Damian
Jędrzejowski‡
ab,
Marzena
Pander‡
ac,
Emilian
Stachura
c,
Krzysztof
Matlak
d,
Wojciech
Bury
*c and
Dariusz
Matoga
*a
aFaculty of Chemistry, Jagiellonian University, Gronostajowa 2, Kraków 30-387, Poland. E-mail: dariusz.matoga@uj.edu.pl
bDoctoral School of Exact and Natural Sciences, Jagiellonian University, Łojasiewicza 11, Kraków 30-348, Poland
cFaculty of Chemistry, University of Wrocław, F. Joliot-Curie 14, Wrocław 50-383, Poland. E-mail: wojciech.bury@uwr.edu.pl
dNational Synchrotron Radiation Centre SOLARIS, Czerwone Maki 98, Kraków 30-392, Poland
First published on 24th June 2025
Metal–organic frameworks (MOFs) have emerged as proton conductors, however, understanding conduction mechanisms and pathways in MOFs is limited by the common polycrystalline form of these materials, resulting in the presence of grain boundaries. Herein, we report model core–shell systems based on the UiO-68 platform with incorporated tetrazine function for studying proton conduction in polycrystalline MOFs. The solvent-assisted linker exchange (SALE) method, applied to two model MOFs of the UiO-68 family, enables core shell swapping, control over the degree of linker exchange, and stability of the system. The subsequent use of the inverse electron-demand Diels–Alder (iEDDA) reaction with an acid dienophile precisely in the core or shell of microcrystals, followed by encapsulation of imidazole (HIm), resulted in the formation of a diverse group of polycrystalline proton-conducting systems differing in the distribution of pendant carboxylic groups and concentration of imidazole charge carriers. Comprehensive impedance studies of these covalently modified model systems revealed minor differences between their proton conductivity values, and considerable differences between activation energies, and pseudocapacitances. These unprecedented observations demonstrate the significant role of external surface conduction in polycrystalline MOFs.
We hypothesized that the study of proton conduction pathways in polycrystalline samples may be possible with materials that offer precise control over crystal structure and composition. In this context, we planned to synthesize a pair of core–shell and reverse core–shell MOFs with corresponding reference core-only and shell-only compounds as a model for such studies. In general, core–shell MOFs are specific representatives of the so-called 4th generation of MOFs12 or hierarchical systems, which can exhibit enhanced properties such as stability,13 processability,14 and synergistic effects in specific applications.15,16 Such hierarchical structures have already been demonstrated in multivariate MOFs (MTV-MOFs)17–19 with regularity on molecular20 or domain21 scales, and in MOF-X composites, where X may represent polymers,22 carbons,23 metal oxides,24 or other MOFs (in MOF–MOF systems).25–27 In this view, core–shell MOFs, as a specific category of MTV-MOFs, are typically obtained either through the epitaxial growth of a shell-MOF on a pre-synthesized core-MOF,28 or via solvent-assisted linker exchange, SALE (also known as post-synthetic exchange (PSE) of linkers).29 The latter approach is often limited to building blocks with similar structural parameters and relies on diffusion as a rate-limiting step.30,31 However, although core–shell MOFs have been explored extensively recently, such systems have never been used to study proton conduction before (Fig. 1).
In this work, to study proton conduction in polycrystalline MOF samples, we employed model core–shell systems based on the UiO-68(TZ) MOF (TZ = 1,2,4,5-tetrazine or s-tetrazine), which allows the introduction of acid sites in the form of carboxyl groups through covalent modification. In order to precisely control the distribution of carboxyl moieties in our core–shell MOFs, we combined the SALE method and inverse electron-demand Diels–Alder (iEDDA) reaction (Fig. 2). In addition, to make our investigations independent of the influence of humidity, our model materials were designed to exhibit good measurable conductivity under anhydrous conditions (above 100 °C), which was achieved by vapor adsorption of imidazole (HIm) proton carriers. From an application point of view (in PEMFCs), higher operating temperatures of proton conductors reduce the poisoning potential of Pt catalysts and the potential for flooding of electrodes by condensing water; improve reaction kinetics and provide an alternative to Nafion, which dehydrates above 80 °C.
