minor, F-containing phase that is too broad to be attributed solely to LiF. To identify this secondary phase, a candidate rock salt phase (Li3TiO3F) was synthesized through a solid-state reaction. As shown in Fig. S4 (ESI†), XRD and ssNMR measurements indicate this material is phase-pure with a single Li crystallographic environment resonating at 0 ppm and a single F crystallographic site resonating at about –192 ppm. Both chemical shifts are consistent with the impurity signals observed in the ssNMR spectra for Li1.25Mn0.5Ti0.3O1.95F0.05 (Fig. 2(c) and (d)). While the 19F resonance for Li3TiO3F perfectly matches that of the impurity signal, these phases may contain different F content. Therefore, the impurity is more appropriately described by the general formula Li(2+δ)/3Ti(1−δ)/3O1–δFδ, where δ > 0. As Li(2+δ)/3Ti(1−δ)/3O1−δFδ also adopts the Fm
m rock salt structure with similar cell parameters to the DRX phase, its presence was not detected by XRD patterns in Fig. 2(b).
The ssNMR and XRD findings illustrate the importance of using complementary techniques to evaluate phase composition of DRX oxyfluorides. Collectively, these results indicate that Li1.25Mn0.5Ti0.3O1.95F0.05 contains a majority DRX phase along with secondary phases including ordered diamagnetic Li(2+δ)/3Ti(1−δ)/3O1−δFδ (19F NMR signal at −193 ppm), paramagnetic Mn-containing (e.g., Li2Mn1–xTixO3) monoclinic rock salt phases (7Li NMR signal at ∼320 ppm), and a small amount of orthorhombic LiMnO2 (7Li signal at ∼36 ppm). With the present dataset, we cannot rule out the presence of trace, amorphous impurities, such as Li2CO3, LiOH, or LiF.
Additional characterization including SEM and ICP-OES/F-ISE were performed to assess the final products’ morphology and overall stoichiometry. Fig. 5 shows that Li1.2Mn0.5Ti0.3O1.95 and Li1.25Mn0.5Ti0.3O1.95F0.05 contain micron-sized primary particles which form large agglomerates (>10 μm). Interestingly, the oxyfluoride sample contains fused grains which may be the result of liquid-phase sintering enabled by a liquid flux (e.g., LiF, Tm = 848 °C).54 Similar grain structure was also observed for the Li1.25Mn0.5Ti0.3O1.95F0.05 heated at 800 °C (see Fig. S5, ESI†), suggesting the solid-state reaction (Scheme 1, path C) involves a eutectic containing the oxide precursor, intermediate phases, and/or LiF. As shown in Table S3 (ESI†), oxyfluoride powders heated at 800 and 1000 °C had measured compositions of Li1.25Mn0.36Ti0.41O1.95F0.05 and Li1.23Mn0.36Ti0.40O1.95F0.03, respectively, indicating minimal Li and F losses occur at 1000 °C. Surprisingly, these samples had a higher-than-expected Mn/Ti ratio. This result is attributed to aging (i.e., partial evaporation) of the Ti-based precursor which increased the effective Ti concentration when preparing the oxide precursor. As such, investigations on Mn-rich DRX cathodes utilized a fresh Ti reagent which was not subject to this error.
