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Rare-earth magnet

Strong permanent magnet made from alloys of rare-earth elements

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  • 6 chapters

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Through Magnet, Alloy and Ferrite (magnet)

There are two types: neodymium magnets and samarium–cobalt magnets. Rare-earth magnets are extremely brittle and are vulnerable to corrosion, so they are usually plated or coated to protect them from breaking, chipping, or crumbling into powder.

The development of rare-earth magnets began around 1966, when K. J. Strnat and G. Hoffer of the US Air Force Materials Laboratory discovered that an alloy of yttrium and cobalt, YCo5, had by far the largest magnetic anisotropy constant of any material then known.

The term "rare earth" can be misleading, as some of these metals are as abundant in the Earth's crust as tin or lead, but rare earth ores do not exist in seams (as do coal or copper, for example), so in any given cubic kilometre of crust they are "rare". China produces more than any other country but it imports significant amounts of REE ore from Myanmar. As of 2025, China produces 90% of the world's supply of rare-earth magnets. Some countries classify rare earth metals as strategically important. Chinese export restrictions on these materials have led countries such as the United States to initiate research programs to develop strong magnets that do not require rare earth metals.

Properties

According to Lucas et al, "To produce ferromagnetism and then a magnet the first condition is to select materials having a high concentration of paramagnetic atoms. A paramagnetic atom contains unpaired electrons, each of them being equivalent to a local magnet due to the orientation of the electronic spin." The RE sequence of metals are characterized by a gradual filling of the 4f level, resulting in a large number of unpaired electrons. For instance, neodymium has three unpaired electrons, while samarium has five. The resulting magnetic moment is due to the combined effects of spin and orbit. Yet, because RE metals have large metallic radii, their magnetic properties are limited on their own. They must be alloyed with transition metals such as Fe and Co, to produce a permanent magnet, especially if the magnetic dipoles align along a crystalline direction, called magnetic anisotropy. This anisotropy facilitates easy magnetization through dipole alignment, and difficulty with demagnetization, called coercivity. Both Fe and Co are very rich in unpaired electrons, ensuring strong magnetization.

Some important properties used to compare permanent magnets are: remanence (Br), which measures the strength of the magnetic field; coercivity (Hci), the material's resistance to becoming demagnetized; energy product (B·Hmax), the density of magnetic energy; and Curie temperature (TC), the temperature at which the material loses its magnetism. Rare-earth magnets have higher remanence, much higher coercivity and energy product, but (for neodymium) lower Curie temperature than other types. The table below compares the magnetic performance of the two types of rare-earth magnets, neodymium (Nd2Fe14B) and samarium–cobalt (SmCo5), with other types of permanent magnets.

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