Stefan
Smetaczek
a,
Eva
Pycha
a,
Joseph
Ring
a,
Matthäus
Siebenhofer
a,
Steffen
Ganschow
b,
Stefan
Berendts
c,
Andreas
Nenning
a,
Markus
Kubicek
a,
Daniel
Rettenwander
def,
Andreas
Limbeck
a and
Jürgen
Fleig
*a
aInstitute of Chemical Technologies and Analytics, TU Wien, Vienna, Austria. E-mail: Juergen.Fleig@tuwien.ac.at
bLeibniz-Institut für Kristallzüchtung, Berlin, Germany
cInstitute of Chemistry, TU Berlin, Berlin, Germany
dDepartment of Material Science and Engineering, NTNU Norwegian University of Science and Technology, Trondheim, Norway
eInternational Christian Doppler Laboratory for Solid-State Batteries, NTNU Norwegian University of Science and Technology, Trondheim, Norway
fGraz University of Technology, Institute for Chemistry and Technology of Materials, NAWI Graz, Graz, Austria
First published on 17th June 2021
Cubic Li7La3Zr2O12 (LLZO) garnets are among the most promising solid electrolytes for solid-state batteries with the potential to exceed conventional battery concepts in terms of energy density and safety. The electrochemical stability of LLZO is crucial for its application, however, controversial reports in the literature show that it is still an unsettled matter. Here, we investigate the electrochemical stability of LLZO single crystals by applying electric field stress via macro- and microscopic ionically blocking Au electrodes in ambient air. Induced material changes are subsequently probed using various locally resolved analysis techniques, including microelectrode electrochemical impedance spectroscopy (EIS), laser induced breakdown spectroscopy (LIBS), laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), and microfocus X-ray diffraction (XRD). Our experiments indicate that LLZO decomposes at 4.1–4.3 V vs. Li+/Li, leading to the formation of Li-poor phases like La2Zr2O7 beneath the positively polarized electrode. The reaction is still on-going even after several days of polarization, indicating that no blocking interfacial layer is formed. The decomposition can be observed at elevated as well as room temperature and suggests that LLZO is truly not compatible with high voltage cathode materials.
One of the most promising solid electrolytes is cubic Li7La3Zr2O12 (LLZO), first reported by Murugan et al. in 2007,5 which is usually stabilized at room temperature by aliovalent substitution. Numerous substitution elements including Al, Ga, Nb, Ta, and Fe have been reported and Li-ion conductivities in the range of 10−4 to 10−3 S cm−1 have been achieved.6–16 Beside its high conductivity, the garnet-type solid ion conductor is known for its good electrochemical stability, particularly its chemical stability against elemental Li, enabling the use in Li metal batteries.2,5,17,18 However, despite intensive research on LLZO in recent years, many aspects are still not understood and several challenges remain. For example, the instability of LLZO in an ambient environment as well as interface issues can limit the application of LLZO in all-solid-state batteries.19,20
Also the electrochemical stability of LLZO is still an unsettled matter. Early experimental studies report a very wide electrochemical window ranging from 0 V vs. Li+/Li to at least 5 V vs. Li+/Li, implying the possible compatibility with high voltage cathode materials.7,16,21 In contrast to that, density functional theory (DFT) calculations show a much narrower electrochemical window of 0.05–2.91 V vs. Li+/Li.22,23 According to these calculations, LLZO gets oxidized at 2.91 V to form Li2O2, Li6Zr2O7, and La2O3.22,23 In another computational study based on DFT calculations, Richards and et al.24 report an oxidation potential of approx. 3.4 V vs. Li+/Li.
According to several studies, cyclic voltammetry (CV) measurements based on semiblocking electrodes, which were used in the early experimental studies,7,16,21 lead to an overestimation of the electrochemical stability of LLZO and are thus not suitable to determine the true electrochemical window of the material.22,23,25 Han et al.23 claim that the overestimation is caused by kinetic stabilization and propose the use of a Li/LLZO/LLZO-C cell for reliable CV measurements. Using this cell design, the authors determined that the oxidation of LLZO starts at about 4.0 V vs. Li+/Li.23 Another approach was used by Thompson et al.,25 who combined direct current (DC) chronoamperometry, alternating current electrochemical impedance spectroscopy (EIS), optical absorption band gap measurements, and first-principles calculations, leading to the conclusion that LLZO has a sufficiently large band gap of 6.4 eV to enable its use with high-voltage cathodes. Due to these controversial reports, it is obvious that more research is necessary to truly understand the stability behavior of LLZO.