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| Fig. 5 SEM images of (a) and (b) Li1.2Mn0.5Ti0.3O1.95 heated at 1000 °C for 4 h (Scheme 1, path A) and (c), (d) Li1.25Mn0.5Ti0.3O1.95F0.05 heated at 1000 °C for 1 h (Scheme 1, path C). All images were collected on as-synthesized DRX powders. Notably, composite cathodes for electrochemical testing were prepared using high-energy ball milling to reduce particle size as described in prior work.55 | ||
| Li1.2Mn0.7Ti0.1O1.85 + 0.15LiF → Li1.35Mn0.7Ti0.1O1.85F0.15 | (3) |
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| Fig. 6 (a) and (b) Rietveld plots (Mo radiation) of the product obtained from heating Li1.2Mn0.7Ti0.1O1.85 at 1000 °C for 1 h (a) without LiF (Schematic 1, path A), Rwp = 12.655%, χ2 = 3.641 and (b) with LiF (Scheme 1, path C and eqn (3)) to yield Li1.35Mn0.7Ti0.1O1.85F0.15, Rwp = 13.107%, χ2 = 2.020. Blue curves = observed data; red curves = calculated pattern; grey curves = difference between observed and calculated. Tick marks correspond to reflections arising from each phase. m-Rock Salt and o-Rock Salt refer to monoclinic and orthorhombic rock salt phases, respectively. (c) and (d) ssNMR results for Li1.35Mn0.7Ti0.1O1.85F0.15 including (c) 7Li (D1 = 20s) and (d) 19F (D1 = 20 ms) spectra. Side bands are denoted with asterisks (*). ssNMR spectra were obtained at a 100 MHz field and at 40 kHz magic angle spinning (MAS). | ||
Unlike the Li1.25Mn0.5Ti0.3O1.95F0.05 sample, the Li1.35Mn0.7Ti0.1O1.85F0.15 powder contained a crystalline LiF impurity, which suggests that either: (i) the reaction did not go to completion and/or (ii) the Mn-rich DRX has a lower-than-targeted F− solubility (see eqn (3)). This finding is consistent with previous reports that have shown it is difficult to substitute F− into Mn-rich DRX materials.26
ssNMR was again employed to probe the distribution of Li and F local environments in the Li1.35Mn0.7Ti0.1O1.85F0.15 product. The 7Li ssNMR spectrum (Fig. 6(c)) contains a sharp resonance near 0 ppm attributed to Li in diamagnetic impurities (LiF and monoclinic Li2TiO3), which were also detected by XRD. The various 7Li signals in the 100 to 1500 ppm region correspond to Li species in paramagnetic environments, including: (i) a very broad resonance spanning 1000 to 0 ppm attributed to Li in the DRX phase29 and (ii) sharp resonances arising from Li species in ordered rock salt phases. More specifically, the 731 ppm and 1460 ppm signals are assigned to Li in the Li and transition metal layers in monoclinic Li2MnO3, and the signal at 131 ppm is assigned to Li in monoclinic LiMnO2.53,56,57 It should be noted that monoclinic LiMnO2 and monoclinic Li2MnO3 cannot be readily distinguished by XRD. Two additional resonances are observed at ∼528 ppm and 1220 ppm, which are attributed to Li in a monoclinic Li2Mn1–xTixO3 phase, where partial substitution of Mn by Ti reduces the 7Li chemical shifts compared to that of Li2MnO3.
The 19F ssNMR spectrum collected on Li1.35Mn0.7Ti0.1O1.85F0.15 is shown in Fig. 6(d). The sharp resonance at ca. −204 ppm is assigned to LiF, while the broad resonance spanning 270 to −380 ppm is attributed to F in the DRX phase.58 A fit of the data (Fig. S3b, ESI†) indicates at least 42% of the F was incorporated into the DRX structure. Overall, these results demonstrate that the synthesis route reported herein is viable to produce DRX oxyfluorides without the need for high-energy ball milling.
The morphologies of Li1.2Mn0.7Ti0.1O1.85 and Li1.35Mn0.7Ti0.1O1.85F0.15 were assessed using SEM as shown in Fig. 7. Both samples contain micron-sized agglomerates similar to Li1.2Mn0.5Ti0.3O1.95 and Li1.25Mn0.5Ti0.3O1.95F0.05 (Fig. 5). While not a primary focus of the current work, modifying the solution composition is anticipated to enable one to control the DRX particle morphology. For example, the fuel-to-oxidizer ratio in combustion reactions often has a dramatic impact on particle shape, size, and agglomeration.42,59 These morphological variations are largely influenced by differences in heat released and gas evolution during the exothermic reaction. Such investigations are recommended for future work on DRX cathodes prepared using this route.
