Abstract

Oxygen evolution energies were calculated for the {100}, {110}, {111}, and {112} type facets of the rock-salt-structured cation-disordered Li-excess, Mn-rich Li-ion (DRX) cathode Li2MnO2F at the fully lithiated, 25% delithiation, and 50% delithiation states. Our calculations showed that Li2MnO2F remains much more robust to O loss than its nonfluorinated counterparts, as has been shown in experimental work. In particular, the {110} and {112} facets are the most resilient against O loss. Focusing on the {100} type facet, which previous work has shown to be the most likely exposed facet of Li2MnO2F, it was found that higher proportions of Li in an O coordination shell lead to lower O evolution energy (ẼO) and facilitate O loss. It was also found that at higher states of delithiation, surface fluorine had a weaker effect in increasing ẼO, meaning the protective effect of F against O loss is more effective at higher lithiation states. Electronic structure chemical bonding analysis revealed weaker bonding interactions between Li and O correlated with lower ẼO and hence a higher propensity for surface O loss..
Introduction
Given the urgent need to shift consumption from nonrenewable fossil-fuels toward sustainable energy resources,1 the demand for energy storage is rapidly increasing and projected to continue increasing.2 Disordered rock-salt Li-excess (DRX) cathode materials3−5 have emerged as a promising candidate for Li-ion battery applications, offering a wide chemical space allowing for the use of cheap, earth-abundant materials. Fluorination has been shown to improve the performance of DRX materials,6−10 simultaneously increasing the transition metal redox capacity and mitigating the capacity and voltage fade associated with surface O loss.
Both DRX materials11−13 as well as cation-ordered, layered materials14,15 have been observed to exhibit O loss. To investigate the chemical nature of the bulk O loss, Seo et al.16 examined Li-rich layered oxides and DRX cathodes with density functional theory (DFT) and highlighted that the O 2p orbital in Li–O–Li configurations remains unhybridized. The lack of hybridization in turn leads to an increased O energy state and liability toward O oxidation at high charge. Other studies have shown the formation of peroxo-like species17 as well as transition metal migration18 correlated with voltage fade. Shin and Persson19 predicted the thermodynamic driving force for O evolution to increase with delithiation in the layered material Li2MnO3. In particular, they noted that while the release of O already becomes spontaneous at 25 and 50% states of delithiation for all facets studied, the (110) surface is most resistant to O loss. Hu et al. studied various cathode materials including layered LiMO2 (M = Co, Ni, Mn) and LiNi1/3Co1/3Mn1/3O2 (NCM-333), spinel LiMn2O4, and Li-rich Li2MnO3 and found that all materials except for Li2MnO4 were more likely to lose O after delithiation.20 Using computational methods and focusing on the DRX material Li2MnO2F, Sharpe et al.21 showed that 5 Li-, 1 Mn-coordinated O were more prone to oxidation upon charge as compared to those surrounded by only 3 or 4 Li. They also found, using a combination of computations and RIXS spectroscopy, that at high levels of Li deintercalation, molecular O2 is energetically favored to form within the bulk of the material, and O2 to be reversibly reduced to O2– on discharge. Surface reconstruction and phase changes have also been observed following O loss. Using first-principles based Monte Carlo simulations, Xiao et al.22 suggested that densified phases of the types Ni0.25NiO2 and Ni0.5NiO2 can form by Ni back diffusion from the surface owing to O loss at highly charged states. Interestingly, they also found that slow kinetics preclude the conventional Li0.5NiO2 spinel formation from its layered parent phase at room temperature. Mukherjee et al.23 leveraged electron microscopy and spectroscopy to study the effects on O loss in LiNi0.8Co0.15Al0.05O2 (NCA) cathodes held at 4.75 V and 60 °C. They observed phase transformations from layered to rock salt followed by metal dissolution leading to the irreversible formation of a porous surface layer with high impedance. Kwon et al.24 found that following O loss, both Li1.2Ni0.333Ti0.333Mo0.133O2 (LNTMO) and Li1.2Mn0.6Nb0.2O2 (LMNO) experience metal densification at the surface. However, LMNO forms a surface phase that allows fast Li transport and alleviates further loss of O, whereas LNTMO’s densified DRX surface structure does neither. In the DRX material Li2MnO2F, McColl et al.25 found that irreversible transition metal migration is required before molecular O2 can form in the bulk structure, such that O2– ions move to sites with different coordination causing a voltage fade corresponding to 0.3 V.
Responding to the detrimental effect of O loss, mitigation strategies have been proposed. Craften et al.10 suggested that fluorination can completely suppress O loss in the DRX material Li1.2Mn0.625Nb0.175O1.95F0.05 when cycled between 1.5 and 4.45 V. Even increasing the charging protocol to 4.8 V showed only a small amount of O evolution on the first cycle and none thereafter. Park et al.26 employed a graphene-based hermetic surface coating that reduced O loss in layered LiNiO2 at high states of charge. Shin et al.27 used DFT to study the effect of surface dopants on the oxygen evolution energy (ẼO) in layered Li2MnO3 and found a beneficial effect from Os, Sb, Ru, Ir, and Ta, while Ti and Al did not improve O retention. The authors explained the improved O retention through an increase in the hybridization of p-orbitals between the O and dopant atoms. Experimental differential electrochemical mass spectroscopy confirmed that Ta-doping (Li1.3Nb0.285Ta0.015Mn0.4O2) reduced O evolution compared to undoped Li1.3Nb0.3Mn0.4O2. Ning et al.28 found that a defective graphene coating can suppress O loss on Li2MnO3 by modifying the potential energy surface.
