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Article  |  Open Access  |  25 Aug 2026

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

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Energy Mater. 2026, 6, 600103.
10.20517/energymater.2026.98 |  © The Author(s) 2026.
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Abstract

Understanding how trace-metal doping directs the electrochemical reconstruction of MOF precatalysts into the true active phase remains a key challenge in designing efficient oxygen evolution reaction (OER) electrocatalysts. Here, a bimetallic Mn-Co zeolitic imidazolate framework-67 material, denoted as Mn-ZIF-67, was prepared through a facile room-temperature self-assembly route that incorporated trace Mn into the ZIF-67 lattice. Compared with undoped ZIF-67, Mn-ZIF-67 exhibits enhanced alkaline OER performance, with the overpotential at 10 mA cm-210) value decreasing from 276 to 235 mV, a reduced Tafel slope of 36.49 mV dec-1, and sustained stability during long-term durability testing. A combination of structural characterization and density functional theory (DFT) calculations demonstrates that Mn-ZIF-67 undergoes electrochemical surface reconstruction into Mn-modified Co (oxy)hydroxides, which serve as the real catalytically active phase. Mn-mediated electronic modulation optimizes intermediate adsorption energetics and lowers reaction free energies, thereby accelerating reaction kinetics. Notably, the catalyst sustains stable oxygen evolution during 100 h of continuous alkaline seawater electrolysis at 50 mA cm-2, and the assembled electrolyzer can additionally be driven by a commercial solar panel, demonstrating practical applicability. Overall, this work highlights transition-metal doping as a viable route for tailoring the reconstruction of MOF-derived precursors, paving the way for durable and scalable OER electrocatalysts.

Keywords

Oxygen evolution reaction, metal-organic frameworks, electrochemical reconstruction, Mn-Co bimetallic catalysts, seawater splitting

INTRODUCTION

Driving electrocatalytic water splitting with renewably generated electricity provides a sustainable means of producing hydrogen. Its large-scale deployment, however, is limited by the oxygen evolution reaction (OER), whose four-electron transfer character makes the kinetics sluggish and the energy barriers intrinsically high[1,2]. Although noble-metal catalysts, particularly Ir- and Ru-based materials, exhibit excellent OER activity, their scarcity and cost have hindered industrial application[3]. As a result, research has increasingly focused on developing low-cost, earth-abundant transition-metal catalysts based on Mn, Fe, Co, and Ni[4].

Although numerous non-noble-metal OER catalysts, including metal-organic frameworks (MOFs), sulfides, and borides, have been widely reported recently, many lack stability under strongly oxidative conditions[5,6]. Rather than remaining structurally invariant during catalysis, these materials often undergo electrochemically induced surface reconstruction[7], involving ligand or anion leaching and metal oxidation to form high-valence (oxy)hydroxides that constitute the real active species[5,8]. Despite the ubiquity of dynamic transformation, research largely centers on the static properties of pristine catalysts, with limited insights into how OER-induced reconstruction governs activity. In particular, the mechanisms by which atomic doping directs structural evolution toward optimized active phases are rarely studied, limiting the rational design of high-performance catalysts.

Against this backdrop, the structurally well-defined and compositionally tunable nature of MOFs makes them valuable model precursors for sysstematically investigating how multimetallic interactions influence electrochemical reconstruction[9,10]. Among them, zeolitic imidazolate framework-67 (ZIF-67), a cobalt-based zeolitic imidazolate framework, has been widely explored for OER because of its ordered Co-N coordination environment, tunable structure, and compositional flexibility. Previous studies have improved the OER performance of ZIF-67-based catalysts through facet engineering, low-temperature deligandation to form quasi-ZIF-67, and construction of ZIF-67-derived Co-based compounds or carbon composites[11-13]. Meanwhile, in situ spectroelectrochemical studies have shown that ZIF-67 can reconstruct into Co(OH)2/CoOOH-like species under anodic OER conditions[14], indicating that the reconstructed cobalt oxyhydroxides rather than the original Co nodes act as the dominant active sites. However, how trace heterometal incorporation regulates the reconstruction pathway of intact ZIF-67 precatalysts remains poorly understood.

Here, we report a Mn-doped ZIF-67 (Mn-ZIF-67) obtained through a facile ambient-temperature self-assembly route and systematically reveal the impact of trace Mn incorporation on the pristine catalyst and its evolution under OER conditions. Unlike previous ZIF-67-based OER studies focusing on precursor optimization or derivative design, this work targets the reconstruction process itself, using trace Mn to regulate the evolution of ZIF-67 into a Co-Mn (oxy)hydroxide active layer and establish a direct link between precursor structure, reconstruction pathway, and catalytic performance. Benefiting from earth-abundant Mn/Co elements and mild solution-phase synthesis, this system offers potential advantages in cost and scalability compared with Ir/Ru-based benchmark catalysts. Mn doping increases electrochemically accessible sites and accelerates charge-transfer kinetics, while steering in situ reconstruction toward a highly active Co-Mn (oxy)hydroxide phase. The resulting catalyst exhibits durable performance in alkaline seawater splitting and is compatible with photovoltaic-powered operation. Overall, this work highlights transition-metal doping as an effective strategy for modulating MOF-based catalysts and their OER-induced reconstruction behavior, providing a rational basis for the design of efficient and robust OER electrocatalysts.

