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. 2017 Jul 1;8(7):4779-4794.
doi: 10.1039/c7sc01239j. Epub 2017 May 5.

Design of template-stabilized active and earth-abundant oxygen evolution catalysts in acid

Affiliations

Design of template-stabilized active and earth-abundant oxygen evolution catalysts in acid

Michael Huynh et al. Chem Sci. .

Abstract

Oxygen evolution reaction (OER) catalysts that are earth-abundant and are active and stable in acid are unknown. Active catalysts derived from Co and Ni oxides dissolve at low pH, whereas acid stable systems such as Mn oxides (MnO x ) display poor OER activity. We now demonstrate a rational approach for the design of earth-abundant catalysts that are stable and active in acid by treating activity and stability as decoupled elements of mixed metal oxides. Manganese serves as a stabilizing structural element for catalytically active Co centers in CoMnO x films. In acidic solutions (pH 2.5), CoMnO x exhibits the OER activity of electrodeposited Co oxide (CoO x ) with a Tafel slope of 70-80 mV per decade while also retaining the long-term acid stability of MnO x films for OER at 0.1 mA cm-2. Driving OER at greater current densities in this system is not viable because at high anodic potentials, Mn oxides convert to and dissolve as permanganate. However, by exploiting the decoupled design of the catalyst, the stabilizing structural element may be optimized independently of the Co active sites. By screening potential-pH diagrams, we replaced Mn with Pb to prepare CoFePbO x films that maintained the high OER activity of CoO x at pH 2.5 while exhibiting long-term acid stability at higher current densities (at 1 mA cm-2 for over 50 h at pH 2.0). Under these acidic conditions, CoFePbO x exhibits OER activity that approaches noble metal oxides, thus establishing the viability of decoupling functionality in mixed metal catalysts for designing active, acid-stable, and earth-abundant OER catalysts.

