Edvin K. W.
Andersson
a,
Christofer
Sångeland
a,
Elin
Berggren
b,
Fredrik O. L.
Johansson
cd,
Danilo
Kühn
c,
Andreas
Lindblad
b,
Jonas
Mindemark
a and
Maria
Hahlin
*ab
aDepartment of Chemistry, Ångström Laboratory, Uppsala University, SE-751 21 Uppsala, Sweden. E-mail: maria.hahlin@kemi.uu.se
bDepartment of Physics and Astronomy, Uppsala University, SE-751 21 Uppsala, Sweden
cInstitute for Methods and Instrumentation in Synchrotron Radiation Research PS-ISRR, Helmholtz-Zentrum Berlin für Materialien und Energie, Albert-Einstein-Strasse 15, 12489 Berlin, Germany
dInstitut für Physik und Astronomie, Universität Potsdam, Karl-Liebknecht-Strasse 24-25, 14476 Potsdam, Germany
First published on 21st September 2021
Development of functional and stable solid polymer electrolytes (SPEs) for battery applications is an important step towards both safer batteries and for the realization of lithium-based or anode-less batteries. The interface between the lithium and the solid polymer electrolyte is one of the bottlenecks, where severe degradation is expected. Here, the stability of three different SPEs – poly(ethylene oxide) (PEO), poly(ε-caprolactone) (PCL) and poly(trimethylene carbonate) (PTMC) – together with lithium bis(trifluoromethanesulfonyl)imide (LiTFSI) salt, is investigated after they have been exposed to lithium metal under UHV conditions. Degradation compounds, e.g. Li–O–R, LiF and LixSyOz, are identified for all SPEs using soft X-ray photoelectron spectroscopy. A competing degradation between polymer and salt is identified in the outermost surface region (<7 nm), and is dependent on the polymer host. PTMC:LiTFSI shows the most severe decomposition of both polymer and salt followed by PCL:LiTFSI and PEO:LiTFSI. In addition, the movement of lithium species through the decomposed interface shows large variation depending on the polymer electrolyte system.
Extensive investigation, primarily by photoelectron spectroscopy (PES) using both soft and hard X-rays (SOXPES, HAXPES), has been and is continuously performed to identify the degradation in the interphase region for liquid electrolytes.11,12 For polymer electrolytes, due to the experimental challenges involved, there are only a few pioneering studies, including work from both our own group and others.13–15 While these ex situ studies have allowed characterization of the chemical nature of the passivation layers on lithium metal after they have been formed, complementary techniques are necessary to gain additional insights into the operating reaction mechanisms. The detection of gaseous species as they are formed during the degradation reactions,16 for example, has added important pieces to the puzzle of deciphering reaction pathways and polymer stability under these conditions. Our group has also investigated the degradation of polymer hosts in contact with lithium metal (i.e., at extreme low potentials) by computational means using density functional theory (DFT) and ab initio molecular dynamics (AIMD) methods.17,18 These efforts have given additional detailed insights into the reactions between lithium metal and ion-conducting polymers, which constitute the initial degradation reactions in lithium metal battery systems. One complicating factor of experimentally replicating these computational studies, however, is the extreme reactivity of lithium metal. This reactivity makes it unlikely that the surface of a piece of lithium metal will ever practically be pure lithium metal and the surface of, e.g., lithium foil will not accurately represent a chemical environment where fresh lithium is generated, such as in an operating lithium metal cell. A key challenge for studying the initial degradation reactions of these systems with PES is thus to create a chemical environment that accurately represents a pure lithium metal surface. These conditions can instead be mimicked through the method introduced by Wenzel et al., where a thin layer of lithium metal is applied on the electrolyte surface in situ, after which the degradation can be followed by PES measurements through the electron-transparent lithium film.19 Here, we have applied this approach in order to replicate the conditions in our earlier modeling work by studying the initial degradation reactions between three ion-conducting polymers and lithium metal. Several different polymer and salt degradation products are identified in the interface layer using SOXPES. Going beyond the previous DFT and AIMD findings, we have investigated poly(ethylene oxide) (PEO), poly(ε-caprolactone) (PCL) and poly(trimethylene carbonate) (PTMC) both as pure polymers and complexed with lithium bis(trifluoromethanesulfonyl)imide (LiTFSI) salt. Including the salt is of extreme interest since it is an essential component of the electrolyte, and is itself prone to degrade.
