| Literature DB >> 33410273 |
Konrad Ehelebe1,2, Julius Knöppel1,2, Markus Bierling1,2, Britta Mayerhöfer1,2, Thomas Böhm1,2, Nadiia Kulyk1, Simon Thiele1,2, Karl J J Mayrhofer1,2, Serhiy Cherevko1.
Abstract
Pt dissolution has already been intensively studied in aqueous model systems and many mechanistic insights have been gained. Nevertheless, transfer of new knowledge to real-world fuel cell systems is still a significant challenge. To close this gap, we present a novel in situ method combining a gas diffusion electrode (GDE) half-cell with inductively coupled plasma mass spectrometry (ICP-MS). With this setup, Pt dissolution in realistic catalyst layers and the transport of dissolved Pt species through Nafion membranes were evaluated directly. We observed that 1) specific Pt dissolution increased significantly with decreasing Pt loading, 2) in comparison to experiments on aqueous model systems with flow cells, the measured dissolution in GDE experiments was considerably lower, and 3) by adding a membrane onto the catalyst layer, Pt dissolution was reduced even further. All these phenomena are attributed to the varying mass transport conditions of dissolved Pt species, influencing re-deposition and equilibrium potential.Entities:
Keywords: Nafion; Pt dissolution; catalyst degradation; electrochemistry; gas diffusion electrodes
Year: 2021 PMID: 33410273 PMCID: PMC8048487 DOI: 10.1002/anie.202014711
Source DB: PubMed Journal: Angew Chem Int Ed Engl ISSN: 1433-7851 Impact factor: 15.336
Figure 1Scheme of the novel gas diffusion electrode (GDE) half‐cell setup coupled to an inductively coupled plasma mass spectrometer (ICP‐MS) used in the current work to detect catalyst dissolution.
Figure 2Pt dissolution measured via gas diffusion electrode setup coupled to an inductively coupled plasma mass spectrometer (GDE‐ICP‐MS) in 0.1 M HClO4. A–C) Pt dissolution profiles from Pt/C gas diffusion electrodes (HiSPEC 4000 on Freudenberg H23C8) with different loadings. A) Whole protocol, B) slow cycling at 10 mV s−1 between 0.1 and 1.5 V vs. RHE, C) fast cycling at 200 mV s−1 in the same potential range. D–F) Quantitative results for the Pt dissolution, respectively (E and F normalized per cycle). G) Qualitative comparison of 10 mV s−1 CVs before and after degradation cycles. H) Cross‐sectional scanning electron microscope (SEM) images of the corresponding GDEs with different loadings.
Figure 3Pt dissolution measured via gas diffusion electrode setup coupled to an inductively coupled plasma mass spectrometer (GDE‐ICP‐MS) in 0.1 M HClO4. A–C) Pt dissolution profiles from Pt/C gas diffusion electrodes (0.12 mgPt cm−2, HiSPEC 4000 on Freudenberg H23C8) without membrane (blue) compared to similar samples with hot‐pressed Nafion membranes of two different thicknesses (yellow: NR‐211, 25.4 μm; orange: NR‐212, 50.8 μm). A) Whole protocol, B) slow cycling at 10 mV s−1 between 0.1 and 1.5 V vs. RHE, C) fast cycling at 200 mV s−1 in the same potential range. D–F) Quantitative results for the Pt dissolution, respectively (E and F normalized per cycle). G) Qualitative comparison of the first CV with 10 mV s−1. H) Comparison of peak tailing with potentiostatic hold, I) cross‐sectional scanning electron microscope (SEM) images of the corresponding GDEs with different membrane thickness.
Figure 4Membrane‐induced time‐shift of the dissolution response on reductive step (1.5 to 0.1 V vs. RHE) measured in scanning flow cell (SFC) (red) and GDE‐ICP‐MS (blue) in comparison to the modeled time delay for two different values of D in m2 s−1 (gray).
Comparison of different diffusion coefficients stated in literature.
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|
Method |
Comments on the method |
Reference |
|---|---|---|---|
|
0.18 |
Experimental |
Permeation experiments with PtCl6 2− in Nafion 117 |
Kang 1999 |
|
10 |
Theoretical |
Assumed arbitrarily to be a factor of 10 lower than in water |
Darling 2005 |
|
8 |
Theoretical |
Mobility of Pt2+ in the ionomer derived from calculation, based on the Pt‐ion mobility in water and the volume fraction of ionomer etc. |
Ferreira 2005 |
|
0.015 |
Theoretical |
Model first run with assumed value from ref. 24 but did adjust to match experimental degradation data. |
Bi 2008 |
|
7 |
Theoretical |
Assumption diffusion coefficient is the same for all doubly ionized aqueous metal cations:
|
Holby 2012 |
|
0.1 |
Theoretical |
Value calibrated to their model using experimental data with Nafion NR‐212 membrane. |
Barrici 2018 |
|
4 |
Experimental |
Measured via online ICP‐MS |
This work |
Figure 5Comparison of Pt dissolution in GDE (this work) and model system (scanning flow cell (SFC), data extracted from [6c, 11]). The difference in Pt dissolution can be explained by the varying mass transport in model systems (RDE, SFC) with flooded catalyst layer (top) and realistic catalyst layers (GDE, MEA, bottom).