double-refracting crystal
1. What Double Refraction (Birefringence) Is
Double refraction / birefringence = a single incident ray splits into two refracted rays with orthogonal polarizations and different speeds/directions inside an anisotropic crystal (e.g., calcite , quartz).
- Ordinary ray (): obeys Snell's law, speed same all directions; wavefront spherical; refractive index constant.
- Extraordinary ray (): does not obey ordinary Snell's (direction depends on crystal orientation), speed varies with angle to optic axis; wavefront ellipsoidal; index varies between and .
2. Optic Axis and Principal Section
- Optic axis: direction in crystal where and travel with same speed (no double refraction along this axis). In calcite, optic axis is diagonal of rhombohedron.
- Principal section: plane containing optic axis and incident ray's normal — and both lie in this plane (for calcite).
3. Huygens Construction
Two wavelets: sphere () radius and ellipsoid () with semi-axes along optic axis and perpendicular. Tangent envelope gives refracted wavefront.
For negative crystal (calcite, ): -ellipsoid outside -sphere except along optic axis. For positive (quartz, ): inside.
4. Worked Illustration
Incident ray at 45° to calcite surface, optic axis inclined: splits into o (μo≈1.658) and e (μe≈1.486) with separation visible as double image through calcite slab (text appears doubled).
Along optic axis: μe = μo ⇒ no separation (single image).
Through Nicol prism? Uses birefringence + total internal reflection of o-ray (next topic).
5. Uses
Wave plates (quarter/half-wave use to introduce phase ), compensators, polarizing prisms.
6. Exam Points
- Define birefringence, vs ray differences — 5 marks, very frequent.
- Sketch optic axis, spherical vs ellipsoidal wavefronts — 5 marks, frequent.
- Negative vs positive crystal — 3-5 marks, frequent.
- Simple Snell's for vs angle-dependent for — 3 marks.