In this work, the electrochemical stability of LLZO single crystals is investigated using field stress experiments in combination with subsequent electrochemical, chemical, and structural analysis. DC voltages up to 3 V were applied in ambient air using ionically blocking Au electrodes in two different geometries. In a first set of experiments, macroscopic stripe electrodes were used to conduct field stress experiments at elevated temperatures. The effects induced by the polarization were investigated using microelectrode EIS, scanning electron microscopy (SEM), as well as laser induced breakdown spectroscopy (LIBS). The revealed LLZO decomposition was further investigated using another set of experiments, in which individual microelectrodes were positively polarized against a macroscopic counter electrode. After these polarization experiments at elevated temperatures, compositional and structural changes within the material were investigated using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) and microfocus X-ray diffraction (XRD), respectively. Strong Li-depletion beneath the microelectrodes is revealed, leading to the formation of Li-poor phases like La2Zr2O7. The LLZO decomposition is still on-going even after several days of polarization and is also observable at room temperature, questioning if LLZO is compatible with high voltage cathode materials.
Ta:LLZO was grown from the stoichiometric melt of nominal composition which would naturally lead to the same composition of the grown crystal only if the compound melted congruently. This crystal was severely defective in its upper, first grown part where it contained expanded white opaque regions and many cracks. The last grown part, however, was transparent and colorless. In contrast, the Ga:LLZO was grown from a melt with 20 mol% Li2O excess. Also this crystals was of low quality in its first grown part and transparent with yellow color in the last part.
The powder mixtures, either stoichiometric or Li2O excessive, were pressed isostatically at 500 bar and sintered for 70 hours at 680 °C (Ta:LLZO) or 6 hours at 850 °C, consequently ground and pressed again at 2000 bar and sintered a second time at 1230 °C for 6 hours (Ga:LLZO). The sintered material was melted in a 40 ml inductively heated iridium crucible under protective atmosphere (N2 for Ta:LLZO, Ar for Ga:LLZO). In case of Ta:LLZO growth was initiated at an iridium wire that was dipped into the melt serving as a cold finger where formation of crystal nuclei was expected to occur when the melt was undercooled. For Ga:LLZO we used a roughly [100]-oriented small piece of crystal obtained in a previous experiment. In both cases, the wire, respectively the seed, was slowly pulled upwards at rates between 0.4 and 1.0 mm h−1 and the power of the generator was used to control the mass growth rate and therewith the diameter of the growing crystal (≈15 mm). Growth was stopped when about one third of the melt crystallized. The crystal was withdrawn from the melt and cooled down to room temperature in 15 hours.
For the investigation described in this study, samples were prepared from the transparent last parts of both crystals. The chemical composition of the synthesized samples was determined via ICP-OES analysis. Sample compositions of Li6.12La3Zr0.88Ta1.03O11.9 (normalized to 3 La pfu) and Li6.43Ga0.14La2.84Zr2O11.68 (normalized to 2 Zr pfu) were determined for the Ta:LLZO and Ga:LLZO crystal, respectively. Accordingly, only about one third of Ga was incorporated during crystal growth. Details on the instrumental parameters used for the ICP-OES can be found in the ESI (Table S1†). More information regarding the chemical analysis of LLZO via ICP-OES can be found elsewhere.26
Crystal slices with a thickness of about 1 mm were used for all experiments. To remove near surface reaction layers, the samples were polished by SiC grinding paper (#4000) directly before electrode preparation. Ionically blocking Au electrodes (100–200 nm thickness) were deposited by DC sputtering (MSC 010, Bal-Tec, Germany) at room temperature. Micro-structuring was performed using two different procedures. As first approach, photolithography in combination with subsequent ion beam etching was used. For the photolithography process, a negative photoresist (ma-N 1420, Micro Resist Technology, Germany) in combination with a tetramethylammoniumhydroxid (TMAH) based, aqueous-alkaline, metal ion free developer (ma-D 533/S, Micro Resist Technology, Germany) was employed. Additionally, the sample came into contact with distilled water (stopping the development process) as well as ethanol p.a. (removing remaining photoresist) during the procedure. As second approach for micro-structuring, direct sputtering using Ni shadow masks (Temicon GmbH, Germany) was applied.
