James C.
Pramudita
a,
Siegbert
Schmid
*b,
Thomas
Godfrey
b,
Thomas
Whittle
b,
Moshiul
Alam
c,
Tracey
Hanley
c,
Helen E. A.
Brand
d and
Neeraj
Sharma
*a
aSchool of Chemistry, UNSW Australia, Sydney NSW 2052, Australia. E-mail: neeraj.sharma@unsw.edu.au
bSchool of Chemistry, The University of Sydney, Sydney NSW 2006, Australia. E-mail: siegbert.schmid@sydney.edu.au
cAustralian Nuclear Science and Technology Organisation, Kirrawee DC NSW 2253, Australia
dAustralian Synchrotron, 800 Blackburn Road, Clayton Victoria 3168, Australia
First published on 23rd July 2014
The development of electrodes for ambient temperature sodium-ion batteries requires the study of new materials and the understanding of how crystal structure influences properties. In this study, we investigate where sodium locates in two Prussian blue analogues, Fe[Fe(CN)6]1−x·yH2O and FeCo(CN)6. The evolution of the sodium site occupancies, lattice and volume is shown during charge–discharge using in situ synchrotron X-ray powder diffraction data. Sodium insertion is found to occur in these electrodes during cell construction and therefore Fe[Fe(CN)6]1−x·yH2O and FeCo(CN)6 can be used as positive electrodes. NazFeFe(CN)6 electrodes feature higher reversible capacities relative to NazFeCo(CN)6 electrodes which can be associated with a combination of structural factors, for example, a major sodium-containing phase, ∼Na0.5FeFe(CN)6 with sodium locating either at the x = y = z = 0.25 or x = y = 0.25 and z = 0.227(11) sites and an electrochemically inactive sodium-free Fe[Fe(CN)6]1−x·yH2O phase. This study demonstrates that key questions about electrode performance and attributes in sodium-ion batteries can be addressed using time-resolved in situ synchrotron X-ray diffraction studies.
The limiting factors for sodium-ion battery development currently are: the small number of insertion electrodes, particularly anodes; their energy densities; and the reversibility of the sodium insertion–extraction processes. Electrodes range from selected carbons, to metal oxides, phosphates, and fluorophosphates.4,5 An alternative class of materials for insertion electrodes in sodium-ion batteries are framework-based materials.6–9 Framework materials are a combination of metal nodes and organic bridging linkers or ligands, e.g. metal–organic frameworks (MOFs)/coordination polymers10,11 extended in 3-dimensional space, and these lead to an exceptionally large array of 3-dimensional materials, with seemingly infinite combinations of metals and linker units. Such frameworks in turn exhibit a vast array of properties, such as negative thermal expansion and spin-crossover, and can be used in potential applications, such as gas separation. Cyanide bridged frameworks form an important class of framework materials showing a high level of structural flexibility.12–14 Prussian blue analogues belonging to this class of framework materials, have been applied as insertion electrodes for lithium-ion batteries,15,16 and recently they have been adapted to sodium-ion batteries.6–9
The investigations of Prussian blue analogues as electrodes in sodium-ion batteries focus on the electrochemistry and require further study in order to determine what features of frameworks are ideally suited for electrode applications.8,9 Typically the positive electrode is referred to as the sodium source in a full rechargeable sodium-ion battery, providing the initial source of sodium-ions to generate battery capacity. However, sodium is also present in the electrolyte and this can provide a certain amount of capacity for the battery. The concept of where, how and by what means sodium inserts/extracts from electrode materials can shed light on electrochemical performance and further electrode/battery development. Ideally, electrodes will be able to reversibly insert/extract large quantities of sodium, i.e. high energy densities, and this process can be cycled thousands of times with only minor structural changes, i.e. will present longevity or long lifetimes. These factors can be probed using specialised techniques, in particular in situ synchrotron powder X-ray diffraction (XRD), which has the capability to provide detail on the structure and sodium site evolution while a battery is functioning.17,18 In any sodium-ion battery, sodium will carry the charge,19 and thus it is important to know what happens to sodium, and specifically how it evolves crystallographically in the electrodes. Time-resolved in situ synchrotron XRD data provide insight on the structural reaction mechanism evolution of electrodes in a battery during charge–discharge or as they function.17,18 This is distinctly different to providing a snapshot of the equilibrated structure at equilibrium conditions as ex situ (post mortem) or pseudo in situ data provide.20,21 With sufficient time-resolution, in situ data show what happens under non-equilibrium real battery operation conditions.