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Fig. 1 Molecular structure of (a) poly(ethylene oxide) (PEO), (b) poly(ε-caprolactone) (PCL), (c) poly(trimethylene carbonate) (PTMC) and (d) lithium bis(trifluoromethanesulfonyl)imide (LiTFSI) salt. |
Following in situ deposition of lithium metal under UHV and at ambient temperature conditions, triggering interfacial degradation, PES spectra of the O 1s, C 1s, and Li 1s core levels were measured for each polymer and SPE. In addition, for each SPE also the F 1s, N 1s, and S 2p core levels were measured. PES measurements were performed both before and after Li deposition, and the results are presented in Fig. 2, 3, 5, and 6. The PES spectra are calibrated versus the CF3-peak positioned at a binding energy of 293 eV.14 The PES spectra obtained before lithium deposition are deconvoluted based on the molecular structure and using references. The peaks are assigned as follows; in the F 1s spectra a F–C (salt) peak at ∼688 eV,14 in the O 1s spectra a OC peak at ∼532 eV,15 and a S
O (salt) peak at ∼532 eV,14 a C–O peak at ∼533 eV,15 in the N 1s spectra a SO2–N–SO2 (salt) at ∼399.5 eV, in the C 1s spectra a hydrocarbon peak (C–C/C–H) at ∼285 eV,15 a C–O peak at ∼287 eV,15 a O–C
O peak at ∼289 eV,20 a O–(C
O)–O peak at ∼290 eV,15 a C–F3 (salt) peak at ∼293 eV, in the S 2p spectra a spin orbit split N–S–O2 (salt) peak with the S 2p3/2 at 169 eV, and in the Li 1s spectra a Li+ peak at ∼56.5 eV. All these characteristic peaks for the polymers and the salt have been labelled in Fig. 2–4. The additional peaks that emerge after lithium deposition are identified and discussed further below, and are in the figures indicated by a pink color.
Starting with the pure PEO, a large decrease in the C–O peak intensity relative to the C–C/C–H peak is observed in the C 1s spectrum. In addition, a new O 1s peak emerges at 530.4 eV after lithium deposition, see Fig. 2. This O 1s peak is, based on its position, assigned to Li–O–R.14 This clearly shows that some (but not all) of the C–O bonds in PEO are breaking upon contact with metallic lithium, forming Li alkoxides. In contrast, computational AIMD simulations of PEO oligomers on lithium metal surfaces predict a strong thermodynamic driving force to form Li2O along with C2H2 and H2 gas.18 In the PES spectra for PEO no Li2O peak is observed. That this stage in the decomposition is not reached to a larger extent indicates a kinetic barrier for the reaction. The formation of Li alkoxides instead of Li2O is possibly a consequence of the longer polymer chains – compared to the simulations – “trapping” the decomposition at the Li alkoxide stage. The relative intensity between the C–O and the Li–O–R in the O 1s spectra is 2:
1 and indicates that in the surface region (a few nm) approximately a third of the O–C bonds in the PEO have broken, assuming a uniform surface composition.
Moving further to the PEO:LiTFSI film, similar degradation of the PEO is observed also when the salt is present. The intensity ratio between the C–O relative to the C–C/C–H peak decreases to a similar extent as for the pure PEO. However, it is noticed that the relative intensity difference of the C–O peak relative to Li–O–R is different for PEO and PEO:LiTFSI. To some degree this is explained by the presence of the salt, were the SO is expected to have a similar binding energy as the C–O peak.
