Edward F.
Holby
a,
Wenchao
Sheng
b,
Yang
Shao-Horn
*c and
Dane
Morgan
*d
aUniversity of Wisconsin, Materials Science Program, 1509 University Ave., Madison, WI 53706. E-mail: holby@wisc.edu
bMassachusetts Institute of Technology, Department of Chemistry, Electrochemical Energy Laboratory, 77 Mass Ave., Cambridge, MA 02139. E-mail: wsheng@mit.edu
cDepartments of Mechanical Engineering and Materials Science and Engineering, Electrochemical Energy Laboratory, 77 Mass Ave., Cambridge, MA 02139. E-mail: shaohorn@mit.edu
dUniversity of Wisconsin, Materials Science and Engineering, 1509 University Ave., Madison, WI 53706. E-mail: ddmorgan@wisc.edu; Tel: +1 608 265 5879
First published on 20th April 2009
This work demonstrates the essential role of particle size and crossover hydrogen on the degradation of platinum polymer electrolyte membrane fuel cell (PEMFC) cathodes. One of the major barriers to implementation of practical PEMFCs is the degradation of the cathode catalyst under operating conditions. This work combines both experimental and theoretical techniques to develop a validated and thermodynamically consistent kinetic model for the coupling of degradation and the catalyst particle size distribution. Our model demonstrates that, due to rapid changes in the Gibbs–Thomson energy, particle size effects dominate degradation for ∼2 nm particles but play almost no role for ∼5 nm particles. This result can help guide synthesis of more stable distributions. We also identify the effect of hydrogen molecules that cross over from the anode, demonstrating that in the presence of this crossover hydrogen surface area loss is greatly enhanced. We demonstrate that crossover hydrogen changes the surface area loss mechanism from coarsening to platinum loss through dissolution and precipitation off of the carbon support.
Broader contextPolymer electrolyte membrane fuel cells (PEMFCs) are a promising technology for replacing internal combustion engines. Such a change could lead to higher energy efficiencies as well as a decrease in environmentally hazardous emissions from transportation. Platinum nanoparticles supported on carbon are used in PEMFC cathodes to provide a large catalytic surface area for the oxygen reduction reaction. However, cathode catalyst surface area loss under PEMFC operating conditions leads to a loss of fuel cell efficiency, eventually limiting PEMFC lifetime.1,30 Unfortunately, the dominant mechanisms and driving forces for the degradation are not established.3 We use an experimentally validated electrochemical model to demonstrate that surface area loss can be dramatically reduced by increasing nanoparticle sizes to just 4–5 nm. We also show that the presence of crossover hydrogen from the anode plays a crucial role in catalyst degradation, both enhancing surface area loss and changing the dominant loss mechanism. This effect must be considered to accurately extrapolate from ex-situ experimental data to real fuel cells. These findings will help direct the creation of more durable PEMFC cathodes. |
Understanding the size dependence of the dissolution rate is essential for understanding how the PSD affects surface area loss, since Pt dissolution is at the root of both off-support deposition and coarsening. The Gibbs–Thomson (or Kelvin) equation yields an estimate5 for the size dependence of particle stability, and is generally written as a shift in particle chemical potential:
![]() | (1) |
Here d is the particle diameter, γ is the particle surface energy, and Ω is the molar volume of the particle. The Gibbs–Thomson energy (EGT) for Pt (based on values given in Table 1) is 0.18 eV/atom at d = 5 nm, and as large as 0.91 eV/atom by d = 1 nm. If we assume that dissolution is dominated by terms exponential in the particle stability (dissolution rate proportional to exp((1 − β1)EGT/kT), where β1 the transfer coefficient6 with a value of 0.5) then this increase in EGT equates to an increase vs. bulk in the dissolution rate by 1 order of magnitude for a 5 nm particle, 3 orders of magnitude for a 2 nm particle and 6 orders of magnitude for a 1 nm particle. The impact of Gibbs–Thomson on the stability is therefore far more important for particles below 5 nm than above it, and by 2 nm provides a powerful driving force for dissolution and coarsening. The size dependence of dissolution rates shows that the PSD should play an important role in both mass loss and coarsening mechanisms of surface area loss, particularly for particles in the commercially relevant range of a few nanometers.