Two different electrode configurations were used, which are illustrated in Fig. 1. In both cases the bottom side of the samples was completely covered with an Au electrode.
![]() | ||
Fig. 1 Schematic illustration of the used electrode configurations: (a) macroscopic stripe electrode with circular microelectrodes in between and (b) array of circular microelectrodes. |
Locally resolved EIS measurements were performed to investigate the impact of the field stress on the conductivity behaviour of the material. For that purpose, a row of microelectrodes located between the macroscopic polarization electrodes was analysed before as well as after the polarization experiment. Measurements were performed at room temperature using the Au layer on the bottom side of the sample as counter electrode. An Alpha-A high performance frequency analyser (Novocontrol Technologies, Germany) and a frequency range of 1 to 500 kHz was used for all EIS measurements. The obtained impedance spectra were fitted according to ref. 28. From the spreading resistance Rspread and the microelectrode diameter d, the local ionic conductivity of the probed sample volume σMe was calculated using eqn (1).29
![]() | (1) |
After polarization, the morphology of the electrodes was investigated via SEM using a Quanata 200 instrument (FEI, USA) operated at 10 kV acceleration voltage. Energy-dispersive X-ray spectroscopy (EDX) was conducted to investigate the material deposited on the cathode using an Octane Pro Silicon Drift detector (EDAX, USA) equipped on the instrument. To prevent electrostatic charging, the samples were coated with Au prior to the SEM analysis.
LIBS was used to gain spatially resolved information about the chemical composition of the sample. For that purpose, line-scans across the polarization axis were performed after the polarization experiment and EIS measurements were finished. Prior to each experiment, a pre-ablation line-scan removing the electrodes was carried out to avoid that the obtained signals are affected by the Au on top of the sample. Measurements were performed using a commercially available J200 LIBS system (Applied Spectra Inc., USA) equipped with a 266 nm frequency quadrupled Nd:YAG laser and a six-channel Czerny–Turner type spectrometer covering a wavelength range from 188 to 1048 nm. LIBS data was collected using Axiom 2.0 software provided by the manufacturer. Details on the instrumental parameters used for the LIBS measurements can be found in the ESI (Table S2†).
LA-ICP-MS was used to investigate field stress induced changes in the chemical composition. For the investigation, multiple line-scans across the polarized microelectrodes were performed. An untreated electrode was always investigated together with a polarized electrode and was used as reference measurement. An iCAP Qc quadrupole ICP-MS (Thermo Fisher Scientific, Germany) coupled to a NWR213 laser ablation system (ESI, USA) equipped with a 213 nm Nd:YAG laser and a fast-washout ablation cell always positioned above the actual ablation site was employed. Qtegra software provided by the manufacturer of the instrument was used for data acquisition. Prior to the experiments, the tune settings of the MS instrumentation were optimized for maximum 115In signal using a NIST 612 trace metal in glass standard (National Institute of Standards and Technology, USA). Detailed information about the used instrumental settings can be found in the ESI (Table S3†). The sampling depth of the experiment was determined using a DektakXT profilometer (Bruker, USA).
XRD measurements were performed using an Empyrean diffractometer (Malvern Panalytical, Germany) equipped with a focusing mirror, a 0.3 mm microfocus, and a GaliPIX3D detector. Cu Kα radiation (45 kV, 40 mA) and a 2θ scan range from 20° to 80° was used. For the measurements, the X-ray beam was focused on individual microelectrodes. All scans were done with a measuring time of 4.5 h per sample. The obtained diffractograms were analyzed using Panalytical Highscore.30
2Li+ + 2e− + CO2 + ½O2 → Li2CO3 |
Accordingly, oxygen is reduced at this electrode. This is confirmed by the EDX spectrum of the deposited solid (Fig. 3h). Beside Au, most likely originating from sample coating prior to the SEM analysis, only C and O can be observed. This shows that the deposited substance does not contain La, Zr, or Ta, leaving only Li as a possible cation (Li cannot be detected by conventional EDX). In principle, this electrochemical reaction is expected to occur close to the triple phase boundaries. The fact that large parts of the electrode surface are covered by reaction products indicates that the Au layer becomes porous during the field stress experiment. Another possible option is that Li2CO3 (or another Li-containing salt) is not formed directly, but initially metallic Li or an Li/Au alloy accumulates at the cathode, which is then converted to Li2CO3 due to reaction with the ambient environment. Strong alloying, however, should cause a severe shift of the Li chemical potential in the electrode, which is not confirmed by the polarization experiments performed on microelectrodes shown later in this work (cf. Section 4). Hence, we suppose that some defects in the Au films (cracks, etc.) allow direct access of gas phase to the LLZO surface also ‘within’ the electrode and thus enable growth of Li-containing salts. This may cause further morphological changes of the electrode and further growth.
