Ladder graph
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.
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]
where is the volume of a unit parallelepiped defined as
For the special case of a monoclinic cell (a common case) where α=γ=90° and β>90°, this gives:
Conversion from cartesian coordinates
The above fractional-to-cartesian transformation can be inverted as follows
Supporting file formats
References
43 year old Petroleum Engineer Harry from Deep River, usually spends time with hobbies and interests like renting movies, property developers in singapore new condominium and vehicle racing. Constantly enjoys going to destinations like Camino Real de Tierra Adentro. http://www.ruppweb.org/Xray/tutorial/Coordinate%20system%20transformation.htm
- ↑ Unit cell definition using parallelepiped with lengths a, b, c and angles between the edges given by α,β,γ
- ↑ http://graphics.med.yale.edu:5080/TriposBookshelf/sybyl/crystal/crystal_appendix2.html Probably a slightly unstable reference for the transformation matrix
- ↑ OpenBabel source code
- ↑ http://www.angelfire.com/linux/myp/FracCor/fraccor.html Another transformation matrix that is defined differently