Open Access Article
Yang Huamei
ab,
Wang Beileia,
Yu Mengjuna,
He Haiyanbc and
Li Changzhi
*bc
aSchool of Materials and Chemical Engineering, Xuzhou University of Technology, Xuzhou, Jiangsu 221018, China
bCAS Key Laboratory of Science and Technology on Applied Catalysis, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, Dalian, 116023, China. E-mail: licz@dicp.ac.cn
cUniversity of Chinese Academy of Sciences, Beijing 100049, China
First published on 19th November 2025
Low-cost, high-performance catalysts are pivotal for advancing water electrolysis toward industrial applications. As an abundant, renewable, and readily available carbon feedstock, lignin offers a sustainable platform for the development of a carbon-supported catalyst. In this study, manganese-loaded lignin-derived carbon (Mnx@C) was synthesized via an in situ chelation–anchoring strategy using lignin as the carbon source. The in situ chelation–anchoring carbonization process enabled effective incorporation and uniform dispersion of Mn species. Mn species in Mnx@C were mainly Mn2O3, MnO2, and MnO. Among these Mn species, MnO was dispersed in the lignin-based carbon support as aggregation nanoparticles, while Mn2O3 and MnO2 were primarily dispersed in an amorphous state. The electrocatalytic performances of Mnx@C were systematically evaluated for the oxygen evolution reaction (OER) and hydrogen evolution reaction (HER). The Mn content and NH4Cl modification significantly influenced the OER and HER activities. The Mn1@C prepared at 1 mmol Mn/g lignin, with the final Mn content of 8.7%, exhibited optimal performances of 517 mV (OER) and 448 mV (HER) at 50 mA cm−2. Further improvement was achieved by modulating the pore structure using NH4Cl as a pore-forming agent, resulting in a Mn-loaded and nitrogen-doped carbon (Mn1@NC). NH4Cl modification induced a morphological transition from a bulk structure to a layered microporous structure with a high surface area. The modified Mn1@NC demonstrated excellent OER and HER performances, requiring low overpotentials of 299 mV (OER) and 409 mV (HER) at 50 mA cm−2. In addition, the overall water-splitting demonstrated a low potential of 1.65 V to reach 10 mA cm−2. This in situ anchoring and direct carbonization strategy provides a simple, cost-effective, and scalable route to high-performance Mn-based catalysts from low-cost lignin, offering potential for industrial water electrolysis and high-efficient utilization of lignin.
Transition metals and their oxides, nitrides, phosphides, hydroxides and sulfides have been widely investigated.7,8,10–13 Manganese (Mn), a typical 3d transition metal, is derived primarily from parent materials in soil, and exhibits multiple oxidation states. Mn-based materials have been explored as electrocatalysts for the OER and HER owing to their inherent catalytic activity, environmental compatibility, low cost, and natural abundance.14–19 Particularly, Mn-based oxides (MnOx) exhibit good chemical stability in alkaline electrolytes20,21 and facilitate O–O bond formation steps in the OER owing to its variable oxidation states (commonly +2 in MnO, +3 in Mn2O3, +4 in MnO2, and mixed states in Mn3O4).20 Therefore, focused development of Mn-based catalysts remains necessary, as they possess irreplaceable potential in large-scale commercial applications. However, Mn-based materials always exhibit poor OER and HER performances compared to other transition metal-based materials (such as iron, nickel, and cobalt-based materials), limiting their practical applications.7,12,21,22 The lower electrocatalytic activity of Mn-based catalysts, leading to low intrinsic catalytic activity,3,8,12,23 is primarily caused by the poor electrical conductivity and the electronic configuration that results in weak electronic coupling with intermediates.20,21
The performance of Mn-based catalysts can be improved through the following strategies: constructing heterostructures (e.g., composites with carbon materials or oxides) to increase the number of active sites and enhance the electron transfer rate and charge transfer efficiency. Regulating the morphology (e.g., preparing nanosheets or hollow spheres) to increase specific surface area exposes more active sites for the OER and the HER. Carbon-based materials are employed as electrically active materials or conductive substrates to create oxygen vacancies and heterogeneous interfaces. The OER and HER performance of MnOx-based electrocatalysts can be improved by tuning the morphology of carbon materials and synergistic effects between Mn species and carbon.18,19,24–26 Carbon supports such as activated carbon, carbon nanotubes, graphene, and carbon nanofibers are always employed to prepare Mn-loading carbon catalysts via an impregnation method. However, these carbon supports need to be prepared in advance, making the process labor- and time-intensive. Meanwhile, these carbon supports often possess inert surfaces that limit metal dispersion during impregnation.27 Recently, well-synthetic carbon materials such as carbon dots18,28 and metal–organic frameworks29,30 were employed to incorporate with Mn species. This strategy can provide Mn-based carbon catalysts with high surface areas, enhanced conductivity, greatly promoted electrocatalytic activity and high stability for the OER. However, the reliance on pure chemicals as carbon precursors incurs high costs, hindering large-scale application.
