M. Tauhidul
Islam
a,
Harald
Fitzek
bc,
Bernhard
Gollas
a and
Qamar
Abbas
*ad
aInstitute for Chemistry and Technology of Materials, Graz University of Technology, Stremayrgasse 9, 8010 Graz, Austria. E-mail: qamar.abbas@tugraz.at
bGraz Centre for Electron Microscopy, Steyrergasse 17, 8010 Graz, Austria
cInstitute of Electron Microscopy and Nanoanalysis, Graz University of Technology, Steyrergasse 17, 8010 Graz, Austria
dInstitute of Chemistry and Technical Electrochemistry, Poznan University of Technology, Berdychowo 4, 60965 Poznan, Poland
First published on 20th March 2025
Understanding the interplay between ion association, desolvation, and electric double layer (EDL) structure is crucial for designing high-performance energy storage devices with concentrated electrolytes. However, these ion dynamics in water-in-salt electrolytes within the nanopores of carbon electrodes are not fully understood. Based on Raman spectroscopy of electrolytes and electrochemical investigations of non-porous electrodes, the classical Gouy–Chapman–Stern model has been modified by incorporating ionicity to estimate the Debye length. The modified model shows a sharp Debye length decrease as the concentration rises from 1 to 10 mol kg−1, followed by an increase due to ion pairing above 10 mol kg−1. The modified model accurately reflects differential and EDL capacitance values obtained from cyclic voltammetry and electrochemical impedance spectroscopy. The data obtained for non-porous electrodes was divided by the MacMullin number (ratio of tortuosity to porosity) of the carbon electrode to estimate the Debye length in the pores. The introduction of the MacMullin number into the Stokes–Einstein equation allowed the estimation of ionic radii within pores, which was subsequently used to calculate the extent of ion desolvation/dehydration in micro- and mesopores. The concentration-dependent ion association governs the Debye length trends in pores, correlating radii of confined ions, ion desolvation, and EDL charging dynamics. Our findings suggest a concentration of 5 mol kg−1 LiTFSI as optimal for fastest charging rates and 10 mol kg−1 for highest energy density, providing critical insights for developing efficient electrolytes and porous carbon electrodes.
The concept of the EDL began with Helmholtz in 1879,16,17 who described it as a simple capacitor formed by ions in the electrolyte aligning near a charged surface. In the early 1900s, Gouy and Chapman expanded this idea with the Gouy–Chapman (GC) model, introducing the concept of a diffuse layer where the ions remain mobile and do not adsorb directly onto the charged surface.18 Instead, the ion distribution within this layer is governed by a balance of electrostatic attraction and thermal motion, where the ion concentration decays exponentially over a distance known as the Debye length. In 1920, Stern combined the Helmholtz and GC models to create the Gouy–Chapman–Stern (GCS) model, which accounts for both an immobile Stern layer closest to the electrode surface and a mobile diffuse layer beyond it.19 However, these classical theories are generally ineffective in describing the electrode–electrolyte interface for concentrated 2 to 10 M aqueous solutions of e.g. LiCl, NaCl, and CsCl as has been experimentally demonstrated by Gaddam et al.20 and Smith et al.21
Most of the earlier models fall short in capturing the intricate interfacial behavior observed in ionic liquids (ILs) due to the interplay of van der Waals, coulombic, dipolar, and solvophobic interactions.22–24 To this end, Kornyshev and co-workers in 2007 used the Poisson–Fermi equation to model concentrated ionic liquid interfaces employing a mean-field lattice-gas model to derive an analytical expression for the differential capacitance.25 Around the same time, Bazant et al. independently arrived at a similar analytical solution by applying a modified Poisson–Nernst–Planck equation, developing similar expressions for capacitance and potential distribution.26 Interestingly, Oldham,27 when adapting the GCS model for IL-electrode interfaces, achieved the same potential profile predictions as those from Goodwin–Kornyshev's mean-field theory in selected scenarios. Recently, Safran and Pincus,28 and the team of Kornyshev29,30 demonstrated the effect of ion pairs on the EDL of ILs. In a recent review, Coskun et al. mapped the electrode–electrolyte interfaces of ionic liquids and deep eutectic solvents, offering a highly recommended resource for understanding the chronological progress in this field.23
Particularly for water-in-salt electrolytes, prior scattering, spectroscopy, and surface force studies have revealed that the EDL comprises both short-range (<10 nm) and long-range (10–50 nm) interfacial layers of ordered ions near the electrode surface.31–36 McEldrew et al. adapted the Poisson–Fermi theory to explain the EDL structure in concentrated LiTFSI using molecular dynamics.37 However, they ignored the effect of ion-pairing in water-in-salt electrolytes. Moreover, there are limited reports on theories explaining experimental EDL results in bulk water-in-salt solutions. Furthermore, these theories still need to be adapted to adequately explain the EDL structure of water-in-salt electrolytes in carbon pores. Some intricate efforts have been made by Huang et al. and Zuliani et al. to adapt the GCS model to carbon pores for a wide range of diluted electrolytes.10–12 These modified models are still limited if the average pore size is close to the size of the solvated or desolvated ions.38–40 In addition, commercially available carbons usually have pores of different sizes, making it challenging to efficiently probe and differentiate the EDL structure in multiporous carbons using these theories.6,40,41 Modelling the EDL structure of water-in-salt electrolytes in the porous carbon using Goodwin–Kornyshev's mean-field theory including ion-pairing effects and parameters for pores of different sizes, would lead to a highly complex model with numerous elements.
