Open Access Article
Sol A
Lee
a,
Myeong Je
Jang
a,
Zhiyuan
Qi
a,
Kaiwen
Wang
a,
Ian
Sullivan
a,
Laura
Paradis-Fortin
b,
Dilworth Y.
Parkinson
c,
Walter S.
Drisdell
*b,
Harry A.
Atwater
*a and
Chengxiang
Xiang
*a
aDepartment of Applied Physics and Materials Science, California Institute of Technology, Pasadena, 91125, CA, USA. E-mail: haa@caltech.edu; cxx@caltech.edu
bChemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA. E-mail: wsdrisdell@lbl.gov
cLawrence Berkeley National Laboratory, Berkeley, CA 94720, USA
First published on 13th August 2025
We utilize operando X-ray computed tomography, coupled with real-time electrochemical analysis, to reveal the underlying failure mechanisms of membrane electrode assemblies (MEAs) for electrochemical CO2 reduction (eCO2R). Through operando imaging, we can obtain unprecedented insights into the dynamic behavior of the MEA under different operating conditions, revealing critical changes in interface interactions, phase distribution, and structural integrity over time. Our findings identify phenomena giving rise to the transition from CO2R to the hydrogen evolution reaction (HER), as evidenced by shifts in cathode potential and CO2R selectivity. The formation of inhomogeneous precipitates at the gas diffusion electrode disrupts the CO2 supply and reduces the active sites for eCO2R, resulting in a shift toward H2 production during low current density operation. Additionally, under high current density conditions, rapid water crossover up to the microporous layer/gas diffusion layer promotes the transition from CO2R to HER, further shifting cell potential toward anodic direction. Oscillating voltage conditions reveal the dissolution and regrowth of precipitates, providing direct visualization of the competing selectivity of CO2R and HER. This work offers new insight into the degradation mechanisms of MEAs, with implications for the design of more durable CO2R systems.
Broader contextConverting waste CO2 into value-added fuels and chemicals using renewable electricity is a net-zero carbon emission technology that addresses climate change caused by greenhouse gas emissions. Zero-gap membrane electrode assemblies (MEA) utilizing a gas diffusion electrode are promising electrochemical reactor designs for high-rate CO2 reduction. However, key challenges for MEA operation in electrochemical CO2 reduction (eCO2R) include salt precipitation and flooding at the gas diffusion electrode (GDE), which limit stability. Despite their importance, the failure mechanisms behind these issues are not yet fully understood. We report direct visualization of the dynamic behavior and structural changes of the MEA under various operating conditions, using operando X-ray computed tomography, coupled with real-time electrochemical analysis. This powerful operando analytical approach provides insights into MEA degradation mechanisms, providing guidance for future design strategies to achieve stable CO2R MEA operation. |
The main degradation phenomena are salt precipitation, which blocks the CO2 diffusion channels, and flooding that hinders the CO2 supply and transit CO2R to the hydrogen evolution reaction (HER). eCO2R at high current densities generates hydroxide ions (OH−) at the cathode, raising the local pH near the cathode surface and driving CO2 to react with OH− to form bicarbonates (HCO3−), which further convert into carbonates (CO32−).3,8 Concurrently, potassium ions (K+) from the anode diffuse to the cathode side, where they react with bicarbonates and carbonates to form salts, hindering CO2 supply and lowering eCO2R. In addition, the application of high reduction potential can drag water from the anolyte to the cathode, altering its hydrophobicity, wetting the GDE, and causing flooding.9,10 There have been efforts to mitigate precipitation and flooding through increasing water content and pulse operation (operation/regeneration), operation in acidic electrolytes, and operation at elevated temperatures, leading to enhanced stability.11–17 However, it still requires a deeper understanding of the underlying progress of degradation mechanisms during operation.
While ex situ analysis methods have provided valuable insights into MEA degradation, they primarily capture static snapshots of post-mortem samples.18 To address this gap, monitoring the primary degradation phenomena of MEA has been advanced with in situ/operando techniques.19–23 For example, Moss et al. used operando X-ray diffraction (XRD) to identify the cause of cell performance degradation, demonstrating that salt formation exacerbates electrolyte flooding, leading to selectivity changes under eCO2R conditions.24 Disch et al. employed high-resolution neutron imaging to study salt precipitation and water transport in a zero-gap CO2R cell.25 However, a missing piece remains in the systematic investigation of the intermediate stage for MEA degradation caused by the propagation of precipitation, flooding, and mechanical deformation within the GDE under operating conditions. Studies have monitored the backside of the GDE or in the gas flow channels, and although some of the measurements can provide detailed chemical information, they cannot reveal the morphological changes within the GDE. X-ray tomography offers a promising approach for studying electrochemical cell dynamics by enabling non-destructive observation of solid/liquid/gas interfaces, 3D voids, defects, and phase distribution.26–28 These capabilities motivate the investigation of the predominant failure mechanisms of eCO2R cells by tracking structural phase changes over time under various conditions.
