In crystallography, a fractional coordinate system (crystal coordinate system) is a coordinate system in which basis vectors used to describe the space are the lattice vectors of a crystal (periodic) pattern. The selection of an origin and a basis define a unit cell, a parallelotope (i.e., generalization of a parallelogram (2D) or parallelepiped (3D) in higher dimensions) defined by the lattice basis vectors a 1 , a 2 , … , a d {\displaystyle \mathbf {a} _{1},\mathbf {a} _{2},\dots ,\mathbf {a} _{d}} where d {\displaystyle d} is the dimension of the space. These basis vectors are described by lattice parameters (lattice constants) consisting of the lengths of the lattice basis vectors a 1 , a 2 , … , a d {\displaystyle a_{1},a_{2},\dots ,a_{d}} and the angles between them α 1 , α 2 , … , α d ( d − 1 ) 2 {\displaystyle \alpha _{1},\alpha _{2},\dots ,\alpha _{\frac {d(d-1)}{2}}} .
Most cases in crystallography involve two- or three-dimensional space. In the three-dimensional case, the basis vectors a 1 , a 2 , a 3 {\displaystyle \mathbf {a} _{1},\mathbf {a} _{2},\mathbf {a} _{3}} are commonly displayed as a , b , c {\displaystyle \mathbf {a} ,\mathbf {b} ,\mathbf {c} } with their lengths denoted by a , b , c {\displaystyle a,b,c} respectively, and the angles denoted by α , β , γ {\displaystyle \alpha ,\beta ,\gamma } , where conventionally, α {\displaystyle \alpha } is the angle between b {\displaystyle \mathbf {b} } and c {\displaystyle \mathbf {c} } , β {\displaystyle \beta } is the angle between c {\displaystyle \mathbf {c} } and a {\displaystyle \mathbf {a} } , and γ {\displaystyle \gamma } is the angle between a {\displaystyle \mathbf {a} } and b {\displaystyle \mathbf {b} } .