Editing Birefringence

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[[Birefringence]], or double refraction, is the decomposition of a ray of light into two rays (the ordinary ray and the extraordinary ray) when it passes through certain types of material, such as calcite crystals or boron nitride, depending on the polarization of the light. This effect can occur only if the structure of the material is anisotropic (directionally dependent). If the material has a single axis of anisotropy or optical axis, (i.e. it is uniaxial) birefringence can be formalized by assigning two different refractive indices to the material for different polarizations.
[[Birefringenc]]e, or double refraction, is the decomposition of a ray of light into two rays (the ordinary ray and the extraordinary ray) when it passes through certain types of material, such as calcite crystals or boron nitride, depending on the polarization of the light. This effect can occur only if the structure of the material is anisotropic (directionally dependent). If the material has a single axis of anisotropy or optical axis, (i.e. it is uniaxial) birefringence can be formalized by assigning two different refractive indices to the material for different polarizations.


The reason for birefringence is the fact that in anisotropic media the electric field vector \vec E and the dielectric displacement \vec D can be nonparallel (namely for the extraordinary polarisation), although being linearly related.
The reason for birefringence is the fact that in anisotropic media the electric field vector \vec E and the dielectric displacement \vec D can be nonparallel (namely for the extraordinary polarisation), although being linearly related.
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