Open Access Article
Gema
Martinez†
abcd,
Stefan
Delgado†
e,
Ainhoa
Madrid
ac,
Sergio
Díaz-Coello
e,
Ekaterina
Pakrieva
abc,
María
del Carmen Arévalo
e,
Elena
Pastor
*e,
Jose L.
Hueso
*abcfg and
Jesus
Santamaria
abcf
aInstituto de Nanociencia y Materiales de Aragon (INMA) CSIC-Universidad de Zaragoza, Campus Rio Ebro, Edificio I + D, C/Poeta Mariano Esquillor, s/n, 50018, Zaragoza, Spain. E-mail: jlhueso@unizar.es
bDepartment of Chemical and Environmental Engineering, University of Zaragoza, Campus Rio Ebro, C/María de Luna, 3, 50018 Zaragoza, Spain
cNetworking Research Center on Bioengineering, Biomaterials and Nanomedicine (CIBER-BBN), 28029, Madrid, Spain
dCentro Universitario de la Defensa (CUD), Ctra. de Huesca, 50090 Zaragoza, Spain
eInstituto de Materiales y Nanotecnología, Departamento de Química, Universidad de La Laguna, Av. Astrofísico Francisco Sánchez s/n, 38206, San Cristóbal de La Laguna, España. E-mail: epastor@ull.edu.es
fInstituto de Investigación Sanitaria (IIS) de Aragón, Avenida San Juan Bosco, 13, 50009 Zaragoza, Spain
gEscuela Politécnica Superior, U. Zaragoza, Crta. de Cuarte s/n 22071, Huesca, Spain
First published on 5th January 2026
This work describes how the presence of Fe single atom catalysts (Fe-SAC) dispersed on a nitrogen-enriched carbon matrix favours the selective electrocatalytic reduction of dissolved carbon dioxide to formic acid in neutral medium. Fe-SAC and Fe-free carbons were prepared by laser pyrolysis of phthalocyanine-pyridine aerosols.
Fig. 1b–d and Fig. S1 show evidence of atomically dispersed Fe features in N-doped carbons. Additional evidence from EXAFS data was presented in previous works.24 The carbon particles hold an uneven size distribution and exhibit partial interconnection as previously observed in other particle morphologies synthesized by laser pyrolysis. The brighter contrast spots correspond to the presence of atomically dispersed Fe atoms with higher Z number. Overall, the EDX signal of Fe could only be detected after accumulation in broad areas (Fig. S3). Furthermore, N signal could be also detected for both the Fe-SACs and specially its Fe-free N-Cs counterpart (Fig. S2c). The N2 adsorption–desorption isotherms showed a slight separation between the adsorption and desorption branches at higher relative pressures (p/p0 > 0.8), suggesting the presence of mesopores but with only a minor hysteresis loop (Fig. 1e and Fig. S2e).
Given the limited Fe content, partial pore blockage can be ruled out, and a change of chemical properties due to structural rearrangements caused by metal coordination seems a more likely cause. The pore size distributions, calculated using the non-local density functional theory (NLDFT) method, confirm that both materials possess pores within the mesoporous range (2–13 nm) (Fig. S4). The Fe-free N-Cs featured a broader mesoporous distribution, along with a total pore volume of 0.24 cm3 g−1, whereas the Fe-SAC exhibited substantially lower porosity (0.12 cm3 g−1), indicating that the presence of Fe effectively produces a denser material (Table S1). Raman analysis confirmed the presence of both disordered and graphitic domains at ∼1350 cm−1 and ∼1590 cm−1, respectively (Fig. 1f and Fig. S2f). The higher ID/IG ratio for the Fe-SAC further suggested a higher disorder state induced by the presence of isolated Fe. X-ray photoelectron spectroscopy (XPS) revealed the surface composition for both samples with significant presence of C, N and O and trace signals of S or F (from SF6, employed as a sensitizer). Fe signal was barely detectable for Fe-SAC (Fig. S5 and Table S2). Fitting of the C 1s region revealed the presence of C–N/C–O species at B.E.s of 286.5 eV, O–C
O species at 287.9 eV and π–π* interactions at 290 eV, respectively (Fig. 1g and Fig. S2g). Likewise, the fitting of the N 1s region27 revealed the presence of pyridinic-N (B.E. = 398.3 eV), pyrrolic-N (400.1 eV), quaternary-N (401.5 eV) in both samples, along with the additional appearance of oxidized-N in the Fe-free N-C above 403 eV confirming the presence of N-enriched domains formed by laser pyrolysis (Fig. S1h). The catalytic response of Fe-SAC was evaluated towards the ECO2RR in neutral medium (phosphate buffer solution; pH = 7.4) using Differential Electrochemical Mass Spectrometry (DEMS)28 to simultaneously monitor the faradaic current and the ionic currents associated with the reaction products (see Note S1, Fig. 2 and Fig. S6–S8). Briefly, the experiment was carried out in a three-electrode half-cell where a glassy carbon disk was modified with 20 µL of the catalytic ink and used as working electrode. The amount of ink was set to obtain a metallic load of 0.09 µg of Fe. The electrode was immersed at 0.2 V in a buffer phosphate solution (0.1 M Na2HPO4/0.1 M NaH2PO4·2H2O; pH = 7.5) saturated with CO2 (99.998%). Then, the surface potential was linearly swept towards cathodic values while recording both the faradaic current and the respective ionic currents (see the Experimental methods in the SI for further details). A control experiment in Ar ambient (in absence