In physics, a ferromagnetic material is said to have magnetocrystalline anisotropy if it takes more energy to magnetize it in certain directions than in others. These directions are usually related to the principal axes of its crystal lattice. It is a special case of magnetic anisotropy. In other words, the excess energy required to magnetize a specimen in a particular direction over that required to magnetize it along the easy direction is called crystalline anisotropy energy.
The spin-orbit interaction is the primary source of magnetocrystalline anisotropy. It is basically the orbital motion of the electrons which couples with crystal electric field giving rise to the first order contribution to magnetocrystalline anisotropy. The second order arises due to the mutual interaction of the magnetic dipoles. This effect is weak compared to the exchange interaction and is difficult to compute from first principles, although some successful computations have been made.
Magnetocrystalline anisotropy has a great influence on industrial uses of ferromagnetic materials. Materials with high magnetic anisotropy usually have high coercivity, that is, they are hard to demagnetize. These are called "hard" ferromagnetic materials and are used to make permanent magnets. For example, the high anisotropy of rare-earth metals is mainly responsible for the strength of rare-earth magnets. During manufacture of magnets, a powerful magnetic field aligns the microcrystalline grains of the metal such that their "easy" axes of magnetization all point in the same direction, freezing a strong magnetic field into the material.
On the other hand, materials with low magnetic anisotropy usually have low coercivity, their magnetization is easy to change. These are called "soft" ferromagnets and are used to make magnetic cores for transformers and inductors. The small energy required to turn the direction of magnetization minimizes core losses, energy dissipated in the transformer core when the alternating current changes direction.
The magnetocrystalline anisotropy energy is generally represented as an expansion in powers of the direction cosines of the magnetization. The magnetization vector can be written, where is the saturation magnetization. Because of time reversal symmetry, only even powers of the cosines are allowed. The nonzero terms in the expansion depend on the crystal system (e.g., cubic or hexagonal). The order of a term in the expansion is the sum of all the exponents of magnetization components, e.g., is second order.
More than one kind of crystal system has a single axis of high symmetry (threefold, fourfold or sixfold). The anisotropy of such crystals is called uniaxial anisotropy. If the axis is taken to be the main symmetry axis of the crystal, the lowest order term in the energy is[1]
E/V=K1\left(\alpha2+\beta2\right)=
| 2\right). | |
| K | |
| 1\left(1-\gamma |
The ratio is an energy density (energy per unit volume). This can also be represented in spherical polar coordinates with,, and :
\displaystyleE/V=K1\sin2\theta.
The parameter, often represented as, has units of energy density and depends on composition and temperature.
The minima in this energy with respect to satisfy
| \partialE | |
| \partial\theta |
=0 and
| \partial2E | |
| \partial\theta2 |
>0.
Many models of magnetization represent the anisotropy as uniaxial and ignore higher order terms. However, if, the lowest energy term does not determine the direction of the easy axes within the basal plane. For this, higher-order terms are needed, and these depend on the crystal system (hexagonal, tetragonal or rhombohedral).
In a hexagonal system the axis is an axis of sixfold rotation symmetry. The energy density is, to fourth order,
E/V=K1\sin2\theta+K2\sin4\theta+
| 6\theta | |
| K | |
| 3\sin |
\cos6\phi,
The uniaxial anisotropy is mainly determined by these first two terms. Depending on the values and, there are four different kinds of anisotropy (isotropic, easy axis, easy plane and easy cone):
The basal plane anisotropy is determined by the third term, which is sixth-order. The easy directions are projected onto three axes in the basal plane.
Below are some room-temperature anisotropy constants for hexagonal ferromagnets. Since all the values of and are positive, these materials have an easy axis.
| Structure | K1 | K2 | |
|---|---|---|---|
| 45 | 15 | ||
| α (hematite) | 120 | ||
| 3 | |||
| 550 | |||
| 89 | 27 |
Higher order constants, in particular conditions, may lead to first order magnetization processes FOMP.