In addition, ion desolvation/dehydration plays a pivotal role in the charging dynamics of sub-nanometer pores.42 Understanding the intricate relationships among ion pairing, ion desolvation, and the resulting EDL structure is essential for designing high-performance electrochemical capacitors with water-in-salt electrolytes. In situ techniques such as NMR, EQCM, and EQCA are commonly used to investigate desolvation in diluted electrolytes.14,15,42,43 However, to the best of our knowledge, ion desolvation in water-in-salt electrolytes within carbon pores has not been systematically studied yet.
Furthermore, carbon electrodes often possess a complex architecture with sub-nanometer micro-, meso-, and macropores, which results in sluggish ion transport of water-in-salt electrolyte.5,6 Slow electrosorption in sub-nanopores present significant challenges for utilizing those mentioned experimental techniques and models to effectively determine and differentiate ion desolvation and the resulting EDL structures within different pores of a multiporous framework.
In this work, we first adapted the Gouy–Chapman–Stern model for bulk water-in-LiTFSI electrolyte by incorporating ionicity into the calculation of the Debye length, i.e. the diffuse layer thickness. The trend of the EDL capacitance as a function of the electrolyte concentration using the modified expression for the Debye length closely matches the values obtained from electrochemical impedance spectroscopy (EIS). Likewise, the trend of the diffuse layer thickness aligns with the experimental differential capacitance. We used a commercial carbon containing micro- and mesopores to comprehend the Debye length in the pores. Rather than using complex models,10–12 we simply divided the Debye length at non-porous electrode by the MacMullin number, i.e. the ratio of tortuosity to porosity,44–46 to differentiate the Debye length distribution in micro- and mesopores. Furthermore, introducing the MacMullin number into the Stokes–Einstein equation enabled the estimation of ionic radii within pores, which was subsequently used to determine ion desolvation in micro- and mesopores. Our findings reveal that ion association governs the Debye length trends in pores, aligning precisely with patterns of confined ionic radii, desolvation, and resulting EDL structure.
The observed impedance behavior, with a tail-like Nyquist plot and the absence of maxima in the plots of imaginary impedance (Z′′) (Fig. S2†), real permittivity (ε′) (Fig. 1b), and imaginary capacitance (C′′) vs. frequency (Fig. 1c), indicate the water-in-LiTFSI systems do not have a distinct dielectric relaxation between 1 MHz and 1 mHz, where the capacitive or permittivity properties would significantly change at open circuit potential. The real part of the capacitance of the non-porous electrode also gives no reasonable information (Fig. S3†). Such a phenomenon is typical also for other reported homogeneous diluted electrolytes including KCl and NaCl, where the double-layer capacitance is the primary contributor to the impedance response across the measured frequency range.47,48
In this case, representations of conductance (eqn (S8)†) and susceptance (eqn (S9)†) would be insightful,48 as the major focus of this study is the EDL response. These two quantities are also often termed as real (Y′) and imaginary (Y′′) parts of admittance (Fig. S4†). Khademi et al. compared both equivalent circuit models and admittance for determining the EDL capacitance in NaCl/surfactant mixtures and found similar values.48 Hence, they recommended utilizing admittance for accurate and direct measurement of capacitance, eliminating the necessity for additional modelling assumptions.48 However, for broad reader interest, we further normalized the real and imaginary part of admittance with the cell constant to obtain the real (σ′) and imaginary (σ′′) ionic conductivity from eqn (S10) and (S11),† respectively.47 Notably, according to these equations, the entire measurement cell is treated as a single capacitor.