The positively polarized electrode (anode) shows a rough surface after polarization (Fig. 3i–k). The roughness appears to be caused by gas bubbles, possibly arising from O2 formation due to oxidation of oxide ions, lifting parts of the electrode from the sample surface. To compensate the occurring loss of O2− ions, negatively charged Li vacancies need to be created, ultimately leading to either (1) LLZO with a sub-stoichiometric amount of O2− and Li+:
Li7La3Zr2O12 → Li7−2xLa3Zr2O12−x + x/2O2 + 2x Li+ + 2x e− |
Or (2) the formation of Li-poor phases such as La2Zr2O7 and La2O3:
The substitution element is not considered in the given reaction equations for simplicity reasons. Additional decomposition products might be formed due the presence of a dopant (e.g., LaTaO3 in case of Ta). The formation of La2Zr2O7 due to electric field stress is confirmed by XRD later in this work (see Fig. 10).
The measured current flowing through the sample during polarization (see ESI, Fig. S1†) is also in accordance with our assumption of a continuous electrochemical reaction. After a rapid decrease within the first minutes of the experiment, the current stabilized and remained at approx. 1 μA for the rest of the measurement. Given the electrode and sample geometry (distance between electrodes = 2 mm; cross section = 0.5 mm2), an electronic conductivity of about 1.3 × 10−5 S cm−1 would be necessary to reach such a high steady-state current, which is unlikely considering the values reported in literature (5 × 10−12 to 2 × 10−9 S cm−1 at room temperature14,25,31 and in the range of 10−7 S cm−1 at 350 °C (ref. 32)). We therefore attribute the measured current to continuous decomposition of the sample caused by field stress, and thus largely Li+ current.
The microelectrode measurements reveal a clear impact of the polarization experiments on the conductivity behavior of the material. While the local ionic conductivity increased close to the cathode, the opposite effect can be observed close the anode: the conductivity decreased up to 15% (see Fig. 4a and b). Interestingly, this effect cannot be correlated to changes in the Li stoichiometry, since chemical analysis via LIBS did not reveal any variations of the Li-content between the electrodes (Fig. 4c). The changes in the conductivity behavior were therefore either caused by Li stoichiometry changes too small to be observed via our LIBS measurements, or by other factors like local variations of site occupancies or oxygen vacancies.34 However, in contrast to the region between the electrodes, the LIBS analysis revealed huge variations in Li very close and/or beneath the stripe electrodes with almost no change in La. While an increased Li content can be observed on the cathode, most likely due to the formation of Li2CO3 as already confirmed by EDX (see above), the Li concentration strongly decreased at the anode, confirming the presence of Li-poor phases and/or LLZO with a Li+ sub-stoichiometry. The results thus confirm that the applied electric field stress leads to an electrochemical reaction decomposing the material.
To summarize our findings, the processes taking place during sample polarization are visualized in Fig. 5. As already discussed, O-ions of LLZO are oxidized and O2 from the surrounding air is reduced anode and cathode, respectively. Overall, Li-ions are transported through the sample, first leaving vacant Li+ sites as well as O-vacancies in LLZO at the anodic side, and ultimately leading to the formation Li-poor phases like La2Zr2O7.
Please note: the conducted experiments show that LLZO decomposes when a bias of 3 V is applied at 400 °C, but this does not mean that the electrochemical window of LLZO is <3 V. The reason for this is that the Li chemical potentials of neither the cathode nor the anode is fixed, since ionically blocking Au electrodes are used on both sides. We also do not have sufficient information so far, which impurity levels are allowed in inert gases to avoid this process.
