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The 'cubic crystal system' (or 'isometric') is a crystal system where the unit cell is in the shape of a cube. This is one of the most common and simplest shapes found in metallic crystals.

Contents

Bravais lattices and point/space groups

Atomic packing factors and examples

Single-element lattices

Multi-element compounds

See also

References

Bravais lattices and point/space groups

The three Bravais lattices which form the cubic crystal system are

The 'simple cubic' system consists of one lattice point on each corner of the cube. Each atom at the lattice points is then shared equally between eight adjacent cubes, and the unit cell therefore contains in total one atom (1/8
★ 8). The 'body centered' cubic system has one atom in the center of the unit cell in addition to the eight corner points. It has a contribution from 2 atoms per cell ((1/8)
★ 8 + 1). Finally, the 'face centered' cubic has atoms on the faces of the cube of which each unit cube gets exactly one half contribution, giving a total of 4 atoms per unit cell ((1/8 for each corner)
★ 8 corners + (1/2 for each face)
★ 6 faces). Attempting to create a C-centered cubic crystal system would result in a simple tetragonal Bravais lattice.
There are 8 lattice points on a simple cubic for each corner of the shape. There are 9 lattice points for a body centered because of the extra point in the center of the unit. There are 14 lattice points on a face centered cubic.
The point groups and space groups that fall under this crystal system are listed below, using the international notation.

Point group	#	Cubic space groups
$23,!$	195-199	P23	F23	I23	P213	I213
	200-206	Pm	Pn	Fm	Fd	I	Pa	Ia
$432,!$	207-214	P432	P4232	F432	F4132	I432	P4332	P4132	I4132
	215-220	P3m	F3m	I3m	P3n	F3c	I3d
	221-230	Pmm	Pnn	Pmn	Pnm	Fmm	Fmc	Fdm	Fdc
		Imm	Iad

There are 36 cubic space groups, of which 10 are hexoctahedral: Fd3c, Fd3m, Fm3c, Fm3m, Ia3d, Im3m, Pm3m, Pm3n, Pn3m, and Pn3n. Other terms for hexoctahedral are normal class, holohedral, ditesseral central class, galena type.

Atomic packing factors and examples

The cubic crystal system is one of the most common crystal systems found in elemental metals, and naturally occurring crystals and minerals. One very useful way to analyse a crystal is to consider the atomic packing factor. In this approach, the amount of space which is filled by the atoms is calculated under the assumption that they are spherical.

Single-element lattices

Assuming one atom per lattice point, the atomic packing factor of the simple cubic system is only 0.524. Due to its low density, this is a high energy structure and is rare in nature, but is found in Polonium ^[1]. Similarly, the body centered structure has a density of 0.680. The higher density makes this a low energy structure which is fairly common in nature. Examples include iron, chromium, and tungsten.
Finally, the face centered cubic crystals have a density of 0.741, a ratio that it shares with several other systems, including hexagonal close packed and one version of tetrahedral BCC. This is the most tightly packed crystal possible with spherical atoms. Due to its low energy, FCC is extremely common, examples include lead (for example in lead(II) nitrate), aluminum, copper, and gold.

Multi-element compounds

When the compound is formed of two elements whose ions are of roughly the same size, they have what is called the 'interpenetrating simple cubic' structure, where two atoms of a different type have individual simple cubic crystals. However, the unit cell consists of the atom of one being in the middle of the 8 vertices, structurally resembling body centered cubic. The most common example is caesium chloride CsCl.
However, if the cation is slightly smaller than the anion (a cation/anion radius ratio of 0.414 to 0.732), the crystal forms a different structure, 'interpenetrating FCC'. When drawn separately, both atoms are arranged in an FCC structure. The unit cell for this is shown to the left.

See also

★ Reciprocal lattice

★ Atomium: building which is a model of a bcc unit cell, with vertical body diagonal.

★ Dislocations

References

★ Hurlbut, Cornelius S.; Klein, Cornelis, 1985, ''Manual of Mineralogy'', 20th ed., Wiley, ISBN 0-471-80580-7
1.