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File:Carbon lattice diamond.png
The diamond crystal structure belongs to the face-centered cubic lattice, with a repeated 2-atom pattern.

In crystallography, the terms crystal system, crystal family, and lattice system each refer to one of several classes of space groups, lattices, point groups, or crystals. Informally, two crystals tend to be in the same crystal system if they have similar symmetries, though there are many exceptions to this.

Crystal systems, crystal families, and lattice systems are similar but slightly different, and there is widespread confusion between them: in particular the trigonal crystal system is often confused with the rhombohedral lattice system, and the term "crystal system" is sometimes used to mean "lattice system" or "crystal family".

Space groups and crystals are divided into 7 crystal systems according to their point groups, and into 7 lattice systems according to their Bravais lattices. Five of the crystal systems are essentially the same as five of the lattice systems, but the hexagonal and trigonal crystal systems differ from the hexagonal and rhombohedral lattice systems. The six crystal families are formed by combining the hexagonal and trigonal crystal systems into one hexagonal family, in order to eliminate this confusion.

OverviewEdit

File:Hanksite.JPG
Hexagonal hanksite crystal, with three-fold c-axis symmetry

A lattice system is a class of lattices with the same point group. In three dimensions there are seven lattice systems: triclinic, monoclinic, orthorhombic, tetragonal, rhombohedral, hexagonal, and cubic. The lattice system of a crystal or space group is determined by its lattice but not always by its point group.

A crystal system is a class of point groups. Two point groups are placed in the same crystal system if the sets of possible lattice systems of their space groups are the same. For many point groups there is only one possible lattice system, and in these cases the crystal system corresponds to a lattice system and is given the same name. However, for the five point groups in the trigonal crystal class there are two possible lattice systems for their point groups: rhombohedral or hexagonal. In three dimensions there are seven crystal systems: triclinic, monoclinic, orthorhombic, tetragonal, trigonal, hexagonal, and cubic. The crystal system of a crystal or space group is determined by its point group but not always by its lattice.

A crystal family also consists of point groups and is formed by combining crystal systems whenever two crystal systems have space groups with the same lattice. In three dimensions a crystal family is almost the same as a crystal system (or lattice system), except that the hexagonal and trigonal crystal systems are combined into one hexagonal family. In three dimensions there are six crystal families: triclinic, monoclinic, orthorhombic, tetragonal, hexagonal, and cubic. The crystal family of a crystal or space group is determined by either its point group or its lattice, and crystal families are the smallest collections of point groups with this property.

In dimensions less than three there is no essential difference between crystal systems, crystal families, and lattice systems. There are 1 in dimension 0, 1 in dimension 1, and 4 in dimension 2, called oblique, rectangular, square, and hexagonal.

The relation between three-dimensional crystal families, crystal systems, and lattice systems is shown in the following table:

Crystal family Crystal system Required symmetries of point group Point groups Space groups Bravais lattices Lattice system
Triclinic None 2 2 1 Triclinic
Monoclinic 1 twofold axis of rotation or 1 mirror plane 3 13 2 Monoclinic
Orthorhombic 3 twofold axes of rotation or 1 twofold axis of rotation and two mirror planes. 3 59 4 Orthorhombic
Tetragonal 1 fourfold axis of rotation 7 68 2 Tetragonal
Hexagonal Trigonal 1 threefold axis of rotation 5 7 1 Rhombohedral
18 1 Hexagonal
Hexagonal 1 sixfold axis of rotation 7 27
Cubic 4 threefold axes of rotation 5 36 3 Cubic
Total: 6 7 32 230 14 7

Crystal classesEdit

The 7 crystal systems consist of 32 crystal classes (corresponding to the 32 crystallographic point groups) as shown in the following table.

