(a) The Unit Cell,
(b) The Crystal Lattice,
(c) The Origin in Reciprocal Space,
(d) The Origin in the Crystal,
(e) The Space-Group Symmetry of the Crystal.
[5 Marks]
(a) The Unit Cell
Chosen by the crystallographer. The 'Unit cell' in 3D space is a parallelepiped. It is
a repeat unit which when attached to itself many times over, forms the 3D structure of
the material. Cubic, hexagonal and trigonal structures have very different unit cells.
(b) The Crystal Lattice
Due to the packing of atoms/molecules. The crystal lattice is the consequence of how
atoms/molecules pack together throughout the crystal structure. The crystal lattice
can be drawn and it shows the positions of the atoms/molecules in the crystal. They are
represented as points. The lattice can be thought of as an infinite set of equally spaced
points.
(c) The Origin in Reciprocal Space
Not chosen by the crystallographer, nor due to the packing of atoms/molecules. It corresponds
to the natural point that the 'straight-through' X-ray beam contacts the Ewald sphere. The origin is assigned
the hkl values (0,0,0).
(d) The Origin in the Crystal
The origin of the crystal lattice and the origin of the unit cell are chosen by the crystallographer.
The origin of the unit cell is chosen to conveniently describe the contents of the unit cell e.g.
points of high symmetry such as on an axis or where two or more axes intersect. Unit cells are also
chosen to contain the smallest number of lattice points.
(e) The Space-Group Symmetry of the Crystal
Due to the packing of atoms/molecules. The 230 Space Groups describe all the combinations of
rotation and screw axes, mirror and glide planes, plus points of inversion that can be applied
to the different crystal types. Therefore, the Space-Group symmetry is a consequence of the
the crystal structure and hence the packing of its atoms/molecules.
[5 Marks]
The Laue Class is the name used to describe a class of
symmetry point groups that are associated with a crystal system.
A Point Group may be defined as any group of symmetry operators that
leave a point in space unmoved. The simplest point groups are due
to rotation axis (point groups 1, 2, 3, 4 and 6) and rotary-inversion
axes (point groups -1, m(-2), -3, -4 and -6). All of the other 32
crystallographic point group are combinations of these 10 point
groups. For each Laue Class there can be two or more point groups (each
representing a specific symmetry element.
Of the 32 crystallographic point groups, 11 possess a centre of inversion
and are called centrosymmetric. These are known as the Laue classes and
describe 3-dimensional diffraction symmetry (the symmetry applied to
diffraction data).
| Crystal System | Laue Classes | |
|---|---|---|
| Triclinic | -1 | |
| Monoclinic | 2/m | |
| Orthorhombic | mmm | |
| Tetragonal | 4/m | 4/mmm |
| Trigonal | -3 | -3m |
| Hexagonal | 6/m | 6/mmm |
| Cubic | m-3 | m-3m |
Example 1:
Monoclinic Crystal System - Laue class 2/m
This has one mirror plane perpendicular to a two-fold rotation axis.The trans isomer of E-1,2-dibromoethylene has a Laue class of 2/m.
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| Top view down 2 axis | Side view |
Example 2:
Orthorhombic Crystal System - Laue class mmm
This has 3 mirror planes, one parallel to each of the x,y,z axes, and thus perpendicular to each other.The oxalate anion has 3 mutually perpendicular mirror planes, 3 twofold rotation axes, and a point of inversion and has a Laue class of mmm.
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| Top view | Side view |