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| Fig. 7 SEM images of (a), (b) Li1.2Mn0.7Ti0.1O1.85 (Scheme 1, path A) and (c), (d) Li1.35Mn0.7Ti0.1O1.85F0.15 (Scheme 1, path C). All images were collected on as-synthesized DRX powders prepared by heating at 1000 °C for 1 h. Notably, composite electrodes for electrochemical testing were prepared using high-energy ball milling to reduce particle size as described in prior work.55 | ||
For the oxyfluoride sample, ICP-OES/F-ISE results indicate an overall composition of Li1.26Mn0.72Ti0.11O1.85F0.15 (see Table S3, ESI†), which is in good agreement with the nominal stoichiometry (Li1.35Mn0.7Ti0.1O1.85F0.15). The product's slight Li deficiency (Li1.26versus Li1.35) suggests some Li loss occurs during either the combustion reaction or high-temperature annealing step. As such, the effect of lower annealing temperatures was also investigated as shown in Fig. S2d (ESI†). Heating Li1.2Mn0.7Ti0.1O1.85 with LiF at 800 °C for 1 h resulted in only 12.6(7)% DRX, compared to 92.0(2)% DRX for Li1.25Mn0.5Ti0.3O1.95F0.05 heated under the same conditions (Fig. S2b, ESI†). The need for higher reaction temperatures to produce Mn-rich DRX powders has also been reported in previous studies.10,26 The increased difficulty in forming these phases may be related to the stability of the ordered rock salt Li2MnO3, for which an order–disorder transition has not been reported.20 To address the moderate DRX purity in the present study, future work is recommended to explore alternative precursor designs (e.g., altering the Li and/or vacancy content) which may influence the reaction pathway and product's structure.
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22 w
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w) followed by (ii) slurry mixing and electrode casting. As described in previous work,55 graphite is a preferable conductive additive due to formation of a robust electronically conductive network and a more stable cathode/electrolyte interface. During the first cycle, the Li1.35Mn0.7Ti0.1O1.85F0.15 cathode had a high charge capacity of 274 mA h g−1 and reversible capacity of 209 mA h g−1, corresponding to an initial coulombic efficiency of 76%. Interestingly, the cathode with lower Mn content (Li1.25Mn0.5Ti0.3O1.95F0.05) had slightly higher capacity (see Fig. S7, ESI†), which is attributed to the sample's higher DRX purity. These results indicate charge compensation occurs through Mn and O redox centers as expected.7,18,60 In general, the performance of Mn/Ti-based DRX cathodes is highly dependent on the Mn content and processing history. For example, materials prepared through sol–gel,7 mechanochemical,61 and solid-state62 reactions have been reported with initial reversible capacities ranging from approximately 200–250 mA h g−1. For a more detailed discussion on the topic, we refer to a comprehensive review by Li et al.63
While the initial cycles showed a sloping voltage profile, extended cycling of Li1.35Mn0.7Ti0.1O1.85F0.15 yielded a plateau ∼3 V vs. Li/Li+ due to formation of a spinel-like δ phase which is well-known for Mn-rich DRX cathodes.19,64 The material also showed good cycling stability with 65% capacity retention after 150 cycles. Capacity fade in these cells is primarily attributed to an unstable cathode/electrolyte interface due to electrolyte breakdown at high states of charge. This effect is also illustrated by the moderate coulombic efficiency ∼95% during extended cycling (Fig. 8(b)) which is a result of parasitic reactions occurring at both the DRX cathode and Li metal anode. As recently reported for Li1.2Mn0.5Ti0.3O1.9F0.1, catalytic decomposition of the electrolyte is heavily influenced by the conductive additive's structure, surface area, and loading.55 While efforts to optimize the cathode/electrolyte interface are outside the present study's scope, the results in Fig. 8 demonstrate that cathodes derived from a combustion reaction have reproducible and competitive performance with materials obtained through traditional solid-state reactions.7 Ongoing work is aimed at fine-tuning the synthesis conditions (e.g., to eliminate secondary phases such as LiMnO2 that may be electrochemically active), which is anticipated to further improve the cathode's performance.
Mn-rich oxyfluoride DRX cathodes prepared using this route showed promising electrochemical performance with reversible capacities ∼210 mA h g−1 and good cycling stability in half cells. These results are competitive with similar DRX formulations prepared using conventional solid-state routes. Future investigations are recommended to optimize other reaction parameters (e.g., fuel content/composition, precursor stoichiometry, thermal quenching rate, and F content) to maximize yield of the desired oxyfluoride phase and control particle morphology. Beyond energy storage applications, this synthesis approach can also be used to prepare other metastable phases not accessible through traditional routes.
Footnote |
| † Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ma01287a |
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