Multiferroics

From Wikipedia, the free encyclopedia

Multiferroics are materials that have coupled electric, magnetic and structural order parameters that result in simultaneous ferroic properties (i.e. ferroelectric, ferromagnetic, or ferroelastic). Some materials having not ferromagnetic but antiferromagnetic, ferrimagnetic, ferrotoroidic, or helimagnetic ordering are accepted as multiferroics as well.

Only a few single phase multiferroic materials exist. This is, amongst other reasons, because the classical ferroelectric perovskites (BaTiO3, PZT, etc) contain d ions with empty shells (e.g. Ti4+ is 3d0) and thus bear no magnetic moment. Exceptions include some orthorhombic manganites, like TbMnO3, and Bi-based perosvkites like BiFeO3 or BiMnO3. In addition, most multiferroics are antiferromagnetic or weak-ferromagnets, BiMnO3 being one of the very few ferromagnetic and ferroelectric multiferroics. Some multiferroics, like TbMnO3, exhibit the magnetoelectric effect. The scientific community has a large interest in this subgroup of multiferroic materials, because promising phenomena exist in these materials for technical applications.


Languages