EXPERIMENTAL

Synthesis of ZIF-67 and Mn-ZIF-67

Reagents used in this study are listed in Supplementary Note 1 of the Supplementary Materials. For ZIF-67, 0.582 g of Co(NO3)2·6H2O was first dissolved in 30 mL of methanol, and 1.312 g of 2-methylimidazole was separately dispersed in another 20 mL of methanol; the two methanol solutions were then combined. After being stirred at ambient temperature for 1 h, the mixture was left undisturbed to age for 24 h. The resulting solid was separated by centrifugation, rinsed with methanol three times, and dried under vacuum at 65 ℃ overnight. Mn-ZIF-67 was obtained by an identical protocol, with the only difference that 0.524 g of Co(NO3)2·6H2O together with 0.050 g of Mn(NO3)2·4H2O were dissolved together in the starting 30 mL of methanol [Supplementary Figure 1]. The catalyst characterization procedures are described in Supplementary Note 2 of the Supplementary Materials.

Electrochemical measurements

Electrochemical tests were carried out on a Princeton PARSTAT MC workstation using two different configurations: a three-electrode configuration for the OER measurements in 1.0 M KOH, and a two-electrode configuration for overall seawater splitting in alkaline natural seawater. For the three-electrode measurements, catalyst-loaded nickel foam (NF, 1 cm2) served as the working electrode, a graphite rod as the counter electrode, and an Hg/HgO electrode as the reference. The catalyst ink was prepared by ultrasonication of 5 mg of catalyst for 30 min in a solvent mixture of 450 μL ethanol, 500 μL deionized water, and 50 μL Nafion (5 wt%); 100 μL of this ink was then coated onto the pretreated NF and dried in air. After activation via 20 cyclic voltammetry (CV) cycles, linear sweep voltammetry (LSV) was conducted at 5 mV s-1 to evaluate OER activity. Electrochemical impedance spectroscopy (EIS) measurements were performed at 1.47 V vs. reversible hydrogen electrode (RHE) over a frequency range from 100 kHz to 0.01 Hz. The double-layer capacitance (Cdl), used to estimate the electrochemically active surface area (ECSA), was derived from non-Faradaic CV scans recorded at 40, 60, 80, 100 and 120 mV s-1. Long-term stability was assessed via 12 h chronoamperometry at 1.465 V vs. RHE, and durability at high current density by chronopotentiometry at 1 A cm-2 for 24 h, using a separately prepared Mn-ZIF-67/NF electrode (1 cm2). All potentials in the three-electrode configuration were corrected for 90% of the iR drop, with an uncompensated resistance of Ru = 0.9 Ω, and referenced to the RHE using ERHE = EHg/HgO + 0.098 + 0.059 × pH[15]. For the two-electrode measurements, Mn-ZIF-67/NF (1 cm2) was used as the anode and a graphite rod as the cathode in alkaline natural seawater prepared by adding KOH to a concentration of 1.0 M to natural seawater collected from Shenzhen Bay. Details of seawater collection and electrolyte preparation are provided in Supplementary Note 3 of the Supplementary Materials, and the major-ion composition of the collected natural seawater before KOH addition is summarized in Supplementary Table 1. LSV was recorded at 5 mV s-1, and long-term durability was assessed by chronopotentiometry at a constant current density of 50 mA cm-2 for 100 h, with deionized water periodically replenished to compensate for water consumption. Cell voltages measured in the two-electrode configuration are reported as measured, without iR correction.

Computational method

Density functional theory (DFT) computations were carried out in the Vienna Ab Initio Simulation Package (VASP), employing the Perdew-Burke-Ernzerhof (PBE) functional under the generalized gradient approximation (GGA)[16-18]. Interactions between ionic cores and valence electrons were treated with the projected augmented-wave (PAW) method, and the plane-wave basis set was expanded up to a kinetic energy cutoff of 450 eV[19,20]. Gaussian smearing (0.05 eV) was applied to the Kohn-Sham orbital occupancies. To correct for strong electron correlation, Dudarev’s DFT+U approach[21] was applied to the 3d electrons of Co (Ueff = 3.3 eV) and Mn (Ueff = 5.2 eV). Dispersion interactions were accounted for using Grimme’s D3 dispersion correction (DFT-D3) methodology[22]. The convergence thresholds for total energy and residual force were set to 10-5 eV and 0.02 eV Å-1, respectively. The Co ZIF-67 cluster was placed in a 20 Å cubic cell and fully relaxed with sampling restricted to the Γ point. For the CoOOH bulk, hexagonal lattice parameters were optimized to a = b = 2.826 Å and c = 12.936 Å. A CoOOH (001) surface model was subsequently constructed using a p (4 × 4) supercell with one stoichiometric layer and a 15 Å vacuum gap. The Mn-doped CoOOH model was constructed by substituting one Co site in the CoOOH (001) slab with Mn, and the CoOOH/Mn-doped CoOOH surfaces were used to represent the reconstructed active phases after OER activation. Structural relaxation of the slab was performed using a 2 × 2 × 1 k-point grid. Adsorption energies (Eads) were calculated as follows[23]:

$$ E_{\mathrm{ads}}=E_{\mathrm{A} / \mathrm{surf}}-E_{\mathrm{surf}}-E_{\mathrm{A}(\mathrm{~g})} \\ $$

In this expression, EA/surf is the total energy after adsorption, Esurf is the energy of the bare slab, and EA(g) denotes the energy of the isolated adsorbate calculated in a 20 Å box. Free-energy corrections at 298.15 K were introduced through[23]:

$$ G=E+\mathrm{ZPE}-T S $$

Here, E denotes the electronic energy obtained from DFT, while ZPE and S correspond to the zero-point-energy correction and entropy, respectively.