In the high-frequency regime, Fig. S5† demonstrates the real part of ionic conductivity as a function of excitation frequency, which corresponds inversely to the trend previously observed in impedance. In all spectra, σ′ shows an initial rise with increasing frequency, eventually reaching a plateau in the mid to high-frequency range. As frequency increases, the current begins to bypass the charge transfer resistance through the EDL capacitor.
Moreover, the plateau observed at mid to high frequencies corresponds inversely to the series resistance. In contrast, the key feature of these σ′′ spectra (Fig. 1d) is the presence of a characteristic frequency (f0) at the local maxima, which refers to the charging of the EDL capacitance. This peak shifts towards higher frequencies with increasing LiTFSI concentration until 5 mol kg−1. Beyond this concentration, both σ′′ and f0 decrease, becoming gradually lower towards 20 mol kg−1.
Most likely, at an open circuit voltage of around 30 mV, the stainless-steel rod current collector could be treated as a blocking (non-reactive) electrode. Thus, the f0 of the σ′′ spectrum can be related to EDL capacitance, CEDL, and equivalent series resistance RS, as expressed in eqn (1). The values of Z′ at 1 MHz correspond to RS.
![]() | (1) |
The CEDL obtained using the characteristic frequency method (Fig. 1e) was compared with the differential capacitance derived from cyclic voltammetry. A narrow potential window (Fig. S6†) was chosen for recording the voltammograms to prevent the emergence of cathodic and anodic humps caused by the decomposition of TFSI−.49 The capacitive current was divided by the scan rate to estimate the average differential capacitance. In an ideal system, capacitive current increases proportionally with the scan rate keeping the differential capacitance constant. However, the currents in CVs of water-in-LiTFSI solutions deviated from such ideal behaviour, probably due to faradaic contributions. This results in a decrease in differential capacitance determined from the voltammetric currents as demonstrated in Fig. S7 and S8.† Therefore, the differential capacitance was determined by averaging the values across five scan rates (10, 20, 50, 100, and 500 mV s−1) at 0 V versus SCE (Fig. 1e). The CEDL values were an order of magnitude higher than Cdiff., reaching a maximum value at 5 mol kg−1. The difference between CEDL and Cdiff. can be attributed to variations in cell setup, electrochemical methodology, electrode material, and applied potential range. Above this concentration, a declining trend in the capacitance was recorded due to inadequate ion dissociation at these very high concentrations. Based on the above electrochemical characteristics, it is envisioned that quicker polarization, i.e. improved charge/discharge rate performance or power performance of the capacitor cell, could be achieved at 5 mol kg−1 due to higher permittivity values. Conversely, 10 mol kg−1 may be more suitable for delivering higher EDL capacitance and greater energy density.
The following section provides a broader insight into ion-pairing, using several qualitative, configurational, and quantitative approaches to narrate a proper understanding of EDL structure in water-in-salt electrolytes.
The high-frequency semicircle indicates high mobility of free Li+ and TFSI− and rapid solvent relaxation, with minimal ion pairing. The intermediate-frequency semicircle suggests the presence of loosely bound ion pairs, indicating moderate ion pairing. The low-frequency semicircle reflects the slow dynamics of tightly bound ion pairs or larger complexes, indicative of strong ion pairing or aggregation. The diameter of the semicircle varied as a function of salt concentration, endowing a maximum for 5 mol kg−1, thereby following the trend of ionic conductivity (Fig. 1f). A large diameter signifies a high capacity for charge storage, often due to the presence of free or loosely bound ions, while a small diameter for 15 and 20 mol kg−1 indicates lower charge storage capacity, typically due to tightly bound ion pairs.