of CO2) was also carried out for comparison. Fig. 2a shows that the saturation of the electrolyte with CO2 increased the faradaic response during the cathodic polarization (linear sweep voltammetry, LSV) of the catalyst. In particular, the total current at −1.0 V increases from −0.8 mA to −1.5 mA, revealing the existence of an additional process corresponding to the ECO2RR. This aligns well with the works reported by Varela et al.29,30 On the other hand, Fig. 2b and c display the mass spectrometry signals (MSLSVs) corresponding to the evolution of hydrogen (m/z = 2) and formate (m/z = 45), respectively. While linking the m/z = 2 signal with the [H2]+ ion is straightforward, the correspondence of m/z = 45 with the [HCOO]+ fragment from formate was established from the conditions of the experiment. Note S1 and Fig. S6 further explain about the most plausible product distribution and the species ruled out according to DEMS experiments. It is interesting to note that the responses for m/z = 2 were practically identical in the presence and absence of CO2 beyond the onset overpotential (approx. −0.5 V) until −0.8 V, but then the production of H2 was lower for the CO2 saturated solution. This indicates that the hydrogen evolution reaction (HER) is partially blocked during the ECO2RR (Scheme S1). No additional by-products associated with the ECO2RR were identified by DEMS (e.g., methane monitored by the signal m/z = 15, Fig. S7b, or methanol by the mass m/z = 31, Fig. S8d). This is important since it contrasts with the high efficiency towards methane reported for other Fe-based materials.30
At −0.5 V the signal for m/z = 45 started being detected, revealing the formation of formate as the main product of the ECO2RR process (Fig. 2c). Hence, the Fe-SAC: (i) preferentially produces formic acid during the ECO2RR in neutral medium (Scheme S1); and (ii) does not lead to the formation of C2 products. The faradaic efficiencies (FE) towards the HER have been estimated by comparing the ionic currents before and after CO2 saturation of the electrolyte (see Fig. S9). As no other products besides H2 and formate were detected in the potential range between −0.65 and −0.90 V vs. RHE, we assume that the difference between FE for H2 in CO2-saturated conditions is due to the generation of formate. Thus, a FE of ∼57% at −0.90 V have been derived from the experiments. This agrees with the characteristics of SACs materials since each isolated Fe site acts as a center of reaction for the CO2 molecule, sterically avoiding the C–C coupling of two different molecules.18
As shown in Table S3, analogous materials exhibit high selectivity towards the formation of CO due to the preferential adsorption of the CO2 molecule to form the *COOH intermediate. In contrast, the laser pyrolysis method induces the generation of O-based functional groups, promoting instead the *OHCO adsorbate and formate formation (Note S2). As specified in the latter, as well as in Table S3, the selectivity towards formate was linked not only to the material itself, but also to the usage of pH = 5 phosphate buffer as electrolyte for the reaction. Finally, an increase in the signals for m/z = 32 and m/z = 28 was observed but these ionic currents are not related to other products of the ECO2RR (see discussion below). In addition to the formation of formate as the main product of the ECO2RR, DEMS also provided information about the mechanism from the Tafel slopes for H2 production (Fig. 3 and Note S3). Indirectly, the evaluation of HER kinetics can shed light on the performance of the ECO2RR since both reactions compete for the same active sites.31–33 Typically, Tafel slopes are derived from LSV experiments. However, if the polarization response during the experiment does not exclusively arise from the HER, Tafel slope values are overestimated, as can be seen in Fig. 3a, with values that are clearly over the theoretical limit of 120 mV dec−1 (364 and 627 mV dec−1 respectively in the presence and absence of CO2). Instead, we have used the method previously reported by Diaz-Coello et al.,28,34 in which the Tafel slopes are derived for the HER from the m/z = 2 ionic currents recorded during the DEMS experiments. In this method, the linear regression of the slopes was calculated from the onset potential of the reaction (easily readable at the m/z = 2 panel of the DEMS experiment) and extended for 50 – 100 mV of the cathodic scan (if linearity is maintained in this range). Fig. S9 also marks the specific range used in this work, and Note S3 extends the information of the method and theory of the HER mechanism. Fig. 3b shows that this approximation resulted in Tafel slopes inside the range theoretically accepted (from 30 to 120 mV dec−1). In the Ar saturated solution, a Tafel slope of 79 mV dec−1 was obtained, while in the CO2 saturated electrolyte it shifted to 120 mV dec−1. This implies a modification in the kinetics of HER. In the former reaction scenario, both the Volmer and the Heyrovsky reactions are involved in the rate-determining step (RDS) of the whole process.34 