Electrochemical
in situ ATR-FTIR at different potential, was used on BiAg-600, Bi-600 and Ag-600 and the results were reported in
Fig. 4 and Fig. S15 (Supporting information). A list of IR band assignments can be found in Table S3 (Supporting information), and detailed explanations are provided in Note S3 and Fig. S16 (Supporting information). Bridge bonded CO species (*CO
B) are considered as a crucial intermediate in the formation of CO during CO
2 reduction [
29]. In the IR spectra, this intermediate was exclusively detected on Ag-600, explaining its high selectivity towards CO compared to Bi-based catalysts (Fig. S7d). Linear-bonded CO species (*CO
L) were observed on the surface of all catalysts, although the band intensity of *CO
L was significantly lower for Bi-600, indicating the important role of Ag in its formation on the BiAg-600 catalyst. Notably, the IR band of *CO
L on BiAg-600 exhibited a blue shift of approximately 11 cm
−1 compared to Bi-600, which can be attributed to the presence of Ag. This shift indicates a downshift of the d-band of Bi upon the introduction of Ag [
30]. Besides, the high band intensity of the *OCHO species observed on Bi-based catalysts explained their high
FEformate. Moreover, the band intensity of *OCHO
− in the BiAg-600 was the highest and could be associated with the high selectivity of this catalyst toward formate formation. It is worth noting that the presence of *OCHO
− and *CO
L species was also observed in the spectra of BiAg-600 under Ar (Fig. S17 in Supporting information). This, suggests that HCO
3− from the electrolyte may play a role in the formation of formate and CO during the
eCO
2RR process. Furthermore, the fact that HCO
3*
− was only present in the spectra of Ag-600 and BiAg-600 indicated that the HCO
3− species tended to only adsorb onto Ag sites. This could be closely related to the higher
eCO
2RR activity against formate formation observed on BiAg-600 compared to Bi-600. A linear relationship was established between the partial current density of formate and the concentration of HCO
3−. The fitting results yielded a quasi-one-order relationship with a coefficient of 0.76 (Fig. S18 in Supporting information). This result confirmed the direct participation of HCO
3− in the formate formation pathway [
31]. Isotopic labeling was used to clarify the nature of the protons involved during the reaction. Deuterium oxide (D
2O) was firstly employed in a CO
2 saturated solution of D
2O + 0.5 mol/L KHCO
3, where H-formate and D-formate could be produced according to the source of protons.
1H NMR revealed that less than 5% of the protons from HCO
3− were involved in the formate formation in the potential range of −0.55 V to −1.3 V (assuming no protons transfer between D
2O and KHCO
3) [
8]. These findings indicates that the protons involved in the hydrogenation of OCO* species were primarily derived from H
2O activation. Thus, it was assumed that HCO
3− acted more as a carbon source for formate rather than solely serving as a pH buffer. To validate this assumption, two control tests were conducted. Firstly, constant-potential tests were performed on BiAg-600 and Bi-600 in a CO
2 saturated phosphate buffer (0.5 mol/L, pH 7) with HCO
3− concentrations, C(HCO
3−), below 0.14 mol/L. The obtained
FEformate was significantly lower compared to that in the CO
2 saturated KHCO
3 solution (Fig. S19 and Note S4 in Supporting information), especially at high overpotential (
η). Secondly, constant-potential electrolysis experiments were carried out in an Ar-saturated KHCO
3 solution at −0.8 V. Under these conditions, a non-negligible amount of formate was detected, corresponding to 38.7% and 18.7%
FEformate for BiAg-600 and Bi-600, respectively. These data confirmed that HCO
3− adsorbed on Ag sites participate directly in formate generation and promote
FEformate in a broad potential window. It should be noted that there were no peak related to HCO
3− or CO
32− species on the BiAg-600 IR spectra under Ar- (Fig. S17). This indicates that the signals of HCO
3*
− and CO
3*
2− on Ag sites were attributed to the presence of molecular CO
2, as described by Eq. 1. It can be inferred that HCO
3− species behaves as a mediator for the transfer of CO
2 from the electrolyte to the catalyst's surface, following Eqs. 1–3. The appearance of the CO
32− band near 1396 cm
−1 only in the spectra of BiAg-600 suggests that the local pH near the surface of BiAg-600 was higher compared to Bi-600 [
7]. This is because CO
32− is formed through the dehydrogenation of HCO
3− in response to the local pH increase near the electrode's surface, as described by Eq. 4 [
32]. Based on the combined findings from ATR-FTIR and isotopic labeling experiments, we propose that CO
2 reacts with water to form HCO
3−. Simultaneously, Ag sites adsorb HCO
3− species and releases CO
2 through a rapid equilibrium (Eqs. 2 and 3), resulting in a high local concentration of CO
2 and an increase in the local pH (Eq. 5) near the Bi sites.