Abstract
In zero-gap CO2 electrolyzers, maintaining the balance of water and cations is crucial. Excessive accumulation at the cathode causes performance degradation, leading to flooding and salt precipitation. Using operando wide-angle X-ray scattering and X-ray fluorescence techniques, we observed the dynamic evolution of H2O and Cs+ inside a membrane-electrode-assembly. Our findings reveal that Cs+ movement across the membrane from the anode to the cathode is governed by migration and drags H2O via electroosmosis. H2O diffusion then allows Cs+ diffusion further within the gas diffusion electrode. When decreasing the applied voltage, the concentration gradient causes Cs+ quickly to diffuse back to the anode. The H2O content in the macro-porous layer remains at the same level, thus showcasing an origin of gas diffusion electrode flooding. By regulating the electrolyte concentration, we deconvolute the correlation of water and cations for selectivity changes. Our work underscores the significance of water/cation management strategies in zero-gap electrolyzers.
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