The capability of time-resolved determination of sodium atomic parameters was only recently demonstrated for Na3V2O2x(PO4)2F3−2x electrodes with in situ synchrotron XRD detailing reaction mechanism, lattice and sodium site occupancy evolution as a function of charge–discharge.17,22 Considering the larger quantity of lithium-ion battery literature, only a few in situ studies describe the lithium site occupancy and evolution as a function of charge–discharge.21,23,24 Note, for lithium-ion batteries, neutron powder diffraction (NPD) is required due to the weak signal lithium generates in XRD data. Thus XRD has a distinct advantage in the study of sodium-ion batteries; it is sensitive to sodium atomic parameters, due to the larger atomic number of sodium relative to lithium. Additionally, smaller samples, e.g., simple coin cells can be probed with XRD, as compared to the larger, more challenging batteries required for in situ NPD. Limited research has been conducted utilising in situ XRD at both laboratory and synchrotron based sources on sodium batteries.17,18,25–37 There is clearly the ability to track in detail the evolution of sodium in coin cells as a function of time during charge–discharge using in situ synchrotron XRD.
In this study, we determine the sodium uptake, insertion and extraction in Prussian blue analogues, Fe[Fe(CN)6]1−x·yH2O and FeCo(CN)6, using time-resolved in situ synchrotron XRD data. We detail how cell preparation can turn the sodium-free versions of these compounds into sodium-containing compounds and thus act as a positive electrode in sodium-ion batteries. Further insight is detailed on storage time of the electrode and the influence of charging versus discharging the electrode as a first step.
The positive electrodes were manufactured by mixing 80 wt% of the active material, 10 wt% conductive carbon (Super C65, Timcal) and 10 wt% polyvinylidenefluoride binder (PVDF, MTI Corporation). A few mL N-methylpyrrolidone (NMP, MTI Corporation) were added and the resulting slurry was stirred overnight. This slurry was then coated on aluminium foil using a notch bar. The electrode film was dried at 100 °C in a vacuum oven overnight. The electrode sheets were pressed to 100 kN using a flat plate press (MTI corporation) and dried overnight at 100 °C before transfer to the Ar-filled glovebox. Coin cells with 3 mm diameter holes in the casing and 5 mm diameter holes in the stainless spacer were used for the construction of the coin cells for the in situ measurements. The coin cells contained Na metal (∼1 mm thickness), glass fibre separators with 1 M NaPF6 in dimethyl carbonate and diethyl carbonate (1:
1 wt%) electrolyte solution. Further details regarding coin cell construction and beamline setup can be found in ref. 17, 18, 39 and 40.
Laboratory XRD experiments were conducted on a Panalytical X'pert MPD employing Cu Kα radiation. In situ synchrotron X-ray diffraction experiments were performed within 3–4 days after cell construction. The first Fe[Fe(CN)6]1−x·yH2O cell was initially discharged to 1 V and then charged at 0.1 mA, while the second cell was initially charged to 3.8 V at 0.2 mA held at 3.8 V for 10 minutes and then discharged to 0.1 V at 0.2 mA. The FeCo(CN)6 cell was cycled twice, by discharging to 1 V at 0.05 mA and charging to 4 V at 0.2 mA. These procedures were used to ensure sufficient information could be extracted from the limited beamtime available.
In situ synchrotron XRD data were collected on the powder diffraction beamline41 at the Australian Synchrotron with a wavelength (λ) of 0.73716(2) Å, determined using the NIST 660b LaB6 standard reference material. Data were collected continuously in 4.36 minute acquisitions on the coin cell in transmission geometry throughout the charge–discharge cycles described above. Further details about this experimental setup can be found in ref. 39 and 42. The powder diffraction beamline employs two detector positions, and each position was exposed for 2 minutes and the changeover time between positions was 0.36 minutes, resulting in an overall collection time of 4.36 minutes. These two detector positions are merged to provide a diffraction pattern. Rietveld refinements were carried out using the GSAS43 software suite with the EXPGUI44 software interface. For the in situ data, in the first dataset the lattice parameters and atomic displacement parameters (ADPs) for all atoms were refined. The ADPs were then fixed and the sodium occupancies refined. For the sequential refinements, the ADPs were kept fixed and the lattice and sodium occupancies refined.