Further computational work studying the energetics of O loss of oxygen on DRX surfaces could lead to design rules to help synthesize DRX cathodes with increased resistance to O loss. Here, we use the highly fluorinated Li-excess, Mn-rich DRX cathode Li2MnO2F as a model system to study the thermodynamic driving force for O release. Previously, the low Miller index surfaces of Li2MnO2F were studied using computational methods, which revealed the {100} type surface as the lowest-energy facet, which hence dominated the equilibrium particle shape. It was also found that the surface was enriched in Li and F.29 Following these results, we here calculate the O release energy (ẼO) on the low Miller index surfaces {100}, {110}, {111}, and {112} at 0, 25, and 50% levels of delithiation. We base our disordered structures on a cluster expansion method described in Ouyang et al.30 as well as a surface-symmetrizing procedure described in Burns et al.29 For each facet and delithiation level, we calculate the ẼO on surfaces of varying chemistry and arrangements (guided by the aforementioned findings on the preferred surface chemistry) and use Boltzmann weighting to get average O release energies.
Methods
DFT Calculations
All first-principles calculations were performed using the Vienna ab initio simulation package (VASP)31−34 using the projector augmented-wave potentials35 with the Perdew–Burke–Ernzerhof generalized-gradient approximation functional.36 Structure optimizations were used to fully relax the atomic positions and lattice parameters in the bulk structures. Slab optimizations were used to fully relax the atomic positions of the 3 outermost surface layers of slabs using at least 20 Å of vacuum in both pristine and O deficient slabs. All bulk and slab total energies were then improved by using static calculations. The max force cutoff was relaxed from 0.25 to 1 eV/Å for the 50% delithiated structures for all facets, as well as the 25% delithiated {100}, {110}, and {111} structures. Static calculations were performed prior to the chemical bonding analysis using the software package LOBSTER.37−40 All INCAR parameters used were bench-marked by the Materials Project and are documented in MPRelaxSet, MPStaticSet, and LobsterSet in Python Materials Genomics (pymatgen).41
Oxygen Evolution Energy Workflow
All bulk structures were generated using Monte Carlo simulations based on a previously trained cluster expansion.30 Structures were equilibrated with at least 100,000 Monte Carlo steps and then sampled during a production run of at least 100,000 Monte Carlo steps at a temperature of 2573 °C. Symmetric surfaces were generated from the sampled structures as described in Burns et al.29 Bulk structure relaxations were performed, and the resulting relaxed structures were used to create supercells of dimensions 1 × 1 × 2. The relaxed bulk structures were used in the pristine slab calculations. To create O deficient slabs, one O atom was removed from the outermost top and bottom layer of relaxed pristine slabs, and a slab calculation was performed on the resulting O deficient slab. Slab dimensions in both the x- and y-directions were created at a minimum of 8 Å in order to avoid defect–defect interactions by the removed O and its periodic images.
Delithiating Structures
To identify low-energy Li vacancy orderings, we trained an L2 regularized least-squares regression model on total energies obtained from 33 DFT calculations of slabs with random orderings of Li vacancies, achieving a root mean squared error of 11 meV per atom. The regression model predicts an increase in the energy for clusters of Li vacancies and vacancy-F coordination. Furthermore, it predicts a lowering in energy for undercoordinated surface Li vacancies, in agreement with prior work.42 To sample structures with reasonable vacancy decorations, at least 1000 random Li vacancy orderings were generated, and our model was used to predict the energy of these structures. The final selected structures were sampled from the lowest predicted energy orderings.
Surface and Oxygen Evolution Energy Calculations
Surface energies were calculated as follows
| 1 |
where γ is surface energy, Eslab is the total energy output of the pristine slab calculation, N is the number of bulk layers in the supercell (two for all calculations here), Ebulk is the total energy of the bulk calculation of the parent bulk structure of each specific pristine slab, and A is the surface area of the pristine slab.
The ẼO was calculated according to the following equation
| 2 |
where
is the total
energy of the O deficient
slab, ΔμO is the corrected O chemical potential
as calculated by Wang et al. and Aykol et al.43,44 and Eslab is the total energy of the
pristine slab.
Boltzmann Weighted Oxygen Evolution Energy Calculations
To obtain a single value of the ẼO for each facet and delithiation state, Boltzmann weighting is performed according to the following equation
| 3 |
where ẼOBoltzmann is the Boltzmann weighted ẼO for a given facet and lithiation state, ẼOi is the ẼO of calculation i and wi is defined as
| 4 |
where Ωi is the multiplicity of surface i, Ei is the energy per atom of the pristine slab, E0 is the lowest per atom slab energy calculated for the given facet and delithiation state, kB is the Boltzmann constant and T is the temperature. The multiplicities were calculated similarly to the method in Burns et al.29 Statistics for each facet were taken from at least 1,000,000 structures generated by Monte Carlo. Laplace smoothing with an α value of 1 was applied to all multiplicities. As the number of possible surfaces is intractably large for direct calculation by DFT, we use a sample of the population of possible surfaces to estimate the ẼO on each facet and bootstrap our results to explore the possible ranges of energies that might have been found with a different sample.
