Dysprosium Dy · 66

A heavy rare earth added in small amounts to magnets so they keep working when they get hot.

Why does it matter?

Without dysprosium a neodymium magnet starts losing strength around 80 C. A traction motor or a turbine nacelle routinely runs hotter than that.

Where it is in the Earth

Dysprosium belongs to the heavy rare earth elements, a group that behaves chemically in ways subtly different from the lighter members of the rare earth family. That chemical difference governs where it ends up in the Earth's crust. Rare earth elements are not, despite the name, particularly scarce in absolute terms; what is rare is finding them concentrated enough to mine economically. Dysprosium forms alongside other heavy rare earths in two quite different geological settings, and understanding those settings explains almost everything about where the world's supply comes from.

The first setting is a phosphate mineral called xenotime, which has the formula YPO4. Xenotime crystallises inside certain granites and pegmatites — coarse-grained igneous rocks that form when the last, fluid-rich fraction of a cooling magma body solidifies slowly. Because dysprosium and the other heavy rare earths fit comfortably into xenotime's crystal structure, they become concentrated there as the melt cools. Xenotime grains can persist through erosion and be reworked into river and beach placer deposits, where they accumulate alongside other dense, chemically resistant minerals such as zircon and ilmenite.

The second and currently more consequential setting is the ion-adsorption clay deposit of southern China. Here the geological process is not igneous but weathering. Granite bedrock naturally enriched in rare earths breaks down over millions of years under the warm, wet conditions of a subtropical climate. As the feldspar minerals in the granite decompose to kaolinite clay, the rare earth ions released from the original minerals are not washed away entirely; instead, they adsorb loosely onto the surfaces of the clay particles. Heavy rare earths, including dysprosium, are disproportionately concentrated in these clay profiles compared with the original rock, because the weathering process partitions them differently from the light rare earths. The result is a shallow, low-grade deposit with a flat, diffuse geometry — nothing like the hard-rock ore bodies most people picture when they think of mining.

Getting it out

The way dysprosium is extracted depends almost entirely on which type of deposit is being worked. Xenotime recovered from hard-rock deposits or placers is mined by conventional open-pit methods or dredging, exactly as one would mine for any dense mineral in a sand or gravel deposit. The xenotime grains are then separated from the other minerals by physical and gravity-based techniques before any chemistry is applied. This is a well-understood process, but xenotime is a relatively minor contributor to global dysprosium supply.

The dominant source is the ion-adsorption clay deposit, and the mining method there is fundamentally different. Because the rare earth ions are not locked inside a hard mineral grain but are instead loosely attached to clay surfaces, they can be released by flushing the ground with a dilute salt solution — ammonium sulfate has historically been used. This approach is called in-situ leaching: rather than digging up the clay and transporting it to a processing plant, the solution is injected through boreholes into the weathered profile and collected at the base of the deposit as a weak rare-earth-bearing liquid. The ground is disturbed but not removed in the way conventional mining removes it. Grade in this context means very little material per tonne of clay, and the processing chain begins in the ground itself rather than at a mill.

The environmental footprint of in-situ leaching is a subject of ongoing scrutiny. Ammonia from leaching solutions has historically migrated beyond the intended recovery zone, affecting groundwater and nearby agricultural land. Chinese regulators have applied progressively stricter controls on this, which affects both the cost and the pace at which these deposits can be worked. A reader looking at production statistics should bear in mind that officially reported output from these mines reflects a regulated, partially consolidated industry rather than a straightforwardly free market.

What pulls on it

Dysprosium's role is narrow but not easily replaced. A neodymium-iron-boron magnet — the strongest type of permanent magnet available — begins to lose its magnetism at elevated temperature through a process called thermal demagnetisation. The temperature at which this becomes a problem is well below the operating temperature of an electric vehicle traction motor or a wind turbine generator. Adding dysprosium to the magnet's alloy raises the threshold at which demagnetisation occurs, a property measured as coercivity. The more demanding the thermal environment, the more dysprosium the design requires.

This explains the pattern visible in the intensity table. A magnet used in a relatively cool application may need no dysprosium at all, or only a small fraction of a kilogram per kilogram of finished magnet. A traction motor, which runs hot and must not lose torque unpredictably, sits higher in the range. A large direct-drive offshore wind turbine — which uses a permanent magnet generator rather than a gearbox, because gearboxes are a maintenance liability offshore — requires a substantial quantity per megawatt of capacity. As offshore wind capacity expands and as the vehicle fleet electrifies, these two end markets are the main drivers pulling on dysprosium supply. Robotics and automation add further demand as factories deploy more servo motors with demanding duty cycles.

What would have to change for demand to shift sharply? The principal scenario is a change in magnet design. If motor designers could move to magnet grades with lower dysprosium content without sacrificing performance, or if non-rare-earth motor technologies such as wound-field synchronous motors or induction motors displaced permanent-magnet designs in large applications, demand growth would slow. Neither change is costless: alternative motor types involve trade-offs in weight, efficiency, or complexity. The data storage application listed in the US statistics represents an older demand category — dysprosium was used in certain magneto-optical recording media — that is less prominent in current discussions of supply risk.