![]() | ||
Fig. 1 The structure of the initial cathode material in the sodium-ion battery using the vacancy-free model. Rietveld refined fit of the (a) FeFe(CN)6 and (c), (e) Na0.516(12)FeFe(CN)6 models to the synchrotron XRD data in the (a), (b) 8 ≤ 2θ ≤ 20° and (e) 6 ≤ 2θ ≤ 48° regions. Data are shown as crosses, calculated data resulting from the Rietveld refinement of the model are shown as a line through the crosses, and the difference between the observed and calculated data as the line below. Arrows indicate data and model mismatches. The vertical reflection markers are for the two FeFe(CN)6 phases present in the electrode. The crystal structure and remaining Fourier electron density (yellow) of the major (b) FeFe(CN)6 and (d) Na0.516(12)FeFe(CN)6 phase with iron in light brown, carbon in dark brown, nitrogen in blue and sodium in yellow with the shading indicating occupancy. Note in (a), (c) and (e) there are excluded regions for the sodium metal and aluminium reflections, in addition the features in the background (indicated in (c)) arise in part due to carbon-containing components in the electrode, e.g. PVDF and carbon black.47 |
Atom | x | y | z | SOF | Isotropic ADPa (×100)/Å2 |
---|---|---|---|---|---|
a Refined for the sample-only pattern and subsequently fixed. Space group = Fm![]() |
|||||
Fe(1) | 0 | 0 | 0 | 1 | 2.91 |
Fe(2) | 0.5 | 0 | 0 | 1 | 2.89 |
C | 0.196 | 0 | 0 | 1 | 3.89 |
N | 0.303 | 0 | 0 | 1 | 0.92 |
Na | 0.25 | 0.25 | 0.227(11) | 0.083(4) | 6.50 |
The as-synthesized dry Fe[Fe(CN)6]1−x·yH2O powder was found to be single-phase with a refined lattice parameter of a = 10.2260(6) Å (see ESI,† Fig. S1) which corresponds to the minor phase of the electrode inside a sodium-ion cell. Before proceeding further it is important to note that there are structural features that may not be wholly captured by structural models38 in the literature for FeFe(CN)6. The simple model (termed the vacancy-free model in this paper) assumes Fe3+ is present at both metal centres and any water remaining in the pores is removed by drying and/or electrode manufacturing conditions resulting in the composition Fe[Fe(CN)6]. If these assumptions are made the major phase in the electrode shows the structural features presented in Table 2. The location of the sodium sites for the vacancy-free model is determined by investigating the Fourier difference maps, locating the site at x = y = z = 0.25 which results in a significant improvement of the fit (Fig. 1 and detailed below). The more complex model (vacancy-containing model) involves considering the potential for mixed valent Fe sites, e.g. some of Fe3+ reduced to Fe2+. In order for this to occur, vacancies are required for Fe(1), C and N sites with precedents existing in the literature,45,46 and which also show OH groups replacing CN. A further complicating factor is the potential for water to remain in the pores of the structure as Prussian blue analogues are known to absorb water. Laboratory powder XRD data fitted to the water-free vacancy-free model show mismatched observed and calculated reflection intensities (ESI,† Fig. S1). Using Fourier analysis, this leads to a model where Fe, C and N vacancies are modelled and are found to be ∼12% and O is located at the x = y = z = 0.25 site, leading to a = 10.2260(5) Å and a composition of Fe[Fe0.85(7)(C0.88(4)N0.88(4))6]·0.473(24)H2O or x ∼ 0.15, y ∼ 0.47 in Fe[Fe(CN)6]1−x·yH2O. Note, OH groups are not considered to substitute on the CN sites. Crystallographic data for the refined model and fits to the XRD data are shown in ESI,† Fig. S2 and Table S1. In this analysis of the in situ synchrotron XRD data we have utilised both models (vacancy-free and vacancy-containing) to gauge whether any differences are found.