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Fig. 3 a) PXRD patterns of the phase-pure MOFs: UiO-68(TZ), UiO-68(Me), and derived core–shell materials: UiO-68(TZ@Me), UiO-68(Me@TZ), compared to UiO-68 (simulated). (b) N2 sorption isotherms (at 77 K) of the core–shell materials, closed symbols (adsorption), open symbols (desorption). (c) SEM images of the core–shell materials. (d) X-ray absorption spectra of UiO-68(TZ@Me) collected along the axis from crystal center (points 1–13). Areas A1 and A2 marked for the calculation of AN parameter, for nitrogen abundance estimation. For details see ESI, Section S12† (e) X-ray absorbance at 390 eV for the UiO-68(TZ@Me) crystal probed at 13 points shown in the inset, together with the calculated AN. The limiting values of both the absorbance at 390 eV and AN determine the crystal surface boundary (grey dashed line) and the limit of the presence of nitrogen in the crystal (pink dashed line). |
As a complementary UiO-68 analogue for our studies, we selected UiO-68(Me), also known as PCN-56,37 that contains deprotonated H2TPDC-Me as a linker (Fig. 2). The usage of H2TPDC-Me instead of H2TPDC36 in UiO-68 offers significantly improved solubility and control over the MOF synthesis. Pure-phase UiO-68(Me) was synthesized following reported protocol (ESI, Section 3.2†).37 Enhanced solubility of H2TPDC-Me in DMF enabled the formation of larger crystals with improved yield and uniform size distribution, as shown in SEM images (Fig. S33†). PXRD analysis (Fig. 3a and S9†) confirmed the retention of crystallinity after a standard activation procedure (acetone exchange and drying at 80 °C). TG analysis (Fig. S50†) demonstrated good thermal stability, with decomposition beginning at approximately 450 °C. N2 sorption analysis at 77 K confirmed the porosity of UiO-68(Me), showing N2 uptake of 820 cm3 g−1 (Fig. S29b and Table S4†), which aligns well with theoretical values of 900 cm3 g−1 (Fig. S54b†). These findings further emphasize the stability differences between UiO-68(TZ) and UiO-68(Me).
The yield of SALE in both systems was quantified via1H NMR analysis of digested samples (ESI, Fig. S16 and Section S5.5†). PXRD analysis confirmed well-preserved crystallinity and isostructural nature of both core–shell systems (Fig. 3a and S10†). SEM images (Fig. 3c, S34 and S35†) showed consistent octahedral crystallite morphologies and revealed preserved crystallite size distributions. N2 sorption at 77 K (Fig. 3b and S30†) indicated retained porosity in UiO-68(TZ@Me), closely resembling N2 uptake of UiO-68(Me), whereas UiO-68(Me@TZ) showed reduced porosity. TG analysis (Fig. S51†) revealed two decomposition steps for both samples: the first around 260 °C and the second above 500 °C, mirroring the thermal behavior of the phase-pure UiO-68(x) analogues studied here.
Additional SALE experiments were conducted to study the formation of UiO-68(TZ@Me) in successive cycles. NMR analysis of linkers content showed almost complete exchange of TZDC to TPDC-Me after five cycles (Fig. S17 and S20†). A decrease in exchange ratio was observed in subsequent cycles, likely due to the increasing difficulty of linker diffusion into the MOF crystal core. DRIFT analysis confirmed the presence of both linkers, with differences in band intensities in the 1480–1320 cm−1 region reflecting composition changes in UiO-68(TZ@Me) after each SALE cycle (Fig. S24†). PXRD (Fig. S11†) and SEM analyses (Fig. S36†) supported the retention of crystallinity and morphology. Additionally, scaling up the preparation of UiO-68(TZ@Me) with 500 mg of starting MOF yielded consistent linker composition (ESI, Section S3.3†). For UiO-68(Me@TZ), extending the reaction time increased the TZDC content to 50%; however, DRIFT spectra indicated the presence of uncoordinated H2TZDC in the sample (Fig. S23†).