Bonding Analysis
In order to analyze the bonding and antibonding character between the removed O atom and its nearest neighbor atoms, a Crystal Orbital Hamiltonian Population analysis was performed using the Local-Orbital Basis Suite Toward Electronic-Structure Reconstruction (LOBSTER) package.37−40 LOBSTER input parameters were generated using pymatgen, and all interactions within 6 Å were calculated. Results were obtained with less than 1% charge spilling, indicating that LOBSTER was able to transfer over 99% of the charge density from the occupied levels of the original wave functions obtained from DFT into the local basis chosen.
Results and Discussion
ẼO were calculated for the {100}, {110}, {111}, and {112} type facets of DRX Li2MnO2F at three lithiation states: 0, 25, and 50% delithiation. In total, 439 ẼO were calculated through first-principles methods. Figure 1 shows the energy spread of calculated ẼO for each facet and lithation state. Across facets, there is a consistent trend in decreasing ẼO as a function of decreasing Li content within Li2MnO2F.
Figure 1.
Calculated ẼO are shown for the {100}, {110}, {111}, and {112} type facets of DRX Li2MnO2F for the (a) 50% delithiated state Li1.0MnO2F, (b) 25% delithiated state Li1.5MnO2F, and (c) the fully lithated state Li2MnO2F. A small amount of jitter was added in the x direction for each point to ease viewing of the data. (d) The three lowest ẼO and their corresponding coordination environments and (e) the three highest ẼO and their coordination environments for the {100} type surface at the 50% delithiation state. Red atoms represent O, green atoms represent Li, and purple atoms represent Mn.
Previous work has shown that the equilibrium particle shape of Li2MnO2F is dominated by {100} type facets.29 O evolution has also been shown to more severely affect cathode materials at deeper states of delithiation.10 Hence, we choose the {100} type facet at the deepest delithiation level of 50% for a closer study. Selecting the three O ions with the highest/lowest ẼO, we examine the coordination environment, which is shown as an inset (d,e) in Figure 1. We find that the O with the highest evolution energies, ẼO, are relatively highly coordinated with a larger representation of Mn as nearest neighbors. In contrast, the O with the lowest ẼO are relatively sparsely coordinated and are mostly or entirely coordinated with Li.
Inspection of the ẼO, calculated for the {100} type surface at the 50% delithiation state, Figure 2a shows that there is a strong relationship between the ẼO and the proportion of Li-ions in the O coordination shell. A line of best fit and 95% confidence interval were calculated using Seaborn45 and Scikit-learn46 which predict that a change from 0 to 100% coordination by Li corresponds to a significant ẼO decrease of −4.43 eV. Similarly, and aligned with the findings of Seo et al.16 that Li–O–Li exhibit unhybridized Op states, the lowest ẼO in Figure 1d,e correspond to O almost entirely coordinated by Li and the highest ẼO correlate with relatively high occurrence of nearest neighbor Mn. Figure 2b shows that as the surface energy of a given surface increases, the ẼO decreases. Using Seaborn and Scikit-learn to create a line of best fit, the data predicts that for the {100} type surface at the 50% delithiation state, an increase in surface energy of 1 J/m2 would cause a corresponding, significant decrease of −4.60 eV. The surface energy provides a general measure of the stability of the surface, and hence, we expect that higher surface energies should correlate with a higher tendency toward O loss.
Figure 2.

Lines of best fit are shown for (a) the relationship between ẼO, and the percentage of Li nearest neighbors for the considered O and (b) the energy of the surface from which the O was removed. The light blue regions show a 95% confidence interval for the lines of best fit by bootstrapping the data resampling 1000 times. These data are both from the {100} type surface at the 50% delithiation state of Li1.0MnO2F.
Figure 3 depicts the Boltzmann weighted ẼO for Li2MnO2F for each facet at all three levels of lithiation next to the average ẼO found by Shin and Persson19 for the layered cathode material Li2MnO3. An area of inset (a) is magnified to more clearly show the cluster of points at the 50% delithiation state. Table 1 shows the values for each Boltzmann weighted ẼO of Li2MnO2F. While the ẼO quickly fall below zero in the case of Li2MnO3 as delithiation proceeds, the average ẼO remain positive for DRX Li2MnO2F, even at the 50% delithiation state, where just the {100}- and {111}-type facets approximately attain zero. Indeed, prior work10 supports our findings here by showing a strong correlation between F substitution for O and increased O retention.
Figure 3.