In addition to degradation of the PEO, degradation of the TFSI anion is also observed in the PEO:LiTFSI film. This is seen by the appearance of a LiF peak at ∼684.1 eV in the F 1s spectrum14 as well as two new S 2p features at 167.6 eV and 166.6 eV, respectively. The assignment of the two new S 2p peaks are not clear; however, the position of the peak at 167.6 eV coincides with a feature previously attributed to Li2SO3.14 However, we note that the formation of the SO3 fragment from the SO2 moieties present in the TFSI anion would require the abstraction of an additional oxygen atom from another source, which we deem unlikely. As there are a range of possible sulfur oxyanions with a range of oxidation numbers for sulfur, we have opted to label this peak as LixSyOz to reflect its uncertain origin. After lithium deposition, the N 1s peak has a broader FWHM that suggest multiple components. This supports the finding of salt degradation. The relative ratio between the LiF and the C–F component, as well between the degradation peaks in S 2p relative to the TFSI anion are both small. Together with the relatively large decomposition observed for the PEO, this suggests a preferential decomposition of the PEO chains as compared to the TFSI anion for the PEO:LiTFSI system. Previous studies have shown a strong correlation between the formation of TFSI-derived compounds (e.g., LiF and Li3N) and the concentration of H2O in the electrolyte.14,15,21,22 However, the absence of a prominent LiOH peak, suggests negligible quantities of H2O. This being said, given the hydrophilic quality of PEO, greater TFSI decomposition can be expected under less strict atmospheric conditions. Nevertheless, the degradation species observed in this work closely match those previously reported between PEO:LiTFSI and lithium metal foil.14,15
For the pure PCL sample, a large decrease in the C–O and O–CO peak intensities relative to the C–C/C–H peak is observed in the C 1s spectra. The C–C/C–H peak is after lithium deposition completely dominating the spectra, making an accurate deconvolution difficult. At the same time a Li–O–R peak shows up in the O 1s spectrum, constituting approximately half of the intensity. Alkoxide species may be formed by the breaking of the C–O bonds, as previously suggested by computational work.17 However, the large quantity of lithium alkoxide observed in the O 1s spectra following lithium deposition can only explained by the breaking of the C–O bond in addition to reduction of the C
O bond. Reductions of carboxylic esters to form alkoxides are ubiquitous reactions in organic chemistry, but generally rely on addition of hydrogen in the form of, e.g., hydrides, something which is not available in the studied system. However, as illustrated in Fig. 4a, direct reduction of the carbonyl group of carboxylic esters by reaction with between alkali metals may form the free-radical intermediate 1. This reactive species may then go on to further react through a multitude of reactions. Radical coupling (Fig. 4b) leads to a reaction pathway that is analogous to acyloin condensation, wherein a diketone species 2 is formed following the release of alkoxide species. This can then be further reduced by the action of lithium metal to form the dialkoxide 3, thereby effectively converting C
O to Li–O–R species.
Moving further to the PCL:LiTFSI sample, similarities with the degradation of both the pure PCL and PEO:LiTFSI are seen. The intensities of the C–O and CO peaks decrease relative to the C–C/C–H peak after deposition, although not to the same extent as for the PCL sample. This suggests less degradation of the PCL chains when the salt is present. Similar to the pure PCL, a Li–O–R peak appears also for PCL:LiTFSI. The relative intensity ratio between the C–O and Li–O–R peaks is for PCL slightly larger to that of PEO both when salt is present and absent. Degradation of the TFSI anion is observed for PCL:LiTFSI as well, although in general smaller changes are observed for the PCL:LiTFSI compared to PEO:LiTFSI. Specifically, less LiF and LixSyOz can be seen. In addition, two new peaks emerge for the PCL:LiTFSI, one at 397.2 eV in the N 1s spectra that is assigned to Li3N, and one at ∼528 eV in the O 1s spectra assigned to Li2O.
