Adwitiya Raoa,
Jacob Rempel
a,
Ming Jiang
b,
Parvin Adelic,
Chae-Ho Yim
d,
Mohamed Houached,
Yaser Abu-Lebdehd and
Chandra Veer Singh
*ae
aDepartment of Materials Science and Engineering, University of Toronto, Toronto, Ontario M5S 3E4, Canada. E-mail: chandraveer.singh@utoronto.ca
bInstitute of Physical Science and Information Technology, Anhui University Hefei, Hefei 230601, China
cDepartment of Chemistry, Department of Chemical Engineering and the Waterloo Institute for Nanotechnology, University of Waterloo, Waterloo, Ontario N2L 3G1, Canada
dEnergy, Mining, and Environment Research Centre, National Research Council of Canada, 1200 Montreal Road, Ottawa, Ontario K1A 0R6, Canada
eDepartment of Mechanical and Industrial Engineering, University of Toronto, 5 King's College Road, Toronto, Ontario M5S 3G8, Canada
First published on 29th April 2025
Halogen substitution has been a widely accepted strategy to boost ionic conductivity of lithium argyrodites. Mixed halide argyrodites containing Cl and Br have been shown to be promising candidates as solid electrolytes, featuring high room temperature ionic conductivities >10 mS cm−1. This study focuses on the less explored halide-rich Cl–I mixed halide argyrodites as solid-state electrolytes, comparing them to their Cl–Br analogues. DFT calculations reveal that Cl–I argyrodites possess enhanced phase stability and electrode compatibility. Despite differences in the type of halogen used, Cl–I and Cl–Br argyrodites exhibit similar ionic conductivities at equivalent Cl/X (X = Br, I) ratios. AIMD simulations of Li5.5PS4.5Cl1.5−xIx systems identify an optimal I and Cl content of 0.75 each, yielding a maximum conductivity of 23.5 mS cm−1, attributed to enlarged Li+ migration channels.
One of the most notable compound groups for applications in SSEs are sulfide-based lithium argyrodites which have shown great progress in recent years through the discovery of compounds featuring very high ionic conductivities. By making use of various cationic and anionic substitution strategies, several compounds have been discovered with ionic conductivities in the range of 10−4–10−2 S cm−1.7 Amongst all other strategies, halogen substituted lithium argyrodites, i.e. Li7−yPS6−yXy (X = Cl, Br, I) have been more popular. This is due to the resulting lithium vacancies generated when halogens are added and the S−2/X− anionic site disorder, which occurs in argyrodites substituted with Cl and Br anions, where the halogens, to some degree, swap their 4a crystallographic positions with 4d sites of S−2 ions, due to being similar in size. This shift results in a modification of the energy landscape for Li+ ions, which results in better transport kinetics. Such a phenomenon is absent in the case of I− anions as they only occupy 4a crystallographic positions in the structure.8 Previous experimental studies have reported an ionic conductivity value of 1.9 mS cm−1 for Li6PS5Cl and 0.7 mS cm−1 for Li6PS5Br. However, depending on the synthetic method used, the ionic conductivity could be increased to ∼3.1 mS cm−1 for both Li6PS5Cl and Li6PS5Br.9,10
Based on the halogen substitution strategy to generate lithium vacancies, excess halogen substituted or halide-rich argyrodites of the type Li6−xPS5−xX1+x (0 < x < 0.5) have also been studied. Out of all the compounds, Li5.5PS4.5Cl1.5 exhibited the best performance, reaching an experimental ionic conductivity value of 12 mS cm−1. Synthesizing a pure crystalline phase of Li6−xPS5−xX1+x (X = Br, I) proved to be difficult due to the large anionic size and the formation of LiX (X = Br, I) phase which negatively affected ionic conductivity.11 Yu et al. were able to create a stable Li5.5PS4.5Br1.5 phase, which exhibited an ionic conductivity of 4.35 mS cm−1.12 Zhang et al. were able to synthesize a stable Li5.5PS4.5I1.5, which had an ionic conductivity of 0.31 mS cm−1.13 Other literature studies on similar single halogen substitution strategies involve an addition of other elements such as Si, Ge, Sb, or Se for boosting conductivity via vacancy generation, change in anionic polarizability etc.14–16
