Cubic crystal system


In crystallography, the cubic 'crystal system 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 crystals and minerals.
There are three main varieties of these crystals:
  • Primitive cubic
  • Body-centered cubic
  • Face-centered cubic
Note: the term fcc is often used synonymously for the
cubic close-packed or ccp structure occurring in metals. However, fcc stands for a face-centered cubic Bravais lattice, which is not necessarily close-packed when a motif is set onto the lattice points. E.g. the diamond and the zincblende lattices are fcc' but not close-packed.
Each is subdivided into other variants listed below. Although the unit cells in these crystals are conventionally taken to be cubes, the primitive unit cells often are not.

Bravais lattices

The three Bravais latices in the cubic crystal system are:
Bravais latticePrimitive
cubic
Body-centered
cubic
Face-centered
cubic
Pearson symbolcPcIcF
Unit cell

The primitive cubic lattice consists of one lattice point on each corner of the cube; this means each simple cubic unit cell has in total one lattice point. Each atom at a lattice point is then shared equally between eight adjacent cubes, and the unit cell therefore contains in total one atom.
The body-centered cubic lattice has one lattice point in the center of the unit cell in addition to the eight corner points. It has a net total of two lattice points per unit cell.
The face-centered cubic lattice has lattice points on the faces of the cube that each give exactly one half contribution, in addition to the corner lattice points, giving a total of four lattice points per unit cell.
The face-centered cubic lattice is closely related to the Hexagonal [crystal system|hexagonal close packed] system, where the two systems differ only in the relative placements of their hexagonal layers. The Miller index| plane of a face-centered cubic lattice is a hexagonal grid.
Attempting to create a base-centered cubic lattice results in a simple tetragonal Bravais lattice.
Coordination number is the number of nearest neighbors of a central atom in the structure. Each sphere in a cP lattice has coordination number 6, in a cI lattice 8, and in a cF lattice 12.
Atomic packing factor is the fraction of volume that is occupied by atoms. The cP lattice has an APF of about 0.524, the cI lattice an APF of about 0.680, and the cF lattice an APF of about 0.740.

Crystal classes

The isometric crystal system class names, point groups, type, examples, international tables for crystallography space group number, and space groups are listed in the table below. There are a total 36 cubic space groups.
Other terms for hexoctahedral are: normal class, holohedral, ditesseral central class, galena type.

Single element structures

As a rule, since atoms in a solid attract each other, the more tightly packed arrangements of atoms tend to be more common. Accordingly, the primitive cubic structure, with especially low atomic packing factor, is rare in nature, but is found in polonium. The bcc and fcc, with their higher densities, are both quite common in nature. Examples of bcc include iron, chromium, tungsten, and niobium. Examples of fcc include aluminium, copper, gold and silver.
Another important cubic crystal structure is the diamond cubic structure, which can appear in carbon, silicon, germanium, and tin. Unlike fcc and bcc, this structure is not a lattice, since it contains multiple atoms in its primitive cell. Other cubic elemental structures include the A15 structure found in tungsten, and the extremely complicated structure of manganese.

Multi-element structures

Compounds that consist of more than one element often have crystal structures based on the cubic crystal system. Some of the more common ones are listed here. These structures can be viewed as two or more interpenetrating sublattices where each sublattice occupies the interstitial sites of the others.

Caesium chloride structure

One structure is the "interpenetrating primitive cubic" structure, also called a "caesium chloride" or B2 structure. This structure is often confused for a body-centered cubic structure because the arrangement of atoms is the same. However, the caesium chloride structure has a basis composed of two different atomic species. In a body-centered cubic structure, there would be translational symmetry along the direction. In the caesium chloride structure, translation along the direction results in a change of species. The structure can also be thought of as two separate simple cubic structures, one of each species, that are superimposed within each other. The corner of the chloride cube is the center of the caesium cube, and vice versa.
It works the same way for the NaCl structure described in the next section. If you take out the Cl atoms, the leftover Na atoms still form an FCC structure, not a simple cubic structure.
In the unit cell of CsCl, each ion is at the center of a cube of ions of the opposite kind, so the coordination number is eight. The central cation is coordinated to 8 anions on the corners of a cube as shown, and similarly, the central anion is coordinated to 8 cations on the corners of a cube. Alternately, one could view this lattice as a simple cubic structure with a secondary atom in its cubic void.
In addition to caesium chloride itself, the structure also appears in certain other alkali halides when prepared at low temperatures or high pressures. Generally, this structure is more likely to be formed from two elements whose ions are of roughly the same size.
The space group of the caesium chloride structure is called Pmm, or "221". The Strukturbericht designation is "B2".
There are nearly a hundred rare earth intermetallic compounds that crystallize in the CsCl structure, including many binary compounds of rare earths with magnesium, and with elements in groups 11 element|11], 12, and 13 element|13]. Other compounds showing caesium chloride like structure are CsBr, CsI, high-temperature RbCl, AlCo, AgZn, BeCu, MgCe, RuAl and SrTl.