(a) Boltzmann weighted ẼO are shown for all facets and lithiation states. (b) A corresponding data set for the ordered, layered material Li2MnO3 showing the average ẼO is shown for comparison (adapted from Shin, Y.; Persson, K. A. Surface morphology and surface stability against oxygen loss of the lithium-excess Li2MnO3 cathode material as a function of lithium concentration. ACS Appl. Mater. Interfaces 2016,8, 25595–25602. Copyright [2016] American Chemical Society). A small amount of jitter was added to the x-value of each data point to ease viewing of the data, but each point was calculated at exactly the fully lithiated, 25 or 50% delithiation state. Error bars in (a) were calculated by bootstrapping the data resampling 1000 times and taking the standard deviation of the resulting samples. A magnification of the ẼO at the 50% delithiation state from the area indicated by the dashed box is shown in an inset in (a).
Table 1. Boltzmann Weighted ẼO for all Facets and Lithiation States at 298 K.
| Boltzmann weighted ẼO(eV) | |||
|---|---|---|---|
| facet | 50% | 75% | 100% |
| {100} | –0.001 | 0.36 | 2.23 |
| {110} | 0.20 | 1.19 | 2.17 |
| {111} | –0.04 | 2.20 | 2.54 |
| {112} | 0.37 | 0.91 | 2.69 |
Substituting O with F atoms has been shown to reduce O loss at the surface of DRX materials through multiple mechanisms. As reported in previous studies,47,48 substituting O2– ions with F– ions lowers the valence state of the Mn ions, allowing for more Mn redox and minimizing the participation of O2– for the same delithiation state. Second, Li–F surface decoration is more stable than O–Mn in Li2MnO2F, which means that surface oxygen is simply less abundant29 and, as shown here, reduces the oxygen release energy, ẼO. Here, we also investigate the role of F on the surface of Li2MnO2F in reducing the oxygen loss across different states of delithiation. Figure 4 shows the relationship between the percent of surface fluorine and ẼO. This relationship is investigated for the {100} surface at the fully lithiated, 25% delithiated, and 50% delithiated states. While there is clearly a large difference in protection against O loss by the presence of F when comparing fluorinated Li2MnO2F with its unfluorinated, layered counterpart Li2MnO3 as shown in Figure 3, Figure 4 shows that there is some variation in this protection from O loss which depends on the lithiation level. Lines of best fit and 95% confidence intervals were calculated using Seaborn45 showing that for all three delithiation levels, increasing levels of surface F predict a higher ẼO. However, calculating the slopes of these lines of best fit using Scikit-learn,46 we found the fluorine stabilizing effect subsides at higher levels of delithiation. A change from 0% surface F to 50% surface F at the fully lithiated state predicts an increase in ẼO of 2.6 eV, whereas the predicted increase in ẼO is only 1.9 eV for the 25% delithiation state and 1.1 eV for the 50% delithiation state. As delithiation proceeds, an increasing fraction of surface F is required to confer protection against oxygen loss.
Figure 4.

Lines of best fit are shown for the relationship between ẼO, and the percentage of surface fluorine for the {100} surface at the fully lithiated, 25% delithiated and 50% delithiated states. The light colored regions surrounding the lines of best fit show a 95% confidence interval for the lines of best fit by bootstrapping the data resampling 1000 times.
There are a few surfaces with negative ẼO even in their fully lithiated state. Examining these cases (see Figure 5), we find that the surface O pertaining to these specific data points is entirely coordinated by Li. Previous experimental work10 showed that fluorinated DRX cathodes do lose a small amount of O during their first cycle and then passivate against further O loss. We hypothesize, from our findings and in agreement with prior work that shows low O hybridization for Li–O–Li environments, that the O that are lost upon the first cycle are highly coordinated by Li.
Figure 5.

Coordination environments are shown for the O with evolution energies below 0 eV at the fully lithiated state Li2MnO2F. Red atoms represent the O, and green atoms represent Li.
LOBSTER was performed to analyze the bonding interactions of the O atom with its nearest neighbors for the O atoms with the highest and lowest ẼO calculated on the {100} type surface at the 50% delithiation state. Figure 6 shows (a) the total crystal orbital Hamiltonian population (COHP) and (b) total negative integrated crystal orbital Hamiltonian population (–ICOHP) for the highest and lowest ẼO calculated on the {100} type surface at the 50% delithiation state. The total includes all of the bonding interactions between the removed O atom and all of its nearest neighbors. The total COHP in (a) shows that the highest ẼO has more positive bonding interactions in both the deeper core states around −15 to −20 eV as well as some states just below the Fermi energy around −3 to −4 eV. As would be expected in b), the value of the –ICOHP has a larger value at the Fermi energy for the highest ẼO, indicating stronger bonding between the removed O atom and its nearest neighbor atoms.
Figure 6.
Total (a) COHP and (b) –ICOHP are shown for the highest and lowest ẼO calculated on the {100} type surface at the 50% delithiation state.