After lithium deposition, there are drastic changes in the surface composition. Compared to the PEO:LiTFSI and PCL:LiTFSI systems these changes appear to be much more extensive. A recent DFT studies have also suggested that PTMC:LiTFSI is more susceptible towards reduction compared to both PEO:LiTFSI and PCL:LiTFSI, respectively,23 the polycarbonate PTMC also has a structure with several possible points of attack for bond cleavage. Considering C–O bond cleavage to be the main source of polymer fragmentation, PTMC can be cleaved at either side of the carbonyl group, producing shorter C3 species compared to PCL, which is expected to give C6 species through C–O bond cleavage. PTMC may also release CO2 through the C–O cleavage route,16 which should also be a powerful driving force for fragmentation.
Starting with the O 1s spectrum, the formation of Li–O–R is seen for PTMC:LiTFSI. In addition to this, a Li2O peak also appears at ∼528.1 eV. Together, the Li–O–R and the Li2O degradation products are dominating the O 1s spectrum, and the relative intensity ratios between these and the intact polymer peaks suggest that almost all of the PTMC:LiTFSI is decomposed throughout the surface region, assuming a uniform sample. Severe changes are also observed in the C 1s spectrum of PTMC:LiTFSI; the characteristic O–(CO)–O of PTMC has been smeared out towards lower binding energy, and is most likely composed of two different components. The lower binding energy peak is ∼290.0 eV, tentatively fluorinated species or carbonate anions. These results therefore suggest that one of the C–O bonds in PTMC breaks on contact with lithium. Severe salt decomposition is also seen for PTMC:LiTFSI. In comparison with both PEO:LiTFSI and PCL:LiTFSI, the salt decomposition is much more pronounced and other salt decomposition products are also being formed. Similar to PCL:LiTFSI, the LiF Li3N, and LixSyOz peaks are observed after lithium deposition on PTMC:LiTFSI. Also, the formation of a new compounds is seen in S 2p spectra, where a large peak emerges at 160.5 eV. This peak is assigned to Li2S. The intensity ratio between the decomposition products relative to the intact PTMC:LiTFSI components are 1.72 in the F 1s spectrum, 0.63 in the N 1s spectrum, and 16.5 in the S 2p spectrum. These differences suggest that the reactions with lithium lead to breakdown of primarily the sulfur center of the TFSI anion, followed by the fluorinated part. However, this omits any gaseous reactions products. The intensity ratio between the LiTFSI and O–(C
O)–O peaks in the C 1s spectra only changes from 0.47 to 0.34, indicating that the salt decomposition is a little bit higher than decomposition of the PTMC polymer in the PTMC:LiTFSI sample. Overall, the same decomposition compounds have been reported at the interface between PTMC:LiTFSI and lithium metal foil for post mortem samples, albeit in much smaller quantities.15 This indicate that the native oxide film found on lithium metal foil may indeed act as a passivation layer, protecting the PTMC:LiTFSI membrane from severe decomposition. In contrast, deposition of lithium under UVH conditions exacerbates the decomposition of PTMC:LiTFSI, resulting in intense LiF, Li–O–R, Li2O Li3N and Li2S formation.
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Fig. 6 Li 1s spectra over time for each sample. To facilitate comparison, an intensity shift was applied to the spectra so that the backgrounds overlapped. |
The lithium metal deposition time was equal in all cases; however, the time required for the evolution of the lithium peak is different depending on the SPE. The fastest return towards original intensity and binding energy position is observed for PEO:LiTFSI, where the spectra after 3 h have almost same intensity as before lithium deposition and with only a small difference in binding energy position. Following is PCL:LiTFSI, where the intensity has decreased approximately half way back to its original value after ∼6 h. The peak is however, still to a large extent shifted in binding energy from its original position. The PTMC:LiTFSI sample, on the other hand, still shows a similar main Li 1s intensity after 20 h as directly after lithium deposition and the peak is also shifted in binding energy similar to that of PCL:LiTFSI. To fully understand the diffusion of lithium species more experiments are needed, however these differences clearly show that there are profound differences between the different SPEs.