In characterizing the two hybrid materials, substantial indirect evidence supported the core–shell-like distribution of ligands in the crystallites, but direct confirmation requires advanced physicochemical methods. Since UiO-68(TZ) and UiO-68(Me) differ only in one aromatic ring structure, with no particular distinctions, basic imaging methods like SEM-EDS or Raman microscopy are insufficient. Similar challenges were addressed in the work of A. Centrone et al.,38 where infrared nanoscopy and diffraction-limited hyperspectral photoluminescence were applied to analyze ligand distribution in core–shell materials based on UiO-68 analogues (UiO-68(TPDC@TZ) systems with tetrazine shell).
Here, we used Scanning Transmission X-ray Microscopy (STXM) with synchrotron radiation to confirm the core–shell structure in UiO-68(TZ@Me) (ESI, Section S11†). Samples were activated and measured under vacuum, focusing on the nitrogen absorption edge (398.50 eV) to trace the tetrazine core. STXM imaging was performed along the C2 axis of the octahedral crystallites, sampling areas from the center outwards (Fig. 3e, inset). X-ray absorption spectra for 13 regions indicated a crystal boundary at 930 nm and a nitrogen-rich region extending to 750 nm, yielding a shell thickness of 180 nm for a 1.86 μm crystallite (Fig. 3e). These results closely match NMR-based shell thickness estimates (175 nm, ESI, Section S11†). Additional measurements along different axes and for other crystallites confirmed these findings (Fig. S59†). Together, these analyses validate the core–shell structure of UiO-68(TZ@Me) and demonstrate the utility of STXM for mapping ligand distributions in complex materials.
Here, our objective was to influence proton conduction properties by introducing groups that could act as proton donors or acceptors. To verify reactivity in a model core–shell system, UiO-68(TZ@Me), we explored three dienophiles with the following functional groups (Fig. S1†): an amine (ncn), monocarboxylic (nca), and dicarboxylic (ndc), all of them being norbornene derivatives for faster reaction kinetics (ESI, Section S3.3, Fig. S12, S18 and S25†). For better reaction control and increased proton donor concentration, ndc was selected as the primary dienophile for further study, yielding UiO-68(TZndc@Me) (Fig. 2). This reaction proceeded under mild conditions (at 60 °C for 12 h, see Section 3.3 in ESI† for details). Reaction completion was visually confirmed by color change from pink to bright yellow (Fig. S5†), while FT-IR analysis showed the disappearance of the 1380 cm−1 (Fig. S26†) tetrazine band, and NMR analysis of the digested sample confirmed quantitative formation of the TZndc ligand (Fig. S18†). PXRD analysis indicated that crystallinity was fully retained (Fig. S13†), and SEM images confirmed preservation of crystallite size distribution and morphology (Fig. S37†). As expected, the porosity of UiO-68(TZndc@Me) decreased (SBET = 2446 m2 g−1; before modification 3455 m2 g−1, Vpore = 1.00 cm3 g−1; before modification 1.42 cm3 g−1, Table S4 and Fig. S31†). Despite the incorporation of relatively large side groups, the remaining voids in the unit cell volume are considerable, allowing for potential applications, such as proton carrier diffusion.
To further demonstrate the versatility of our modification method and analyze the influence of free carboxyl group distribution on proton conductivity, the modifications with ndc were also performed on UiO-68(TZ) and UiO-68(Me@TZ) (Fig. 2). Each of these materials reacted similarly to UiO-68(TZ@Me), with physicochemical studies confirming modification completeness and crystallite shape and morphology preservation (ESI, Fig. S13, S26, S38 and S39†).
Due to the large voids present in the investigated materials, their proton conduction is likely mediated by carriers occupying these voids. Consequently, the proton carrier should be a Brønsted base, have high mobility, and remain inert to the material itself. Based on these criteria and a literature review,53,54 imidazole (HIm) was selected as an optimal proton carrier. We studied HIm incorporation in a series of materials with varying free carboxyl content, i.e. composed of UiO-68(Me) and UiO-68(TZndc) domains, with the content of the latter at 0, 25, 55 and 100%. This series underwent a standard imidazole adsorption procedure, reaching thermodynamic equilibrium under specified conditions (100 mbar, 120 °C, see ESI, Section S3.4† for details). The amount of adsorbed imidazole, determined by 1H NMR analysis (Sections S5.4 and S5.6†), correlated positively with the concentration of free carboxyl groups (Fig. S21†). This observation was further corroborated with the simulated incorporation of HIm in UiO-68 type models based on the studied linkers (Fig. 2), where a higher affinity of physisorbed imidazole towards the “acid-rich” UiO-68(TZndc) material was observed (ESI, Section S10.2†). All studied materials retained crystallite size and morphology upon imidazole infiltration (Fig. S40–S43†). PXRD analysis verified the retention of the crystalline structure (Fig. S14†), except for UiO-68(TZndc), which did not maintain crystallinity during earlier stages, and confirmed the absence of extra HIm phases.