The influence of ion association on electrochemical data was further confirmed by Raman spectra, showing successive shifts of the sulfur–nitrogen–sulfur (S–N–S) bending band from ∼744 cm−1 (1 mol kg−1) to ∼748 cm−1 (20 mol kg−1) as illustrated in Fig. 2a.53 The LiTFSI salt crystal exhibits an S–N–S band at 751.6 cm−1, as demonstrated in Fig. S10.† This shift results from significant changes in the hydration structure of Li+ and TFSI−, forming various Li+–TFSI− clusters, such as the free anion (FA) at 738.6 cm−1, the loose ion pair (LIP) at 743.9 cm−1, the intimate ion pair (IIP) at 747.4 cm−1, and the aggregate ion pair (AP) at 749.1 cm−1. These regions were deconvoluted to estimate the ion-pair contribution percentages based on their corresponding peak area to total area ratio. Peak fitting details along with error ranges are provided in Tables S1 and S2.† At a low concentration of 1 mol kg−1, FA, LIP, and IIP contributions were 22.3%, 45.8%, and 31.9%, respectively. At a moderate concentration of 5 mol kg−1, the FA signature diminished, with LIP and IIP contributions of 45.8% and 54.2%, respectively. At a very high concentration of 20 mol kg−1, AP was the predominant type, contributing 68.9%, with negligible LIP (2.7%) and IIP (28.4%). These values of different ion-pair shares align well with the results of Suo et al. as shown in Table S3.53†
![]() | ||
Fig. 2 (a) Raman spectra of 1, 10, and 20 mol kg−1 LiTFSI (top to bottom) showing their corresponding free anion, loose ion pair, intimate ion pair, and aggregate ion pair. Vertical red and blue dotted lines indicate the wavenumbers of LIP and IIP. The chemical structures show: the vibration of free TFSI-(FA), the vibration of loosely mono-coordinated TFSI-(LIP), the vibration of loosely/strongly bi-coordinated TFSI-(IIP), the vibration of highly strong bi-coordinated TFSI-(AP); (b) ionic tortuosity and relative permittivity (adopted from ref. 57) of water-in-LiTFSI; (c) inner frictional constant and ionicity of water-in-LiTFSI. The dotted lines in (b) and (c) serve as a guide to the eye. |
PFG-NMR shows the co-existence of these ion pairs to result in a dramatic decrease in the diffusivity of Li+ and TFSI−.2,7,54,55 The self-ion diffusivity values listed in Tables S4 and S5† were used to obtain ion-pair (mutual) diffusivity values DLiTFSI in Table S6.† This was achieved by applying the modified Darken's relationship for binary diffusivity, as proposed by Krachkovskiy et al.56 and summarized in Method S5. The ionic tortuosity of the water channels imposed by the ion pairs could be expressed as the ratio of diffusivity in the 1 mol kg−1 solution to that at any specific concentration between 5 and 20 mol kg−1.55Fig. 2b and Table S6† illustrate a notable monotonic increase in ionic tortuosity with respect to salt concentration, aligning with the observations reported by Han et al.55 Therefore, the polarizability of electrolyte solutions decreases with increasing salt concentration, resulting in a very low relative permittivity in Fig. 2b, as determined by Kim et al. using dielectric relaxation spectroscopy (fitting parameters).57
These spatial phenomena result in a monotonic increase in the inner frictional constant ξ, calculated on the basis of Stokes' law in eqn (2) and illustrated in Fig. 2c.58
ξ = 8πηRH3 | (2) |
The higher inner friction ξ eventually decreases progressively the degree of ion dissociation, i.e. ionicity (Fig. 2c and Table S7†), producing larger ion-pairing up to ∼3.25 nm at 20 mol kg−1 (Fig. 3a). The ion-pairing length is also termed as Bjerrum length, lB, and can be defined by eqn (3).20,58
![]() | (3) |
![]() | (4) |
The above observations on ion pairing motivated us to incorporate the ion dissociation i.e. ionicity values into classical models of diluted solutions to outline the EDL structure in water-in-salt electrolytes as discussed in the following section.
![]() | (5) |
![]() | (6) |
![]() | (7) |
![]() | (8) |
However, eqn (8) is valid only for diluted solutions. Considering the resulting Bjerrum length ranging in a few nanometers, we introduced the ionicity into eqn (8) to adjust it for water-in-salt electrolytes, as expressed in eqn (9).
![]() | (9) |
Fig. 3a shows that, according to the classical Debye model, lDL varies with the square root of the inverse ionic strength, i.e. the bulk electrolyte concentration.
Consequently, the classical CDL values in Fig. 3b increase proportionally with the square root of the electrolyte concentration. However, the trend of the classical CDL does not match the pattern of experimental differential capacitance in Fig. 3c, resulting in potentially unrealistic values larger by an order of magnitude. In contrast, the modified Debye model shows an initial drop of lDL until 10 mol kg−1.
Beyond this concentration, the lDL shifts to higher values due to a major contribution of larger ion pairs i.e. Bjerrum length. Our observed trend and range of the modified lDL align with the findings of the Debye length (∼3–10 nm) in various concentrated electrolytes (1–10 M LiCl, 1–5 M NaCl) reported by Gaddam et al.20 and Smith et al.,21 adopting various techniques and models. In addition, the trend of the modified lDL matches the experimental results of various electrochemical properties. A deviation within the same order of magnitude between the modified CDL and experimental differential capacitance is demonstrated in Fig. 3b. However, the trend of the modified CDL does not align with the experimental one. This inconsistency could be due to the significantly declining values of the numerator εr,DLi.e. relative permittivity of the electrolytes.57
In order to determine the EDL capacitance, we still need to estimate the CSL. This is not straightforward, because lSL is not readily available through any direct experimental methods, and there are no ways to deduce the exact εr,SL of the Stern layer. However, some approximations were adopted following the propositions of Khademi et al.48 for both the Stern layer thickness and permittivity, which are within the correct order of magnitude.