Lignin, a renewable biomass resource, possesses a highly aromatic, three-dimensional conjugated network with abundant oxygen-containing functional groups (e.g., hydroxyl, carbonyl, and methoxy) and high carbon content.31 These structural characteristics endow lignin with compelling potential for synthesizing multifunctional carbon materials, particularly in applications such as energy storage, adsorption, and catalysis.31–37 Notably, the oxygen functional groups can effectively anchor metal species through chelation or coordination, promoting uniform metal dispersion and enhancing catalytic performance.36 Owing to these advantages, lignin is regarded as an ideal precursor for designing high-performance functional carbon supports in catalytic applications. At the same time, lignin is a large-volume by-product of the pulping and papermaking as well as biorefinery industries. Lignin is a large-volume byproduct of the pulping and papermaking as well as biorefinery industries. It exhibits a substantial annual production volume, yet the majority is currently underutilized through low-value applications such as disposal or inefficient combustion, which pose environmental and economic challenges. Using it as a carbon source can achieve “waste resource utilization” and reduce the preparation cost of carbon materials.
In this work, a Mn-loaded lignin-derived carbon catalyst (Mnx@C) was prepared for water electrolysis via an in situ anchoring and one-step carbonization strategy. The effect of Mn proportion was investigated, and Mn1@C obtained at the Mn proportion of 1 mmol g−1 lignin exhibited the best OER and HER performances. Furthermore, morphological modulation using ammonium chloride (NH4Cl) as a pore-forming agent yielded Mn1@NC with a porous lamellar structure, characterized by high surface area and abundant micropores. This optimized structure significantly enhanced bifunctional OER and HER performances. The Mn1@NC catalyst exhibited a remarkably low overpotential of 299 mV for the OER and 409 mV for the HER at a current density of 50 mA cm−2. In addition, the overall water-splitting device demonstrated a low potential of 1.65 V to reach 10 mA cm−2. This performance conclusively demonstrates the viability of fabricating high-performance bifunctional electrocatalysts for water electrolysis through the in situ chelation and carbonization methodology utilizing lignin as a carbon precursor.