Prior work on bulk DRX and Li-excess layered cathodes have shown low O hybridization for Li–O–Li environments, which motivates a comparison with surface Li–O bonding interactions and associated trends for the ẼO. Figure 7 shows (a) the per-Li COHP and (b) the per-Li –ICOHP for the removed O atom and its nearest Li neighbors. Similar to the total COHP, the per-Li COHP shows that the O with the highest ẼO exhibit more positive bonding interactions with its nearest neighbor Li atoms in the deeper core state region than the lowest ẼO removed O. From Figure 7b, we observe that the per-Li atom –ICOHP has a lower value for the lowest ẼO at the Fermi level, indicating weaker bonding between the removed O atom and its nearest neighbor Li atoms. This weaker Li–O bond correlating with a lower ẼO, and hence a propensity to lose surface O, agrees with previous findings showing that weak Li–O interaction at higher levels of charge leads to O loss at the surface of DRX materials.
Figure 7.
Per-Li atom (a) COHP and (b) –ICOHP between the removed O and its nearest Li neighbors are shown for the highest and lowest ẼO calculated on the {100} type surface at the 50% delithiation state.
From Figure 3a, we observe that, while the Boltzmann weighted ẼO are very similar for all facets studied at the 50% delithiation state (xLi = 1.00), the {112} and {110} remain the most robust to O loss. We note that previous work29 showed that the thermodynamic equilibrium particle shape for DRX Li2MnO2F is dominated by {100} type surfaces and enriched in Li/F. In light of the findings here that Li-coordinated, surface-exposed O on {100} is less resilient against gassing during delithiation, there may be interest in exploring different synthesis conditions and their respective resulting particle morphologies; particularly with the goal of maximizing the exposure of {112} and {110} surface facets.
Conclusions
Over 400 first-principles calculations and Boltzmann weighted oxygen evolution energies (ẼO) for 159 unique surface terminations of the four majority facets; {100}, {110}, {111}, and {112} type surfaces at the fully lithiated, 25% delithiated, and 50% delithiated states of DRX Li2MnO2F are presented. In agreement with previous work, ẼO drop as delithiation progresses. However, in contrast to chemically similar layered and nonfluorinated materials, DRX Li2MnO2F is predicted to remain much more robust to O loss. At the 50% delithiated state, the {110} and {112} facets were the most resilient to O loss. Examining the {100} surface, it was found that a higher degree of Li coordination correlates strongly with thermodynamic susceptibility toward O loss. The role of surface fluorine in protecting against O loss was also examined. While fluorine generally stabilizes against oxygen loss, we found that the effect subsides as a function of delithiation, for example higher levels of surface of fluorine is needed to achieve the same effect on ẼO at higher states of charge. The cases with highest and lowest ẼO were examined for electronic structure trends, and their bonding analyzed with the LOBSTER software. Higher ẼO was shown to have an overall higher –ICOHP at the Fermi level which indicates overall stronger bonding. In agreement with previous work examining Li–O bonding, our LOBSTER results show that a lower per-Li –ICOHP at the Fermi level between the removed O and its Li nearest neighbors, and hence weaker bonding interactions, is correlated with a lower ẼO and therefore increases the risk of surface O loss.
Acknowledgments
This work was supported by the Assistant Secretary for Energy Efficiency and Renewable Energy, Vehicle Technologies Office, of the U.S. Department of Energy under Contract no. DEAC02-05CH11231 and DE-LC-000L053 under the program of Next Generation Cathode. This research also used resources of the National Energy Research Scientific Computing Center (NERSC), a U.S. Department of Energy Office of Science User Facility located at Lawrence Berkeley National Laboratory, operated under contract no. DE-AC02-05CH11231. The authors would like to thank Jianli Cheng, Caitlin McCandler, Oxana Andriuc, and Ruoxi Yang for stimulating conversations about surfaces and Alex Epstein for always answering questions about figures and LaTeX.
