Double refraction | Definition, Examples, & Facts
Double refraction, an optical property in which a single ray of unpolarized light entering an anisotropic medium is split into two rays, each traveling in a
In double refraction, light enters a crystal the optical properties of which differ along two or more of the crystal axes. What is observed depends on the angle of the beam with respect to the entrant face. Double refraction was first observed in 1669 by Erasmus Bartholin in experiments with Iceland spar crystal and elucidated in 1690 by Huygens.
We observe that in double refraction light is unpolarized and it divides into two rays when passed through the doubly refracting crystal that deviates the rays into different directions. We can also observe the Double refraction of light by comparing two materials, viz: glass and calcite.
If the incident ray enters the crystal along the direction of its optic axis, however, the light ray will not become divided. In double refraction, the ordinary ray and the extraordinary ray are polarized in planes vibrating at right angles to each other.
All transparent crystals except those of the cubic system, which are normally optically isotropic, exhibit the phenomenon of double refraction: in addition to calcite, some well-known examples are ice, mica, quartz, sugar, and tourmaline. Other materials may become birefringent under special circumstances.
Birefringence is responsible for the phenomenon of double refraction of light. It is a phenomenon in which a ray of light, when incident upon a birefringent material, gets split by polarization into two rays going in slightly different paths. 3. What causes double refraction?
Double refraction is caused by all crystals, except those in the cubic system; such material is called anisotropic or duplicate media. Double refraction will not see in any direction along the optic axis, or when viewed at right angles to such an axis. This effect has been applied to polariscopes, dichroscope, or Nicolls crosses.
Double refraction, an optical property in which a single ray of unpolarized light entering an anisotropic medium is split into two rays, each traveling in a
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