:
V 2
:
1). Under ultrasonication, the MnCl2 solution was added dropwise using a pipette to the lignin–ethanol suspension, forming a mixture. This mixture was then magnetically stirred for 24 hours. Subsequently, 50 mL of deionized water was added to the ethanol suspension of Mn–lignin, and the suspension was left to stand for 30 minutes. Mn–lignin complex precipitated out and settled. Vacuum filtration was performed to obtain the Mn–lignin complex. The Mn–lignin complex was dried in a vacuum oven at 80 °C for 10 hours. The dried Mn–lignin sample was placed in a porcelain boat and transferred to a tubular furnace for high-temperature carbonization. The heating program, under a nitrogen atmosphere, was as follows: ramp the temperature at 15 °C min−1 to 800 °C and then hold at 800 °C for 2 hours. After carbonization, the furnace was cooled naturally to room temperature under nitrogen, and Mn-loaded lignin carbon-based materials were obtained, which were labelled as Mnx@C (x was the millimole ratio of MnCl2·4H2O to lignin). For example, samples prepared with 0.198 g (1 mmol) of MnCl2·4H2O added to 1 g lignin were labelled as Mn1@C. The effect of Mn loading was investigated with the Mn proportion x being 0 (0 g), 0.05 (0.010 g of MnCl2·4H2O, 0.05 mmol), 0.25 (0.049 g of MnCl2·4H2O, 0.25 mmol), 0.5 (0.099 g of MnCl2·4H2O, 0.5 mmol), 1 (0.198 g of MnCl2·4H2O, 1 mmol), and 2 (0.396 g of MnCl2·4H2O, 2 mmol).
Additionally, NH4Cl was employed to modify the catalytic performance of Mn1@C, which served as a pore-forming agent and a nitrogen source. The preparation of the Mn–lignin complex followed the same procedure as Mn1@C. Wetting grinding was employed to achieve thorough mixing of Mn–lignin and NH4Cl with the ratio of NH4Cl to lignin as 0.5
:
1. 0.5 g NH4Cl was added to the complex of Mn–lignin, and the mixture was subjected to wetting grinding for complete homogenization. The mixture of Mn–lignin and NH4Cl was dried in a vacuum oven at 80 °C for 12 hours. Finally, the mixture of Mn–lignin and NH4Cl was carbonized via the same procedure of Mn1@C. The modified N-doped carbon was labelled as Mn1@NC. An N-doped lignin-based carbon without Mn-loading (Mn0@NC) was also prepared using the same procedure as Mn1@NC.
For control experiments, activated carbon (AC) was employed to prepare a Mn-loaded activated carbon (Mn1@AC) with 0.198 g of MnCl2·4H2O, using the same method as Mn1@C.
:
1
:
1) of carbon black, PVP and samples. Typically, 0.08 g of carbon black, 0.01 g of PVP and 0.01 g of samples were weighed and mixed. The mixture was ground with 2 ml of ethanol to form a homogeneous slurry. The nickel foam was immersed in the above slurry for 1 minute and rapidly dried using a heat lamp. The nickel foam was weighed before and after loading catalytic materials by a microbalance. The average loaded mass was 0.8 ± 0.05 mg cm−2. Then, the loaded foam nickel was placed in a vacuum oven at 60 °C for 12 hours.
All electrochemical OER and HER tests were performed on a CHI660E electrochemical workstation using a standard three-electrode system in 1 M KOH electrolyte (pH = 14) at room temperature. The fabricated nickel foam electrode (clamped with an electrode holder) was used as the working electrode, and the area of the working electrode immersed in the KOH solution was kept as 1 × 1 cm2. The platinum sheet was used as the counter electrode. The mercury/mercury oxide (Hg/HgO) electrode (1 M KOH, 25 °C, standard potential +0.098 V vs. SHE) was used as the reference electrode.