RESULTS AND DISCUSSION

Uniform rhombic dodecahedral ZIF-67 and Mn-ZIF-67 were successfully prepared via a room-temperature self-assembly method [Figure 1A-C]. Mn2+ incorporation modulates nucleation and suppresses crystal growth, reducing the average particle size from 0.94 ± 0.25 μm for ZIF-67 [Supplementary Figure 2] to 0.42 ± 0.09 μm for Mn-ZIF-67 [Supplementary Figure 3], which may improve electrolyte accessibility by increasing the external surface-to-volume ratio and shortening ion-diffusion pathways. Consistently, nitrogen adsorption-desorption measurements show that, although Mn-ZIF-67 has a slightly lower Brunauer-Emmett-Teller (BET) surface area than ZIF-67 (1,238.33 vs. 1,264.18 m2 g-1), its t-plot external surface area increases from 23.50 to 40.97 m2 g-1, accompanied by increased Barrett-Joyner-Halenda (BJH) adsorption cumulative pore area and volume from 15.49 m2 g-1 and 0.03025 cm3 g-1 to 30.96 m2 g-1 and 0.04332 cm3 g-1, respectively [Supplementary Figures 4 and 5 and Supplementary Table 2]. These results suggest enhanced external surface accessibility and mesoporous/interparticle pore contribution in Mn-ZIF-67, which are favorable for electrolyte penetration, ion transport, and anodic reconstruction. Energy-dispersive X-ray spectroscopy (EDS) mapping in Figure 1D confirms the homogeneous spatial distribution of constituent elements. Transmission electron microscopy (TEM) images retain the characteristic polyhedral outline, and the diffraction pattern recorded from an individual particle is consistent with a highly crystalline single-domain specimen (Figure 1E and inset). High-resolution TEM (HRTEM) exhibits ~ 1.21 nm lattice fringes corresponding to the ZIF-67 (011) plane [Figure 1F]. High-angle annular dark-field scanning transmission electron microscopy (HAADF-STEM) mapping likewise shows Mn and Co distributed across the same particle [Figure 1G]. Collectively, the characterization results demonstrate the incorporation of Mn2+ into the metal sites of the MOF without detectable formation of phase-separated Mn oxide particles.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 1. Microscopy of the pristine materials. (A) Scanning electron microscopy (SEM) micrograph of ZIF-67; (B and C) SEM micrographs of Mn-ZIF-67 at different magnifications; (D) Mn-ZIF-67 image and the corresponding EDS elemental maps for C, N, O, Mn and Co; all elemental maps were acquired from the same field of view and are displayed at the same spatial scale as the accompanying original image; (E) TEM micrograph with the corresponding selected-area electron diffraction (SAED) pattern in the inset; (F) HRTEM view and an enlarged lattice-fringe region; and (G) composite Mn/Co map acquired from a single Mn-ZIF-67 particle. TEM: Transmission electron microscopy; HRTEM: high-resolution transmission electron microscopy; ZIF-67: zeolitic imidazolate framework-67.