The authors declare no competing financial interest.
References
- Working Group II Contribution to the Sixth Assessment Report of the Intergovernamental Panel on Climate Change; Pörtner H.-O., Roberts D., Poloczanska E., Mintenbeck K., Tignor M., Alegría A., Craig M., Langsdorf S., Löschke S., Möller V., Okem A., Eds.; Cambridge University Press, 2022; pp 3–33. [Google Scholar]
- Olivetti E. A.; Ceder G.; Gaustad G. G.; Fu X. Lithium-Ion Battery Supply Chain Considerations: Analysis of Potential Bottlenecks in Critical Metals. Joule 2017, 1, 229–243. 10.1016/j.joule.2017.08.019. [DOI] [Google Scholar]
- Lee J.; Urban A.; Li X.; Su D.; Hautier G.; Ceder G. Unlocking the potential of cation-disordered oxides for rechargeable lithium batteries. Science 2014, 343, 519–522. 10.1126/science.1246432. [DOI] [PubMed] [Google Scholar]
- Clément R. J.; Lun Z.; Ceder G. Cation-disordered rocksalt transition metal oxides and oxyfluorides for high energy lithium-ion cathodes. Energy Environ. Sci. 2020, 13, 345–373. 10.1039/C9EE02803J. [DOI] [Google Scholar]
- Chen D.; Ahn J.; Chen G. An Overview of Cation-Disordered Lithium-Excess Rocksalt Cathodes. ACS Energy Lett. 2021, 6, 1358–1376. 10.1021/acsenergylett.1c00203. [DOI] [Google Scholar]
- Richards W. D.; Dacek S. T.; Kitchaev D. A.; Ceder G. Fluorination of Lithium-Excess Transition Metal Oxide Cathode Materials. Adv. Energy Mater. 2018, 8, 1701533. 10.1002/aenm.201701533. [DOI] [Google Scholar]
- House R. A.; Jin L.; Maitra U.; Tsuruta K.; Somerville J. W.; Förstermann D. P.; Massel F.; Duda L.; Roberts M. R.; Bruce P. G. Lithium manganese oxyfluoride as a new cathode material exhibiting oxygen redox. Energy Environ. Sci. 2018, 11, 926–932. 10.1039/C7EE03195E. [DOI] [Google Scholar]
- Lee J.; Papp J. K.; Clément R. J.; Sallis S.; Kwon D.-H.; Shi T.; Yang W.; McCloskey B. D.; Ceder G. Mitigating oxygen loss to improve the cycling performance of high capacity cation-disordered cathode materials. Nat. Commun. 2017, 8, 981. 10.1038/s41467-017-01115-0. [DOI] [PMC free article] [PubMed] [Google Scholar]
- Ahn J.; Chen D.; Chen G. A Fluorination Method for Improving Cation-Disordered Rocksalt Cathode Performance. Adv. Energy Mater. 2020, 10, 2001671. 10.1002/aenm.202001671. [DOI] [Google Scholar]
- Crafton M. J.; Yue Y.; Tong W.; McCloskey B. D.; McCloskey B. D. Anion Reactivity in Cation-Disordered Rocksalt Cathode Materials: The Influence of Fluorine Substitution. Adv. Energy Mater. 2020, 10, 2001500. 10.1002/aenm.202001500. [DOI] [Google Scholar]
- Lebens-Higgins Z.; Chung H.; Temprano I.; Zuba M.; Wu J.; Rana J.; Mejia C.; Jones M. A.; Wang L.; Grey C. P.; Du Y.; Yang W.; Meng Y. S.; Piper L. F. J. Electrochemical Utilization of Iron IV in the Li 1.3 Fe 0.4 Nb 0.3 O 2 Disordered Rocksalt Cathode. Batteries Supercaps 2021, 4, 771–777. 10.1002/batt.202000318. [DOI] [Google Scholar]
- Chen D.; Kan W. H.; Chen G. Understanding Performance Degradation in Cation-Disordered Rock-Salt Oxide Cathodes. Adv. Energy Mater. 2019, 9, 1901255. 10.1002/aenm.201901255. [DOI] [Google Scholar]
- Yue Y.; Li N.; Li L.; Foley E. E.; Fu Y.; Battaglia V. S.; Clément R. J.; Wang C.; Tong W. Redox Behaviors in a Li-Excess Cation-Disordered Mn-Nb-O-F Rocksalt Cathode. Chem. Mater. 2020, 32, 4490–4498. 10.1021/acs.chemmater.9b05221. [DOI] [Google Scholar]
- Lee E.; Persson K. A. Structural and Chemical Evolution of the Layered Li-Excess LixMnO3 as a Function of Li Content from First-Principles Calculations. Adv. Energy Mater. 2014, 4, 1400498. 10.1002/aenm.201400498. [DOI] [Google Scholar]
- Dogan F.; Croy J. R.; Balasubramanian M.; Slater M. D.; Iddir H.; Johnson C. S.; Vaughey J. T.; Key B. Solid State NMR Studies of Li 2 MnO 3 and Li-Rich Cathode Materials: Proton Insertion, Local Structure, and Voltage Fade. J. Electrochem. Soc. 2015, 162, A235–A243. 10.1149/2.1041501jes. [DOI] [Google Scholar]
- Seo D.-H.; Lee J.; Urban A.; Malik R.; Kang S.; Ceder G. The structural and chemical origin of the oxygen redox activity in layered and cation-disordered Li-excess cathode materials. Nat. Chem. 2016, 8, 692–697. 10.1038/nchem.2524. [DOI] [PubMed] [Google Scholar]