Linear sweep voltammetry (LSV) for the OER was performed in the potential range of 0 to 1 V vs. Hg/HgO. All measured potentials (vs. Hg/HgO) were converted to the reversible hydrogen electrode (RHE) scale using the formula under alkaline conditions: V (vs. RHE) = V (vs. Hg/HgO) +0.098 + 0.059 × pH. Tafel slopes (b) were calculated by fitting the linear region of the Tafel plot using the equation: η = a + b
log
j, where η is the overpotential (η = E − Erev, Erev = 1.23 V), a is a constant, and j is the current density. Cyclic voltammetry (CV) was performed within the non-faradaic potential range (typically 0.1 to 0.2 V vs. RHE is recommended; confirm suitability for your system) at various scan rates (e.g., 10, 40, 80, and 100 mV s−1). The double-layer capacitance (Cdl) was estimated from the slope of the plot of the charging current density difference (Δj = |ja − jc|/2) at a fixed potential within this range versus the scan rate. The long-term electrochemical stability of the catalyst was evaluated by chronopotentiometry or chronoamperometry at a constant current density or potential in 1 M KOH (pH = 14) for 20 hours. Electrochemical impedance spectroscopy (EIS) was conducted from a potential of 238 to 458 mV vs. RHE for the OER over a frequency range from 100 kHz to 0.1 Hz with an AC amplitude of 10 mV. LSV measurements for the HER were performed in the potential range of −0.9 to 0.0 V vs. Hg/HgO. LSV measurements for the overall water-splitting were conducted using a two-electrode system in 1.0 M KOH solution, with Mn1@NC serving as both the cathode and the anode (Mn1@NC‖Mn1@NC).
| Samples | Mna/% | Cb/% | Hc/% | Nd/% | Oe/% | I40.5/I22.4f |
|---|---|---|---|---|---|---|
| a Determined by ICP-OES.b Determined by using an elemental analyzer.c Determined by using an elemental analyzer.d Determined by using an elemental analyzer.e Determined by the difference of 100 and the sum of a–d.f I40.5/IC calculated based on XRD, as shown in Fig. 1. | ||||||
| Lignin | — | 63.32 | 5.91 | 1.87 | 28.90 | — |
| Mn0@C | 0.02 | 83.82 | 2.67 | 0.43 | 13.06 | — |
| Mn0.05@C | 0.55 | 83.71 | 2.21 | 0.42 | 13.11 | 0.98 |
| Mn0.25@C | 2.87 | 80.54 | 2.73 | 0.51 | 13.35 | 1.42 |
| Mn0.5@C | 5.84 | 78.63 | 1.32 | 0.74 | 13.47 | 4.65 |
| Mn1@C | 8.65 | 75.48 | 1.45 | 0.82 | 13.60 | 5.28 |
| Mn2@C | 9.74 | 72.22 | 0.94 | 0.85 | 16.25 | 3.74 |
| Mn1@AC | 6.63 | 87.37 | 1.42 | 0.38 | 4.20 | — |
| Mn1@NC | 8.92 | 72.23 | 2.13 | 4.36 | 12.36 | 5.22 |
The addition of NH4Cl during the carbonization process achieved N-doped carbon (Mn1@NC) with the Mn proportion of 1 mmol g−1 lignin, which had a much higher N content than Mn1@C and Mn1@AC as listed in Table 1. As mentioned above, lignin has abundant active functional groups in its structure, including hydroxyl, carbonyl, and carboxyl groups. Meanwhile, lignin was decomposed to form active carbon intermediates during carbonization.38 The co-carbonization of NH4Cl and the Mn–lignin complex achieved nitrogen doping and morphology regulation through a synergistic effect due to the abundant active structures in lignin.39 At around 280 °C, NH4Cl decomposed to generate gases (NH3 and HCl). NH3 reacted with these carbon intermediates or active groups, and N was embedded into the carbon skeleton through substitution, cyclization, and other reactions, realizing in situ N-doping.38–40 As the carbon skeleton further graphitized, nitrogen stably existed in the carbon structure (mainly in three forms: pyrrole nitrogen, pyridine nitrogen, and graphitic nitrogen). The EDS and XPS analysis results in the following section will confirm the N-doping and its existing forms.