Mixed halide rich argyrodites have gained significant popularity in recent years, with argyrodites containing 2 or more halogens substituted in the structure which have yielded ionic conductivity values greater than 10 mS cm−1. Experimental and computational studies done on Li6−xPS5−xClBrx showed that Li5.3PS4.3ClBr0.7 was the best choice amongst other candidates in the family, with an ionic conductivity of 24 mS cm−1 at room temperature with a low lithium ion migration barrier.17 Li et al. conducted a thorough exploration of the Li5.5PS4.5Cl1.5−xBrx chemical space, establishing the role of configurational entropy in boosting ionic conductivity of these systems, and discovering a novel Li5.5PS4.5Cl0.8Br0.7 phase exhibiting a bulk ionic conductivity of 22.7 mS cm−1.18 There have been limited experimental studies on Cl–I mixed halide rich compositions. Most notably, Li5.4PS4.4Cl1.4I0.2 and Li5.6PS4.6Cl1.3I0.1 with an ionic conductivity of 16.43 and 10.45 mS cm−1 respectively.19,20
Although mixed halide substitution strategies show a lot of promise, there exist a few unanswered questions which demand exploration. In this work, we focus on the less explored Cl–I mixed halide argyrodite chemical space, to evaluate and compare their performance with the widely explored Cl–Br chemical space. In the first section, ground state calculations revealed that Cl–I mixed argyrodites exhibited a better overall stability than their Cl–Br analogues due to their low energy phase equilibrium compounds and lower charge per unit volume leading to lower electrostatic repulsions in the structure. Furthermore, interface reaction energy calculations show that Cl–I mixed compounds have a slight edge in terms of compatibility with commercial electrodes. AIMD simulations showed that despite having different halogens altogether, both Cl–I and Cl–Br mixed argyrodites exhibited similar ionic conductivity, if the composition ratios of Cl/Br and Cl/I are the same. Lastly, AIMD simulations were conducted to understand the effect of varying I/Cl ratios on ionic conductivity for Li5.5PS4.5Cl1.5−xIx systems. The maximum ionic conductivity of 23.5 mS cm−1 was achieved for x = 0.75, due to this composition having the maximum average Li Voronoi polyhedron volume, indicating wide migration channels. To this end, these results may be used to complement experimental work, to provide a sense of direction to researchers working on screening different formulations of these mixed halide rich Cl–I argyrodites.
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To keep the computational costs reasonable, 4a/4d antisite site disorder between Cl− and S2− ions have been avoided. Halogen substitutions were carried out on 4d sites containing S2− ions, with Cl, Br and I atoms with rigorous enumeration. These structures were optimized using DFT and the structures with minimum energy was considered for further analysis and AIMD simulations. It was found that both Br and I atoms preferred 4a sites over 4d sites, with the difference in energy being 0.14 eV per atom and 0.35 eV per atom for Br and I respectively. This site selectivity is due to the higher ionic radius of Br− and I− ions, as compared to S−2 and Cl− ions.