- McCalla E.; Abakumov A. M.; Saubanère M.; Foix D.; Berg E. J.; Rousse G.; Doublet M. L.; Gonbeau D.; Novák P.; Van Tendeloo G.; et al. Visualization of O-O peroxo-like dimers in high-capacity layered oxides for Li-ion batteries. Science 2015, 350, 1516–1521. 10.1126/science.aac8260. [DOI] [PubMed] [Google Scholar]
- Qian D.; Xu B.; Chi M.; Meng Y. S. Uncovering the roles of oxygen vacancies in cation migration in lithium excess layered oxides. Phys. Chem. Chem. Phys. 2014, 16, 14665–14668. 10.1039/C4CP01799D. [DOI] [PubMed] [Google Scholar]
- Shin Y.; Persson K. A. Surface Morphology and Surface Stability against Oxygen Loss of the Lithium-Excess Li 2 MnO 3 Cathode Material as a Function of Lithium Concentration. ACS Appl. Mater. Interfaces 2016, 8, 25595–25602. 10.1021/acsami.6b07259. [DOI] [PubMed] [Google Scholar]
- Hu W.; Wang H.; Luo W.; Xu B.; Ouyang C. Formation and thermodynamic stability of oxygen vacancies in typical cathode materials for Li-ion batteries: Density functional theory study. Solid State Ionics 2020, 347, 115257. 10.1016/j.ssi.2020.115257. [DOI] [Google Scholar]
- Sharpe R.; House R. A.; Clarke M. J.; Förstermann D.; Marie J. J.; Cibin G.; Zhou K. J.; Playford H. Y.; Bruce P. G.; Islam M. S. Redox Chemistry and the Role of Trapped Molecular O2in Li-Rich Disordered Rocksalt Oxyfluoride Cathodes. J. Am. Chem. Soc. 2020, 142, 21799–21809. 10.1021/jacs.0c10270. [DOI] [PMC free article] [PubMed] [Google Scholar]
- Xiao P.; Shi T.; Huang W.; Ceder G. Understanding surface densified phases in Ni-rich layered compounds. ACS Energy Lett. 2019, 4, 811–818. 10.1021/acsenergylett.9b00122. [DOI] [Google Scholar]
- Mukherjee P.; Faenza N. V.; Pereira N.; Ciston J.; Piper L. F.; Amatucci G. G.; Cosandey F. Surface Structural and Chemical Evolution of Layered LiNi0.8Co0.15Al0.05O2 (NCA) under High Voltage and Elevated Temperature Conditions. Chem. Mater. 2018, 30, 8431–8445. 10.1021/acs.chemmater.7b05305. [DOI] [Google Scholar]
- Kwon D. H.; Lee J.; Artrith N.; Kim H.; Wu L.; Lun Z.; Tian Y.; Zhu Y.; Ceder G. The Impact of Surface Structure Transformations on the Performance of Li-Excess Cation-Disordered Rocksalt Cathodes. Cell Rep. Phys. Sci. 2020, 1, 100187. 10.1016/j.xcrp.2020.100187. [DOI] [Google Scholar]
- McColl K.; House R. A.; Rees G. J.; Squires A. G.; Coles S. W.; Bruce P. G.; Morgan B. J.; Islam M. S. Transition metal migration and O2 formation underpin voltage hysteresis in oxygen-redox disordered rocksalt cathodes. Nat. Commun. 2022, 13, 5275–5278. 10.1038/s41467-022-32983-w. [DOI] [PMC free article] [PubMed] [Google Scholar]
- Park K.-Y.; Zhu Y.; Torres-Castanedo C. G.; Jung H. J.; Luu N. S.; Kahvecioglu O.; Yoo Y.; Seo J. W. T.; Downing J. R.; Lim H. D.; Bedzyk M. J.; Wolverton C.; Hersam M. C. Elucidating and Mitigating High-Voltage Degradation Cascades in Cobalt-Free LiNiO2 Lithium-Ion Battery Cathodes. Adv. Mater. 2022, 34, 2106402. 10.1002/adma.202106402. [DOI] [PubMed] [Google Scholar]
- Shin Y.; Kan W. H.; Aykol M.; Papp J. K.; McCloskey B. D.; Chen G.; Persson K. A. Alleviating oxygen evolution from Li-excess oxide materials through theory-guided surface protection. Nat. Commun. 2018, 9, 4597–4611. 10.1038/s41467-018-07080-6. [DOI] [PMC free article] [PubMed] [Google Scholar]
- Ning F.; Shang H.; Li B.; Jiang N.; Zou R.; Xia D. Surface thermodynamic stability of Li-rich Li2MnO3: Effect of defective graphene. Energy Storage Mater. 2019, 22, 113–119. 10.1016/j.ensm.2019.01.004. [DOI] [Google Scholar]
- Burns J.; Ouyang B.; Cheng J.; Horton M. K.; Siron M.; Andriuc O.; Yang R.; Ceder G.; Persson K. A. Equilibrium Particle Shape and Surface Chemistry of Disordered Li-Excess, Mn-Rich Li-ion Cathodes through First-Principles Modeling. Chem. Mater. 2022, 34, 7210–7219. 10.1021/acs.chemmater.2c00804. [DOI] [Google Scholar]
- Ouyang B.; Artrith N.; Lun Z.; Jadidi Z.; Kitchaev D. A.; Ji H.; Urban A.; Ceder G. Effect of Fluorination on Lithium Transport and Short-Range Order in Disordered-Rocksalt-Type Lithium-Ion Battery Cathodes. Adv. Energy Mater. 2020, 10, 1903240. 10.1002/aenm.201903240. [DOI] [Google Scholar]