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Figures

Fig. 1
Fig. 1. Tafel plots of oxygen evolution for unary metal oxides in 0.10 M Pi and 1.0 M KNO3 at (a) pH 7.0 and (b) pH 2.5 of CoOx (red , 60 and 82 mV per decade Tafel slope at pH 7.0 and 2.5, respectively), NiOx (light magenta , 90 mV per decade at pH 7.0), FeOx (orange , 45 and 51 mV per decade at pH 7.0 and 2.5, respectively), MnOx (blue , 125 and 650 mV per decade at pH 7.0 and 2.5), PbOx (brown , 130 and 121 mV per decade at pH 7.0 and 2.5), and IrOx (purple , 41 and 32 mV per decade at pH 7.0 and 2.5).
Fig. 2
Fig. 2. Cyclic voltammograms (CVs) of a 1 cm2 FTO electrode at 50 mV s–1 in 50 mM MePi buffer at pH 8.0 with 0.25 mM of each metal: (a) Co2+ and Mn2+ (red ); and (b) Co2+ and Pb2+ (light green ) with addition of Fe2+ (dark green ). Background CV of metal-free MePi buffer (grey ) included for comparison.
Fig. 3
Fig. 3. Tafel plots of oxygen evolution for CoMnOx in 0.10 M Pi and 1.0 M KNO3 at (a) pH 7.0 and (b) pH 2.5 of: CoMnOx deposited at 0.90 (dark green , 65 and 81 mV per decade at pH 7.0 and 2.5), 0.65 (light green , 85 mV per decade at pH 2.5), and 1.15 V (cyan , 83 mV per decade at pH 2.5). Unary metal oxides provided for comparison with slopes defined in Fig. 1, CoOx (red ), MnOx (blue ), and IrOx (purple ).
Fig. 4
Fig. 4. Tafel plots of oxygen evolution in 0.10 M Pi and 1.0 M KNO3 at (a) pH 7.0 and (b) pH 2.5 for CoPbOx (light green , ∼72 mV per decade at both pH 7.0 and 2.5) and CoFePbOx (dark green , ∼70 mV per decade at both pH 7.0 and 2.5). CoFeOx (orange , ∼70 mV per decade at both pH 7.0 and 2.5) and unary metal oxides are provided for comparison with slopes defined in Fig. 1, CoOx (red ), PbOx (brown ), and IrOx (purple ).
Fig. 5
Fig. 5. Electrochemical stability for acidic OER measured by sustained chronoamperometry at: (a) 0.1 mA cm–2 in pH 2.5 Pi for CoMnOx deposited at 0.65 (light green ), 0.90 (dark green ), and 1.15 V (cyan ) along with CoOx (red ), NiOx (light magenta ), MnOx (blue ), IrOx (purple ), and FTO (grey ) for comparison; (b) 1.0 mA cm–2 in pH 2.5 Pi for CoPbOx (light green ) and CoFePbOx (dark green ) with CoFeOx (orange ), CoOx (red ), and PbOx (brown ) for comparison; and (c) 1.0 mA cm–2 in pH 2.0 sulfate for CoFePbOx (dark green ). The inflection of potential in the plots indicates film dissolution.
Fig. 6
Fig. 6. FESEM images of CoMnOx electrodeposited at (a) 0.65, (b) 0.90, and (c) 1.15 V with (d) CoOx and (e) MnOx for comparison. All samples were prepared on FTO substrate, and scale bars are 200 nm.
Fig. 7
Fig. 7. FESEM images of (a) CoPbOx and (b) CoFePbOx with (c) PbOx and (d) FTO for comparison. All samples were electro-deposited on FTO, and scale bars are 100 nm.
Fig. 8
Fig. 8. EDS elemental maps recorded through SEM of (a) CoMnOx (deposited at 0.90 V) and (b) CoFePbOx. Individual elemental channels for Co (red), Mn (blue), Fe (orange), and Pb (green) were combined and overlaid on the respective SEM image. All samples were prepared on FTO substrate, and scale bars are 200 nm for CoMnOx and 100 nm for CoFePbOx.
Fig. 9
Fig. 9. High-resolution EDS elemental maps recorded through STEM of (a) CoMnOx (deposited at 0.90 V) and (b) CoFePbOx. Individual elemental channels for Co (red), Mn (blue), Fe (orange), and Pb (green) were combined and overlaid on the respective image. Scale bars are 15 nm for a resolution of 7.4 Å per px.
Fig. 10
Fig. 10. High-resolution XPS spectra in the (a) Co 2p and (b) Mn 2p regions for: CoMnOx (deposited at 0.90 V, dark green ) compared to CoOx (red ), and MnOx (blue ). Grey dotted lines are presented as guides.
Fig. 11
Fig. 11. High-resolution XPS spectra in the (a) Co 2p and (b) Pb 4f regions for: CoPbOx (light green ) and CoFePbOx (dark green ) compared to CoOx (red ), and PbOx (brown ). Grey dotted lines are presented as guides.
Fig. 12
Fig. 12. Progression of designing an active, stable, and earth-abundant acidic OER catalyst. The first generation system focused on demonstrating film stability at low pH with MnOx., The activity of MnOx was improved in the second generation by activating MnOx for OER. The catalyst was reformulated as a mixed metal oxide for the third generation, where functionality was separated into catalytic and structural elements comprising Co and Mn, respectively. Finally, the degradation of Mn oxides at high anodic potentials was solved by replacing it with a FePb oxide structural component to create the fourth-generation catalyst.
Fig. 13
Fig. 13. Process for independently optimizing the structural component of mixed metal films to discover a metal oxide that is both stable at high anodic potentials and at acidic pH. Pourbaix diagrams of metals (shown as simplified representations of stability and corrosion, generated from the Materials Project and experimental data) were analysed for stability in the top left region of the plots (corresponding to high anodic potentials and low pH). The candidates were then filtered by removing precious and rare metals; then further refined by excluding oxides that were incompatible with anodic electrodeposition in buffer. In this manner, Pb was identified as a promising replacement for Mn for stabilizing OER catalysts in acid.

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