Birefringence: Double Refraction in Anisotropic Materials

Birefringence is a phenomenon where a material splits incoming light into two rays traveling at different speeds due to having different refractive indices along different optical axes.

How it works:

  • Occurs in anisotropic materials like calcite or quartz.
  • When light enters such a material, it divides into an ordinary ray and an extraordinary ray, each experiencing a different refractive index.
  • These rays travel at different velocities and exit the material with a relative phase shift, leading to double images or polarization effects.

Observable effects:

  • A clear double image when viewing objects through birefringent crystals.
  • Bright interference colors under crossed polarizers in polarized light microscopy.

Applications:

  • Used in polarized light microscopy, optical mineralogy, LCD displays, and stress analysis through photoelasticity.

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