crystal family crystal system point group / crystal class Schönflies Hermann-Mauguin Orbifold Coxeter Point symmetry Order Group structure
triclinic triclinic-pedial C1 1 11 [ ]+ enantiomorphic polar 1 trivial
triclinic-pinacoidal Ci Template:Overline 1x [2,1+] centrosymmetric 2 cyclic
monoclinic monoclinic-sphenoidal C2 2 22 [2,2]+ enantiomorphic polar 2 cyclic
monoclinic-domatic Cs m *11 [ ] polar 2 cyclic
monoclinic-prismatic C2h 2/m 2* [2,2+] centrosymmetric 4 2×cyclic
orthorhombic orthorhombic-sphenoidal D2 222 222 [2,2]+ enantiomorphic 4 dihedral
orthorhombic-pyramidal C2v mm2 *22 [2] polar 4 dihedral
orthorhombic-bipyramidal D2h mmm *222 [2,2] centrosymmetric 8 2×dihedral
tetragonal tetragonal-pyramidal C4 4 44 [4]+ enantiomorphic polar 4 cyclic
tetragonal-disphenoidal S4 Template:Overline 2x [2+,2] non-centrosymmetric 4 cyclic
tetragonal-dipyramidal C4h 4/m 4* [2,4+] centrosymmetric 8 2×cyclic
tetragonal-trapezoidal D4 422 422 [2,4]+ enantiomorphic 8 dihedral
ditetragonal-pyramidal C4v 4mm *44 [4] polar 8 dihedral
tetragonal-scalenoidal D2d Template:Overline2m or Template:Overlinem2 2*2 [2+,4] non-centrosymmetric 8 dihedral
ditetragonal-dipyramidal D4h 4/mmm *422 [2,4] centrosymmetric 16 2×dihedral
hexagonal trigonal trigonal-pyramidal C3 3 33 [3]+ enantiomorphic polar 3 cyclic
rhombohedral S6 (C3i) Template:Overline 3x [2+,3+] centrosymmetric 6 cyclic
trigonal-trapezoidal D3 32 or 321 or 312 322 [3,2]+ enantiomorphic 6 dihedral
ditrigonal-pyramidal C3v 3m or 3m1 or 31m *33 [3] polar 6 dihedral
ditrigonal-scalahedral D3d Template:Overlinem or Template:Overlinem1 or Template:Overline1m 2*3 [2+,6] centrosymmetric 12 dihedral
hexagonal hexagonal-pyramidal C6 6 66 [6]+ enantiomorphic polar 6 cyclic
trigonal-dipyramidal C3h Template:Overline 3* [2,3+] non-centrosymmetric 6 cyclic
hexagonal-dipyramidal C6h 6/m 6* [2,6+] centrosymmetric 12 2×cyclic
hexagonal-trapezoidal D6 622 622 [2,6]+ enantiomorphic 12 dihedral
dihexagonal-pyramidal C6v 6mm *66 [6] polar 12 dihedral
ditrigonal-dipyramidal D3h Template:Overlinem2 or Template:Overline2m *322 [2,3] non-centrosymmetric 12 dihedral
dihexagonal-dipyramidal D6h 6/mmm *622 [2,6] centrosymmetric 24 2×dihedral
cubic tetrahedral T 23 332 [3,3]+ enantiomorphic 12 alternating
hextetrahedral Td Template:Overline3m *332 [3,3] non-centrosymmetric 24 symmetric
diploidal Th mTemplate:Overline 3*2 [3+,4] centrosymmetric 24 2×alternating
gyroidal O 432 432 [4,3]+ enantiomorphic 24 symmetric
hexoctahedral Oh mTemplate:Overlinem *432 [4,3] centrosymmetric 48 2×symmetric

Point symmetry can be thought of in the following fashion: consider the coordinates which make up the structure, and project them all through a single point, so that (x,y,z) becomes (-x,-y,-z). This is the 'inverted structure'. If the original structure and inverted structure are identical, then the structure is centrosymmetric. Otherwise it is non-centrosymmetric. Still, even for non-centrosymmetric case, inverted structure in some cases can be rotated to align with the original structure. This is the case of non-centrosymmetric achiral structure. If the inverted structure cannot be rotated to align with the original structure, then the structure is chiral (enantiomorphic) and its symmetry group is enantiomorphic.[1]

A direction is called polar if its two directional senses are geometrically or physically different. A polar symmetry direction of a crystal is called a polar axis.[2] Groups containing a polar axis are called polar. A polar crystal possess a "unique" axis (found in no other directions) such that some geometrical or physical property is different at the two ends of this axis. It may develop a dielectric polarization, e.g. in pyroelectric crystals. A polar axis can occur only in non-centrosymmetric structures. There should also not be a mirror plane or 2-fold axis perpendicular to the polar axis, because they will make both directions of the axis equivalent.