Since lSL is the closest distance of any hydrated Li+ or TFSI− ion to the electrode surface, the summed RH values of Li+ and H2O, and TFSI− and H2O were considered for determining the lSL of Li+ and TFSI−, respectively. The detailed methodology of obtaining RH of Li+, TFSI−, and H2O is discussed in Method S6† and the calculated values are illustrated in Fig. 3d. With increasing salt concentration, lSL was found to decrease from ∼7 to 5 Å (Fig. 3d). This range of lSL values is in line with the range ∼3 to 10 Å reported in the literature, as obtained using different techniques.24,31–36,61–63
The presence of strong electric fields within the Stern layer, even at relatively low potential drops of 10 mV, significantly reduces the permittivity of water due to the reorientation of water molecules and the accumulation of counterions at the electrode surface. This reduction in permittivity of water can vary significantly, ranging from ∼78 to 6, influenced by factors such as surface charge density, electrolyte composition, and distance from the surface.10,11,64
Hence, we calculate the CSL using both original (Fig. 2e) and tenfold reduced permittivity values to cover a comprehensive range within the correct order of magnitude.48Fig. 3e demonstrates the CSL of Li+ and TFSI− with (R) and without reduction (NR) of relative permittivity. Li+ shows a higher CSL due to its smaller RH and lSL compared to TFSI−. The relative permittivity of 1 mol kg−1 and 20 mol kg−1 solutions is 68.17 and 17.26,57 respectively, resulting in a fivefold decrease in CSL from 1 mol kg−1 to 20 mol kg−1. Finally, by combining different CDL and CSL using the GCS eqn (5), the overall CEDL was obtained. Fig. 3f shows the trend of CEDL using the modified lDL matching the experimentally obtained values within the same order of magnitude. This range of CEDL aligns with findings from other experimental and modelling studies, as demonstrated in recent literature review of Schott et al.24 In contrast, using the classical lDL, underestimation of the CEDL was evident, deviating from the experimental trend.
Utilizing the above properties of non-porous electrode, we have extended our study to the EDL structure within a multiporous carbon electrode of electrochemical capacitor cells as described in the following section.
![]() | (10) |
It provides insight into how the structure of the porous electrode affects the movement of ions within it. Understanding the MacMullin number can help to explain various aspects of the electrochemical behavior of capacitors, including EDL formation, ion transport, and the charge–discharge time constant. The detailed method for obtaining NM is provided in Method S7.† Related parameters including porosity (∅) and tortuosity (℧) were estimated using eqn (S16)–(S24)† with values presented in Fig. 3 and Tables S11 and S12.†5 Following Landesfeind et al.44 and Xu et al.,45 we recently reported the effective ion diffusivities in micro and mesopores after dividing the bulk electrolyte diffusivity by NM (Table S12†).5
The range of diffusivity aligns with in situ PFG NMR studies of organic electrolytes in carbons with different pore sizes.40,41 We also adopted the similar concept for deriving lDL in pores. Micropores, being smaller in size offer more tortuous networks than mesopores, resulting in higher NM and smaller lDL values shown in Fig. 4a and b, respectively. With increasing salt concentration, multiple factors shown in Fig. 2 influenced NM, resulting in a complex trend. In contrast, the lDL values in pores followed a pattern similar to those in the bulk, displaying a minimum at 10 mol kg−1. Our calculated lDL values for micro and mesopores closely match the results (∼0.4 to 1.2 nm) obtained with different models such as electric double-cylinder capacitors (EDCC) and electric wire-in-cylinder capacitors (EWCC).10,11 These EDCC/EWCC models were applied to various activated microporous, mesoporous, templated, and carbide-derived carbons in several aqueous, organic, and ionic liquid-based electrolytes, as reported by Huang et al.11 and Zuliani et al.10
In addition, the in-pore lDL values align with the presence of short-range and long-range interfacial layers of ordered ions near the mica electrode surface as demonstrated by Berlinger et al. for water-in-salt LiTFSI and Zn(TFSI)2 electrolytes using scattering, spectroscopy, and surface force measurements.36 The similarity of the values obtained in this work, different reported experiments, and EDCC/EWCC models confirm the accuracy of our approach.