The energy density for a tetragonal crystal is
\displaystyleE/V=K1\sin2\theta+K2\sin4\theta+
| 4\theta | |
| K | |
| 3\sin |
\cos4\phi
Note that the term, the one that determines the basal plane anisotropy, is fourth order (same as the term). The definition of may vary by a constant multiple between publications.
The energy density for a rhombohedral crystal is
\displaystyleE/V=K1\sin2\theta+K2\sin4\theta+
| 3\theta | |
| K | |
| 3\cos\theta\sin |
\cos3\phi
In a cubic crystal the lowest order terms in the energy are
E/V=K1\left(\alpha2\beta2+\beta2\gamma2+\gamma2\alpha2\right)+
| 2\beta | |
| K | |
| 2\alpha |
2\gamma2.
If the second term can be neglected, the easy axes are the ⟨100⟩ axes (i.e., the,, and, directions) for and the ⟨111⟩ directions for (see images on right).
If is not assumed to be zero, the easy axes depend on both and . These are given in the table below, along with hard axes (directions of greatest energy) and intermediate axes (saddle points) in the energy). In energy surfaces like those on the right, the easy axes are analogous to valleys, the hard axes to peaks and the intermediate axes to mountain passes.
| Type of axis | K2=+infty -9K1/4 | K2=-9K1/4 -9K1 | K2=-9K1 -infty | |
|---|---|---|---|---|
| Easy | ⟨100⟩ | ⟨100⟩ | ⟨111⟩ | |
| Medium | ⟨110⟩ | ⟨111⟩ | ⟨100⟩ | |
| Hard | ⟨111⟩ | ⟨110⟩ | ⟨110⟩ |
| Type of axis | K2=-infty 9\left\vertK1\right\vert/4 | K2=9\left\vertK1\right\vert/4 9\left\vertK1\right\vert | K2=9\left\vertK1\right\vert +infty | |
|---|---|---|---|---|
| Easy | ⟨111⟩ | ⟨110⟩ | ⟨110⟩ | |
| Medium | ⟨110⟩ | ⟨111⟩ | ⟨100⟩ | |
| Hard | ⟨100⟩ | ⟨100⟩ | ⟨111⟩ |
Below are some room-temperature anisotropy constants for cubic ferromagnets. The compounds involving are ferrites, an important class of ferromagnets. In general the anisotropy parameters for cubic ferromagnets are higher than those for uniaxial ferromagnets. This is consistent with the fact that the lowest order term in the expression for cubic anisotropy is fourth order, while that for uniaxial anisotropy is second order.
| Structure | K1 | K2 |
|---|---|---|
| 4.8 | ±0.5 | |
| −0.5 | (-0.5)–(-0.2)[7] [8] | |
| · (magnetite) | −1.1 | |
| · | −0.3 | |
| NiO· | −0.62 | |
| MgO· | −0.25 | |
| CoO· | 20 | |
The magnetocrystalline anisotropy parameters have a strong dependence on temperature. They generally decrease rapidly as the temperature approaches the Curie temperature, so the crystal becomes effectively isotropic. Some materials also have an isotropic point at which . Magnetite, a mineral of great importance to rock magnetism and paleomagnetism, has an isotropic point at 130 kelvin.
Magnetite also has a phase transition at which the crystal symmetry changes from cubic (above) to monoclinic or possibly triclinic below. The temperature at which this occurs, called the Verwey temperature, is 120 Kelvin.
The magnetocrystalline anisotropy parameters are generally defined for ferromagnets that are constrained to remain undeformed as the direction of magnetization changes. However, coupling between the magnetization and the lattice does result in deformation, an effect called magnetostriction. To keep the lattice from deforming, a stress must be applied. If the crystal is not under stress, magnetostriction alters the effective magnetocrystalline anisotropy. If a ferromagnet is single domain (uniformly magnetized), the effect is to change the magnetocrystalline anisotropy parameters.
In practice, the correction is generally not large. In hexagonal crystals, there is no change in . In cubic crystals, there is a small change, as in the table below.
| Structure | K1 | K'1 | |
|---|---|---|---|
| 4.7 | 4.7 | ||
| −0.60 | −0.59 | ||
| (magnetite) | −1.10 | −1.36 |