X-ray diffraction (XRD) patterns of both ZIF-67 and Mn-ZIF-67 match the simulated patterns [Figure 2A], confirming high phase purity and preservation of the intrinsic crystal structure[24]. The absence of secondary diffraction features such as Mn(NO3)2·4H2O and Mn3O4 further indicates the successful integration of Mn into the MOF framework without the formation of segregated impurity phases[25]. X-ray photoelectron spectroscopy (XPS) confirms the expected elemental composition of Mn-ZIF-67, including C, N, O, Co and Mn, as presented in Figure 2B[26,27]. The high-resolution N 1s spectrum in Figure 2C can be deconvoluted into metal-coordinated pyridinic nitrogen attributed to M-N bonding, where M represents Co or Mn, at approximately 398.8 eV and pyrrolic nitrogen at 400.2 eV[26]. These features confirm the coordination of 2-methylimidazole ligands and the formation of a stable ZIF-type framework[27]. To enable a more direct comparison of surface chemical states, the O 1s spectra of pristine ZIF-67 and Mn-ZIF-67 are plotted together in Figure 2D. Two main components are observed in both samples, corresponding to metal hydroxyl or adsorbed water species at 531.9 eV and to C-O species. The C-O component is located at 533.8 eV for pristine ZIF-67 and at 534.2 eV for Mn-ZIF-67, corresponding to a positive shift of 0.4 eV upon Mn incorporation. In parallel, the ratio of metal hydroxyl or adsorbed water species to C-O decreases from 4.59 to 3.28, indicating reduced surface hydroxylation and a more ligand-dominated surface environment. This result suggests that Mn incorporation modifies the local coordination environment of the pristine ZIF-67 framework. The Mn 2p spectrum in Figure 2E exhibits the characteristic Mn 2p3/2 (~ 641.2 eV) and Mn 2p1/2 (~ 652.8 eV) spin-orbit components, together with an additional satellite-related feature. It should be noted that Mn 2p spectra generally exhibit complex multiplet and final-state structures; therefore, the resolved satellite contribution is distinguished here from the Mn 2p3/2 /Mn 2p1/2 spin-orbit doublet[28]. Based on the overall spectral envelope and comparison with previously reported Mn2+-containing systems, the Mn species in the as-prepared Mn-ZIF-67 are predominantly present in a Mn2+-like chemical environment[29,30]. Nevertheless, considering the complex Mn 2p spectral structure and the surface-sensitive nature of XPS, minor contributions from other Mn chemical states cannot be completely excluded. The directly compared Co 2p spectra of pristine ZIF-67 and Mn-ZIF-67 in Figure 2F further reveal that Mn incorporation significantly modulates the Co electronic structure. In the direct Co 2p comparison, the principal 2p3/2 feature moves by approximately 0.7 eV, from 781.8 eV for ZIF-67 to 781.1 eV after Mn introduction. This negative shift indicates increased electron density at the Co centers via the ligand-bridged framework, analogous to previously reported electron donation from boron to transition metals[31,32]. This result provides evidence of Mn-induced electronic modulation within the pristine ZIF framework, which may influence the subsequent electrochemical evolution of Mn-ZIF-67 under OER conditions.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 2. Structural and surface-chemical analysis of ZIF-67 and Mn-ZIF-67. (A) Experimental diffractograms ZIF-67 and Mn-ZIF-67 with the simulated ZIF-67 reference; (B) XPS spectra of Mn-ZIF-67; (C) N 1s region of Mn-ZIF-67; (D) overlaid O 1s spectra of ZIF-67 and Mn-ZIF-67; (E) Mn 2p region of Mn-ZIF-67; and (F) directly compared Co 2p spectra of ZIF-67 and Mn-ZIF-67. ZIF-67: Zeolitic imidazolate framework-67; XPS: X-ray photoelectron spectroscopy.

Electrochemical OER activity was assessed in 1.0 M KOH[33]. LSV curves shown in Figure 3A reveal that both MOF-based electrodes deliver substantially higher anodic currents than the bare NF substrate, with Mn-ZIF-67 consistently outperforming ZIF-67[34]. A pre-OER anodic response appears in the 1.3-1.4 V versus RHE region. This feature is consistent with oxidation of Co species and the onset of oxyhydroxide-like reconstruction before substantial oxygen evolution[35,36]. This redox feature is more pronounced for Mn-ZIF-67, suggesting that Mn incorporation enhances the redox accessibility of Co sites and facilitates the generation of electrochemically active high-valence Co species under alkaline conditions[37]. Figure 3B displays the potentials needed to sustain the selected geometric current benchmarks. Mn-ZIF-67 requires only 235 mV to reach 10 mA cm-2, 41 mV lower than ZIF-67, and maintains superior activity at 100 mA cm-2 with an overpotential of 310 mV compared with 353 mV for ZIF-67. An LSV backscan was further performed to exclude possible interference from Ni foam oxidation. As shown in Supplementary Figure 6, the backscan curve shows no obvious Ni oxidation peak and gives a similar overpotential at 10 mA cm-2, confirming the reliable OER activity evaluation of Mn-ZIF-67. When both electrodes are compared at 1.53 V versus RHE (η = 300 mV), Mn-ZIF-67 delivers 69.8 mA cm-2, versus 18.5 mA cm-2 for ZIF-67, corresponding to a 3.8-fold increase in geometric current response. Reaction-kinetic trends were next compared using the Tafel analysis in Figure 3C. The fitted slopes are 36.49, 50.12, and 132.56 mV dec-1 for Mn-ZIF-67, ZIF-67, and bare NF, respectively. Combined with the lowered overpotentials, this accelerated electron transfer confirms Mn-ZIF-67 as a highly efficient alkaline OER electrocatalyst. Operational stability is a critical requirement for practical application. During the 12 h chronoamperometric test [Figure 3D], the final current remains at ~ 93% of the initial value, indicating limited activity loss over the measurement period. To further examine the durability under industrially relevant conditions, chronopotentiometry was performed at a high current density of 1 A cm-2 in the same three-electrode configuration. The Mn-ZIF-67 electrode sustains this current density for 24 h with the potential remaining stable at approximately 1.65 V vs. RHE [Supplementary Figure 7], indicating that the reconstructed active layer withstands the intense gas evolution and mechanical stress associated with high-current operation.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 3. Alkaline OER comparison of bare NF, ZIF-67 and Mn-ZIF-67. (A) Polarization profiles recorded in 1.0 M KOH; (B) η values at 10 and 100 mA cm-2 together with current density at 1.53 V vs. RHE; (C) Tafel analysis; and (D) 12 h chronoamperometric response of Mn-ZIF-67 at 1.465 V vs. RHE. OER: Oxygen evolution reaction; NF: nickel foam; ZIF-67: zeolitic imidazolate framework-67; RHE: reversible hydrogen electrode.