The domain structure of our Zr-MOF materials provided the opportunity for quantitative and qualitative analysis of proton conduction in polycrystalline samples due to well-defined distributions of free carboxyl groups. Carboxyl groups serve a dual role in this study: as proton donors to locally increase the concentration of H2Im+ carriers and as intermediates in the conduction pathway, leveraging their strong hydrogen-bonding capability.
Two imidazole-free samples (UiO-68(TZ@Me) and UiO-68(TZndc@Me)) and a series of imidazole-functionalized samples (HIm@Zr-MOF) were analyzed for anhydrous proton conduction in the 110–160 °C temperature range. Details of sample preparation and the equipment used are provided in the ESI (Sections S2 and S12).† Each of the materials underwent immediate amorphization after being exposed to atmospheric conditions after removal from oven at 160 °C, and for this reason we confirmed the stability of the materials by analyzing FT-IR spectra and SEM images after proton conductivity measurements (Fig. S28 and S44–S49†). Each impedance relationship corresponded closely to an R1 + Q2/R2 + Q3 equivalent circuit. In this model, R1 represents the external (system) resistance, Q2 is a constant phase element (CPE) describing non-ideal bulk dielectric behavior, R2 corresponds to the sample resistance associated with proton conduction, and Q3 denotes a CPE related to electrode polarization at the blocking electrode. This circuit is illustrated in the inset of Fig. 4a, which also presents a representative Nyquist plot for HIm@Zr-MOF samples (a summary for all materials is provided in Fig. S60†). The experimental results were fitted to a theoretical model based on the proposed equivalent circuit, serving as the foundation for all further analyses, with additional details available in the ESI (Section 12, Fig. S62–S65 and Table S7†). Imidazole-free samples (e.g., UiO-68(TZ@Me) and UiO-68(TZndc@Me)) showed conductivity below detection limits, contrasting with the considerable conductivity of imidazole-containing samples (Fig. 4b). The HIm@UiO-68(TZ@Me) sample (0.72 μS cm−1) shows the lowest conductivity, which we attributed to the presence of structural defects that introduce labile acidic OH and H2O groups at zirconium nodes, a common feature of Zr-MOFs.55,56 While these defective sites should be present in low concentrations across all tested samples, their contribution is expected to be uniform and remains secondary to the effect of carboxyl group functionalization. The introduction of COOH pendant groups was intended to increase the concentration of protonated imidazole carriers (H2Im+), and the highest conductivity was observed for HIm@UiO-68(Me@TZndc) (5.0 μS cm−1). This value indicates relatively good conductivity under anhydrous conditions.
While conductivity depends on both carrier concentration and mobility, our materials were specifically designed to isolate conduction mechanism effects. The dominant proton carriers are H2Im+ species, whose concentration is influenced by both the anchored COOH group and adsorbed imidazole concentration. However, since both are weak Brønsted acids/bases, their interaction does not lead to a linear relationship between their concentration and the overall conductivity. The differences in conductivity between samples remain small (less than one order of magnitude), enabling us to focus on the activation energy as a reliable indicator of the proton transport mechanism, rather than the absolute quantity of transported charge.