Thus, some reaction sites are available to reduce water molecules, while others are kinetically hampered to facilitate the first reduction step of water.32,33 In contrast, when the electrolyte is saturated with CO2, the Tafel slope showed a value of 120 mV dec−1, which implies the Volmer reaction as sole RDS of the process. This behavior suggests that CO2 occupies active surface sites, thereby hindering H adsorption and inhibiting the HER. This is well aligned with the DEMS experiment presented on Fig. 2b, where the generation of H2 significantly decreases. Additionally, the stability of Fe-SAC was studied by chronoamperometry (CA)-DEMS in the potential range of the HER. Fig. 4 shows an experiment carried out by recording the current transients at 0.2 V for 120 s, and then at −1.0 V for 300 s, respectively. Applying the latter potential to the material in the presence of CO2 resulted in higher faradaic currents in comparison with the Ar saturated experiment (Fig. 4a) due to CO2 electroreduction, confirming the results obtained in Fig. 2a. Furthermore, there was a significant inhibition in the formation of H2 (m/z = 2, Fig. 4b) coupled with an enhanced formation of formate (m/z = 45, Fig. 4d) under CO2 saturated conditions. This was also in agreement with the results presented in Fig. 2b and c. However, further screening of m/z from 15 to 32 values in DEMS experiments confirmed the sole presence of signals for m/z = 32 (Fig. 4c) and m/z = 28 (Fig. S7c and f) which led us to assign these mass ratios to [N2H4]+ and [N2]+ fragments from the hydrazine molecule, respectively. The formation of hydrazine is obviously not arising from the reduction of CO2, but rather as a product of the Fe center environment degradation, that is, hydrazine is produced from the N atoms anchoring the Fe to the C network. In the absence of CO2, m/z = 32 (Fig. 4c, black line) increased after reaching −1.0 V and then it decreased over time, revealing the loss of active sites for hydrazine production under the applied potential. Remarkably, this process was accompanied by a decrease in the generation of H2 (Fig. 4b, black line), which strengthens the hypothesis of the close correlation between both processes (Scheme S2). While hydrazine may hold certain safety concerns, in this study, our proposed degradation mechanism suggests the transformation of 1 mol of hydrazine per mol of Fe in the material (approx. 1.57 × 10−6 mol of Fe on top of the working electrode). Assuming complete degradation of the material, which was not the case, the amount of hydrazine generated would not reach the safety threshold. Remarkably, the DEMS experiment allowed the detection of this molecule, even at trace levels. Altogether, it seems reasonable that the hydrazine is formed by the hydrogenation of the N atoms in the Fe-based SAC due to the adsorption of H2 at the Fe active centers (Scheme S2). However, this reaction was almost suppressed in the presence of dissolved CO2 (Fig. 4c, red line) and the H adsorption step on the active site became the slowest process, and became impeded (Fig. 4b, red line), thereby increasing the stability and enabling the use of Fe-SAC for the ECO2RR. To validate the specific influence of Fe to direct the selectivity towards hydrazine, we performed a control experiment with the Fe-free NCs (Fig. S10). This experiment was key to evaluate the behavior of the target material since no increase was found in m/z = 32 or 45 for the Fe-free carbon support. This demonstrated: (i) the catalytic activity of the metallic centers in the formation of formate; and (ii) the lack of formation of hydrazine in the absence of Fe. In both cases, the role of the Fe as reaction center was corroborated. This also confirmed that the active sites of the electrocatalyst are protected during the ECO2RR. The stability towards the CO2 reaction has also been tested (Fig. S11). The results show good stability under operating conditions for 1 hour with constant hydrogen and formate production. Remarkably, the same experiment in absence of CO2 resulted in loss of activity caused by the degradation of the metallic center to form hydrazine after 45 min of applied potential (Fig. S11c). This confirms both the intrinsic stability of the material for the ECO2RR reaction as well as the proposed mechanism for the degradation of the Fe center. In addition, the FE of the products have been calculated in this chronoamperometric experiment, showing approximately the same values as the polarization experiments in Fig. S9, corroborating the previous result. Summarizing, this work demonstrates the active role of Fe-SAC synthesized by laser pyrolysis to selectively electro-generate formate from CO2 thereby paving the way towards the design of novel electrocatalysts based on Fe-SAC.
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| Fig. 3 Tafel plots derived from (a) faradaic currents and (b) m/z = 2 ionic currents recorded for Fe-SAC during the DEMS experiment shown in Fig. 2. | ||
Footnote |
| † Equal contribution. |
| This journal is © The Royal Society of Chemistry 2026 |