The origin of the distinct catalytic activity of ZIF-67 and Mn-ZIF-67 was further unraveled through combined electrochemical analysis and post-reaction characterization. Under alkaline OER conditions, the measured catalytic activity can reflect several coupled contributions, notably interfacial electron transfer, electrochemical accessibility, transport, and reconstruction of the precursor surface[38-40]. Recent studies on water/seawater-splitting electrodes have also emphasized that reliable physicochemical characterization, including structural analysis, surface chemical-state evolution, electrochemical impedance, accessible surface-area evaluation, normalized activity comparison, and post-reaction examination, is essential for establishing meaningful structure-activity relationships[41]. Interfacial kinetic differences were first probed by EIS. As revealed by the Nyquist plots and corresponding fitting curves in Figure 4A, Mn-ZIF-67 exhibits a significantly smaller semicircle diameter than both ZIF-67 and bare NF, indicating a lower interfacial resistance under OER-relevant conditions. Quantitative fitting using an equivalent circuit model, with details provided in Supplementary Figure 8 and Supplementary Table 3, reveals that Mn-ZIF-67 possesses a low charge-transfer resistance (Rct) of 2.17 Ω. This value is less than half that of ZIF-67 (4.60 Ω) and far lower than that of NF (35.36 Ω). The pronounced decrease in resistance demonstrates that Mn incorporation effectively facilitates interfacial electron transfer and reduces kinetic polarization losses during the OER process[42]. The density of electrochemically accessible active sites is another critical factor in determining catalytic activity[38]. Electrochemical accessibility was evaluated next from Cdl values fitted to the non-Faradaic CV data in Figure 4B and C and Supplementary Figures 9 and 10. Based on ECSA = Cdl/Cs, with Cs taken as 40 μF cm-2, the Cdl values correspond to estimated ECSA values of 120.50, 63.25, and 72.50 cm2 for Mn-ZIF-67, ZIF-67, and NF, respectively. These Cdl-derived ECSA values should be regarded as apparent electrochemically accessible areas rather than absolute physical surface areas, and are used here mainly for relative comparison under identical testing conditions. The larger apparent ECSA of Mn-ZIF-67 indicates more electrochemically accessible sites, which contributes to the enhanced OER performance[43]. To further evaluate the intrinsic activity of individual active sites, the LSV currents were normalized to the respective ECSA values. As displayed in Figure 4D, the ECSA-normalized polarization curves show that Mn-ZIF-67 still outperforms ZIF-67, suggesting that the improved activity is not solely caused by the increased electrochemically accessible area[44,45]. A comparison with representative ZIF-67/MOF-based and transition-metal OER electrocatalysts is summarized in Supplementary Table 4. Notably, Mn-ZIF-67 delivers a lower overpotential and Tafel slope than pristine ZIF-67 and many previously reported catalysts, highlighting its superior catalytic kinetics. The enhanced activity can be attributed to the synergistic contributions of increased electrochemically accessible surface area, accelerated interfacial charge transfer, and the formation of a Mn-containing Co oxyhydroxide-like active layer with enhanced intrinsic activity during reconstruction.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 4. (A) Experimental and fitted Nyquist responses of NF, ZIF-67 and Mn-ZIF-67 at 1.47 V vs. RHE; (B) non-Faradaic CV series for Mn-ZIF-67; (C) linear dependence of Δj/2 on scan rate used to extract Cdl; and (D) ECSA-normalized polarization profiles, with estimated ECSA values shown in the inset. ZIF-67: Zeolitic imidazolate framework-67; NF: nickel foam; RHE: reversible hydrogen electrode; ECSA: electrochemically active surface area; CV: cyclic voltammetry.