The variation in Energy above convex hull (Ehull) and formation energy with respect to halogen composition in shown in Fig. 1(b). Although perfectly stable compounds are on the convex hull, with energy above hull equal to 0, we consider a threshold value of 40 meV per atom for determining stable argyrodite configurations. This is because most of the compounds in ICSD were determined to have Ehull < 36, which means that some of these compounds could be stabilized via entropic effects.28,29 The obtained energy above hull (Ehull) value of 24 meV for Li6PS5Cl is in good agreement with the literature value of 21 meV.25 We observe that for pure Cl substitution case the Ehull increases to 28 meV for Li5.5PS4.5Cl1.5. However, we observe that addition of Br leads to a slight decrease in Ehull and addition of I results in a decrease in Ehull resulting in the most phase stable configurations, with Li5.5PS4.5ClI0.5 being the most phase stable compounds out of all with Ehull value of 18 meV. This implies that the addition of small amounts of larger halogens such as Br and especially I result in the formation of stable configurations. The phase decomposition products for all argyrodites were Li3PS4, Li2S and LiX (X = Cl, Br, I). Therefore, in this case Ehull = Ef(argyrodite) − (aEf(Li3PS4) + bEf(Li2S) + cEf(LiX)), where Ef denotes formation energy and a, b, c are constants. As documented in the Materials Project,30 the formation energy for LiX follows the order of LiCl > LiBr > LiI (ELiCl = −2.03 eV per atom, ELiBr = −1.83 eV per atom, ELiI = −1.39 eV per atom). Despite Li–Cl and Li–Br interactions being energetically more favorable for the argyrodites than Li–I interactions, as evidenced by slightly lower formation energies for I-substituted systems, the resulting Ehull value was still lower than their Cl and Br-substituted counterparts. To better understand this phenomenon, Bader charge calculations were conducted for all halides with a total halogen content of 1.5, to determine the average Bader charge and Bader charge per unit volume as documented in Table 1.
Material | QCl (|e|) | QCl (|e| Å−3) | QBr (|e|) | QBr(|e| Å−3) | QI (|e|) | QI (|e| Å−3) |
---|---|---|---|---|---|---|
Li5.5PS4.5Cl1.5 | −0.898 | −0.0232 | — | — | — | — |
Li5.5PS4.5ClBr0.5 | −0.897 | −0.0231 | −0.889 | −0.0202 | — | — |
Li5.5PS4.5ClI0.5 | −0.897 | −0.0231 | — | — | −0.857 | −0.0163 |
An increase in halogen content would lead to an increase in electrostatic repulsion in the anionic sublattice which could affect the stability of the system. A lower Bader charge for Li5.5PS4.5ClI0.5 as compared to Li5.5PS4.5Cl1.5 and Li5.5PS4.5ClBr0.5 indicated a lower charge polarization in this system. This resulted in a lower charge per unit volume for Li5.5PS4.5ClI0.5 systems which caused the decrease of overall electrostatic repulsion in the anionic sublattice of these systems. As a result of this phenomenon, despite Li–Cl and Li–Br interactions being much stronger than Li–I interactions, the formation energy for I-substituted systems did not decrease significantly. This phenomenon combined with lower energy phase decomposition products, resulted in a higher phase stability of I-substituted systems as compared to Cl and Br-substituted systems.
Band structures were determined as shown in Fig. 1(c) and (d) for Li5.5PS4.5ClBr0.5 and Li5.5PS4.5ClI0.5, respectively. Band structures for all other compounds of study are shown in Fig. S1 in the ESI.† The bandgap for Li5.5PS4.5ClBr0.5 was 2.19 eV, which was lower than the value of 2.32 eV for Li5.5PS4.5ClI0.5. A larger bandgap is desirable for application in solid-state batteries, as it prevents leakage of electrons and increases dendrite formation resistance, resulting in an increased stability. Overall, all compounds exhibited poor electronic conductivity and were sufficiently insulating for application as solid-state electrolytes, with Li5.5PS4.5ClI0.5 being the best candidate amongst all of them.
The electrode compatibility of all compounds with common cathodes like LiCoO2, LiFePO4 or sulfur (S) with their lithiated/delithiated configurations were studied to determine the practical applicability of these materials as solid electrolytes. All detailed results for have been provided in Tables S2–S4 (ESI†).
The reaction energy for each argyrodite composition with respective cathode materials has been shown in Fig. 2. In the case of LiCoO2 and Li0.5CoO2, the interfacial reaction energy is quite high, which makes argyrodites an unsuitable class of materials for this type of cathode. Furthermore, the delithiated variant Li0.5CoO2, showed much higher reaction energies, which implied that the cathode would become even more susceptible to degradation during the beginning of discharge and end of charge cycles. The general trend that was observed was that reaction energy increased with an increase in halogen content in the system. However, for all systems, I-substituted compounds performed slightly better as the reaction products included LiX (X = Cl, Br, I), and as discussed before, due to LiI having the lowest formation energy, the energy of reaction for I-substituted compounds was slightly lower.