In this work, we employ operando synchrotron X-ray tomographic imaging combined with real-time electrochemical measurement to link the microscopic morphological changes in Cu GDE with their degradation behavior. We correlate variations in electrochemical performance (e.g., voltage and selectivity) with observed precipitation and flooding phenomena at the MEA, revealing the predominant failure mechanisms under different operating conditions. Our findings provide direct observations of the transition from CO2R to HER, driven by shifts in cathode potential and CO2R selectivity. We first visualize inhomogeneous precipitates at the Cu/membrane interface, which block the CO2 supply and reduce the number of active sites, leading to increased H2 production. Oscillating voltage conditions enable us to visualize the dissolution and regrowth of precipitates, highlighting the competing dynamics between CO2R and HER. Lastly, at high current densities, we track predominant water crossover and subsequent salt precipitation at the microporous layer (MPL)/gas diffusion layer (GDL) interface, which accelerates the transition from CO2R to HER. By identifying key failure pathways, our study provides insights that can guide the design of more durable MEAs, ultimately improving the viability of eCO2R for large-scale carbon utilization.
The GDE used in this study featured hydrophobic MPL to prevent rapid electrolyte flooding, a common design in large-scale MEA for eCO2R.29 The 300 nm-thick Cu catalyst layer was observed as a thin white layer that overlaps with the AEM and MPL in the 2D slice. The components of the MEA are shown in Fig. S2a (SI). Scanning electron microscope (SEM) images (see Fig. 1c) reveal the surface morphology of carbon paper, which features randomly distributed trenches, and the particle-shaped Cu catalysts formed on carbon paper (Fig. S2b, SI). Before performing the electrochemical measurement, cross-sectional micro-CT images of the pristine MEA without flowing electrolytes were taken (marked by the blue dotted line in Fig. S2c, SI) to confirm the initial microstructural features of the MEA. Distinguishable components were observed in the cross-sectional micro-CT images: the GDL exhibited a porous microstructure, the MPL showed a relatively uniform intensity, the Cu layer appeared as a bright, thin layer, and both the AEM and spacer had a uniform contrast distribution. As shown in Fig. 1d, the trenches in the MPL appear as darker intensity holes, which match the top-view SEM image (Fig. 1c).
We then compared the behavior of Cu GDE at higher operating current density, where Cu catalysts can promote the conversion of CO2 to C2 products (see Fig. S5, SI). Ethylene selectivity was observed at an operating current density of −100 mA cm−2, with an approximate 10% ethylene selectivity. The total faradaic efficiency (FE) remained below 100%, which could be attributed to the exclusion of liquid products in the FE calculation. Some liquid products might have diffused to the anode side and undergone oxidation. The Cu GDE showed the oscillating voltage profile and subsequent FE fluctuations after 7 hours of operation. When the MEA was operated at high-concentration (0.5 M, 1 M) KHCO3 electrolytes, the Cu GDE showed an increase in H2 selectivity with voltage oscillation or complete H2 evolution (see Fig. S6, SI).
We investigated the interface dynamics and morphological change of the MEA under conditions where the Cu GDE exhibits high ethylene selectivity. As shown in Fig. 2a, a shift in selectivity was observed over 1 hour of operation, with an increase in H2 selectivity and a decrease in CO2R activity. To track the structural change and interface dynamics, we obtained visualized interior images of the MEA at 0.2 h intervals. As shown in Fig. 2b, a white, particle-shaped structure was identified at the 2D micro-CT image showing MPL/Cu/membrane interface. Inhomogeneous precipitate formation, distribution, and growth were observed over time. The extent of precipitate growth reached the MPL during operation, as confirmed by comparing the MPL, GDL/MPL and GDL region (see Fig. S7, SI) and analyzing the cross-sectional micro-CT images (Fig. S8, SI). Notably, precipitation led to mechanical deformation of the Cu/membrane interface, a phenomenon observed for the first time in this study.
