Rare-earth magnet

Ferrofluid on glass, with a rare-earth magnet underneath.

Rare-earth magnets are strong permanent magnets made from alloys of rare earth elements (elements in the lanthanide series, plus scandium and yttrium).[1] Developed in the 1970s and '80s, rare-earth magnets are the strongest type of permanent magnets made, producing significantly stronger magnetic fields than other types such as ferrite or alnico magnets. The magnetic field typically produced by rare-earth magnets can exceed 1.4 teslas, whereas ferrite or ceramic magnets typically exhibit fields of 0.5 to 1 tesla. There are two types: neodymium magnets and samarium-cobalt magnets. Magnetostrictive rare-earth magnets such as Terfenol-D also have applications—e.g. in loudspeakers. Rare earth magnets are extremely brittle and also vulnerable to corrosion, so they are usually plated or coated to protect them from breaking, chipping, or crumbling into powder.

The term "rare earth" can be misleading as these metals are not particularly rare or precious;[2][3] they are about as abundant as tin or lead.[4] 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.[5][6]

Neodymium magnets (small cylinders) lifting steel balls. As shown here, rare-earth magnets can easily lift thousands of times their own weight.

Explanation of strength

The rare earth (lanthanide) elements are metals that are ferromagnetic, meaning that like iron they can be permanently magnetized, but their Curie temperatures are below room temperature, so in pure form their magnetism only appears at low temperatures. However, they form compounds with the transition metals such as iron, nickel, and cobalt, and some of these have Curie temperatures well above room temperature. Rare earth magnets are made from these compounds.

The greater strength of rare earth magnets is mostly due to two factors. First, their crystalline structures have very high magnetic anisotropy. This means a crystal of the material preferentially magnetizes along a specific crystal axis but is very difficult to magnetize in other directions. Like other magnets, rare earth magnets are composed of microcrystalline grains which are aligned in a powerful magnetic field during manufacture so their magnetic axes all point in the same direction. The resistance of the crystal lattice to turning its direction of magnetization gives these compounds a very high magnetic coercivity (resistance to being demagnetized).

Second, atoms of rare earth elements can have high magnetic moments because their orbital electron structure contains many unpaired electrons, in contrast to other elements in which almost all of the electrons exist in pairs with opposite spins, so their magnetic fields cancel out. This is a consequence of incomplete filling of the f-shell, which can contain up to 7 unpaired electrons. In a magnet it is the unpaired electrons, aligned so they spin in the same direction, which generate the magnetic field. This gives the materials high remanence (saturation magnetization Js). The maximum energy density BHmax is proportional to Js2 so these materials have the potential for storing large amounts of magnetic energy. The magnetic energy product BHmax of neodymium magnets is about 18 times greater than "ordinary" magnets by volume. This allows rare earth magnets to be smaller than other magnets which produce the same field strength.

Magnetic properties

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 (BHmax), 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 magnet, neodymium (Nd2Fe14B) and samarium-cobalt (SmCo5), with other types of permanent magnets.

MagnetBr (T)Hci (kA/m)(BH)max (kJ/m3)Tc (°C)
Nd2Fe14B (sintered)1.0–1.4750–2000200–440310–400
Nd2Fe14B (bonded)0.6–0.7600–120060–100310–400
SmCo5 (sintered)0.8–1.1600–2000120–200720
Sm(Co,Fe,Cu,Zr)7 (sintered)0.9–1.15450–1300150–240800
Alnico (sintered)0.6–1.427510–88700–860
Sr-ferrite (sintered)0.2–0.4100–30010–40450

Source:

Types

Samarium-cobalt

Samarium–cobalt magnets (chemical formula: SmCo5), the first family of rare earth magnets invented, are less used than neodymium magnets because of their higher cost and weaker magnetic field strength. However, samarium–cobalt has a higher Curie temperature, creating a niche for these magnets in applications where high field strength is needed at high operating temperatures. They are highly resistant to oxidation, but sintered samarium-cobalt magnets are brittle and prone to chipping and cracking, and may fracture when subjected to thermal shock.