Fig. 1(a) shows the XRD patterns of Mnx@C, Mn1@AC and Mn1@NC. Mn0@C, derived from lignin carbonization without Mn-loading, was composed of an amorphous carbon structure with a diffraction peak at 2θ = 22.4°. With the increasing Mn proportion, the diffraction peaks at 2θ = 35.6°, 40.5°, 59.1°, 70.1°, and 73.6° intensified. These peaks corresponded to the diffraction peaks of the MnO standard card (PDF#89-2804), indicating that Mn was successfully loaded onto the carbon support and existed in the form of MnO. Taking the intensity of the carbon peak (2θ = 22.4°, I22.4) as a reference, the intensity ratio of the MnO characteristic peak (I40.5) to I22.4 (I40.5/I22.4) was calculated to semi-quantitatively analyze the loading amount of MnO as listed in Table 1. The loading amount of MnO increased with the increasing Mn proportion, which was consistent with the results of ICP-OES. The loading amount of MnO in Mn1@C reached the maximum with the peak value of I40.5/I22.4 as listed in Table 1. When NH4Cl was added for pore generation, the XRD pattern of Mn1@NC had no significant changes, indicating that the addition of NH4Cl had no effects on Mn species. However, Mn1@AC had no distinct diffraction peaks of MnO as shown in Fig. 1(a). This demonstrated a clear difference of Mn species between the Mnx@C prepared in situ from lignin and Mn1@AC prepared via the conventional method (i.e., impregnation method).
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| Fig. 1 XRD spectra (a), SEM images (b), TEM images (c), N2 adsorption–desorption curves (d) and elemental mapping (e) of Mnx@C and Mn1@NC. | ||
Fig. 1(b) shows the SEM images of Mn1@C and Mn1@NC. In the absence of NH4Cl, Mn1@C exhibited a bulk morphology with obvious agglomeration of Mn species. The addition of NH4Cl significantly altered the morphology of Mn1@NC, transforming from a bulk structure of Mn1@C to a porous lamellar structure of Mn1@NC. Fig. 1(b) also shows a substantial population of pores in Mn1@NC, partially labelled with red circles. Fig. 1(c) shows the TEM images of Mn1@C and Mn1@NC. Obviously, a large number of pores were observed in Mn1@NC with 7–10 nm of nanoparticles, while Mn1@C possessed large nanoparticles without pores observed. Fig. 1(c) also illustrates the MnO nanocrystals that are surrounded by amorphous carbon or graphene. The lattice fringe with a spacing of 0.25 nm corresponded to the (111) plane of the cubic MnO phase, and a spacing of 0.34 nm corresponded to the highly organized crystal carbon structure, which was thought to be the graphene layer. These results were consistent with the XRD results, as shown in Fig. 1(a). Fig. 1(d) shows the N2 adsorption–desorption isotherm of Mn1@NC. N2 adsorption–desorption test did not provide the isotherm of Mn1@C, which indicated that Mn1@C was a non-porous material. Mn1@NC exhibited a typical type I isotherm, indicating that Mn1@NC was microporous with abundant micropores. The surface area of Mn1@NC was 567.0 m2 g−1 and the micropore area was 549.8 m2 g−1, while the pore diameter in Mn1@NC as shown in Fig. 1(d) was 1.26 nm. As mentioned above, volatiles from lignin decomposition, NH3 and HCl from NH4Cl were formed during the co-carbonization of NH4Cl and the Mn–lignin complex. The evolution of these gases (volatiles, NH3 and HCl) promoted the pore formation in carbon materials. At the same time, NH3 and HCl reacted with carbon-based intermediates or active groups to achieve morphology regulation through a complex synergistic effect.39,40 For example, the released HCl acted as an acid catalyst to break the C–C or C–O bonds and to promote the formation of condensed ring structures during lignin carbonization.41 With the increase in temperature, lignin decomposed extensively to produce small-molecule gases (e.g., CO2, H2O). The continuous escape of these gases generated pores and constructed an interconnected porous network.41,42 Fig. 1(e) shows the elemental mapping of carbon (C), nitrogen (N), oxygen (O) and Mn in Mn1@NC. As shown in Fig. 1(e), there was a certain correlation between the distributions of O and Mn, which corresponds to the formation of MnO. N was doped in the prepared Mn1@NC, exhibiting a distribution similar to that of O and Mn.