The measurements were performed between 15 to 120 min after lithium deposition. As a result of this, changes may still occur at the surface region during the time of acquisition. The C 1s spectra are measured with the smallest and largest probing depth in a rapid succession compared to the time-scale of lithium diffusion, Fig. 6. Intermediate probing depths are measured afterwards. The trends in intensities for different photon energies is used to build a depth profile. It is however important to keep in mind that it is a snapshot of a process rather than a final picture.
In Fig. 7, the C 1s spectra from the most surface- and bulk-sensitive measurements are shown for all polymer electrolytes before and after lithium deposition, whilst the intermediate measurements are presented in ESI, Fig. S1.†Fig. 7 also shows the composition for all probing depths, based on the intensities obtained in the deconvolutions. It is clear that with increased probing depth, features in the C 1s spectra varies in intensity relative to each other. A general trend after lithium deposition is the increase of the hydrocarbon peak intensities relative to the other peaks.
The C 1s spectra of pristine PEO:LiTFSI, Fig. 7a, shows that the C–O peak intensity is increasing relative to the intensity of the C–C/C–H peak with increased probing depth. This confirms that adventitious carbon is present predominantly at the surface. The relative intensity ratio of the LiTFSI peak compared to the C–O is seen to decrease with probing depth, indicating salt accumulation at the surface of the PEO:LiTFSI prior to lithium deposition. Both accumulation of salt and C–C/C–H has previously been observed for liquid electrolytes, and may thus be expected.25 After lithium deposition, the C–O peak intensity is still increasing in regard to the C–C/C–H peak with increasing probing depth. As decomposed PEO forms C–C/C–H upon contact with lithium, this shows that relatively more intact PEO can be found our found at deeper parts of the sample. As the highest probing depth is <7 nm, these results show that the decomposition region is, under these experimental conditions, fairly shallow.
Compared to the other samples, PCL:LiTFSI shows a higher concentration of adventitious carbon, both before and after lithium deposition. This, in combination with the overlap of the polymer peaks and the adventitious carbon peak, makes deconvolution of the spectra more difficult. Still, some trends can be observed. For the pristine PCL:LiTFSI sample (Fig. 7b), the C 1s depth profile shows that the polymer peaks are increasing in intensity relative to the C–C/C–H peak with increased probing depth, again confirming the adventitious carbon being present mainly on the surface. The intensity ratio between LiTFSI and polymer peaks decreases with depth in this sample as well, indicating salt accumulation at the surface. After lithium deposition the O–CO and C–O peaks have relatively lower intensity compared to the C–C/C–H peak. With lithium deposited on the sample, the intensities of the polymer peaks are increasing with probing depth, with one exception at a photon energy of 710 eV. This irregularity could be due to the dominating concentration of adventitious carbon in combination with overlapping peaks, as discussed in the beginning of this paragraph. Nevertheless, the results show as expected that main decomposition occurs within the same depth region (<7 nm) as for PEO:LiTFSI.
The C 1s spectra of pristine PTMC:LiTFSI in Fig. 7c shows that the intensity of the polymer peaks are relatively constant to the C–C/C–H peak for all probing depth, in contrast to both PEO and PCL. We can however still slightly perceive the decrease of the LiTFSI/polymer intensity ratio, although, compared to PEO and PCL, it is a much smaller difference. The different trends seen for the case of PTMC:LiTFSI may indicate less mobility of both salt and C–C/C–H species in this polymer. After lithium deposition it is not possible to identify any depth dependence of the salt concentration. However, the trends for the C–O and C–C/C–H peak intensities in the PEO:LiTFSI and PCL:LiTFSI systems after deposition can still be observed in the PTMC:LiTFSI system. The C–O peak decreases in intensity relative to the C–C/C–H after, again indicating less decomposition at higher depths. The unidentified component found at 283 eV stays constant in intensity over varied probing depth. Like with the other systems, the decomposition region is fairly shallow, within <7 nm.