Symbol | Value | Units | Reference | Description |
---|---|---|---|---|
1 These values are taken as zero in the model for the given values of ν1 and ν2 but may not actually be zero physically. The S′i have been renormalized into the values of ν1 and ν2, i.e., ν1 is actually ν1exp[(![]() ![]() ![]() |
||||
ν | 1 × 1012 | Hz. | Assumed | Dissolution attempt frequency |
![]() |
1.02 × 105 | J mole−1 | Fit | Partial molar dissolution activation enthalpy (cycling) |
1.18 × 105 | J mole−1 | Fit | Partial molar dissolution activation enthalpy (potentiostatic) | |
T | 353 | K | Experiment | Temperature |
Γ | 2.2 × 10−9 | mole cm−2 | Ref. 12 | Pt surface site density |
n 1 | 2 | Assumed | Electrons transferred during dissolution | |
β 1 | 0.5 | Assumed | Butler–Volmer transfer coefficient for dissolution | |
U eq | 1.188 | V | Ref. 19 | Dissolution bulk equilibrium voltage |
Ω Pt | 9.09 | cm3 mole−1 | Ref. 12 | Molar volume of Pt |
c Pt2+,Ref | 1.3 × 10−2 | mole cm−3 | Fit | Reference Pt2+ ion concentration |
γ Pt | 2.4 × 10−4 | J cm−2 | Ref. 12 | Pt [111] surface energy |
ν 1 | 1 × 104 | Hz. | Fit | Forward oxide formation rate constant |
ν 2 | 2 × 10−2 | Hz. | Fit | Reverse oxide formation rate constant |
pH | 0 | Assumed | System pH | |
n 2 | 2 | Assumed | Electrons transferred during oxide formation | |
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1.2 × 104 | J mole−1 | Fit | Partial molar oxide formation activation enthalpy (zero coverage) |
U fit | 1.03 | V | Fit | Oxide formation bulk equilibrium voltage |
ω | 5.0 × 104 | J mole−1 | Fit | Oxide-oxide interaction energy |
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01 | J K−1 mole−1 | Assumed | Non-vibrational water partial molar entropy |
![]() ![]() |
01 | J K−1 mole−1 | Assumed | Difference of activation state and water partial molar entropies (non-vibrational) |
λ | 2.0 × 104 | J mole−1 | Fit | Oxide dependent kinetic barrier constant |
β 2 | 0.5 | Assumed | Butler–Volmer transfer coefficient for oxide formation |
A number of researchers have tried experimentally to establish the role of the PSD in surface area loss, and specifically in driving mass loss and coarsening mechanisms.1,4,7–10 However, the contribution of PSD to surface area loss is difficult to determine because surface area loss is potentially influenced by many factors, including temperature, electrochemical potential, presence of hydrogen, Pt loading and dispersion, particle morphology, and carbon support. For example, over 40 years ago Kinoshita, et al.10 demonstrated that the surface area loss with potential cycling was much faster for Pt nanoparticles on carbon than unsupported Pt black (with micron particle sizes). The PSDs of these two catalysts are significantly different, but the additional differences between the catalysts of particle dispersion, support, and morphology makes it impossible to establish the direct impact of the changing PSD on surface area loss. More recently, Makharia, et al.9 showed that increasing the mean diameter of the catalyst nanoparticles could reduce surface area loss, supporting the hypothesis that PSD plays an important role in degradation. However, Makharia, et al. also found that the PSD effect on stability was far more dramatic for a well-dispersed Pt loading whose particles were grown by heat treatment than for an as-received poorly dispersed catalyst. This finding implies that multiple factors contributed to the observed changes in stability, again making it impossible to establish the particular influence of the PSD.
The model is one dimensional along the direction normal to the cathode and mean-field in the plane orthogonal to this direction as shown in Fig. 1. To simulate in-situ experimental conditions the Pt diffuses along the line to the anode, crossover hydrogen is included, and the volume of electrolyte and Pt loading are 10−4 ml and 0.4 mg per cm2 cathode, respectively. To simulate ex-situ experimental conditions the Pt diffuses radially from the cathode, there is no crossover hydrogen, the Pt is mixed by stirring every 200 cycles, and the volume of electrolyte and Pt loading are 130 ml and 0.01 mg per cm2 cathode, respectively (these conditions match those used in the ex-situ experiments performed in this work and discussed).