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| Fig. 2 The effects of Mn proportion on the OER performance of electrode material Mnx@C. (a) LSV; (b) overpotential at 50 mA cm−2; (c) Tafel value; (d) Cdl. | ||
Comparing the OER performance of Mn1@C and Mn1@AC in Fig. 3, the OER performance of Mn1@C was significantly poorer than that of Mn1@AC prepared with AC as the support. As shown in Fig. 3(b), the E50 of Mn1@AC was 434 mV, lower than that of Mn1@C (517 mV). Fig. 3(c) shows that the Tafel slope of Mn1@AC was 53.9 mV dec−1, slightly higher than that of Mn1@C, indicating that Mn1@AC had a slower OER kinetic process than Mn1@C. As illustrated in Fig. 3(d), the Cdl of Mn1@AC (5.40 mF cm−2) was higher than that of Mn1@C (5.00 mF cm−2), indicating that the electrochemical active area of Mn1@AC was higher than that of Mn1@C. The higher electrochemical active area of Mn1@AC was possibly due to the fact that AC has abundant pores, which facilitated substrate adsorption and electron transmission, thereby improving the OER performance.
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| Fig. 3 NH4Cl effect on the OER performance of electrode materials Mn1@C and Mn1@NC. (a) LSV; (b) overpotential at 50 mA cm−2; (c) Tafel value; (d) Cdl; (e) EIS. | ||
To optimize the pore structure of Mn1@C prepared by in situ carbonization of lignin, NH4Cl was added as a pore-forming agent into the Mn-chelated lignin samples. As discussed in Section 2.1, with the addition of NH4Cl, Mn1@NC had more developed pore structures and higher specific surface area than Mn1@C. Fig. 3(a) and (b) show that the E50 decreased from 517 mV for Mn1@C to 299 mV for Mn1@NC, which was much lower than that of Mn1@AC (434 mV). Fig. 3(c) shows the Tafel slope of Mn1@NC (47.8 mV dec−1) was much lower than that of Mn1@C (51.4 mV dec−1) and Mn1@AC (53.9 mV dec−1), indicating that Mn1@NC had a faster OER kinetic process than Mn1@C and Mn1@AC. As shown in Fig. 3(d), the Cdl of Mn1@NC reached 8.94 mF cm−2, which was much higher than that of Mn1@C (5.38 mF cm−2) and Mn1@AC (5.40 mF cm−2), indicating that the addition of NH4Cl effectively increased the electrochemical active area of the Mn-doped lignin carbon material. Fig. 3(e) illustrates that the charge transfer resistances (Rct) increased in the order of Mn1@NC < Mn1@AC< Mn1@C, indicating that Mn1@NC had the fastest charge transfer rate during the catalytic OER process. Above all, the addition of NH4Cl significantly improved the OER performance of Mn1@NC, due to the adjusted pore structures and high specific surface area.
As shown in Fig. 3, the NH4Cl-added carbon material (Mn0@NC) without Mn-loading was also studied to further illustrate the effects of Mn-loading and NH4Cl-addition on the OER performance. The OER performance of Mn0@NC was slightly enhanced with a lower E50 (590 mV), a smaller Tafel slope (70.6 mV dec−1), and a higher Cdl (4.91 mF cm−2) than Mn0@C, indicating that NH4Cl-addition was beneficial for the improvement of OER performance, possibly due to the regulated morphology and N-doping. Comparing the NH4Cl-free materials (Mn1@C) and Mn-free materials (Mn0@NC) with Mn and N co-doped materials (Mn1@NC), the much better OER performances of Mn1@NC indicated that Mn-loading and NH4Cl-addition played a crucial synergistic role in enhancing the OER performance.