Fig. 4c and d show that the areal gradually increases up to 10 mol kg−1, matching the trend of the lDL values in pores and ionic resistivity in ion-pores (Table S12†). The higher surface area provides a larger capacitance in micropores than in mesopores. In a similar carbon sheet, these intra-and inter-connected pores act as series capacitors. Hence, the reciprocal of micro and mesopore capacitance equals the total experimental capacitance from EIS. At 15 and 20 mol kg−1, however, a further increase in areal
was observed, which is inconsistent with the trend of lDL values in the pores. The gravimetric
in Table S12† also shows the same pattern.
From the trend of lDL values in the pores, we can infer the expected behavior of the diffuse layer capacitance within the pores to double-check the trend of . According to eqn (7) and the EDCC/EWCC models,10,11 it can be assumed that the relative permittivity values (Fig. 2b) in the numerator will significantly decrease, while the in-pore lDL in the denominator will concurrently increase at concentrations of 15 and 20 mol kg−1 for higher values of the Bjerrum length (Fig. 3a). Therefore, this combined effect will lead to a decrease of in-pore diffuse layer capacitance at these concentrations, analogous to the trend seen for non-porous electrode CDL in Fig. 3b. Similarly, a likely monotonic decline of the Stern layer capacitance within the pores aligns with the non-porous electrode CSL. From this, it can be deduced that the general trend of the theoretical CEDL in the pores reflects the pattern of the lDL in the pores, resulting in a maximum at around 5 or 10 mol kg−1.
In order to verify these theoretical statements, the real () and imaginary (
) conductivities of the electrochemical capacitor cells were determined using eqn (S10) and (S11),† as shown in Fig. S11† and 4e, respectively. Similar to the non-porous electrode, we determined the EDL capacitance of capacitor cells using eqn (1). The equivalent series resistance (RS) values were taken from the Nyquist impedance plot of capacitor cells as supplied in Fig. S12.† The characteristic frequency values of eqn (1) were taken from the maximum
positions in Fig. 4e. With increasing salt concentration, the CEDL values in the pores (Fig. 4f) increased until 10 mol kg−1 and then decreased, matching the exact trend of the Debye length in Fig. 4b. The only difference is that the non-porous electrode exhibited a maximum CEDL at 5 mol kg−1. For a better comparison, specific/gravimetric CEDL,in-pore, time constant, and other calculation details are provided in Table S13.† Using EDCC/EWCC models, Huang et al. also obtained similar values for the CEDL between ∼6 and 16 μF cm−2 for various carbons and a wide range of electrolytes.11 The similarity of theoretical and experimental non-porous and porous electrode's CEDL values in this work confirms the accuracy of our approach to modify the Gouy–Chapman–Stern model by introducing the ionicity. In addition, using the MacMullin number is an easy approach that does not require step-by-step complex approximations. Finally, the imaginary conductivity-based CEDL approximation using eqn (1) provides reliable values without the need for any modeling.
However, the inconsistency between the trend of experimental in-pore CEDL and Debye length with is due to the dynamic, frequency-dependent nature of EIS.
encompasses a broader range of phenomena, including ion transport, pore structure effects, and non-ideal behavior not captured by the static EDL capacitance alone.
While EDL capacitance measures charge storage capacity at the electrode surface, imaginary capacitance provides insights into the dynamic response of the electrochemical system in a frequency range. For instance, the pattern of in Fig. 4c indicates that the knee frequency shifts to higher values as salt concentration increases, resulting in a gradually smaller charge/discharge time constant (1/2πf) up to 5 mol kg−1 (440 ms). Above this concentration, the knee frequency shifts to smaller values, resulting in the slowest charge/discharge time at 20 mol kg−1 (1256 ms). This trend matches the EDL length in the pores. The larger Bjerrum length (Fig. 3a) and stronger coulombic interactions restrict ion desolvation beyond 10 mol kg−1, resulting in slower charge/discharge rates. To understand this in more depth, the ion desolvation number has been empirically quantified and is discussed in detail in the following section.
To provide deeper insights into partial desolvation, we first determined the radii of ions confined in micropores (eqn (11)) and mesopores (eqn (12)) by combining the Stokes–Einstein equation with the MacMullin number (eqn (10)).
![]() | (11) |
![]() | (12) |
Fig. 5a shows the radii of ions confined in micropores and mesopores, along with the radii of bulk ion pairs and sole H2O (see Method S6 and Tables S8–S10† for details). As salt concentration increases, the number of available water molecules decreases, resulting in a smaller bulk RH.55 In the larger mesopores, the ions retain a larger RH. An initial decline in in-pore radii is observed up to 5 mol kg−1. Beyond 5 mol kg−1, however, the in-pore ionic radii exhibit an opposite trend compared to bulk ionic radii, indicating that larger ion-pair sizes restrict partial ion desolvation.