![]() | ||
Fig. 1 Schematic representation of processes included in the cathode model. |
Dissolution and precipitation of Pt on the support is assumed to be dominated by the process
Ptsolid ↔ Pt2+aqueous + 2e− | (2) |
Alternate pathways for Pt dissolution, through PtO or PtO2, are possible. For PtO, there is no evidence for direct dissolution playing significant role in overall Pt dissolution rate. Recent results from Wang, et al.15 show that PtO passivates the Pt surface and reduces dissolution strongly suggesting that PtO dissolution is not a dominant dissolution pathway. There is some evidence for dissolution of PtO216 but we are modeling voltages generally below the range for PtO2 formation (∼1.2 V)17 and dissolution data from Bindra et al.18 suggests a Pt2+, not Pt4+, aqueous species. We therefore do not include the process of PtO or PtO2 aqueous dissolution, an assumpion consistent with the very low PtO dissolution rates used in previous models.11,12 The electrochemical rate equation for Pt dissolution and precipitation is modeled using a Butler–Volmer6 rate equation with modification for oxide coverage passivation and a size dependent destabilization energy (given by the Gibbs–Thomson energy, Eqn 1). The bare surface energy is taken to be that for Pt [111] and it is modified by oxygen coverage according to absorption thermodynamics. We write our electrochemical rate equation for Pt dissolution and precipitation as
![]() | (3) |
The attempt frequency is assumed to be that of a phonon frequency (1012 Hz). Dissolution rates for potentiostatic simulations are fit to surface area loss curves from Ferreira et. al.,1 while dissolution rates for cycling simulations are fit to the surface area loss curves shown in this paper for the pristine sample (see experimental section). Cycling requires a faster dissolution rate than potentiostatic holds, presumably due to destabilization of the Pt by oxide formation and removal. Butler–Volmer coefficients of 0.5 are assumed. The reference Pt concentration is fit to so that the forward and backward reaction rates balance to reproduce the equilibrium aqueous Pt concentration of Bindra, et al.18 Bulk equilibrium voltage is taken from Pourbaix.19 The effective surface energy can be derived from the Gibbs adsorption equation6 and the oxide model discussed, and is given by
![]() | (4) |
Formation and removal of surface oxide (following the pathway of Eqn 5) is modeled using a Butler–Volmer rate equation allowing up to 2 layers of PtO growth with modifications for oxide–oxide interactions.
Ptsolid + H2O ↔ PtO + 2H+ + 2e− | (5) |
We write the oxide formation/removal rate as
![]() | (6) |
Here ν1 (ν2) is the forward (backward) reaction attempt frequency, ′i is the partial molar entropy of species i with the vibrational degrees of freedom removed,
2,fit is a fitting parameter that represents the activation barrier when the oxide formation reaction is in equilibrium at zero oxide coverage. We assume that this barrier at reaction equilibrium is linearly dependent on fractional coverage, which introduces the term λθ, where λ is a fitting parameter. Deviation from the equilibrium is treated using the Butler–Volmer formalism where β2 is the symmetry factor (assumed here to be 0.5 for all coverages). Ufit is a fitted parameter that sets the equilibrium voltage. An oxide coverage dependent term is included to account for oxide–oxide interactions on the surface that destabilize the products of the reaction. This interaction is assumed to be linear with a fit interaction energy of ω The voltage term is written in the usual electrochemical manner to account for the energy of the n2 (in this case 2) product electrons. The parameters that need to be determined for this model are ν1,
′PtH2O −
′H2O,
2,fit,λ,β,Ufit,ω,ν2,
′PtH2O.These values are fit to cyclic voltammetry data of Jerkiewicz, et al.,17 which includes oxide coverage vs. potential for a range of temperatures and maximum sweep voltage. Fitting is aimed at reproducing the oxide onset voltage, leveling anodic current density value, and cathodic peak thickness, voltage and current density.