As-prepared Mn-ZIF-67 undergoes pronounced electrochemical surface reconstruction under OER conditions[46,47]. To directly monitor this structural evolution, in situ electrochemical Raman spectroscopy was performed under OER-relevant potentials. As shown in Figure 5A, the Raman spectra collected from open-circuit potential (OCP) to 1.80 V show clear potential-dependent changes. At lower potentials, the spectrum is dominated by Co-based oxide/oxide-like species. When the applied potential increases into the OER region, a Raman band around 503 cm-1 becomes more evident, which is assigned to the Co-O vibration of CoOOH. Meanwhile, the CoOx-related band around 686 cm-1 evolves under anodic polarization. The potential-dependent Raman evolution therefore directly supports the formation of a CoOOH-like surface species during anodic polarization. The in situ Raman spectra mainly confirm the potential-induced formation of CoOOH-like species; Mn-related Raman signals are relatively weak and may overlap with Co-based vibrational features. Post-OER morphological analysis in Figure 5B shows that the initial polyhedral crystals evolve into an interconnected nanosheet architecture. Local lattice ordering in the post-OER material is visible in the HRTEM image of Figure 5C. Measured spacings of 0.193 and 0.235 nm are consistent with the reported CoOOH (104) and (101) reflections, respectively[48]. Two additional spacings, 0.262 and 0.214 nm, are consistent with values reported for MnOOH-related (-102) and (-121) planes[49]. Together with the post-OER Mn 2p evolution and inductively coupled plasma (ICP) retention data, these lattice features support the presence of Mn-containing oxyhydroxide-related regions in the reconstructed catalyst; they do not, by themselves, resolve the exact atomic arrangement of the working Mn sites[50]. XPS further clarifies the evolution of surface chemical states. The post-OER Co 2p spectra in Figure 5D show the main Co 2p3/2 peak shifts from 781.1 eV, characteristic of Co2+ with intense satellite features, to 779.9 eV with markedly suppressed satellites. This change indicates oxidation to a Co3+-dominated surface, consistent with CoOOH formation[51,52]. Similarly, the post-OER Mn 2p spectra in Figure 5E show that the Mn 2p3/2 peak, initially centered at 641.2 eV and characteristic of a Mn2+-like environment, shifts positively to 642.0 eV after the OER, accompanied by a marked change in line shape. This 0.8 eV positive shift and the altered line shape indicate oxidation of Mn toward a Mn3+-dominated environment and support the participation of Mn in the reconstructed oxyhydroxide layer[53]. The ex situ XRD patterns before and after OER further show weakened diffraction features after electrolysis, indicating electrochemical reconstruction and partial loss of long-range crystallinity of the pristine ZIF framework during OER [Supplementary Figure 11]. For comparison, the post-OER surface states of pristine ZIF-67 were also examined [Supplementary Figures 12 and 13]. The post-OER Co 2p spectrum of ZIF-67 exhibits Co 2p3/2 and Co 2p1/2 peaks at 779.9 and 795.6 eV assignable to Co3+-containing oxyhydroxide-like species, while the pronounced satellite features indicate that considerable Co2+ character remains. Meanwhile, the post-OER HRTEM image of ZIF-67 reveals lattice fringes with a spacing of 0.45 nm, corresponding to the CoOOH (003) plane, confirming that undoped ZIF-67 likewise undergoes electrochemical reconstruction into CoOOH-like species during the OER. Compared with post-OER Mn-ZIF-67, whose Co 2p3/2 peak shifts to 779.9 eV with markedly suppressed satellites, the surface oxidation of ZIF-67 is less complete, further indicating that Mn incorporation facilitates the oxidative reconstruction of Co sites toward the active oxyhydroxide phase. To determine the actual Mn doping level and its retention after electrochemical operation, ICP analysis was performed on the catalyst-loaded electrodes before and after long-term OER operation. As summarized in Supplementary Table 5, the as-prepared Mn-ZIF-67 has an Mn/Co atomic ratio of 0.1005 ± 0.0024, close to the nominal feeding ratio of 0.111 and corresponding to an Mn incorporation efficiency of about 91%. After long-term OER operation, the ratio decreases to 0.0901 ± 0.0024, corresponding to a normalized Mn/Co atomic ratio of 89.7% of its initial value. Most Mn species are therefore retained in the reconstructed catalyst layer, consistent with the HRTEM and XPS evidence for the formation of Mn-containing oxyhydroxide species.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 5. (A) In situ Raman spectra of Mn-ZIF-67 collected from OCP to 1.80 V vs. RHE in 1.0 M KOH. (B) TEM and (C) HRTEM images of Mn-ZIF-67 after the OER. High-resolution XPS scans of as-prepared Mn-ZIF-67 compared to the post-OER test for (D) Co 2p and (E) Mn 2p. OER: Oxygen evolution reaction; OCP: open-circuit potential; ZIF-67: zeolitic imidazolate framework-67; RHE: reversible hydrogen electrode; TEM: transmission electron microscopy; HRTEM: high-resolution transmission electron microscopy; XPS: X-ray photoelectron spectroscopy.

To obtain atomic-level insight into Mn-induced activity enhancement, DFT calculations were performed. ZIF-67 and Mn-ZIF-67 precursor models were constructed to evaluate Mn-induced charge redistribution and electronic modulation in the pristine framework [Figure 6A and B]. In addition, considering the post-OER HRTEM and XPS evidence for electrochemical reconstruction into Co/Mn oxyhydroxide species, CoOOH and Mn-doped CoOOH surface models were constructed to evaluate the OER reaction energetics on the reconstructed active surfaces [Figure 6C]. The results indicate that Mn adopts a charge state distinct from Co and induces a redistribution of electron density within the ligand-bridged ZIF framework. Although Mn and Co centers are not directly bonded in the pristine structure, the charge redistribution mediated by imidazolate linkers suggests that Mn incorporation modifies the electronic environment of the framework. This result is consistent with the Co 2p binding-energy shift observed in XPS, indicating Mn-induced electronic perturbation in the pristine Mn-ZIF-67. To further elucidate how this redistribution affects the adsorption of OER intermediates, the d-band center (εd) of the active metal sites was evaluated as an electronic descriptor, as shown in Figure 6B. Mn incorporation shifts εd upward from -2.00 eV in ZIF-67 to -1.70 eV in Mn-ZIF-67. Within the d-band framework, such an upshift of εd indicates stronger metal-oxygen interaction due to modified antibonding state occupancy. This effect optimizes the adsorption energetics and activation of oxygenated intermediates such as *OH, *O, and *OOH, thereby promoting OER kinetics. This trend is consistent with the experimentally observed enhancement in interfacial charge transfer and catalytic activity upon Mn incorporation.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 6. (A) Optimized structure models and Bader charge analysis of ZIF-67 and Mn-ZIF-67. (B) Calculated density of states and d-band centers for ZIF-67 and Mn-ZIF-67. (C) Optimized CoOOH and Mn-doped CoOOH reconstructed active-surface models and the corresponding Gibbs free-energy diagrams for the OER pathway at zero potential. OER: Oxygen evolution reaction; ZIF-67: zeolitic imidazolate framework-67.