Fig. 4 summarizes the OER overpotential (E10) at 10 mA cm−2 of Mn1@NC and the reported Mn-based catalysts.18,19,28,30,43 As illustrated in Fig. 4, Mn1@NC, prepared via an in situ anchoring and direct carbonization strategy in this work, has a much lower E10 (235 mV) than the reported Mn-based catalysts. In other words, Mn1@NC exhibited more excellent OER catalytic activity than the reported Mn-based catalysts. The in situ anchoring and direct carbonization strategy using lignin as the carbon source provided a simple, cost-effective, and scalable route to high-performance Mn-based catalysts from lignin, offering significant potential for industrial water electrolysis.
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| Fig. 5 The effects of Mn proportion (a)–(c) on the HER performance of electrode material Mnx@C, and NH4Cl effect (d)–(f) on the HER performance of electrode materials Mn1@C and Mn1@NC. | ||
Fig. 5(d–f) shows the HER performance of Mn1@C, Mn1@AC and Mn1@NC. Compared with the Mn1@AC prepared via the conventional method, Mn1@C exhibited a lower E50 (448 mV) than Mn1@AC (525 mV) as illustrated in Fig. 5(e), indicating that lignin-derived in situ prepared Mn1@C achieved higher HER performance than Mn1@AC synthesized by the conventional method (i.e., the impregnation method). Similarly with the OER performance, NH4Cl-added and Mn-free carbon materials (Mn0@NC) also exhibited a better HER performance than Mn0@C, as evidenced by a lower E50 (494 mV). Additionally, Mn0@NC outperformed Mn0@C, and Mn1@NC outperformed Mn1@C in HER performance, indicating that the NH4Cl-addition played important roles in improving HER activity. The synergistic effect of the Mn-loading and NH4Cl-addition endowed Mn1@NC with the optimal HER performance. As shown in Fig. 5(d), the LSV curve of Mn1@NC shifted to a lower potential zone than that of Mn1@C. Fig. 5(e) further reveals that Mn1@NC had a lower E50 (409 mV) than Mn1@C (448 mV), demonstrating that NH4Cl-addition obviously lowered the overpotential and improved the HER performance of Mn-loaded carbon materials. Furthermore, Fig. 5(f) shows that the Tafel slope of Mn1@NC (40.2 mV dec−1) was remarkably lower than that of Mn1@C (52.4 mV dec−1), indicating that NH4Cl-addition promoted the Heyrovsky reaction during the HER and accelerated the reaction kinetics. As previously discussed, the decomposition of NH4Cl during the preparation of Mn1@NC generated abundant pores and a high specific surface area, which facilitated proton transfer and thereby improved the HER performance.
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| Fig. 6 (a) Stability test of Mn1@C and Mn1@NC; (b) LSV curves for overall water splitting using Mn1@NC‖Mn1@NC. | ||
Encouraged by the extraordinary activity of Mn1@NC for the HER and the OER in alkaline media, a two-electrode system was assembled in a 1.0 M KOH solution with Mn1@NC serving as both the cathode and anode (Mn1@NC‖Mn1@NC). The LSV curves for overall water splitting using Mn1@NC‖Mn1@NC are shown in Fig. 6(b). The device afforded the current densities of 10 mA cm−2 at cell voltages of 1.65 V, which outperforms NF‖NF (1.946 V).