Pt transport in the electrolyte is modeled as Fickian diffusion taking into account the electrolyte excluded volume and uses a Pt ion diffusion constant in H2O1. Under in-situ conditions, we include the effect of crossover hydrogen. Crossover hydrogen refers to the H2 from the anode that crosses over to the cathode during fuel cell use.4 It is well established that crossover hydrogen precipitates dissolved Pt out of the electrolyte to form what is called the Pt band.1,20,21 The location of the band is determined by a balance of hydrogen and oxygen partial pressures21–23 and represents a catalytically inactive sink for dissolved Pt in the system. The dissolved Pt2+ is removed from the system by the precipitation reaction
Pt2+(aq) + H2 → Pt(s) + 2H+ | (7) |
A complete model of the Pt band formation requires modeling the H2, and O2 partial pressures and permeabilities in the cathode.22 However, including these terms would add significant complexity to the model and is not the focus of this study. Therefore, we adopt a simplified model for the Pt band that is adequate to capture the role that crossover hydrogen plays in ESA loss. First, we assume the band is perfectly sharp, which is justified by the experimental observation that the band is typically very thin (∼1 µm).1,22 Second, we assume the band is a perfect sink for dissolved Pt2+, i.e., that Eqn 7 is Pt2+ limited. This assumption is justified by the fact that typical H2 crossover rates (∼2 mA cm−2)24 correspond to about 2 × 10−8 mol (cm2-s)−1 of H. This amount of H can easily consume the amount of dissolved Pt. In fact, cathode Pt loadings are typically less than 0.4 mg cm−2, or about 2 × 10−6 mol Pt cm−2, which could only use all the crossover H2 for only about 200 s if the reaction of Eqn 7 were H2 limited. Therefore, it is clear that the reaction will be Pt2+ limited. Finally, the position of the Pt band is taken from experiments and set to 11 µm from the cathode surface.1,22 We find that the results are not sensitive to this position to within a few µm. The mathematical model for the Pt band is therefore a perfect Pt2+ sink boundary condition located at 11 µm.
The coupled dissolution and oxide growth equations are time evolved using a variable order solver based on numerical differentiation formulas (as implemented in the Matlab ® ode15s solver). The PSD is sampled nonuniformly at 700 distinct radii, with 200 radii concentrated in the small particle region of the final distribution for accuracy. When fitting to experimental TEM PSDs the PSD is assumed to have a log-normal functional form (suggested by Granqvist and Buhrman25) and match the overall system loading. When simulating Pt diffusion in the electrolyte at least 200 mesh points were used in the concentration profile and meshing was done more finely close to the cathode surface.
A constant non-PSD dependent surface area loss function is added to all cycling distributions to account for non-PSD loss mechanisms such as carbon corrosion and surface blocking in the cycling experiments. This function is taken as the difference in modeled and observed surface area for HT3 (the sample with the largest particles and therefore smallest PSD driven surface loss). The geometric surface area (GSA, measured by Transmission Electron Microscopy, TEM) and ESA (measured by CVs) are not equal and a rescaling parameter, derived from experimental data (typically ESA/GSA = 0.63), was used to adjust model GSA for comparison to experimental ESA. Reported PSDs are normalized to either one (normalized PSD) or total mass (mass normalized PSD; see ESI†). Particle migration and coalescence (Smoluchowski mechanism26) is not investigated in this study as it does not contribute significantly in the temperature range considered.3
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Fig. 2 (a–d) Normalized particle size distributions before and after 1200 voltage cycles (triangular sweep between 0.6 V and 1.0 V with a sweep rate of 20 mV s−1). (e–h) Surface area vs. cycle number for the 1200 voltage cycles of these distributions. |
To quantify the role of the PSD mean diameter in surface area loss, we simulate a common degradation experiment of a cathode under constant potential. Fig. 3 shows the simulated surface area loss of an in-situ test for four log-normal PSDs with identical variances of 0.27 nm2 and loadings of 0.4 mg cm−2 (typical of commercial catalysts1) but with different mean diameters. The smallest mean diameter distribution (2 nm) has dramatic surface area loss, while there is little change in the surface area for distributions with mean diameters of 4–5 nm. The closed circles show experimental results1 for the smallest PSD, and the good agreement with the model helps validate our simulation. These results demonstrate that surface area loss changes dramatically for mean sizes changing from ∼2–3 nm to ∼4–5 nm, and ESA loss (through both mass loss and coarsening) is almost totally eliminated for the larger particle sizes (given the time and voltage ranges considered).