- Kresse G.; Hafner J. Ab initio molecular dynamics for liquid metals. Phys. Rev. B: Condens. Matter Mater. Phys. 1993, 47, 558–561. 10.1103/PhysRevB.47.558. [DOI] [PubMed] [Google Scholar]
- Kresse G.; Hafner J. Ab initio molecular-dynamics simulation of the liquid-metalamorphous- semiconductor transition in germanium. Phys. Rev. B: Condens. Matter Mater. Phys. 1994, 49, 14251–14269. 10.1103/PhysRevB.49.14251. [DOI] [PubMed] [Google Scholar]
- Kresse G.; Furthmüller J. Efficiency of ab-initio total energy calculations for metals and semiconductors using a plane-wave basis set. Comput. Mater. Sci. 1996, 6, 15–50. 10.1016/0927-0256(96)00008-0. [DOI] [PubMed] [Google Scholar]
- Kresse G.; Furthmüller J. Efficient iterative schemes for ab initio total-energy calculations using a plane-wave basis set. Phys. Rev. B: Condens. Matter Mater. Phys. 1996, 54, 11169–11186. 10.1103/PhysRevB.54.11169. [DOI] [PubMed] [Google Scholar]
- Blöchl P. E. Projector augmented-wave method. Phys. Rev. B: Condens. Matter Mater. Phys. 1994, 50, 17953–17979. 10.1103/PhysRevB.50.17953. [DOI] [PubMed] [Google Scholar]
- Perdew J. P.; Burke K.; Ernzerhof M. Generalized gradient approximation made simple. Phys. Rev. Lett. 1996, 77, 3865–3868. 10.1103/PhysRevLett.77.3865. [DOI] [PubMed] [Google Scholar]
- Maintz S.; Deringer V. L.; Tchougréeff A. L.; Dronskowski R. Analytic projection from plane-wave and PAW wavefunctions and application to chemical-bonding analysis in solids. J. Comput. Chem. 2013, 34, 2557–2567. 10.1002/jcc.23424. [DOI] [PubMed] [Google Scholar]
- Deringer V. L.; Tchougréeff A. L.; Dronskowski R. Crystal orbital Hamilton population (COHP) analysis as projected from plane-wave basis sets. J. Phys. Chem. A 2011, 115, 5461–5466. 10.1021/jp202489s. [DOI] [PubMed] [Google Scholar]
- Dronskowski R.; Bloechl P. E. Crystal orbital Hamilton populations (COHP): energy-resolved visualization of chemical bonding in solids based on density-functional calculations. J. Phys. Chem. 1993, 97, 8617–8624. 10.1021/j100135a014. [DOI] [Google Scholar]
- Maintz S.; Deringer V. L.; Tchougréeff A. L.; Dronskowski R. LOBSTER: A tool to extract chemical bonding from plane-wave based DFT. J. Comput. Chem. 2016, 37, 1030–1035. 10.1002/jcc.24300. [DOI] [PMC free article] [PubMed] [Google Scholar]
- Ong S. P.; Richards W. D.; Jain A.; Hautier G.; Kocher M.; Cholia S.; Gunter D.; Chevrier V. L.; Persson K. A.; Ceder G. Python Materials Genomics (pymatgen): A robust, open-source python library for materials analysis. Comput. Mater. Sci. 2013, 68, 314–319. 10.1016/j.commatsci.2012.10.028. [DOI] [Google Scholar]
- Duy T. V. T.; Ohwaki T.; Ikeshoji T.; Inoguchi Y.; Imai H. High-Throughput Computational Approach to Li/Vacancy Configurations and Structural Evolution during Delithiation: The Case of Li2MnO3 Surface. J. Phys. Chem. C 2018, 122, 5496–5508. 10.1021/acs.jpcc.7b12275. [DOI] [Google Scholar]
- Wang L.; Maxisch T.; Ceder G. Oxidation energies of transition metal oxides within the GGA+U framework. Phys. Rev. B: Condens. Matter Mater. Phys. 2006, 73, 195107–195116. 10.1103/physrevb.73.195107. [DOI] [Google Scholar]
- Aykol M.; Wolverton C. Local environment dependent GGA+U method for accurate thermochemistry of transition metal compounds. Phys. Rev. B: Condens. Matter Mater. Phys. 2014, 90, 115105–115118. 10.1103/physrevb.90.115105. [DOI] [Google Scholar]
- Waskom M. Seaborn: Statistical Data Visualization. J. Open Source Softw. 2021, 6, 3021. 10.21105/joss.03021. [DOI] [Google Scholar]
- Pedregosa F.; et al. Scikit-learn: Machine learning in Python. J. Mach. Learn. Res. 2011, 12, 2825–2830. [Google Scholar]
- Lee J.; Kitchaev D. A.; Kwon D.-H.; Lee C.-W.; Papp J. K.; Liu Y.-S.; Lun Z.; Clément R. J.; Shi T.; McCloskey B. D.; Guo J.; Balasubramanian M.; Ceder G. Reversible Mn2+/Mn4+ double redox in lithium-excess cathode materials. Nature 2018, 556, 185–190. 10.1038/s41586-018-0015-4. [DOI] [PubMed] [Google Scholar]
- Lun Z.; Ouyang B.; Kitchaev D. A.; Clément R. J.; Papp J. K.; Balasubramanian M.; Tian Y.; Lei T.; Shi T.; McCloskey B. D.; Lee J.; Ceder G. Improved Cycling Performance of Li-Excess Cation-Disordered Cathode Materials upon Fluorine Substitution. Adv. Energy Mater. 2019, 9, 1802959. 10.1002/aenm.201802959. [DOI] [Google Scholar]




