Ladder graph

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Template:Expert-subject In crystallography, a fractional coordinate system is a coordinate system in which the edges of the unit cell are used as the basic vectors to describe the positions of atomic nuclei. The unit cell is a parallelepiped defined by the lengths of its edges a, b, c and angles between them α, β, γ as shown in the figure below.

Unit cell definition using parallelepiped with lengths a, b, c and angles between the sides given by α,β,γ[1]

Conversion to cartesian coordinates

If the fractional coordinate system has the same origin as the cartesian coordinate system, the a-axis is collinear with the x-axis, and the b-axis lies in the xy-plane, fractional coordinates can be converted to cartesian coordinates through the following transformation matrix:[2][3][4]

[xyz]=[abcos(γ)ccos(β)0bsin(γ)ccos(α)cos(β)cos(γ)sin(γ)00cvsin(γ)][a^b^c^]

where v is the volume of a unit parallelepiped defined as

v=1cos2(α)cos2(β)cos2(γ)+2cos(α)cos(β)cos(γ)

For the special case of a monoclinic cell (a common case) where α=γ=90° and β>90°, this gives:

x=axfrac+czfraccos(β)
y=byfrac
z=czfracsin(β)

Conversion from cartesian coordinates

The above fractional-to-cartesian transformation can be inverted as follows

[a^b^c^]=[1acos(γ)asin(γ)cos(α)cos(γ)cos(β)avsin(γ)01bsin(γ)cos(β)cos(γ)cos(α)bvsin(γ)00sin(γ)cv][xyz]

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References

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