Operando Fe Dissolution in Fe-N-C Electrocatalysts during Acidic Oxygen Reduction and Impact of Local pH Change

05 February 2024, Version 1

Abstract

Atomic Fe in N-doped C (Fe-N-C) catalysts provide the most promising non-precious metal O2 reduction activity at the cathodes of proton exchange membrane fuel cells. However, one of the biggest remaining challenges to address towards their implementation in fuel cells is their limited durability. Fe demetallation has been suggested as the primary initial degradation mechanism. However, the fate of Fe under different operating conditions varies. Here, we monitor operando Fe dissolution of a highly porous and >50% FeNx electrochemical utilization Fe-N-C catalyst in 0.1 M HClO4, under O2 and Ar at different temperatures, in both flow cell and gas diffusion electrode (GDE) half-cell coupled to inductively coupled plasma mass spectrometry (ICP-MS). By combining these results with pre- and post-mortem analyses, we demonstrate that in the absence of oxygen, Fe cations diffuse away within the liquid phase. Conversely, at -15 mA cm-2geo and more negative O2 reduction currents, the Fe cations reprecipitate as Fe-oxides. We support our conclusions with a microkinetic model, revealing that the local pH in the catalyst layer predominantly accounts for the observed trend. Even at a moderate current density of -15 mA cm-2geo and under O2 at 25 oC, a significant H+ consumption and therefore pH increase (pH = 8-9) within the bulk Fe-N-C layer facilitate precipitation of Fe cations. This work provides a unified view on the Fe degradation mechanism for a model Fe-N-C in both high-throughput flow cell and practical operating GDE conditions, underscoring the crucial role of local pH in regulating the stability of the active sites.

Keywords

Oxygen Reduction
Single Atom
Operando
pH

Supplementary materials

Title
Description
Actions
Title
Supplementary Information - Operando Fe Dissolution in Fe-N-C Electrocatalysts during Acidic Oxygen Reduction and Impact of Local pH Change
Description
Contains synthesis, characterisation and modelling details, and supplementary Figures.
Actions

Comments

Comments are not moderated before they are posted, but they can be removed by the site moderators if they are found to be in contravention of our Commenting Policy [opens in a new tab] - please read this policy before you post. Comments should be used for scholarly discussion of the content in question. You can find more information about how to use the commenting feature here [opens in a new tab] .
This site is protected by reCAPTCHA and the Google Privacy Policy [opens in a new tab] and Terms of Service [opens in a new tab] apply.
Comment number 1, Yu-Cheng Wang: Feb 10, 2024, 06:25

This work holds significant value, and I have diligently read and studied the manuscript. However, I have some questions: 1. The post-TEM analysis of the 20°C-O2-ICPMS samples revealed a large number of suspected Fe oxides, yet no signals were evident in the XRD results. The authors also performed post-XAS analysis, but did they provide R-space data to substantiate the presence of Fe oxides? According to the dissolution data presented in Fig. 4, the Fe dissolution under 20°C-N2 conditions should be substantial, possibly exceeding 20% of the initial Fe content. If this portion of Fe forms Fe oxides under the influence of O2, then XAS should detect corresponding signals. 2. Another intriguing point is that post-TEM analysis of the 75°C-O2-ICPMS samples did not show noticeable nanoparticles. However, if compared with the ICPMS data at 75°C-N2, a significant reduction in Fe dissolution should be observed. Where did the Fe that was supposed to dissolve go? Another puzzling is that the post-TEM analysis at 80°C-O2-ICPMS-0.6V-2h, referenced from Nat. Catal., 2023, 1–11, showed a large number of suspected Fe oxides, which seems different from the observations in this manuscript. 3. Another question concerns the formation process of Fe oxides. If it involves the oxidation of trivalent Fe ions by O2 to form Fe oxides, then a higher current would result in more O2 consumption, leading to a more O2-depleted environment, which is less conducive to the formation of Fe oxides. The conclusion should be that higher currents lead to less formation of Fe oxides, hence more Fe ions would be lost and detected by ICPMS. This is contrary to the manuscript's observations, where higher currents were associated with fewer Fe ions detected by ICPMS. Could you please clarify these points?