Magnetic anisotropy is a directional dependence of a material's magnetic properties. A preferred direction must be distinguished from an externally imposed magnetic field.
Dependence of a crystal's magnetic energy on magnetization direction relative to its lattice, commonly generated by spin-orbit coupling and the crystal environment. A half-filled orbital shell with suppresses first-order orbital anisotropy, although smaller admixture and dipolar effects can remain.
A magnetic energy preference for an axis, with the two opposite directions equivalent in a purely uniaxial model. An easy-axis energy can be written for . A unidirectional term distinguishes the two directions and can instead shift a hysteresis.
A directional magnetic preference that distinguishes a Magnetization direction from its reverse, unlike a purely uniaxial easy-axis energy. A pinned interface can supply such a preference and produce exchange bias. In a simple model its interfacial energy term is proportional to .
A displacement of a ferromagnetic hysteresis loop's field centre caused by coupling to a prepared, sufficiently pinned magnetic environment, commonly an antiferromagnet. Field cooling through the ordering/blocking range can establish a unidirectional interfacial spin preference. With switching fields , the shift is , distinct from coercive half-width . Reversing the cooling field, testing a full major loop and comparing uncoupled/zero-field-cooled controls help identify genuine bias.
The tensor connecting spin to magnetic moment in an effective spin Hamiltonian. Its principal values specify direction-dependent Zeeman coupling.

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Magnetic anisotropy refers to the directional dependence of a material's magnetic properties. In other words, the magnetic behavior of a material can vary based on the direction in which it is measured or applied. This phenomenon is crucial in determining how magnetic materials respond to external magnetic fields and how they retain magnetization after an external field is removed.