We found noticeable evidence of interface dynamics and phase distribution changes during the oscillatory period. As the voltage shifted anodically, C2H4 selectivity slightly increased (see Fig. 3a). Prior to the voltage fluctuation (point 1), a significant number of precipitates were distributed at the MPL/Cu (Fig. 3b). To track the changes in precipitation over time, we performed segmentation on the region marked by a cyan box in Fig. 3b, using 2D slices at the same height and position of the Cu GDE. At the beginning of the transient period (point 2), the FE remained stable, while the segmentation image revealed the partial dissolution of the precipitates (Fig. 3c). When the MEA entered the anodically shifted potential region (point 3), a decrease in H2 and CO selectivity, alongside an increase in C2H4 selectivity, was observed, followed by significant dissolution of the salt precipitates.
Cross-sectional micro-CT images (see Fig. 3d) illustrate the extent to which precipitates grow from the Cu/membrane interface to the GDL. The cross-sectional image was taken from the position marked by the green line in Fig. 3b. At point 2, a solution signal was detected in the gap between the Cu GDE and the membrane, accompanied by a reduced contrast of precipitates near the Cu/membrane interface, indicating partial dissolution. Further hollow structures of precipitates were observed at point 3, likely due to significant water crossover. From the observed morphological changes in the precipitates, it can be inferred that water did not reach the GDL, resulting in relatively stable H2 selectivity. After water crossover, the Cu GDE exhibited an increase in active sites for eCO2R due to the removal of precipitates at the MPL and membrane/Cu interface, resulting in a voltage drop and a shift from HER to CO2R, with an increase in CO selectivity. As the reaction continued, regrowth of the precipitates gradually filled the hollow spaces. Furthermore, by comparing the images at points 1 and 5, we observed that the precipitation eventually reached the GDL. 3D micro-CT images (see Fig. 3e) further support the precipitation, dissolution, and regrowth within the GDE, with varying density and distribution of precipitates.
The MEA exhibited repeating oscillatory behavior over 7 hours of operation (see Fig. S11, SI). A comparison of cell potentials at the beginning of the measurement (0 h) and after 6 hours revealed anodic potential shifts of 0.3–0.4 V. As shown in Fig. S11b (SI), a significant accumulation of precipitates was observed at the MPL/GDL, though some precipitates were dissolved during the oscillatory period. Notably, the 2D images confirmed the dissolution of precipitates at the MPL/GDL, implying that water had reached this region. The invasion of water into the GDL can alter the hydrophobic nature of the GDE to hydrophilic, which in turn may trigger a shift from eCO2R to HER. The salt precipitates formed on Cu GDE were K2CO3 and KHCO3 (see Fig. S12, SI).
The voltage oscillation mainly originates from the cathode, as confirmed by the constant anode potential profile in Fig. S13 (SI), regardless of the presence of the spacer. Furthermore, under voltage oscillation, the mass flow from the outlet of the MEA followed the voltage oscillation and FE fluctuations, indicating that the pressure in the Cu GDE changes during operation (see Fig. S14, SI). The mass flow variation that can be induced by the gas chromatography measurements did not affect the oscillating behavior of the Cu GDE. The variations in pressure within the MEA can be attributed to the complete degradation of the Cu GDE. We further investigated the effects of electrolyte pH and temperature on the electrochemical performance of Cu GDE. In the case of the MEA operated at 0.1 M KHCO3, a common trend across different current densities (100–200 mA cm−2) was the increase in voltage, followed by a drastic voltage drop, accompanied by changes in CO2R selectivity that corresponded to the voltage change. The magnitude of the voltage changes increased as repetitive voltage oscillation occurred. At a concentration of 1 M KOH (see Fig. S15, SI), the Cu GDE exhibited similar voltage oscillations, with a gradual increase in voltage change and a corresponding shift in selectivity. The main difference between the operation in 0.1 M KHCO3 and 1 M KOH was the extent of operational time to reach the complete transition from CO2R to HER. This observation is consistent with other studies reporting on the electrolyte concentration-dependent degradation behaviors of GDE. For example, Cofell et al. demonstrated that increasing the alkaline electrolyte concentration can result in increased salt precipitation and accelerating flooding.20 El-Nagar et al. demonstrated that the K+ concentration is a key parameter for K+ crossing the membrane, influencing the selectivity of GDE with a current density dependency.36 We also confirmed that elevating anolyte temperatures mitigates the complete transition from CO2R to HER with decreased amplitude of voltage oscillation (see Fig. S16, SI).
