Ferroics in the context of Ferroelasticity


Ferroics in the context of Ferroelasticity

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👉 Ferroics in the context of Ferroelasticity

Ferroelasticity is a phenomenon in which a material may exhibit a spontaneous strain, and is the mechanical equivalent of ferroelectricity and ferromagnetism in the field of ferroics. A ferroelastic crystal has two or more stable orientational states in the absence of mechanical stress or electric field, i.e. remanent states, and can be reproducibly switched between the states by applying a stress or an electric field greater than some critical value. The application of opposite fields leads to hysteresis as the system crosses back and forth across an energy barrier. This transition dissipates an energy equal to the area enclosed by the hysteresis loop.

The transition of the crystal's parent structure to one of its stable ferroelastic strains is typically accompanied by a reduction in the crystal symmetry. The spontaneous change in strain and crystal structure can be associated with a spontaneous change in other observable properties, such as birefringence, optical absorption, and polarizability. In compatible materials, Raman spectroscopy has been used to directly image ferroelastic switching in crystals.

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Ferroics in the context of Multiferroics

Multiferroics are defined as materials that exhibit more than one of the primary ferroic properties in the same phase:

  • ferromagnetism – a magnetisation that is switchable by an applied magnetic field
  • ferroelectricity – an electric polarisation that is switchable by an applied electric field
  • ferroelasticity – a deformation that is switchable by an applied stress

While ferroelectric, ferroelastics, and ferromagnetics are formally multiferroics, these days the term is usually used to describe the magnetoelectric multiferroics that are simultaneously ferromagnetic and ferroelectric. Sometimes the definition is expanded to include nonprimary order parameters, such as antiferromagnetism or ferrimagnetism. In addition, other types of primary order, such as ferroic arrangements of magnetoelectric multipoles of which ferrotoroidicity is an example, were proposed.

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