Rock-salt structure

The space group of the rock-salt or halite structure is denoted as Fmm, or "225". The Strukturbericht designation is "B1".
In the rock-salt structure, each of the two atom types forms a separate face-centered cubic lattice, with the two lattices interpenetrating so as to form a 3D checkerboard pattern. The rock-salt structure has octahedral coordination: Each atom's nearest neighbors consist of six atoms of the opposite type, positioned like the six vertices of a regular octahedron. In sodium chloride there is a 1:1 ratio of sodium to chlorine atoms.  The structure can also be described as an FCC lattice of sodium with chlorine occupying each octahedral void or vice versa.
Examples of compounds with this structure include sodium chloride itself, along with almost all other alkali halides, and "many divalent metal oxides, sulfides, selenides, and tellurides". According to the radius ratio rule, this structure is more likely to be formed if the cation is somewhat smaller than the anion.
The interatomic distance in some rock-salt-structure crystals are: 2.3 Å for NaF, 2.8 Å for NaCl, and 3.2 Å for SnTe. Most of the alkali metal hydrides and halides have the rock salt structure, though a few have the caesium chloride structure instead.
OxidesSulfidesSelenidesTelluridesPolonides
MagnesiumMagnesium oxideMagnesium sulfideMagnesium selenideMagnesium telluride
CalciumCalcium oxideCalcium sulfideCalcium selenideCalcium tellurideCalcium polonide
StrontiumStrontium oxideStrontium sulfideStrontium selenideStrontium tellurideStrontium polonide
BariumBarium oxideBarium sulfideBarium selenideBarium tellurideBarium polonide

OxidesSulfidesSelenidesTelluridesPolonides
ScandiumScandium monosulfide
YttriumYttrium monosulfide
LanthanumLanthanum monosulfide
CeriumCerium monosulfideCerium monoselenideCerium monotelluride
PraseodymiumPraseodymium monosulfidePraseodymium monoselenidePraseodymium monotelluride
NeodymiumNeodymium monosulfideNeodymium monoselenideNeodymium monotelluride
Promethium????
SamariumSamarium monosulfideSamarium monoselenideSamarium monotellurideSamarium monopolonide
EuropiumEuropium monoxideEuropium monosulfideEuropium monoselenideEuropium monotellurideEuropium monopolonide
GadoliniumGadolinium monosulfide
TerbiumTerbium monosulfideTerbium monopolonide
DysprosiumDysprosium monosulfideDysprosium monopolonide
HolmiumHolmium monosulfideHolmium monopolonide
ErbiumErbium monosulfide
ThuliumThulium monosulfideThulium monopolonide
YtterbiumYtterbium monoxideYtterbium monosulfideYtterbium monopolonide
LutetiumLutetium monosulfideLutetium monopolonide
Actinium????
ThoriumThorium monosulfideThorium monoselenide
Protactinium????
UraniumUranium monosulfideUranium monoselenideUranium monotelluride
NeptuniumNeptunium monosulfideNeptunium monoselenideNeptunium monotelluride
PlutoniumPlutonium monosulfidePlutonium monoselenidePlutonium monotelluride
AmericiumAmericium monosulfideAmericium monoselenideAmericium monotelluride
CuriumCurium monosulfideCurium monoselenideCurium monotelluride

CarbidesNitrides
TitaniumTitanium carbideTitanium nitride
ZirconiumZirconium carbideZirconium nitride
HafniumHafnium carbideHafnium nitride
VanadiumVanadium carbideVanadium nitride
NiobiumNiobium carbideNiobium nitride
TantalumTantalum carbide
ChromiumChromium nitride

Many transition metal monoxides also have the rock salt structure oxide|TiO], VO, CrO, MnO, FeO, CoO, Nickel. The early actinoid monocarbides also have this structure.

