Primitive lattices are the most basic types of crystal lattices, making up the foundation of crystal structures. They consist of points that are arranged in a periodic pattern in three dimensions. Each of these points can represent a unit cell, and in primitive lattices, there is exactly one lattice point per unit cell. This simplicity makes primitive lattices an ideal starting point for understanding the more complex structures found in crystallography.
In three-dimensional space, there are several primitive lattice types, each defined by different arrangements and angles between their axes:
- Cubic lattice: All sides are equal, and all angles are 90°.
- Tetragonal lattice: Two sides are equal, one is different, and all angles are 90°.
- Orthorhombic lattice: All sides are different, but all angles are 90°.
- Rhombohedral lattice: All sides are equal, but none of the angles is 90°.
- Triclinic lattice: All sides and angles are different, with no 90° angles.
These variations allow each lattice to serve distinct roles in forming different crystal structures. Both rhombohedral and triclinic lattices stand out among primitive lattices as their unit cell angles deviate from 90°, making them unique in occupancy and symmetry.