To better visualize the relationship to the applied voltage, the measured currents for each voltage step are plotted on a logarithmic scale in Fig. 7d. In this plot, the currents measured at the end of the corresponding voltage step are shown, representing the ‘stabilized’ current obtained when voltage is applied for a certain time. It becomes clear from the time dependencies in Fig. 7a and b that this does not represent a true steady-state current for the high-voltage regime, but the prevailing trends are well accessible. Interestingly, an almost exponential current increase can be observed for the lower voltages (0.2–1.0 V). The origin of the steady-state current in the regime has not been investigated in detail so far. However, electron conduction is a likely explanation with realistic conductivity values in the 10−9 S cm−1 range. In the high-voltage regime (1.4–2.4 V), the measured currents are nearly constant for each voltage step, once more confirming the distinctly different conductivity behavior for higher voltages. Constant voltage experiments presented later in this work reveal that LLZO decomposition is the main source of current if a voltage of 2 V is applied on the material. Most probably the entire constant current regime is characterized by the same electrochemical process and thus we suggest that already at 1.2–1.4 V LLZO decomposition takes place. The two different regimes (electron conduction and LLZO decomposition) are also indicated in Fig. 7d.
To make any conclusion about the electrochemical stability window of the material, it is necessary to know the chemical potential of Li at the ionically blocking counter electrode, which hardly changes in this experiment (see above), but is not truly well defined in our case. This chemical potential has to be estimated. Since during synthesis of the single crystals the material is surrounded by Li2O in the gas phase, the chemical potential of Li in LLZO is very likely defined by Li2O (around 2.9 V vs. Li+/Li (ref. 35)). Accordingly, also the counter electrode is at 2.9 V vs. Li+/Li. From our experiments we can thus conclude a stability limit of 4.1–4.3 vs. Li+/Li at this elevated temperature. These finding are in agreement with the experimental data of Han et al.23 (LLZO oxidation starts at about 4.0 V vs. Li+/Li at room temperature), and support the hypothesis that extended electrochemical window observed in other experimental studies originates from kinetic stabilization.22,23
In Fig. 8b and c, the obtained Li signal is normalized to the intensity of the corresponding Zr signal. In the normalized signal, variations in material ablation during the measurement are compensated, making it a good representation of the Li-stoichiometry. A decrease of up to 83% can be observed for the longest polarization time (66 h), confirming that Li-ions are strongly depleted in the topmost sample layer beneath the electrode. Comparing different polarization times shows that the observed Li-depletion steadily increases over time (Fig. 8b). This indicates that the induced LLZO decomposition is on-going even after several days of polarization and is not stopped by the formation of an interface layer.
To investigate effects deeper inside the material, each electrode was analyzed two more times after the initial LA measurement. Each ablation pass removed approx. 2 μm material, giving access to (rough) depth-resolved information. In Fig. 8c, the three measurements of the longest polarized electrode (66 h) are compared. The induced Li-depletion is less pronounced for every subsequent ablation pass, however, even for the third and last sample layer significant effects (30% decrease) can be observed. This means that even in a sample depth of approx. 4–6 μm material changes have been induced by the applied field stress. Given the fact the effect is relatively small for the third layer, and is not observable at all for electrodes with lower polarization times, we still can assume that most of the affected sample volume is probed by the analysis.
To investigate if the relatively high currents during electrode polarization were indeed caused by the observed Li-depletion, the total amount of transported Li-ions Li+trans was estimated using the measured stoichiometry changes. The formula
![]() | (2) |
Fig. 9a shows the calculated amounts of transported Li-ions for the already discussed polarization series on Ta:LLZO (cf.Fig. 8). The LA-ICP-MS determination is compared to values obtained from the corresponding current measurements, calculated under the assumption that all measured current solely originates from irreversible transport of Li-ions. The values obtained from the current profiles are generally higher and the relative difference increases with increasing polarization time. However, the results of both quantification approaches show a very similar trend and are in the same order of magnitude even for the longest polarization experiments. This reasonable agreement thus confirms that a substantial part of the polarization current is indeed caused by LLZO decomposition and the associated Li-depletion beneath the anode. The deviation between the values obtained by LA-ICP-MS and DC measurements might be caused by several reasons, namely (1) contribution of other processes (e.g., electronic conduction) to the total current, (2) inaccuracies of the assumptions used for the calculations (e.g., non-uniform Li-ion transport beneath the electrode), and (3) additional Li-depletion deeper in the material not probed by the LA analysis.