Atom | x | y | z | SOF | Isotropic ADPa (×100)/Å2 |
---|---|---|---|---|---|
a Refined and subsequently fixed. Space group = Fm![]() |
|||||
Fe(1) | 0 | 0 | 0 | 1 | 0.57 |
Fe(2) | 0.5 | 0 | 0 | 1 | 1.35 |
C | 0.19 | 0 | 0 | 1 | 0.96 |
N | 0.31 | 0 | 0 | 1 | 0.96 |
Na | 0.25 | 0.25 | 0.25 | 0.516(12) | 0.24 |
For the first in situ synchrotron XRD dataset the structural model of the major phase is detailed in Tables 1 and 2 for each option. In the case of the vacancy-free model, the major phase intensities matched well with the 200 and 331 Fe[Fe(CN)6]1−x·yH2O reflections but were poorly fitted (under-calculated) to the 220 and 400 Fe[Fe(CN)6]1−x·yH2O reflections (indicated by the arrows in Fig. 1a). Investigating the Fourier difference maps a positive scattering intensity is located at the x = y = z = 0.25 site (Fig. 1b), placing sodium at this site (Fig. 1d) improves the fit (Fig. 1c) resulting in the refined formula of Na0.516(12)FeFe(CN)6. Interestingly for the vacancy containing model the minor phase still shows evidence of Fe(1), C and N vacancies and O on the x = y = z = 0.25 site, but for the major phase refined occupancies of Fe(1), C and N converge to 1, full occupation. Furthermore, removing the O x = y = z = 0.25 site from the calculated pattern and probing the difference Fourier densities reveals Fourier intensity in an octahedral arrangement around the x = y = z = 0.25 site (Fig. 2a). This indicates a distribution of ions/molecules along these pores in a disordered manner. Placing oxygen on these sites, refining their positions and occupancies, illustrates a large under-calculation of the electron density. The Fourier difference map shown in Fig. 2b, shows that the electron density contributed by oxygen at this site is not sufficient to capture the intensity observed. The replacement of O with Na (Fig. 2c), where Na contains more electrons or a larger electron density in Fourier maps, results in minimal remaining Fourier density and the fit to the synchrotron XRD data is shown in Fig. 2d. Clearly Na captures the electron density of the species in the pores of the framework more precisely than O in the in situ electrochemical cell. There still exists the possibility of both O and Na occupancy on this site, a mixed site however, this is unlikely as the Na+ is likely to coordinate to H2O in these pores leading to significant local strain on the framework. The refined atomic coordinates of Na are x = y = 0.25 and z = 0.227(11) and a composition of Na0.498(24)FeFe(CN)6. Notably both models provide virtually the same scenario a composition close to Na0.5FeFe(CN)6 with Na located near the centre of the pores. Where the models differ is the location of Na, either at the special position at the centre of the pore or in an octahedral arrangement surrounding this special position. In any case, both models indicate that Na is likely to be in the pores, and if this is the case then it should be possible to remove Na, i.e., use this material as a positive electrode.
![]() | ||
Fig. 2 The structure of the initial cathode material in the sodium-ion battery using the vacancy-containing model. Fourier electron density (yellow) difference maps of the major phase using the (a) FeFe(CN)6 and (b) FeFe(CN)6·0.473(24)H2O models (atoms omitted for clarity). (c) The structural model best capturing the electron density with iron in light brown, carbon in dark brown, nitrogen in blue and sodium is yellow with the shading indicating occupancy. Rietveld refined fit of the (d) Na0.498(24)FeFe(CN)6 model to the synchrotron XRD data in the 8 ≤ 2θ ≤ 20° region. Data are shown as crosses, calculated data resulting from the Rietveld refinement of the model are shown as a line through the crosses, and the difference between the observed and calculated data as the line below. Note there are excluded regions for the sodium metal and aluminium reflections, in addition the features in the background arise in part due to carbon-containing components in the electrode, e.g. PVDF and carbon black.47 |
Therefore, the sodium-free Fe[Fe(CN)6]1−x·yH2O electrode has chemically inserted a proportion of sodium presumably from the electrolyte into its pores prior to electrochemical cycling. By placing the Fe[Fe(CN)6]1−x·yH2O electrode in a battery in contact with the electrolyte there appears to be a spontaneous reaction that allows sodium insertion into the Fe[Fe(CN)6]1−x·yH2O transforming it to a sodium-free FeFe(CN)6 (with or without water) minor phase and a sodium-containing ∼Na0.5FeFe(CN)6 (water free) major phase. The observed insertion of sodium maybe the result of either only the presence of electrolyte solution (i.e., chemical insertion) or the presence of the electrode in an electrochemical cell with an open circuit potential. It is likely that the rate of sodium uptake is dependent on time. To investigate chemical insertion, dried electrodes were soaked in electrolyte solution inside an Ar-filled glovebox for 1 and 24 h. The extracted electrodes were sealed and analysis of XRD data revealed a larger time-dependent decrease in lattice parameters of Fe[Fe(CN)6]1−x·yH2O (1 h a = 10.144(2) Å and 24 h a = 10.109(1) Å) compared to FeCo(CN)6 (1 and 24 h a = 10.192(2) Å). The slight change in lattice parameter indicates that the electrolyte solution influences the structure but other factors are required to account for the observed changes in the first in situ dataset, e.g. the electrochemical cell. The reduction in lattice parameters may suggest dehydration and further experiments are proposed where vacancy content and time dependence of sodium content changes in the electrode are probed.
