Rare earth elements (REEs) are critical for modern electronics, sustainable energy production, and medicine. Ion-adsorption deposits, one of the world’s major REE sources, contain kaolinite and gibbsite, whose mineral surfaces strongly influence REE mobility. This project systematically investigates the effects of water chemistry on REE adsorption to kaolinite and gibbsite by combining adsorption experiments, surface complexation modeling, and spectroscopic investigations. The work improves the understanding and prediction of REE behavior in clay-rich deposits, thereby advancing current knowledge of REE geochemical cycling.