Fluorite structure

Much like the rock salt structure, the [fluorite structure
is also an Fmm structure but has 1:2 ratio of ions. The anti-fluorite structure is nearly identical, except the positions of the anions and cations are switched in the structure. They are designated Wyckoff positions 4a and 8c whereas the rock-salt structure positions are 4a and 4b.

Zincblende structure

The space group of the Zincblende structure is called F3m, or 216. The Strukturbericht designation is "B3".
The Zincblende structure is named after the mineral zincblende, one form of zinc sulfide. As in the rock-salt structure, the two atom types form two interpenetrating face-centered cubic lattices. However, it differs from rock-salt structure in how the two lattices are positioned relative to one another. The zincblende structure has tetrahedral coordination: Each atom's nearest neighbors consist of four atoms of the opposite type, positioned like the four vertices of a regular tetrahedron. In zinc sulfide the ratio of zinc to sulfur is 1:1. Altogether, the arrangement of atoms in zincblende structure is the same as diamond cubic structure, but with alternating types of atoms at the different lattice sites. The structure can also be described as an FCC lattice of zinc with sulfur atoms occupying half of the tetrahedral voids or vice versa.
Examples of compounds with this structure include zincblende itself, lead nitrate, many compound semiconductors, and a wide array of other binary compounds. The boron group pnictogenides usually have a zincblende structure, though the nitrides are more common in the wurtzite structure, and their zincblende forms are less well known polymorphs.
FluoridesChloridesBromidesIodides
CopperCopper fluorideCopper chlorideCopper bromideCopper iodide

SulfidesSelenidesTelluridesPolonides
BerylliumBeryllium sulfideBeryllium selenideBeryllium tellurideBeryllium polonide
ZincZinc sulfideZinc selenideZinc tellurideZinc polonide
CadmiumCadmium sulfideCadmium selenideCadmium tellurideCadmium polonide
MercuryMercury sulfideMercury selenideMercury telluride

This group is also known as the II-VI family of compounds, most of which can be made in both the zincblende or wurtzite form.
NitridesPhosphidesArsenidesAntimonides
BoronBoron nitride*Boron phosphideBoron arsenideBoron antimonide
AluminiumAluminium nitride*Aluminium phosphideAluminium arsenideAluminium antimonide
GalliumGallium nitride*Gallium phosphideGallium arsenideGallium antimonide
IndiumIndium nitride*Indium phosphideIndium arsenideIndium antimonide

This group is also known as the III-V family of compounds.

Heusler structure

The Heusler structure, based on the structure of Cu2MnAl, is a common structure for ternary compounds involving transition metals. It has the space group Fmm, and the Strukturbericht designation is L21. Together with the closely related half-Heusler and inverse-Huesler compounds, there are hundreds of examples.

Iron monosilicide structure

The space group of the iron monosilicide structure is P213, and the Strukturbericht designation is B20. This is a chiral structure, and is sometimes associated with helimagnetic properties. There are four atoms of each element for a total of eight atoms in the unit cell.
Examples occur among the transition metal silicides and germanides, as well as a few other compounds such as gallium palladide.
SilicidesGermanides
ManganeseManganese monosilicideManganese germanide
IronIron monosilicideIron germanide
CobaltCobalt monosilicideCobalt germanide
ChromiumChromium silicideChromium germanide

Weaire–Phelan structure

A Weaire–Phelan structure has Pmn symmetry.
It has three orientations of stacked tetradecahedrons with pyritohedral cells in the gaps. It is found as a crystal structure in chemistry where it is usually known as a "type I clathrate structure". Gas hydrates formed by methane, propane, and carbon dioxide at low temperatures have a structure in which water molecules lie at the nodes of the Weaire–Phelan structure and are hydrogen bonded together, and the larger gas molecules are trapped in the polyhedral cages.