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Fig. 3 Potentiostatic runs at 0.95 V (a) Initial normalized particle size distributions with mean particle sizes of 2, 3, 4, and 5 nm. All distributions have the same variance (0.27 nm2)1 and mass loading (0.4 mgPt cm−2).1(b) Surface area vs. time for the four distributions. Experimental data is taken from Ferreira et. al.1 |
A detailed examination of the final PSDs of the ex-situ (Fig. 2) and in-situ (Fig. 3) studies demonstrates that the surface area is lost by quite different mechanisms in the two simulations. It is necessary to understand the cause of the differences between the two simulations to understand to what extent researchers can use ex-situ measurements as a guideline for the in-situ degradation in fuel cells. We have identified the primary source of the differences between our in- and ex-situ simulations as due to crossover hydrogen, which is present only during in-situ studies. We here demonstrate that crossover hydrogen plays an essential role in both the magnitude of surface area loss and the mechanism by which it occurs.
In Fig. 4a, shows the simulated surface area loss for a 2 nm mean diameter PSD in the presence of crossover H2, as shown previously in Fig. 3. Fig. 4a,
shows the surface area loss for an identical simulation without crossover H2. The surface area loss at 5000 h is more than 50% greater with hydrogen present. Fig. 4b shows the initial (truncated) PSD and the final PSDs after 5000 h for the simulations with and without crossover hydrogen. With crossover hydrogen, none of the particles increase in size and much of the Pt mass is lost from the cathode, as shown by a decrease in the height of the mass normalized PSD at all diameters. Thus, with crossover hydrogen, the surface area loss and PSD changes are dominated by a mass loss mechanism. However, when there is no crossover hydrogen, smaller particles dissolve, larger particles grow, and very little mass is lost from the PSD (as demonstrated by the shift to the right of the mass normalized PSD and mass measurements that are not shown). Thus, without crossover hydrogen, the surface area loss and PSD changes are dominated by coarsening. The mass loss mechanism is more aggressive, leading to a larger surface area loss compared to that in the absence of crossover hydrogen. Crossover hydrogen not only decreases the ionic Pt concentrations (leading to increased dissolution rates) but increases the Pt mass flow from the particle surface due to an increased concentration gradient, which then leads to an increase in the mass loss mechanism of ESA loss. For more detail on the concentration profiles, see ESI†.
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Fig. 4 (a) Surface area vs. time for distributions with and without crossover hydrogen. Distributions are aged potentiostatically at 0.95 V. (b) Initial (truncated) and aged mass normalized PSDs with and without 2 mA cm−2 H2 crossover from the anode at 11 microns. (c) Mean particle diameter vs. time for these distributions. Experimental surface area data is taken from ref. 1. Conditions are the same as those in Fig. 1 for the 2 nm diameter PSD. |
As shown in Fig. 4c, the mean diameter increases during the simulations with and without hydrogen. In the mass loss dominated case, both small and large particles dissolve, and the increase in mean diameter is due to the relatively faster dissolution rate (and disappearance) of smaller particles compared to larger ones. In the coarsening dominated case, the increase in mean diameter is due to particle growth. These results demonstrate the fact that the observation of increased mean diameter of the PSD alone cannot be used to identify coarsening as a major surface area loss mechanism. This fact is essential to interpreting TEM or Small-Angle X-ray Scattering (SAXS) data, where the increased mean diameters that are commonly seen with aging1,8 cannot be interpreted as coarsening without additional information, e.g., about the mass on the support.
Based on these simulations, we predict that in-situ fuel cell catalysts with crossover hydrogen will suffer more surface area loss and lose surface area differently (through mass loss) than catalysts in ex-situ acid experiments (where coarsening is the observed dominant loss mechanism). While both mass loss and coarsening are driven by the instability of small Pt nanoparticles, the fundamentally different mechanisms underlying surface area loss must be taken into account when considering the implications of ex-situ degradation experiments for real fuel cells.
Footnote |
† Electronic supplementary information (ESI) available: Particle size distribution normalization and concentration profiles. See DOI: 10.1039/b821622n |
This journal is © The Royal Society of Chemistry 2009 |