Furthermore, the transformation of the electrode to the sodium-containing and sodium-free phases appears to be two-phase in character. The ∼Na0.5FeFe(CN)6 phase forms at the expense of the Fe[Fe(CN)6]1−x·yH2O phase in both models. It is interesting to note that a range of NazFeFe(CN)6 phases where say z = 0.2, 0.4 and so on were not formed. This may indicate an energetically favourable composition of z ∼ 0.5 and it may also suggest that this is the maximum amount of sodium that can be reversibly inserted/extracted. Additionally, in the vacancy containing model, the Fe, C and N vacancies and water-containing pores are segregated to the minor phase, while the major phase is vacancy and water-free. The question remains whether the minor phase is electrochemically active or acts to ‘trap’ water and vacancies allowing the majority phase to be electrochemically active.
![]() | ||
Fig. 3 Selected 2θ region of in situ synchrotron XRD data highlighting the evolution of the 200 reflections of the two FeFe(CN)6 phases by a colour scale and the potential profile. |
In terms of the two models used, the vacancy-containing and vacancy-free models both follow the same trend in lattice and volume expansion/contraction. The only discrepancy observed between these models is between 110 and 140 minutes where the equivalent sodium content of the vacancy-containing model appears to decrease more rapidly than the vacancy-free model. The vacancy-containing model subsequently shows no sodium occupation while the vacancy free model shows on average 0.12(2) sodium occupancy. It is worthwhile noting that the vacancy-free and vacancy-containing models place sodium on different sites, with the former at the x = y = z = 0.25 site. Investigating the Fourier difference map of the vacancy-containing model, at 140 minutes there is no evidence of electron density near this position.
A second Fe[Fe(CN)6]1−x·yH2O containing battery was examined to determine whether the Na0.516(12)FeFe(CN)6 or majority phase can be cycled as a positive electrode or sodium source, extracting the 0.516(12) sodium ions by initially charging this electrode. Note this battery was stored for a longer period of time before the in situ experiment was undertaken (>1 day relative to the battery discussed above). Thus, first, the initial structure of the electrodes for the two batteries will be compared. Fig. 5 shows the Fourier difference map of the majority phase in the electrode without sodium for both models (vacancy-containing and vacancy-free). In both cases positive electron density is found at the centre of the pores at the x = y = z = 0.25 site. This differs from the 1st battery where the vacancy-containing model shows an octahedral arrangement around the x = y = z = 0.25 site. This may indicate that extended storage helps to locate sodium at the centre of the pores.
For the initial electrode, the overall sodium content and lattice are within error in both batteries using the vacancy-containing model. The vacancy-free model shows subtle differences, slightly larger refined sodium content by 7(3)% (0.550(11) Table 3) and a 0.0020(4) Å difference in the lattice parameter. However, the major difference between the batteries appears to be the phase fractions of the constituent phases where both models show a larger phase fraction of the major phase compared in the 2nd battery relative to the 1st battery, 89.9(7)% which is 5.2(7)% larger for the vacancy-free model and 84.6(1)% which is 6.1(1)% larger for the vacancy-containing model. This evidence indicates that extended storage may generate a more sodium rich electrode or a larger proportion of the electrode that contains sodium prior to first use.
Atom | x | y | z | SOF | Isotropic ADPa (×100)/Å2 |
---|---|---|---|---|---|
a Kept consistent with first electrode. Space group = Fm![]() |
|||||
Fe(1) | 0 | 0 | 0 | 1 | 0.57 |
Fe(2) | 0.5 | 0 | 0 | 1 | 1.35 |
C | 0.19 | 0 | 0 | 1 | 0.96 |
N | 0.31 | 0 | 0 | 1 | 0.96 |
Na | 0.25 | 0.25 | 0.25 | 0.550(11) | 0.24 |
On charging the ∼Na0.5FeFe(CN)6 electrode, a reduction in the lattice and volume is observed (Fig. 6). Therefore, the sodium in the electrode from the construction process can be used as a sodium source – it behaves as a positive electrode. Notably, similar to the battery above, the sodium content is fairly stable using both the vacancy-free and vacancy-containing models, decreasing marginally, until the later stages of charge, 36 to 52 minutes where the sodium content drops rapidly. This may suggest that the actual sodium content in the electrode is higher than 0.550(11) or 0.520(12) per formula unit, but the reminder is in the form of disordered sodium that is not detected by diffraction techniques which are sensitive to the long-range ordered occupancy of crystallographic sites.