In the case of LiFePO4/FePO4, the reaction energy was much lower, making LiFePO4 a better cathode material than LiCoO2. Similar trend of delithiated FePO4 having higher reaction energy than LiFePO4 was observed, but the overall reaction energies were still much lower than LiCoO2. In these systems, however, an increased halogen content showed a lower reaction energy. This could be due to the lower concentration of sulfur in these systems, due to Fe having a high affinity for S atoms. Amongst Cl, Br and I rich halogen compounds, I-substituted compounds had a better edge due to LiI formation with LiFePO4 and I2 formation with FePO4, both having lower formation energies than LiCl/LiBr.
For S cathodes, the reaction energies were higher than LiFePO4 but were in the range of FePO4. However, the lithiated variant Li2S showed no interfacial reaction with any argyrodite, thereby making argyrodites an excellent material of choice for batteries with S cathodes. In this case however, Cl-rich argyrodites performed slightly better than Br and I-substituted argyrodites due to the formation of low energy side products such as SCl, SBr and I2. However, both Br and I-substituted compounds exhibited similar performance with the S electrode.
Overall, the ground state calculations highlighted an increased phase stability and slightly better electrode compatibility for Cl–I mixed halide systems as compared to their Cl–Br analogues, for the same I/Cl and Br/Cl ratios. Furthermore, for a deeper comparison of both material classes, AIMD simulations were conducted to ascertain the Li+ ion transport characteristics in these systems.
The log plot of diffusivity vs. temperature and ionic conductivities vs. total halogen mole fraction is shown in Fig. 3a and b, respectively. The AIMD simulations showed that the ionic conductivity of Li6PS5Cl, Li5.75PS4.75Cl1.25 and Li5.5PS4.5Cl1.5 was 1.33 mS cm−1, 4.69 mS cm−1, and 18.86 mS cm−1, respectively. We obtained a good fit for the experimental conductivity for Li6PS6Cl and Li5.75PS4.75Cl1.25 obtained by Adeli et al., which was 2.5 mS cm−1 and 4.2 mS cm−1 respectively.11 The predicted ionic conductivity for Li5.5PS4.5Cl1.5 was slightly higher than the literature value of 12 mS cm−1, however, both were in the order of 10 mS cm−1. There are multiple factors that could have resulted in this difference. Firstly, Li+ ionic conductivity was determined from diffusivity at high temperatures using Arrhenius law, which could cause the resulting variation. Secondly, in the experimental structure, Cl− ions have shown to occupy both 4a and 4c sites, whereas, we have only considered 4a sites, based on the reference ICSD structure. Moreover, 4a/4d site disorder has not been considered in this work due to simplicity. These slight structural variations could also result in discrepancies in ionic conductivity. Lastly, synthesis methods, macroscopic conditions and different time scales of measurements could also result in the resulting difference. For the mixed halide system, we compare the AIMD results with the available data for Li5.5PS4.5ClBr0.5. The calculated conductivity of 15.79 mS cm−1 was in good agreement with the experimental conductivity of 17 mS cm−1.
