Rare-earth elements that power magnets, batteries, and electronics may be easier to recover from the ocean than previously thought. A new study published in Communications Earth & Environment reports that the secret lies in the elements’ atom-by-atom arrangement inside deep-sea sediments—an arrangement that can actively improve how effectively rare earths can be extracted.
Researchers investigated rare-earth concentrations in seabed deposits, focusing on how these metals bind to the surrounding mineral surfaces. Using advanced micro- and nanoscale characterization, the team mapped the metals’ local chemical environments and determined the structural motifs they adopt at the atomic scale.
The findings show that rare earth ions are not simply trapped as random contaminants. Instead, many occupy specific coordination sites—positions defined by the number and type of surrounding atoms, such as oxygen-containing ligands. This matters because extraction performance depends not only on how much rare earth is present, but also on how tightly it is held and how readily it can be liberated during processing.
By demonstrating a direct link between structural organization and extractability, the work reframes the challenge of deep-sea mining. It suggests that sediments can function as engineered “hosts,” where the rare earth’s chemical neighborhood determines whether conventional leaching approaches can efficiently mobilize the metals.
The study’s results also point to a pathway for more targeted recovery strategies. If future sampling identifies sediment types with the most favorable atomic structures, operators could reduce waste, lower chemical consumption, and improve yields compared with approaches that treat all deposits as equivalent.
In addition, understanding binding mechanisms at this resolution can help forecast how rare-earth release might behave when sediments are disturbed. That knowledge is crucial for balancing resource development with environmental risk, since different bonding configurations may respond differently to changes in chemistry and oxygen conditions.
Overall, the research provides a structural explanation for why some deep-sea deposits are more promising than others. As rare-earth supply chains face tightening constraints, these insights could accelerate the move from “where are the metals?” to “how do we unlock them?”
Just as importantly for the scientific and industrial communities, the study establishes a measurable framework connecting atomic-scale mineral chemistry to macroscopic extraction outcomes, turning a complex geochemical black box into an increasingly actionable design problem.
Subject of Research: Rare earth element extractability in deep-sea sediments via atomic-scale structure
Article Title: The atomic-scale structure of rare earth elements in deep-sea sediments facilitates their extractability.
Article References: Manceau, A., Giacomelli, A., Li, Y. et al. The atomic-scale structure of rare earth elements in deep-sea sediments facilitates their extractability. Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03848-7
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