Similar ranges of ionic radii (∼3–6 Å) for confined monovalent and divalent ions, including Li+, were reported by Eliad et al.15 and for TFSI− (∼4–7 Å) by Largeot et al.65 The consistency between our results and these studies confirms the accuracy of eqn (11) and (12). Subsequently, the hydration number NH of Li+ and TFSI− was calculated separately according to eqn (13).66,67 The NH values for Li+ and TFSI− were then combined to determine the total NH of LiTFSI, as listed in Table S15.†
![]() | (13) |
However, the values of RH in micropores are smaller than the RH of individual water molecules (Fig. 5a). Moreover, in some cases, we found that the RH radii in micropores are smaller than those in the crystalline Li+-TFSI− (0.6 + 3.26 = 3.86 Å). Therefore, we could not directly apply eqn (14) and (15) to determine the in-pore hydration number.
![]() | (14) |
![]() | (15) |
![]() | (16) |
![]() | (17) |
Desolvation# = NH,bulk × volume shrinkage % | (18) |
To this end, we adopted a four-step method as summarized in eqn (16)–(18). First, we measured the volume ratio of micro and mesopores to that of water (Vpore/Vwater) and the volume of bulk ion-pairs to that of water (Vbulk ion pair/Vwater) as displayed in Fig. 5b. Second, we subtracted the values of Vpore/Vwater from Vbulk ion pair/Vwater to achieve the volume shrinkage number and percentage, as demonstrated in Fig. 5c. Third, we multiplied the NH of bulk LiTFSI from Table S15† by the volume shrinkage percentage to obtain the desolvation number, as revealed in Fig. 5d. Lastly, we subtracted the desolvation numbers from the bulk NH to determine the hydration numbers in the pores, as shown in Fig. 5e.
Since the above estimation primarily considers ionic volume where the radius of the water molecule significantly affects the results, we utilized four different water volumes.
Firstly, we derived RH using the diffusivity of H2O for various LiTFSI concentrations54 (Method S6†). Secondly, we used the radius of H2O reported by Han et al.55 Thirdly, we applied a mass and density-based approach (Method S8). Lastly, we considered the water radius to be 3 Å.48Fig. 5b–e display average values derived from these four different radii. To ensure accurate estimations, we utilized effective hydrated radii throughout our work.
This was achieved by correcting the Stokes radii from the Stokes–Einstein equation using the calibration plot of Nightingale (Method S6†).63 The resulting range of hydration numbers in pores (NH ranging from ∼0.05 to 6) is in good agreement with previous reports on various electrolytes, including Li2SO4 and LiCl, confined in several nanoporous carbons (YP-17, BP-880, BP-2000) determined using electrochemical quartz crystal admittance (EQCA) and electrochemical quartz crystal microbalance (EQCM) methods.13,14,43
Fig. 5b–e summarize the behavior of LiTFSI ions during electrosorption, focusing on changes in hydrodynamic volume in micro- and mesopores. Mesopores, being larger, retain a smaller surface area for ionic volume sieving, resulting in approximately fivefold less partial desolvation than in micropores. Ion desolvation is stronger at lower concentrations due to factors related to ion–water interactions and electrolyte structure. At lower concentrations, more water molecules are available relative to the number of ions, allowing each ion to be fully solvated with strong hydration shells. These shells are partially stripped off during electrosorption in the narrow spaces of micro- and mesopores, which leads to greater desolvation of the ions (Scheme 1a). Additionally, the strong hydration shells around ions like cosmotropic Li+ contribute to efficient charge screening, resulting in lower Debye lengths (decreasing from 1 to 10 mol kg−1). As these ions move towards porous carbon electrode surfaces during electrosorption, the hydration shells are partially removed to facilitate closer interactions between ions and pore walls. At lower concentrations, the relative dielectric constant is also higher (e.g. 68.17 at 1 mol kg−1),57 which supports stronger interactions between ions and solvents. This forces ions to lose part of their hydration shell to fit into narrow sub-nanopores, increasing hydrodynamic volume shrinkage and partial ion desolvation. In contrast, as the concentration increases to 15 and 20 mol kg−1, ion pairing becomes more prominent. This pairing reduces the ionicity and the relative permittivity of the solution (e.g. 17.26 at 20 mol kg−1),57 thereby decreasing the hydrodynamic volume and desolvation number within micro- and mesopores. At these concentrations, the formation of EDL is hindered, because the reduced permittivity and increased ion pairing decrease effective ion distribution and charge storage. Larger ion pairings are less easily accommodated in sub-nanosized carbon pores, limiting the ion distribution and sorption characteristics within the pores (Scheme 1b).