To further understand the effect of change in Li transport behavior by the addition of larger halogens in the structure, the radial distribution of Li atoms around anions at 600 K, was plotted for Li5.5PS4.5ClBr0.5 and Li5.5PS4.5ClI0.5, as shown in Fig. 3(c) and (d) respectively. Although average Li clustering was highest around Cl− ions, the peaks for Br− and I− showed significant clustering of Li around these ions showing high Li–Br and Li–I interactions. An increase in concentration of Br and I would further increase these interactions, resulting in sluggish diffusion kinetics.31 Li5.5PS4.5ClBr0.5 showed a slightly lower ionic conductivity than Li5.5PS4.5ClI0.5 as both systems had polarizable ions and the latter had a smaller RDF peak for I− ions which implied lesser Li–I interactions as compared to Li–Br interactions in Li5.5PS4.5ClBr0.5. However, it is to be noted that irrespective of the type of halogen, all argyrodites with total halogen content = 1.5 exhibited ionic conductivities in the order of 10 mS cm−1 which makes them perfectly suitable for application as solid electrolytes. Despite the small difference in ionic conductivities of Li5.5PS4.5ClBr0.5 and Li5.5PS4.5ClI0.5, it was not significant enough to claim that Cl–I mixed argyrodites outperformed Cl–Br systems in terms of ionic transport. However, due to Cl–Br and Cl–I systems showing very similar ionic conductivities for similar Br/Cl and I/Cl ratios, we can expect these systems to exhibit similar ionic conductivities despite having different halogens, if their element ratios with respect to Cl in the system and total halogen content were the same.
Voronoi method was used to determine the Li+ coordination polyhedron, to understand the structure–property relationship governing ionic conductivity in these systems. A larger polyhedron volume would indicate wider migration channels for the Li+ ion to move through the lattice, resulting in a lower activation barrier, boosting ionic conductivity. Fig. 4(b) shows the variation of the average volume of Li+ ion coordination polyhedron and ionic conductivity with varying I/Cl ratios. The average volume shows an increasing–decreasing trend, like ionic conductivity, maximizing for the equiatomic Cl–I composition at 9.39 Å3. The structures undergo lattice expansion due to the addition of I atoms into the structure, which is the main cause of this volume increase, which explains the increasing trend and widening of the migration channels. However, for x > 0.75, the addition of I into the structure resulted in a decrease in average polyhedron volume which is unexpected, as substitution of smaller Cl atoms with larger I atoms would result in lattice expansion. To understand this phenomenon, each Li+ coordination polyhedron was analyzed separately to highlight the effect of local disorder due to structural mismatch caused by mixed halide substitution. Fig. 4(d) shows a schematic of a Li+ coordination polyhedron in Li5.5PS4.5Cl1.25I0.25 and Fig. 4(e)–(g) show individual histograms capturing the overall polyhedron volume distribution for Li5.5PS4.5Cl1.5, Li5.5PS4.5Cl0.75I0.75 and Li5.5PS4.5I1.5. Histograms for other compositions are available in the Fig. S2 of ESI.† Due to an increased concentration of Li vacancies for this composition, instead of forming a standard 4-atom coordinated tetrahedral polyhedron, certain Li sites form a larger distorted 5-atom coordinated polyhedron. These polyhedra contribute the most to ionic conductivity due to having much larger volumes and skewed the results shown in Fig. 4b, causing an increasing-decreasing trend. Till x = 0.75, addition of I resulted in overall increase in polyhedron volumes, including the 5-atom coordinated one, as marked in Fig. 4d, however a further increase in I concentration resulted in reversion of some of the 5-atom coordinated polyhedra back to a 4-atom coordinated configuration, significantly reducing the width of migration channel, thereby lowering the average Li+ polyhedron volume. For x = 1.5, all the 5-atom coordinated polyhedra reverted back to 4 atom coordination, resulting in the lowest ionic conductivity out of all the systems, at 4.3 mS cm−1.
Overall, for Cl–I systems, these results indicate a strong dependency of ionic conductivity on local coordination environments of Li+ ions, where a faster conduction is facilitated by wider migration channels and the presence of 5-atom coordinated Li+ ions. Li et al. discussed the role of site configurational entropy for the increasing-decreasing trend observed in the case of Li5.5PS4.5Cl1.5−xBrx systems, as entropy maximizes for a near equiatomic composition. However, that discussion is beyond the scope of this work, as anti-site disorder was avoided for simplification of systems in this study, which contributes significantly to site configurational entropy.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d5tc00529a |
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