O (carboxyl/ester groups), respectively. More O–C
O was detected on the surface of Mn1@NC after the test. Another two peaks observed in Fig. 7(e) were caused by the K adsorbed on the surface of Mn1@NC during the OER test. Three deconvoluted peaks at 531 eV, 532 eV and 533 eV, as shown in Fig. 7(b and f), were assigned to Mn–O, Mn–O–C, and C
O. There was a new deconvoluted peak assigned to defect O at 529.8 eV, as shown in Fig. 7(f), which was beneficial for the OER.47,48 The high-resolution XPS spectrum of Mn 2p1/2 in Fig. 7(c and g) was at 653.6 eV. The high-resolution XPS spectra of Mn 2p3/2 in Fig. 7(c) were well deconvoluted into five peaks at 638.1 eV, 641.1 eV, 642.8 eV, 644.6 eV and 646.9 eV, which were assigned to Mn0, MnO, Mn2O3, MnO2, and MnO.49,50 Mn exhibited multiple chemical oxidation states on the surface of Mn1@NC before the test. Obviously, Mn 2p3/2 of Mn1@NC after the stability test, as shown in Fig. 7(g), was mainly MnOOH, which worked as the real active site for the OER.20 Mn0 and MnO were oxidized to MnOOH. The N content on the surface of Mn1@NC reduced from 3.47 wt% (before test) to 1.52 wt% after the test, resulting from the N leaching out during the OER process. The N on the surface of Mn1@NC existed as graphitic N (401.1 eV), pyridinic N (399.8 eV) and pyrrolic N (398.8 eV) as assigned in Fig. 7(d and h).51 Among these N species, graphitic N was the main N component on the surface of Mn1@NC due to its higher area proportion. The graphitic N was reported to promote the electron transport with high electron-transfer capacity.51,52 The pyridinic N and pyrrolic N brought heteroatomic doping defects on the surface of Mn1@NC.53 The relative area proportion of pyrrolic N decreased, while the relative area proportion of pyridinic N increased, indicating that pyridinic N was more stable than pyrrolic N during the OER process.
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| Fig. 7 XPS spectra of (a) and (e) C 1s, (b) and (f) O 1s, (c) and (g) Mn 2p, and (d) and (h) N 1s of Mn1@NC before the stability test (a)–(d) and after the stability test (e)–(h). | ||
Above all, the formation process of Mn1@NC and the real active site for the OER process can be summarized as follows. First, Mn2+ underwent self-assembly with lignin due to the chelation–anchoring interaction between the polar oxygen-containing functional groups of lignin and Mn2+. The chelation–anchoring interaction permitted Mn2+ to be well dispersed in lignin carbon. Secondly, carbothermal reduction occurred, generating Mn0 during the in situ carbonization process. Simultaneously, due to the complex and highly reactive nature of lignin depolymerization products, redox reactions took place with Mn0 or Mn2+, forming Mn2O3, MnO2, or MnO. Among these MnOx species, MnO was the main MnOx species, and its aggregation nanoparticles dispersed in the lignin-based carbon support, while Mn2O3, MnO2, and Mn0 were primarily dispersed in an amorphous state on the Mn1@NC surface. NH4Cl was decomposed into HCl and NH3 during the co-carbonization of NH4Cl with Mn–lignin.24 The outgassing of HCl and NH3 acted as a pore-forming agent, regulating the carbonization process of the lignin-derived carbon, which resulted in the formation of a sheet-like porous carbon structure while concurrently achieving N-doped carbon. During the initial stage of the OER, the low-valent manganese species (Mn0 and MnO) in Mn1@NC underwent oxidation to Mn species with +3 valence. MnO2, as a common precursor of Mn-based OER catalysts, underwent reduction–reconstruction reactions to form Mn species with +3 valence in the OER test. The formed Mn species with +3 valence then combined with the hydroxide anion (OH−) in KOH solution to form a stable structure of MnOOH through proton transfer and coordination structure adjustment during the OER test. MnOOH was the real active species. OH− in KOH was first adsorbed on the Mn site of MnOOH forming adsorbed Mn3+–OH intermediates. Then, Mn3+–OH intermediates were oxidized to form Mn4+–O substances with the loss of one electron (e−) and one proton (H+). Two adjacent Mn4+–O intermediates underwent O–O bond coupling to form the Mn–O–O–Mn peroxide intermediate, which continued to undergo an oxidation reaction, losing electrons and adjusting its coordination structure. Finally, the Mn–O bond broke to release O2 molecules. Meanwhile, the Mn active sites were reduced to the initial +3 valence state, recombining with OH− in the electrolyte to enter the next catalytic cycle.20
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