To model the electrochemically reconstructed active surfaces suggested by post-OER characterizations, CoOOH and Mn-modified CoOOH (Mn/CoOOH) were constructed to represent the post-OER surfaces of ZIF-67 and Mn-ZIF-67, respectively[35,54,55]. The Gibbs free energy (ΔG) profiles for the four-electron OER pathway in Figure 6C show that the potenial-determining step (PDS) on CoOOH is the *O to *OOH transformation, with a ΔG of 2.22 eV. In contrast, Mn incorporation optimizes intermediate adsorption. Although the PDS remains the same, the ΔG of Mn/CoOOH decreases to 1.71 eV, significantly lowering the energetic penalty for OER turnover[56,57]. These results indicate that Mn acts as an effective electronic promoter by tuning the Co electronic structure and optimizing intermediate binding on the reconstructed oxyhydroxide surface. The free-energy profile further supports that the Mn-containing reconstructed Co oxyhydroxide surface serves as the active phase responsible for the improved OER kinetics.

To evaluate practical feasibility, a two-electrode alkaline seawater electrolyzer was assembled using a Mn-ZIF-67/Ni foam anode, a graphite rod cathode, and alkaline natural seawater collected from Shenzhen Bay[58]. When the same electrolyzer was connected to a commercial silicon solar panel, continuous gas evolution was observed at both electrodes under natural sunlight [Figure 7A], providing qualitative proof of concept for compatibility with renewable power input[59]. The quantitative data in Figure 7B and C were acquired separately under workstation control. Overall cell performance was evaluated by LSV, as shown in Figure 7B. The Mn-ZIF-67 electrolyzer significantly outperforms the bare NF control. It delivers current densities of 10 and 50 mA cm-2 at 1.84 and 2.06 V, respectively, whereas the NF control requires 1.97 and 2.28 V to reach the same current densities, corresponding to reductions of 130 and 220 mV in cell voltage and indicating reduced overall-cell polarization. Chronopotentiometry measurements shown in Figure 7C further confirm excellent operational durability under harsh anodic conditions. At a constant current density of 50 mA cm-2, the cell voltage remains highly stable at 2.06 V over 100 h of continuous operation without observable decay, demonstrating strong practical viability. During OER, the Mn-ZIF-67 undergoes in situ reconstruction into a nanosheet-like bimetallic (oxy)hydroxide layer composed of CoOOH and MnOOH nanocrystals [Figure 5C][60]. The stable operation over 100 h demonstrates the good durability of the Mn-ZIF-67-derived anode in alkaline seawater. To further examine the structural stability after seawater electrolysis, post-reaction XRD was performed. As shown in Supplementary Figure 14, the characteristic ZIF-related diffraction peaks largely disappear after electrolysis, indicating electrochemical reconstruction of the MOF precursor under anodic conditions. No crystalline chloride-containing corrosion products were detected by ex situ XRD after the test[61]. The surface chemical states after seawater electrolysis were further examined by XPS [Supplementary Figures 15 and 16]. The Co 2p spectrum of Mn-ZIF-67 after alkaline seawater electrolysis exhibits Co 2p3/2 and Co 2p1/2 peaks at 780.1 and 795.2 eV with weak satellite features, indicating that the Co3+-dominated oxyhydroxide-like surface is well preserved. The Mn 2p spectrum retains well-defined Mn 2p3/2 and Mn 2p1/2 peaks at 642.3 and 654.0 eV, consistent with Mn3+ oxyhydroxide-like species, indicating that Mn is retained in the reconstructed layer. These chemical states closely resemble those observed after the OER in 1.0 M KOH [Figure 5D and E], further suggesting that the reconstructed Co-Mn (oxy)hydroxide layer maintains its chemical integrity against chloride attack during long-term alkaline seawater electrolysis. Collectively, these findings identify Mn-ZIF-67 as a promising anode material for solar-driven alkaline seawater electrolysis. To benchmark the overall seawater splitting performance, Mn-ZIF-67 was compared with representative ZIF/MOF-derived and Mn-containing electrocatalytic systems [Table 1]. The Mn-ZIF-67/NF || graphite rod cell requires 1.84 V at 10 mA cm-2 and 2.06 V at 50 mA cm-2 in alkaline natural seawater, showing competitive performance relative to several related systems. Together with its stable operation for 100 h at 50 mA cm-2 and photovoltaic-driven demonstration, these results highlight the practical potential of Mn-ZIF-67 for alkaline seawater electrolysis.

Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

Figure 7. (A) Photograph of the assembled alkaline seawater electrolyzer connected to a commercial silicon solar panel, illustrating solar-powered operation (original photograph taken by the authors); (B) LSV of the overall seawater splitting system; (C) Chronopotentiometry analysis of Mn-ZIF-67 electrolysis for 100 h at 50 mA cm-2. ZIF-67: Zeolitic imidazolate framework-67; NF: nickel foam; LSV: linear sweep voltammetry.

Table 1

Comparison of overall seawater splitting performance of Mn-ZIF-67 with representative ZIF/MOF-derived, Mn-containing, and related electrocatalytic systems

No. Catalyst Electrolyte Overall seawater splitting performance Stability Ref.
1 Mn-ZIF-67/NF || graphite rod (this work) 1.0 M KOH + natural seawater 1.84 V at 10 mA cm-2;
2.06 V at 50 mA cm-2
100 h at 50 mA cm-2 This work
2 ZIF-67/CF-1 || ZIF-67/CF-1 Natural seawater 2.46 V at 10 mA cm-2 - [62]
3 S-HEO/rGO-based cell Alkaline seawater 1.85 V at 10 mA cm-2 100 h at 10 mA cm-2 [63]
4 Co3Fe1@C (Co3Fe1-800)-based cell Alkaline seawater PV-driven: 2.2 V commercial Si solar cell at 50 mA cm-2 280 h at 50 mA cm-2 [64]
5 NZ700 || NZ700 Alkaline seawater 1.72 V at 20 mA cm-2 - [65]
6 RhCoNi-MOF || RhCoNi-MOF Natural alkaline seawater 1.52 V at 10 mA cm-2 >80 h [66]

CONCLUSIONS

This work demonstrates that trace Mn doping can direct the electrochemical reconstruction pathway of ZIF-67 and thereby determine the nature of the true active phase, the OER kinetics, and the catalytic durability. Rather than acting as a static active phase, Mn-ZIF-67 behaves as a structurally dynamic catalyst under OER conditions. During anodic operation, the pristine Mn-ZIF-67 surface reconstructs into a robust bimetallic Co-Mn oxyhydroxide layer, which serves as the catalytically active phase. Density functional theory calculations confirm that Mn-induced electronic redistribution upshifts the Co d-band center, thereby lowering the Gibbs free energys of intermediates, while electrochemical measurements show that Mn incorporation simultaneously increases the density of electrochemically accessible sites and enhances interfacial charge transfer. The practical viability of this dynamically reconstructed interface is demonstrated in a two-electrode alkaline seawater electrolyzer, which sustains a current density of 50 mA cm-2 at approximately 2.06 V for 100 h, and which can also be operated directly using a commercial silicon solar panel. This work establishes a general mechanistic framework in which trace transition metal doping directs the in situ structural evolution of metal-organic frameworks, offering an effective route toward the rational design of next-generation efficient electrocatalysts.

DECLARATIONS

Authors’ contributions

Conceptualization: Lou, X. Y.

Investigation, sample preparation, data curation, and formal analysis: Liu, D.; Luan, H.

Writing - original draft: Liu, D.; Li, H.; Lou, X. Y.

Writing - review and editing: Guo, H.; Li, Y.; Shao, N.; Boada, R.; Dong, Z.; Li, H.; Lou, X. Y.; Chen, Z.

Supervision: Li, H.; Lou, X. Y.; Chen, Z.

All authors discussed the results and contributed to the revision and finalization of the manuscript.

Availability of data and materials

The data supporting the findings of this study are available within the article and its Supplementary Materials. The raw datasets generated and analyzed during the current study, including the original electrochemical measurement files, XPS fitting results, XRD patterns and electron microscopy images, are available from the corresponding authors upon reasonable request.

AI and AI-assisted tools statement

Not applicable.

Financial support and sponsorship

This research was financially supported by the National Natural Science Foundation of China (52578311), Guangdong University Young Innovative Talents Program (KJ2024C034), Key Research Area Scientific Research Project (SZIIT2025KJ046), Scientific Research Start-up Fund for Doctoral and Master's Faculty (SZIIT2024KJ026), the 2025 Central Government Guidance for Local Science and Technology Development Fund Project (YDZJSX2025D092), the Fundamental Research Program of Shanxi Province (202203021221041), and the High-Level Overseas Talent Return Funding Project of the Ministry of Human Resources and Social Security (202506930038). Hanwen Luan acknowledges the financial support from the China Scholarship Council (202308440268).

Conflicts of interest

Chen, Z. serves as a Guest Editor for the Special Issue “Earth-Abundant Materials for Electrocatalytic Small Molecule Conversion” of Energy Materials. Chen, Z. had no involvement in the editorial processing of this manuscript, including reviewer selection, manuscript handling, or editorial decision-making. The other authors declare that they have no conflicts of interest.

Ethical approval and consent to participate

Not applicable.

Consent for publication

Not applicable.

Copyright

© The Author(s) 2026.

Supplementary Materials

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Trace Mn doping activates ZIF-67 through reconstruction to Co-Mn (oxy)hydroxides for enhanced oxygen evolution

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