What is the Difference Between Uniaxial and Biaxial Crystals?
🆚 Go to Comparative Table 🆚Uniaxial and biaxial crystals are two types of anisotropic materials that exhibit different optical properties and behaviors due to their crystal structures. The main differences between them are:
- Optic Axes: Uniaxial crystals have a single optic axis, while biaxial crystals have two distinct optic axes that intersect at a common point, known as the biaxial point.
- Refractive Indices: Uniaxial crystals have two principal refractive indices (nω and ne), while biaxial crystals have three principal refractive indices (nα, nβ, and nγ).
- Double Refraction: When a light beam passes through a uniaxial crystal, it splits into two rays: the ordinary ray (o-ray) and the extraordinary ray (E-ray). In biaxial crystals, the light beam experiences double refraction unless it travels parallel to the optic axes.
- Crystallographic Axes: All minerals with crystals that belong to the tetragonal or hexagonal crystal systems are uniaxial, meaning that they have only one optic axis coincident with the c crystallographic axis. Biaxial crystals have two optic axes that are not coincident with the crystallographic axes (a, b, or c).
Examples of uniaxial crystals include calcite, KDP, quartz, and rutile. Biaxial crystals are found in orthorhombic, monoclinic, or triclinic crystalline structures. Both uniaxial and biaxial crystals are essential components in various scientific and technological applications due to their distinct optical and mechanical characteristics.
Comparative Table: Uniaxial vs Biaxial Crystals
Uniaxial and biaxial crystals are two types of anisotropic materials that exhibit different optical and mechanical characteristics. Here is a table summarizing the differences between uniaxial and biaxial crystals:
Property | Uniaxial Crystals | Biaxial Crystals |
---|---|---|
Optic Axes | Single optic axis | Two optic axes |
Refractive Indices | Two principal refractive indices | Three principal refractive indices |
Light Beam Behavior | When a light beam passes through a uniaxial crystal, it splits into two fractions: the ordinary ray and the extraordinary ray. | When a light beam passes through a biaxial crystal, it splits into two fractions, both of which are extraordinary waves (e-rays) with different directions and speeds. |
Crystal Systems | Uniaxial crystals can be found in various crystal systems, but when described as "biaxial positive" or "biaxial negative", they refer to the sign of the optical activity. | Biaxial crystals typically belong to orthorhombic, monoclinic, or triclinic crystal systems. |
Examples | Calcite, KDP, quartz, rutile | Crystalline structures with orthorhombic, monoclinic, or triclinic symmetries |
Uniaxial crystals have a single optic axis and two principal refractive indices, while biaxial crystals have two optic axes and three principal refractive indices. When light beams pass through these crystals, they split into different fractions, with uniaxial crystals separating into ordinary and extraordinary rays, and biaxial crystals separating into two extraordinary waves.
- Crystalline vs Polycrystalline
- X-ray Crystallography vs X-ray Diffraction
- Crystals vs Quasicrystals
- Polycrystalline vs Monocrystalline
- Lattice vs Crystal
- Crystalline vs Noncrystalline Solids
- Nanocrystalline vs Polycrystalline
- Minerals vs Crystals
- Crystallization vs Recrystallization
- Atomic Structure vs Crystal Structure
- Crystal vs Diamond
- Glass vs Crystal
- Grain Size vs Crystallite Size
- Amorphous vs Crystalline Solid
- Hexagon vs Monoclinic Unit Cell
- Amorphous vs Crystalline Polymers
- Dichroism vs Birefringence
- Lattice vs Unit Cell
- NMR vs X-Ray Crystallography