The determination of activation energy using Arrhenius plots (Fig. 4c, S68 and Table S9†) for each sample sheds light on the dominant conduction mechanism. The results (Fig. 4d) indicate that none of these samples exhibit a pure Grotthuss mechanism, which generally requires a high carrier protonation degree or smaller pores to suppress diffusion.57 HIm@UiO-68(Me@TZndc), with the lowest activation energy (0.50 eV), features a maximum H2Im+ concentration localized within the crystallite shell, whereas HIm@UiO-68(TZndc@Me), with the highest activation energy (0.86 eV), has H2Im+ ions concentrated in the crystallite core. Since the activation energy reflects the rate-limiting step in conduction, these findings align with the proposed conduction mechanism (Fig. 1). In HIm@UiO-68(TZndc@Me), macroscopic conduction relies on H2Im+ transport through a shell that lacks carboxylates, thus favoring a vehicle mechanism. In contrast, HIm@UiO-68(Me@TZndc) exhibits contributions from both the Grotthuss and the vehicle mechanism, as conduction occurs both through the shell and between neighboring crystallite shells. Both HIm@UiO-68(TZ@Me) and HIm@UiO-68(TZndc), with more uniformly distributed defects or carboxyl groups, act as intermediate cases (Fig. 1). Neither of them requires diffusion through the less favorable shell, allowing hydrogen-bonding networks to form throughout the sample volume. The relatively low H2Im+ concentration in these samples favors the vehicle mechanism; however, unlike HIm@UiO-68(Me@TZndc), charge carriers are dispersed also within the crystallite core, not only within the shell.
Close examination of Arrhenius plots reveals points corresponding to the highest temperatures (i.e. above 150 °C), that deviate from the linear trend (marked as empty symbols in Fig. 4c). This deviation is absent only for UiO-68(TZndc@Me), suggesting that above 150 °C, imidazole, the charge carrier, leaks from the material, leading to a reduction in conductivity. For UiO-68(TZndc@Me), the increased concentration of HIm within the crystallite core allows the shell to act as a protective barrier. For all other materials, conduction through or between shells (grain-surface or inter-grain conduction) contributes significantly to global conductivity, and the loss of imidazole at the highest temperatures (160 °C) is reflected in a decline in conductivity.
Impedance measurements and related Nyquist plots were also used to estimate specific pseudocapacitance (pC) for each equivalent circuit, with values between 0.5–5 pF cm−1 across HIm@Zr-MOF samples (Fig. 4e). Literature data indicated that the pC value helps determine the conduction pathway (i.e. bulk vs. surface).57 HIm@UiO-68(TZndc) exhibited the lowest pC (0.65 pF cm−1), which is consistent with a homogeneous distribution of carboxyl groups and bulk-like conductivity similar to that of a uniform solid, in which inter-grain conduction is hardly significant. The highest pC value (3.3 pF cm−1) in HIm@UiO-68(Me@TZndc) suggests significant surface conduction, consistent with its COOH group distribution in crystallite shells along grain boundaries. The inter-grain conduction has the highest significance for UiO-68(TZndc@Me), as manifested by the highest conduction activation energy. In addition, since the charge transport in UiO-68(TZndc@Me) occurs between the cores of neighbouring crystallites (through acid-poor shells), surface conduction has a smaller contribution, i.e. pC = 1.5 pF cm−1 is smaller than for HIm@UiO-68(Me@TZndc), with acid-rich shells (pC = 3.3 pF cm−1).
Theoretical N2 sorption isotherms (at 77 K) and imidazole loadings (at 298 K and 393 K) in UiO-68(x) series were computed in grand canonical Monte Carlo (GCMC) simulations using the RASPA2 software.58 The description of the used models and simulation details are described in ESI (Section S10).†
Direct analysis of ligand distribution for the model material UiO-68(TZ@Me) was performed with a scanning transmission X-ray microscope (STXM) utilizing synchrotron radiation (ESI, Section S11†) and aXis2000 software.59
Proton conduction was examined using Electrochemical Impedance Spectroscopy (EIS) in a four-electrode setup under constant pressure (4.5–5 MPa) and temperatures of 110–160 °C. The detailed assembly of the measurement cell is described in the ESI (Section S2 and Fig. S2).† For each measurement, the imaginary versus real impedance was measured across a frequency range of 4 Hz to 5 MHz, and EC-Lab software was used to fit the most suitable equivalent circuit, yielding the circuit resistance associated with ionic conduction (see ESI, Section S12† for details).
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d5ta01769f |
‡ These authors contributed equally to this work. |
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