On discharge, there appears to be a pseudo-plateau region around 2 V that leads to most of the ordered sodium on the x = y = z = 0.25 site re-inserting and the lattice parameter and volume reaching their respective maximum values. These values are close to the fresh electrode. For example, comparing 0 and 87 minutes or 4.33 and 1.31 V, sodium contents are 0.550(11) and 0.578(15), lattice parameters are 10.3637(3) and 10.3707(4) Å, and volumes are 1113.12(8) and 1115.38(12) Å3 respectively for the vacancy-free model. Below 1.3 V the sodium content, lattice parameter and volume show minimal change in both models. This may indicate that this positive electrode should be cycled to ∼1.2 V in order to re-insert all the crystallographically ordered sodium that was extracted during charge. Additionally, in both Fe[Fe(CN)6]1−x·yH2O batteries using both models, the minor sodium-free FeFe(CN)6 phase is inactive during charge–discharge cycling.
Atom | x | y | z | SOF | Isotropic ADPa (×100)/Å2 |
---|---|---|---|---|---|
a Refined and subsequently fixed. Space group = Fm![]() |
|||||
Co | 0 | 0 | 0 | 1 | 0.44 |
0.24 | |||||
Fe | 0.5 | 0 | 0 | 1 | 0.05 |
0.26 | |||||
C | 0.19 | 0 | 0 | 1 | 0.28 |
0.16 | |||||
N | 0.31 | 0 | 0 | 1 | 0.28 |
0.16 | |||||
Na | 0.25 | 0.25 | 0.25 | 0.224(12) | 0.25 |
0.20 | 0.027(3) | 0.10 |
![]() | ||
Fig. 8 Selected 2θ region of in situ synchrotron XRD data highlighting the evolution of the 200 reflections of the two FeCo(CN)6 phases by a colour scale and the potential profile. |
It is interesting to note the shrinking of the NazFeCo(CN)6 lattice/volume (Fig. 9) relative to the NazFeFe(CN)6 lattice/volume (Fig. 6). Although this is not a direct comparison due to the different number of cycles and procedure undertaken first between the batteries, a result of limited beamtime, it may shed light on the differences between the electrodes. Typically the NazFeCo(CN)6 electrode shows lower capacities relative to the NazFeFe(CN)6 electrode (see ESI,† Fig. S4–S7), thus the reduction in the lattice/volume is likely to correspond to lower insertion of sodium into the electrode as shown in Fig. 9. Other factors that may contribute to this observation include irreversible processes at the electrode and CN vibrations similar to that found during negative thermal expansion of this material.12–14
Initial studies were performed to explore the applicable voltage ranges and the longevity of the electrode, i.e. does cycling to 1.2 V enhance the lifetime of the electrode or is cycling to 0.1 or 1 V more optimal? This was undertaken for both Fe[Fe(CN)6]1−x·yH2O and FeCo(CN)6. The key findings were the same for both chemistries, the longevity, or maintenance of battery capacity and cyclability of the battery, is optimal if the batteries containing these electrodes are discharged first to 1 V and then charged. Discharging to 0.1 V renders them inoperative after a few cycles and charging first also limits battery lifetime (see ESI,† Fig. S3–S7). In situ synchrotron XRD data of the 2nd cycle of the NazFeFe(CN)6 battery shown in Fig. 6, which was discharged to 0.1 V in the 1st cycle, shows minimal changes that correspond to minimal capacity (ESI,† Fig. S3c). Therefore, a discharge to 1 V as the first step appears to be beneficial for battery performance, which presumably acts to activate the electrode, although further work is required to determine precisely why this is so.
Footnote |
† Electronic supplementary information (ESI) available: Rietveld-refined fits of structural models to XRD data, Fourier difference maps, crystallographic table for the vacancy-containing model, electrochemical cycling curves under various conditions (e.g. cutoff potentials, charging first, discharging first). See DOI: 10.1039/c4cp02676d |
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