Neodymium

Main article: Neodymium magnet
Neodymium magnet with nickel plate mostly removed

Neodymium magnets, invented in the 1980s, are the strongest and most affordable type of rare-earth magnet. They are made of an alloy of neodymium, iron, and boron (Nd2Fe14B), sometimes abbreviated as NIB. Neodymium magnets are used in numerous applications requiring strong, compact permanent magnets, such as electric motors for cordless tools, hard disk drives, magnetic holddowns, and jewelry clasps. They have the highest magnetic field strength and have a higher coercivity (which makes them magnetically stable), but they have a lower Curie temperature, m and are more vulnerable to oxidation than samarium–cobalt magnets. Corrosion can cause unprotected magnets to spall off a surface layer, or to crumble into a powder. Use of protective surface treatments such as gold, nickel, zinc, and tin plating and epoxy resin coating can provide corrosion protection.

Originally, the high cost of these magnets limited their use to applications requiring compactness together with high field strength. Both the raw materials and the patent licenses were expensive. However, since the 1990s, NIB magnets have become steadily less expensive, and the low cost has inspired new uses such as magnetic construction toys.

Hazards

The greater force exerted by rare earth magnets creates hazards that are not seen with other types of magnet. Magnets larger than a few centimeters are strong enough to cause injuries to body parts pinched between two magnets, or a magnet and a metal surface, even causing broken bones.[7] Magnets allowed to get too near each other can strike each other with enough force to chip and shatter the brittle material, and the flying chips can cause injuries. There have even been cases where young children who have swallowed several magnets have had a fold of the digestive tract pinched between the magnets, causing injury and in one case intestinal perforations, sepsis and death.[8]

Applications

Since their prices became competitive in the 1990s, neodymium magnets have been replacing Alnico and ferrite magnets in the many applications in modern technology requiring powerful magnets. Their greater strength allows smaller and lighter magnets to be used for a given application.

Common applications

Neodymium magnet balls

Common applications of rare-earth magnets include:

Other applications

Other applications of rare-earth magnets include:

Rare-earth-free permanent magnets

The United States Department of Energy has identified a need to find substitutes for rare earth metals in permanent magnet technology, and has begun funding such research. The Advanced Research Projects Agency-Energy (ARPA-E) has sponsored a Rare Earth Alternatives in Critical Technologies (REACT) program, to develop alternative materials. In 2011, ARPA-E awarded 31.6 million dollars to fund Rare-Earth Substitute projects.[9]

References

  1. ↑ Edited by N G Connelly and T Damhus (with R M Hartshorn and A T Hutton), ed. (2005). Nomenclature of Inorganic Chemistry: IUPAC Recommendations 2005 (PDF). Cambridge: RSC Publ. ISBN 0-85404-438-8. Archived from the original (PDF) on 2008-05-27. Retrieved 2012-03-13.
  2. ↑ McCaig, Malcolm (1977). Permanent Magnets in Theory and Practice. USA: Wiley. p. 123. ISBN 0-7273-1604-4.
  3. ↑ Sigel, Astrid; Helmut Sigel (2003). The lanthanides and their interrelations with biosystems. USA: CRC Press. pp. v. ISBN 0-8247-4245-1.
  4. ↑ Bobber, R. J. (1981). "New Types of Transducers". Underwater Acoustics and Signal Processing. p. 243. doi:10.1007/978-94-009-8447-9_20. ISBN 978-94-009-8449-3.
  5. ↑ Cullity, B. D.; Graham, C. D. (2008). Introduction to Magnetic Materials. Wiley-IEEE. p. 489. ISBN 0-471-47741-9.
  6. ↑ Lovelace, Alan M. (March–April 1971). "More Mileage Than Programmed From Military R&D". Air University Review. US Air Force. 22 (3): 14–23. Retrieved July 4, 2012.
  7. ↑ Swain, Frank (March 6, 2009). "How to remove a finger with two super magnets". The Sciencepunk Blog. Seed Media Group LLC. Retrieved 2009-06-28.
  8. ↑ "Magnet Safety Alert" (PDF). U.S. Consumer Product Safety Commission. Retrieved 20 July 2014.
  9. ↑ "Research Funding for Rare Earth Free Permanent Magnets". ARPA-E. Retrieved 23 April 2013.

Further reading

External links

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