A UChicago team shows that a layered manganese oxide mineral can sort chemically near identical rare earth ions in water, with magnesium ions pinning the channels open.
Splitting neodymium from lanthanum usually means acid baths and organic solvents in many-stage extraction plants, because the 17 rare earths are chemically so similar that pulling one out of the rest is unusually hard. A Nature Chemical Engineering paper this week from the University of Chicago's Pritzker School of Molecular Engineering, with Northwestern and Argonne collaborators, points at a different lever.
The team uses a layered manganese-oxide mineral whose interlayer gap is just a few water molecules wide. Without help, the channel is too floppy to discriminate the trickiest near-neighbor pairs. Magnesium ions added as a scaffold pin the gap to a fixed width, so rare-earth ions slip through at different rates based on the size of their hydration shell rather than the radius of the bare ion. That single change pushes neodymium-over-lanthanum enrichment from 1.6x to 5.4x, and two cycles yield 97% pure neodymium, per the UChicago press release.
The cell runs in water with an electric current, no organic solvents. Co-author George Schatz calls that a chemistry that "could actually change how and where that processing gets done," tying it to the US and EU push to onshore rare-earth separation from China. The honest scale is a lab proof of concept, not a replacement for the solvent-extraction trains that purify these metals today. Liu's group is now testing the remaining lanthanides; Schatz is refining the density-functional-theory models that predict the channel behavior.