To further investigate the continuous increase in H2 selectivity, we focused on the behavior of Cu GDE during the operation between 100 and 150 minutes. Fig. 4b presents selected 2D micro-CT images of the Cu GDE at the AEM/Cu/MPL interfaces. By comparing the images marked with dotted lines, it is evident that the shift to higher potential coincides with the dissolution of salt precipitates, which appeared with faint contrast. A series of cross-sectional micro-CT images further confirmed the dissolution of these salt precipitates from points 2 to 5 (Fig. 4c). Similar to the images shown in Fig. 3d, where Cu GDE exhibited oscillatory behavior, the flooding phenomenon was identified as the primary cause of the observed degradation, which in turn led to the transition from CO2R to HER. As shown in Fig. S17 (SI), the Ag GDE exhibits similar oscillatory behavior with increasing H2 selectivity, as voltage oscillation recurs, implying that the progression of degradation in MEA can be a universal phenomenon, regardless of the catalyst material.
To investigate this further, we conducted X-ray tomography measurements of the MEA at a high operating current density of −250 mA cm−2 in 1 M KHCO3. Initially, the potential shifted to a lower level during the first ∼15 minutes, then moved toward a higher (anodic) level during the subsequent 100 minutes of operation (see Fig. 5a). Corresponding with the voltage change, H2 selectivity gradually increased over 100 minutes of operation, reaching 70%, while CO and C2H4 selectivity decreased (see Fig. 5b).
By comparing the cross-sectional micro-CT images acquired at points 1 and 2, we observed that the hollow spots in MPL, which appeared darker, showed contrast changes without significant precipitate formation at the Cu/membrane interface (see Fig. 5c). This suggests that water crossover (flooding) reached the MPL/GDL and promoting HER. While there is poor micro-CT contrast between pure water and GDE components in our cell, combining electrochemical data with X-ray tomography images provided valuable insights into the behavior under flooding conditions.
After 30 minutes of operation, the salt precipitates, seen as bright signals near the Cu/MPL region, were confirmed. Additionally, the interface between the Cu GDE and the membrane became rougher, revealing gaps. Compared to the hollow spots in MPL (point 1, marked with an orange dotted line), the same area showed a brighter signal, indicating that anolyte cations had reached the MPL/GDL. As the operating time increased, the growth of precipitates became more pronounced, as seen in images taken at points 3 to 5. Although the increase in precipitates may correlate with eCO2R properties, the rapid transition from CO2R to HER suggests that flooding, rather than precipitation, might be the primary degradation mechanism.
Fig. 6a shows the ionic product value of the K2CO3 salt QK2CO3 = [K+]2[CO32−] under different current densities. The solubility product Ksp = 2073 (M3) of the K2CO3 is used as the criterion for precipitation.16 In the case of −100 mA cm−2, −150 mA cm−2 and −200 mA cm−2, regions with QK2CO3 > Ksp near the AEM/CL interface can be seen, which indicates that thermodynamically, the K+ and CO32− ion concentration could facilitate the formation of precipitates in these regions. This is consistent with the experimental observation of the obvious fluctuation in voltage and selectivity and the precipitation under X-ray tomography images when operating −100 mA cm−2, −150 mA cm−2 and −200 mA cm−2. Fig. 6b shows the water vapor partial pressure distribution in the cathode diffusion medium. As the current density increases, the water vapor partial pressure also increases, which promotes the chance of flooding.
To investigate the influence of precipitation and flooding on voltage and selectivity of the cell, we carried out the simulation with three different assumptions: (1) the entire catalyst layer is wetted, having both liquid phase and gas phase with an active surface area density of 1 × 107 m−1, representing the case with no precipitation or flooding; (2) the entire catalyst layer is wetted, but with a reduced active surface area density of 5 × 106 m−1, representing the scenario where precipitates blocks part of the reaction sites; (3) only liquid phase transfer are assumed at the leftmost 250 μm of the catalyst layer and both liquid phase and gas phase transfer are assumed for the remaining 50 μm, representing the scenario where flooding occurs. Fig. 6c and d shows the simulated polarization curve and selectivity under these different assumptions. Comparing the simulation results of scenario (1) and (2), it could be seen that the blockage of surface area by precipitation could cause the voltage to shift to a more negative potential and a decrease in CO selectivity. Comparing scenario (1) and (3), it could be inferred that the flooding of the catalyst layer could cause a significant increase in H2 selectivity and decrease in CO and C2H4 selectivity. This could be attributed to the decrease in CO2 concentration in the catalyst layer due to the slow dissolved CO2 diffusion rate in aqueous phase when flooded compared to the higher CO2 concentration when gaseous pathways are available, which is proven by simulation when comparing the CO2 concentration plotted in Fig. S20 and S21 (SI). Increasing electrolyte concentration can impact dissolved species profile and lead to increased precipitation within GDE, as shown in Fig. S22 (SI).
