Piezomagnetism
Piezo-magnetism is a phenomenon observed in some antiferromagnetic crystals. It is characterized by a linear coupling between the system's magnetic polarisation and mechanical strain. ON a piezomagnetic material, one may induce a spontaneous magnetic moment by applying physical stress, or a physical deformation by applying a magnetic field.
Piezomagnetism differs from the related property of magnetostriction; if an applied magnetic field is reversed in direction, the strain produced changes signs. Additionally, a non-zero piezomagnetic moment can be produced by mechanical strain alone, at zero fields, which is not true of magnetostriction.[1] According to IEEE: "Piezomagnetism is the linear magneto-mechanical effect analogous to the linear electromechanical effect of piezoelectricity. Similarly, magnetostriction and electrostriction are analogous second-order effects. These higher-order effects can be represented as effectively first-order when variations in the system parameters are small compared with the initial values of the parameters".[2]
The piezomagnetic effect is made possible by an absence of certain symmetry elements in a crystal structure; specifically, symmetry under time reversal forbids the property.[3]
The first experimental observation of piezomagnetism was made in 1960, in the fluorides of cobalt and manganese.[4]
The strongest piezomagnet known is uranium dioxide, with magnetoelastic memory switching at magnetic fields near 180,000 Oe.[5]
References
- ^ B. D. Cullity (1971), Fundamentals of magnetostriction. Journal of Metals 1, 323.
- ^ IEEE Std 319-1990 (1991), IEEE Standard on Magnetostrictive Materials: Piezomagnetic Nomenclature.
- ^ I. E. Dzialoshinskii (1958), The problem of piezomagnetism. Soviet Phys. JETP 6, 621.
- ^ A.S. Borovik-Romanov (1960), Piezomagnetism in the antiferromagnetic fluorides of cobalt and manganese. Soviet Phys. JETP 11, 786.
- ^ M. Jaime et al. (2017), Piezomagnetism and magnetoelastic memory in uranium dioxide. Nature Communications 8, 99.