Magneto-optic Kerr effect (MOKE) is one of the magneto-optic effects. It describes the changes of light reflected from magnetized media.
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The light that is reflected from a magnetized surface can change in both polarization and reflected intensity. The effect is identical to the Faraday effect except that the magneto-optical Kerr effect is a measurement of the reflected light, while the Faraday effect is a measurement of the transmitted light. Both effects result from the off-diagonal components of the dielectric tensor . These off-diagonal components give the Magneto Optic material an anisotropic permittivity. The permittivity affects the speed of light in a material:
where is the velocity of light through the material, is the material permittivity, and is the material permeability; and thus the speed of light varies depending on its orientation. This causes fluctuations in the phase of polarized incident light.
MOKE can be further categorized by the direction of the magnetization vector with respect to the reflecting surface and the plane of incidence.
When the magnetization vector is perpendicular to the reflection surface and parallel to the plane of incidence, the effect is called the polar Kerr effect. To simplify the analysis, near normal incidence is usually employed when doing experiments in the polar geometry.
In the longitudinal effect, the magnetization vector is parallel to both the reflection surface and the plane of incidence. The longitudinal setup involves light reflected at an angle from the reflection surface and not normal to it, as above in the polar MOKE case. In the same manner, linearly polarized light incident on the surface becomes elliptically polarized, with the change in polarization directly proportional to the component of magnetization that is parallel to the reflection surface and parallel to the plane of incidence. This elliptically polarized light to first-order has two perpendicular vectors, namely the standard Fresnel amplitude coefficient of reflection and the Kerr coefficient . The Kerr coefficient is typically much smaller than the coefficient of reflection.
When the magnetization is perpendicular to the plane of incidence and parallel to the surface it is said to be in the transverse configuration. In this case, the incident light is also not normal to the reflection surface but instead of measuring the polarity of the light after reflection, the reflectivity is measured. This change in reflectivity is proportional to the component of magnetization that is perpendicular to the plane of incidence and parallel to the surface, as above. If the magnetization component points to the right of the incident plane, as viewed from the source, then the Kerr vector adds to the Fresnel amplitude vector and the intensity of the reflected light is . On the other hand, if the component of magnetization component points to the left of the incident plane as viewed from the source, the Kerr vector subtracts from the Fresnel amplitude and the reflected intensity is given by .
In addition to the polar, longitudinal and transverse Kerr effect which depend linear on the respective magnetization components, there are also higher order quadratic effects, for which the Kerr angle depends on product terms involving the polar, longitudinal and transverse magnetization components. Those effects are referred to as Voigt effect or quadratic Kerr effect. Quadratic magneto-optic Kerr effect (QMOKE) is found strong in Heusler alloys such as Co2FeSi and Co2MnGe[1] [2]
A Kerr Microscope relies on the MOKE in order to image differences in magnetic orientation. In addition to a regular optical microscope, a polarizer and analyzer are needed as a source and sensor for polarized light. Because the different MOKE geometries require different polarized light, the polarizer should have the option to change the polarization of the incident light (circular, linear, and elliptical). When the polarized light is reflected off the sample material, a change in any combination of the following may occur: Kerr rotation, Kerr Ellipticity, or polarized amplitude. The analyzer then receives the incoming light and passes the data to a computer system which can back out the magnetic field from these changes in polarization.
In conjunction with the Kerr Microscope, Magneto Optical Imaging Films (MOIF) can be used to better image magnetic domains in ferromagnetic materials. These films can be made out of an Yttrium Iron Garnet and are usually substituted with certain rare earth elements. Because the manufacturing process of these films is so specialized, they aren't commercially available.
Magneto Optical (MO) Drives were introduced in 1985, and were originally WORM (write once, read many) drives, meaning they could be added to but not erased. Although they are not widely used today, they were reliable both in accurate writing and consistent data retention. Typical sizes ranged from 100 megabytes (MB) up to 9.2 gigabytes (GB). MO drives checked the data as it was being written, and thus took longer than typical CD's or DVD's. However this allowed for increased data integrity.
MO discs were written using laser and an electromagnet. The laser would heat the platter above its Curie Temperature and which point the electromagnet would orient that bit as a 1 or 0. To read, the laser is operated at a lower intensity, and emits polarized light. Reflected light is analyzed showing a noticeable difference between a 0 or 1.
The magneto-optic Kerr effect was discovered in 1877 by John Kerr.[3][4]