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Ferrite (magnet)

Ferrimagnetic ceramic material

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A stack of Tong Ka Cin ferrite magnets shown attracting several iron objects. The north and south poles of the magnets are located on the opposing flat sides. These magnets are designed for use in cab
Omegatron · CC BY-SA 3.0

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Ferrites can be divided into two groups based on their magnetic coercivity, their resistance to being demagnetized:
"Hard" ferrites have high coercivity, so are difficult to demagnetize. They are used to make permanent magnets for applications such as refrigerator magnets, loudspeakers, and small electric motors.
"Soft" ferrites have low coercivity, so they easily change their magnetization and act as conductors of magnetic fields. They are used in the electronics industry to make efficient magnetic cores called ferrite cores for high-frequency inductors, transformers and antennas, and in various microwave components.

Ferrite compounds are extremely low cost, being made mostly of iron oxide, and have excellent corrosion resistance. Yogoro Kato and Takeshi Takei of the Tokyo Institute of Technology synthesized the first ferrite compounds in 1930.

Composition, structure, and properties

Ferrites are usually ferrimagnetic ceramic compounds derived from iron oxides, with either a body-centered cubic or hexagonal crystal structure. Like most of the other ceramics, ferrites are hard, brittle, and poor conductors of electricity.

They are typically composed of α-iron(III) oxide (e.g. hematite Fe2O3) with one, or more additional, metallic element oxides, usually with an approximately stoichiometric formula of MO·Fe2O3 such as Fe(II) such as in the common mineral magnetite composed of Fe(II)-Fe(III)2O4. Above 585 °C Fe(II)-Fe(III)2O4 transforms into the non-magnetic gamma phase. Fe(II)-Fe(III)2O4 is commonly seen as the black iron(II) oxide coating the surface of cast-iron cookware). The other pattern is M·Fe(III)2O3, where M is another metallic element. Common, naturally occurring ferrites (typically members of the spinel group) include those with nickel (NiFe2O4) which occurs as the mineral trevorite, magnesium containing magnesioferrite (MgFe2O4), cobalt (cobalt ferrite), or manganese (MnFe2O4) which occurs naturally as the mineral jacobsite. Less often bismuth, strontium, zinc as found in franklinite, aluminum,yittrium, or barium ferrites are used In addition, more complex synthetic alloys are often used for specific applications.

Many ferrites adopt the spinel chemical structure with the formula AB
2O
4, where A and B represent various metal cations, one of which is usually iron (Fe). Spinel ferrites usually adopt a crystal motif consisting of cubic close-packed (fcc) oxides (O2−) with A cations occupying one eighth of the tetrahedral holes, and B cations occupying half of the octahedral holes, i.e., A2+
B3+
2O2−
4. An exception exists for ɣ-Fe2O3 which has a spinel crystalline form and is widely used a magnetic recording substrate.

However the structure is not an ordinary spinel structure, but rather the inverse spinel structure: One eighth of the tetrahedral holes are occupied by B cations, one fourth of the octahedral sites are occupied by A cations. and the other one fourth by B cation. It is also possible to have mixed structure spinel ferrites with formula [M2+
(1−δ) Fe3+
δ ] [M2+
δ Fe3+
(2−δ) ] O
4, where δ is the degree of inversion.

The magnetic material known as "Zn Fe" has the formula ZnFe
2O
4, with Fe3+
occupying the octahedral sites and Zn2+
occupying the tetrahedral sites, it is an example of normal structure spinel ferrite.

Some ferrites adopt hexagonal crystal structure, like barium and strontium ferrites BaFe
12O
19 (BaO·6Fe
2O
3 ) and SrFe
12O
19 (SrO·6Fe
2O
3 ).

In terms of their magnetic properties, the different ferrites are often classified as "soft", "semi-hard" or "hard", which refers to their low or high magnetic coercivity, as follows.

Soft ferrites

Ferrites that are used in transformer or electromagnetic cores contain nickel, zinc, and/or manganese compounds. Soft ferrites are not suitable to make permanent magnets. They have high magnetic permeability so they conduct magnetic fields and are attracted to magnets, but when the external magnetic field is removed, the remanent magnetization does not tend to persist. This is due to their low coercivity. The low coercivity also means the material's magnetization can easily reverse direction without dissipating much energy (hysteresis losses), while the material's high resistivity prevents eddy currents in the core, another source of energy loss. Because of their comparatively low core losses at high frequencies, they are extensively used in the cores of RF transformers and inductors in applications such as switched-mode power supplies and loopstick antennas used in AM radios.

The most common soft ferrites are:

Manganese-zinc ferrite
"Mn Zn", with the formula Mn
δ Zn
(1−δ) Fe
2O
4. Mn Zn have higher permeability and saturation induction than Ni Zn.
Nickel-zinc ferrite
"Ni Zn", with the formula Ni
δ Zn
(1−δ) Fe
2O
4. Ni Zn ferrites exhibit higher resistivity than Mn Zn, and are therefore more suitable for frequencies above 1 MHz.

For use with frequencies above 0.5 MHz but below 5 MHz, Mn Zn ferrites are used; above that, Ni Zn is the usual choice. The exception is with common mode inductors, where the threshold of choice is at 70 MHz.

Semi-hard ferrites

Cobalt ferrite
CoFe
2O
4 (CoO·Fe
2O
3) is in between soft and hard magnetic material and is usually classified as a semi-hard material. It is mainly used for its magnetostrictive applications like sensors and actuators thanks to its high saturation magnetostriction (~200 ppm). CoFe
2O
4 has also the benefits to be rare-earth free, which makes it a good substitute for terfenol-D.

Moreover, cobalt ferrite's magnetostrictive properties can be tuned by inducing a magnetic uniaxial anisotropy. This can be done by magnetic annealing, magnetic field assisted compaction, or reaction under uniaxial pressure. This last solution has the advantage to be ultra fast (20 min) thanks to the use of spark plasma sintering. The induced magnetic anisotropy in cobalt ferrite is also beneficial to enhance the magnetoelectric effect in composite.

Hard ferrites

In contrast, permanent ferrite magnets are made of hard ferrites, which have a high coercivity and high remanence after magnetization. The high coercivity means the materials are very resistant to becoming demagnetized, an essential characteristic for a permanent magnet. They also have high magnetic permeability. These so-called ceramic magnets are cheap, and are widely used in household products such as refrigerator magnets. The maximum magnetic field B is about 0.35 tesla and the magnetic field strength H is about 30–160 kiloampere turns per meter (400–2000 oersteds). The density of ferrite magnets is about 5 g/cm3.

The most common hard ferrites are:

Strontium ferrite
SrFe
12O
19 (SrO·6Fe
2O
3), used in small electric motors, micro-wave devices, recording media, magneto-optic media, telecommunication, and electronics industry. Strontium hexaferrite (SrFe
12O
19) is well known for its high coercivity due to its magnetocrystalline anisotropy. It has been widely used in industrial applications as permanent magnets and, because they can be powdered and formed easily, they are finding their applications into micro and nano-types systems such as biomarkers, bio diagnostics and biosensors.
Barium ferrite
BaFe
12O
19 (BaO·6Fe
2O
3), a common material for permanent magnet applications. Barium ferrites are robust ceramics that are generally stable to moisture and corrosion-resistant. They are used in e.g. loudspeaker magnets and as a medium for magnetic recording, e.g. on magnetic stripe cards.

Iron oxide and (barium carbonate or strontium carbonate) are used in manufacturing of hard ferrite magnets.

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