The ratio of hydration numbers from bulk to pore could serves as an indicator of ion hydration/desolvation ability at varying concentrations. For micropores, the ratios were 14.66, 12.93, 12.25, 8.39, and 6.20, while for mesopores, they were 5.27, 4.57, 2.94, 1.83, and 1.20 at 0.5, 1, 5, 10, 15, and 20 mol kg−1, respectively. The monotonic decline in these values indicates that with increasing concentration, ion pairs stabilize partially dehydrated states, as ions bound in pairs are less likely to disrupt their hydration shells (Scheme 1b). Consequently, the extent of ion desolvation is governed by the strength and type of ion pairing, with stronger pair interactions promoting reduced solvation and limiting further desolvation within pores. As a result, electrosorption dynamics shift, with high concentrations leading to less structured ion sorption and potentially reduced charge storage efficiency. The strong hydration and structuring effects of cosmotropic Li+ ions are counteracted by the chaotropic nature of TFSI− ions, leading to a complex interplay that influences the overall performance of the electrolyte in electrochemical capacitors. Hence, moderate concentrations, such as 5 and 10 mol kg−1, demonstrated better charge screening performance. Except for CEDL from , the Debye length minima, CEDL from
, differential capacitance from CVs, and other theoretical CEDL values were higher at 10 mol kg−1. This is attributable to the higher desolvation number compared to 5 mol kg−1.
In other words, up to 10 mol kg−1, the decreasing Debye length suggests strong hydration shells around Li+ ions, facilitating effective charge screening and enhancing electrosorption efficiency.
Above 10 mol kg−1, the coexistence of intimate and aggregated ion pairs results in Bjerrum lengths of 2.5 and 3.5 nm for 15 and 20 mol kg−1, respectively, which are larger than the micropores (≤2 nm) (Fig. 3a). This results in a smaller diffuse layer thickness in porous carbon, as shown in Fig. S14,† derived from the loss tangent plot (Method S9). To correlate the ion pairing and desolvation phenomena with the EDL charging rate, we derived the time-constant (τEDL) from the characteristic frequency positions at the maximum and
using eqn (19), as shown in Fig. 5f and listed in Table S16.†
![]() | (19) |
As previously described in Methods S1 and S2,† the and
were obtained using cells with different cell constants. According to the Helmholtz equation (Method S4†), we accounted for the electrode area and distance (for bulk solution) or carbon sheet thickness (for capacitor cells) in eqn (19). Due to varying tortuosities in micro and mesopores across different salt concentrations, the time-constants for EDL charging of the pores were significantly higher than in non-porous electrodes, differing by several orders of magnitude. For example, a 5 mol kg−1 concentration resulted in short τEDL both for non-porous (88.4 μs cm) and porous (370.54 μs cm) electrodes, whereas a 20 mol kg−1 concentration led to large τEDL both for non-porous (261.4 μs cm) and porous (744.8 μs cm) electrodes. The pore-to-non-porous EDL charging time-constant ratios were 3.6, 3.8, 4.2, 4.5, 3.6, and 2.8 for 0.5, 1, 5, 10, 15, and 20 mol kg−1 concentrations, respectively. This concentration-dependent trend exactly follows the patterns of Debye length and ion desolvation, showing a maximum at 10 mol kg−1. Borchardt et al. described the ion diffusivity ratio from bulk to in-pore as ion transport resistance.41 Similarly, the τEDL ratio of porous to non-porous electrodes can be considered as an indicator of EDL charging readiness. The peak τEDL porous/τEDL non-porous at 10 mol kg−1 suggests the highest charge accumulation, signifying the formation of a compact and efficient EDL at this concentration. These findings indicate that a 10 mol kg−1 concentration is better suited for maximizing EDL capacitance and achieving higher energy density (determined using Method S10 and shown in Fig. S15†). Conversely, the time-constants derived from the maximum imaginary conductivity, capacitance, power, and loss tangent (Table S16†) suggest that a 5 mol kg−1 concentration may be more favorable for faster EDL charge/discharge rates, resulting in higher power density (determined using Method S11 and presented in Fig. S16†).
AP | Aggregated ion pair |
CV | Cyclic voltammogram |
EIS | Electrochemical impedance spectroscopy |
EDL | Electric double layer |
EDCC | Electric double-cylinder capacitors |
EWCC | Electric wire-in-cylinder capacitors |
FA | Free anion |
GCS | Gouy–Chapman–Stern |
IIP | Intimate ion pair |
LIP | Loose ion pair |
OCP | Open circuit potential |
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d5ta00596e |
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