In physics, ferroics is the study of ferromagnets, ferroelectrics, and ferroelastics.

Phase transitions

The basis of ferroics is to understand large changes in physical characteristics that can occur over a narrow temperature range. Changes in physical characteristics occur when phase transitions it undergoes a spontaneous phase transition. Such a transition typically results in a small deviation from the nonferroic crystal structure, but with a different shape of the unit cell, the point symmetry of the material is reduced. This breaking of symmetry allows the formation of the ferroic phase.

includes a spontaneous dipole moment unit cells gives rise to a significant electric field.

Ferroelectrics cannot exist in a centrosymmetric.

The spontaneous magnetization of a ferromagnet can be attributed to a breaking of point symmetry in switching from the paramagnetic is known as the Curie temperature.

In ferroelastic crystals, in going from the nonferroic (or prototypic phase) to the ferroic phase, a spontaneous strain is induced. An example of a ferroelastic phase transition is when the crystal structure spontaneously changes from a tetragonal structure (a square prism shape) to a monoclinic structure (a general parallelepiped). Here the shapes of the unit cell before and after the phase transition are different, inducing a strain within the material.

Variants

Multiferroic materials exhibit more than one ferroic property simultaneously in a single phase.

A fourth ferroic order termed ferrotoroidic order has been proposed.

Many ferroic phase transitions have been studied under non-equilibrium conditions. Under energy disspative condition, quantum system or event colloid particles may shows ferrioic-like order which can be regarded as a nonequilibrium analogue to ferroic material. For example, chemically reactive colloidal particles have been observed to exhibit criticality and long-range order, collectively referred to as ferrochemical order.

See also

• Piezoelectricity

• Pyroelectricity

References