A schematic summary of all the PES results is shown in Fig. 8. For all systems both polymers and salt decompose upon contact with lithium. The degree of polymer relative to salt degradation depends on the polymer host. The bare PEO is seen to be more stable than PCL. When the salt is added, PEO still seems more stable than PCL, but at the expense of more severe salt degradation compared to the PCL. Similar degradation compounds are seen in both cases: polymer hydrocarbons, lithium alkoxides (Li–O–C) and LixSyOz. In addition, small quantities of LiF is seen in the PEO:LiTFSI sample, and Li2O and Li3N is seen in small quantities for the PCL:LiTFSI sample. Standing out is the PTMC system, showing much larger quantities of decomposition products from both polymer and salt. Only the PTMC:LiTFSI shows the Li2S decomposition product. Li2O could not be detected for PEO or PEO:LiTFSI. AIMD studies have shown that there is a large thermodynamic driving force for Li2O formation also for PEO on contact with lithium metal,18 but it appears that the reaction does not proceed all the way to the oxide under these conditions, possibly because of some kinetic limitation. Overall, the degree of decomposition observed for the three different SPE systems agrees well with DFT-based computational work: PTMC is expected to have a lower cathodic stability compared to its polyether- and polyester-based counterparts.23 We also note that, in contrast with the semi-crystalline PEO:LiTFSI and PCL:LiTFSI, PTMC:LiTFSI is fully amorphous; since degradation of crystalline structures would require an additional energy input to disrupt these structures, there should be an additional barrier towards degradation of the crystalline domains of these materials. From the analysis of the Li 1s spectra it appears as if PTMC:LiTFSI forms a kinetically more stable interface towards the lithium metal compared to the other SPEs. This puts a finger on the question of how much degradation is too much, and how much is a necessity in order to form a stable, functional interphase. As a final note, it is known that degradation reactions become more severe at elevated temperatures, which is unfortunate given that several of these SPEs require higher temperatures to operate.4 One may therefore expect more severe degradation to occur in batteries operating under more realistic conditions. Common for PEO:LiTFSI, PCL:LiTFSI, and possibly also for PTMC:LiTFSI before deposition is that the concentration of the LiTFSI salt is higher at the outermost layers than deeper into the sample. Another trend seen in all spectra is the relative decrease of the C–O peak intensity in relation to C–C/C–H after deposition of lithium. This difference is the most notable at the lowest probing depth (hv = 370 eV) and subsides with higher probing depths. The concentration of the decomposition products decreasing with probing depth suggests a decomposition layer thickness of similar or smaller depths than the largest probing depth of <7 nm.
The core-level spectra for decomposition analysis were recorded with a 300 eV kinetic energy resulting in similar escape depth for all samples. Energy calibration was done by measuring the C 1s spectra for the corresponding photon energies (see info below). These C 1s PES spectra were subsequently used for depth characterization. The photon energies were (hv) of 1000 eV, 845 eV, 710 eV, 600 eV and 370 eV, the corresponding kinetic energies yields the inelastic mean free paths (IMFP, λ) of 2.3 nm, 1.9 nm, 1.5 nm, 1.2 nm and 0.4 nm (assuming primarily polymer in the near-surface region).32 This value corresponds to the IMFP in PCL but should cohere with that of PEO and PTMC adequately. A universal rule in PES is that 95% of information comes from the depth of 3λ which would result in probing depths of 6.9 nm, 5.7 nm, 4.5 nm, 3.6 nm and 1.2 nm.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d1ta05015j |
This journal is © The Royal Society of Chemistry 2021 |