In case A, we observed inhomogeneous precipitate formation at the Cu/membrane interface. The extent of precipitate growth varied depending on the operating current density, with increased HER attributed to predominant precipitation. Low operating current density can result in a potential shift toward cathodic direction (pale pink line), and high operating current density (bright purple line) can maintain the potential while the eCO2R product distribution decreases. In case B, where the MEA is near the stability threshold, partial dissolution of precipitates occurs near the Cu/membrane interfaces, coinciding with voltage oscillations. This leads to a transient change between CO2R and HER. In case C, at high current densities or under high electrolyte concentrations, rapid water crossover reaches the GDL, promoting H2 production rather than CO2R. Flooding predominates over precipitation in this case, leading to an anodically shifted voltage. Understanding the failure mechanisms of the MEA reveals that these phenomena can be mitigated through the strategic engineering of components and optimization of operational conditions. In terms of component design, it is essential to develop GDEs with stable hydrophobicity and effective through-plane conductivity to prevent precipitation and flooding. Considering that the precipitation and flooding were mainly observed in the MPL, improving the hydrophobicity of MPL can contribute to enhanced CO2R stability. GDEs with improved hydrophobicity should feature smooth surfaces since trenches in commercial GDEs can promote pH gradients and become sites for precipitation and flooding. The use of bipolar membranes that selectively permeate ions may also help alleviate these issues. Operational optimization may involve investigating the effects of cations in the anolytes, as cation crossover through the membrane depends on the size of the cations. Additionally, acidic electrolytes can suppress salt precipitation, although this requires the development of CO2R-selective catalysts to minimize HER interference.
In summary, we investigated the degradation behavior of the MEA, focusing on precipitation and flooding using operando X-ray tomography coupled with real-time electrochemical measurement. X-ray tomography enabled us to visualize interface dynamics at solid/liquid/gas boundaries and track the phase distribution within the MEA, significantly enhancing our understanding of degradation mechanisms through structural changes over time. We categorized the predominant degradation behaviors into three cases by correlating voltage profiles, selectivity distributions, and morphological changes in the MEA caused by water crossover and precipitation. Key findings include: (1) visualization of growth and dissolution of precipitates in Cu GDE, providing deeper insights into the mechanisms of MEA failure. (2) Tracking mechanical deformation at the Cu GDE/membrane interface due to precipitation and flooding, which has not been previously observed. (3) Providing direct visual evidence of the transition from CO2R to HER, with a focus on the distribution of precipitates and water crossover from the catalyst/membrane interface to the GDL.
Understanding and mitigating precipitate formation and flooding mechanisms is critical for scaling eCO2R technology for industrial applications. Persistent flooding and salt formation not only reduce system efficiency and catalyst lifetime but also increase operational costs and maintenance requirements. By identifying key failure pathways, our study provides insights that can guide the design of more durable MEAs, ultimately improving the viability of eCO2R for large-scale carbon utilization.
![]() | (1) |
| ∇·Ni = Ri | (2) |
The gas phase domains feature the mixture-averaged transport model for the gas species (CO2, H2, CO, C2H4),
![]() | (3) |
is the average molecular weight of the mixture. Note that even though CH4 could be present in our system, it is excluded for simplicity from our simulation together with its evolution reaction since we barely observe it in our experiment.
In the bulk aqueous phase, the dissolved inorganic carbon (DIC) species are dynamically converting to each other according to the reactions and the reaction rate constants from the paper by Schulz and Zeebe et al.40
The following cathodic reactions are considered at Cu catalyst layer:
| 2H2O + 2e− → H2 + 2OH− | (4) |
| CO2 + H2O + 2e− → CO + 2OH− | (5) |
| 2CO2 + 8H2O + 12e− → C2H4 + 12OH− | (6) |
| 2CO2 + 9H2O + 12e− → C2H5OH + 12OH− | (7) |
The oxygen evolution reaction (OER) is assumed to happen at the anode:
| 2H2O → O2 + 4H+ + 4e− | (8) |
The partial current densities of the above charge transfer reactions follow the Tafel kinetics,
![]() | (9) |
and charge transfer coefficient αk are used as the same values as the ref. 39.
The mixed phase domain has both Nernst–Planck equation and the mixture average equation, along with the phase transport of dissolved CO2, governed by
![]() | (10) |
Supplementary information is available. See DOI: https://doi.org/10.1039/d5ey00232j
| This journal is © The Royal Society of Chemistry 2025 |