An analogue series of polarization experiments performed on a Ga:LLZO single crystal shows very similar results (Fig. 9b). The total amount of transported Li-ions is significantly higher compared to Ta:LLZO, which is in agreement with the higher decomposition current found in the polarization experiments with stepwise voltage increase (cf.Fig. 7). Beside that, the only observable difference was a higher ablation rate for Ga:LLZO during the LA experiment (about 3 μm per ablation pass). Overall, the substitution element only seems to affect the decomposition rate, not the process itself.
While in all previously shown experiments micro-structuring was performed using a combination of photolithography and ion beam etching, the microelectrodes used for the experiment series on Ga:LLZO were prepared via direct sputtering using a Ni shadow mask. Since this process is solvent-free, it can be excluded that contact with protic solutions during photolithography (see Experimental), potentially leading to Li+/H+ exchange,37–39 is the reason for the observed phenomena.
This also raises the question of the species carrying the current across this zone with decomposition products. This is certainly strongly dependent on the exact 3D distribution of the reaction products in this reaction zone. We hardly expect a simple layer-by-layer structure. However, we may face a situation where not only Li+ transport but also oxide ion transport and electron transport may play a role (see sketch in Fig. 11). Owing to the lack of reducible cations, Li-depletion in LLZO most probably takes place via formation of oxygen vacancies. Substantial oxygen vacancy concentrations and O2− conduction in LLZO was already confirmed in ref. 34. Any further depletion of Li within an LLZO phase (forms Li7−2xLa3Zr2O12−x) thus requires oxide ion conduction in LLZO (path 1 in Fig. 11). Depletion of Li in LLZO without direct contact to the electrode requires further conduction of O2− also in a reaction product (path 2). In parallel to these faradaic currents with electrochemical reactions we may have a certain e− leakage current across the entire sample. However, the LA-ICP-MS measurements clearly showed existence of substantial faradaic processes which do not stop due to the limited O2− conduction in the reaction zone even after 5 μm thick layers of reaction products have formed.
In summary, these experiments clearly show that significant LLZO decomposition is induced at an applied voltage of 2 V, which corresponds to approximately 4.9 V vs. Li+/Li according to our estimation (see above). The reaction is on-going even after several days of polarization, meaning that the formed interfacial layers do not block further decomposition, at least under the given experimental conditions (ambient air, elevated temperature). Our results therefore question the stability of LLZO against high voltage cathode materials. Moreover, the current–voltage curves in Fig. 7 strongly suggest that the entire constant current regime between 1.4 V and 2.5 V is characterized by the same electrochemical process. This means that already above 1.2–1.4 V severe decomposition of LLZO takes place, which translates to a stability limit of 4.1–4.3 vs. Li+/Li at this elevated temperature.
The obtained current profile shows the usual rapid decrease at the beginning of the experiment, which is followed by a current in the 0.01–0.1 nA range (approx. 0.1–1.2 μA cm−2 with respect to the microelectrode) for the rest of the polarization time (Fig. S4†). Analogue to the experiments above, LA-ICP-MS was used to investigate the microelectrode after polarization (Fig. S5†), revealing a significant difference to reference electrodes and thus confirming that Li-depletion occurred during the experiment. As expected, the effects induced by the polarization are significantly less pronounced at room temperature, especially considering the long polarization time. For the sample layers directly beneath the electrode (i.e., the first ablation pass of the LA experiment), 82% of the initial Li-content was measured. This corresponds to a total amount of transported Li-ions of 0.130 nmol. Similar amounts were reached at 350 °C (set temperature) already after 30 min. In Table 1, the results of the analysis are compared to the amount of charge carrier transport derived from the measured current. The values are in the same order of magnitude, once more showing that the results of the LA-ICP-MS analysis are reasonable. Overall, the experiment confirms that significant LLZO decomposition occurs even at room temperature, further questioning the long-term stability of LLZO with high voltage cathode materials.
Total amount of transported Li+ | |
---|---|
LA-ICP-MS | 0.130 nmol |
DC | 0.423 nmol |
Ratio | 30.1% |
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d1ta02983e |
This journal is © The Royal Society of Chemistry 2021 |