The crystal structures of chiral biological molecules (such as protein structures) can only occur in the 11 enantiomorphic point groups (biological molecules are usually chiral).

Lattice systems Edit

The distribution of the 14 Bravais lattice types into 7 lattice systems is given in the following table.

The 7 lattice systems The 14 Bravais Lattices
triclinic (parallelepiped) Triclinic
monoclinic (right prism with parallelogram base; here seen from above) simple base-centered
Monoclinic, simple Monoclinic, centered
orthorhombic (cuboid) simple base-centered body-centered face-centered
Orthohombic, simple Orthohombic, base-centered Orthohombic, body-centered Orthohombic, face-centered
tetragonal (square cuboid) simple body-centered
Tetragonal, simple Tetragonal, body-centered
rhombohedral
(trigonal trapezohedron)
Rhombohedral
hexagonal (centered regular hexagon) Hexagonal
cubic
(isometric; cube)
simple body-centered face-centered
Cubic, simple Cubic, body-centered Cubic, face-centered

Template:- In geometry and crystallography, a Bravais lattice is a category of symmetry groups for translational symmetry in three directions, or correspondingly, a category of translation lattices.

Such symmetry groups consist of translations by vectors of the form

\mathbf{R} = n_1 \mathbf{a}_1 + n_2 \mathbf{a}_2 + n_3 \mathbf{a}_3,

where n1, n2, and n3 are integers and a1, a2, and a3 are three non-coplanar vectors, called primitive vectors.

These lattices are classified by space group of the translation lattice itself; there are 14 Bravais lattices in three dimensions; each can apply in one lattice system only. They represent the maximum symmetry a structure with the translational symmetry concerned can have.

All crystalline materials must, by definition fit in one of these arrangements (not including quasicrystals).

For convenience a Bravais lattice is depicted by a unit cell which is a factor 1, 2, 3 or 4 larger than the primitive cell. Depending on the symmetry of a crystal or other pattern, the fundamental domain is again smaller, up to a factor 48.

The Bravais lattices were studied by Moritz Ludwig Frankenheim (1801–1869), in 1842, who found that there were 15 Bravais lattices. This was corrected to 14 by A. Bravais in 1848.


Crystal systems in four-dimensional spaceEdit

The four-dimensional unit cell is defined by four edge lengths (a, b, c, d) and six interaxial angles (\alpha, \beta, \gamma, \delta, \epsilon, \zeta). The following conditions for the lattice parameters define 23 crystal families:

1 Hexaclinic: a\ne b \ne c \ne d, \alpha \ne \beta \ne \gamma \ne \delta \ne \epsilon \ne \zeta \ne 90 ^\circ

2 Triclinic: a\ne b \ne c \ne d, \alpha \ne \beta \ne \gamma \ne 90 ^\circ, \delta = \epsilon = \zeta = 90 ^\circ

3 Diclinic: a\ne b \ne c \ne d, \alpha \ne 90 ^\circ, \beta = \gamma  = \delta = \epsilon = 90 ^\circ, \zeta \ne 90 ^\circ

4 Monoclinic: a\ne b \ne c \ne d, \alpha \ne 90 ^\circ, \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

5 Orthogonal: a\ne b \ne c \ne d, \alpha = \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

6 Tetragonal Monoclinic: a\ne b = c \ne d, \alpha \ne 90 ^\circ, \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

7 Hexagonal Monoclinic: a\ne b = c \ne d, \alpha \ne 90 ^\circ, \beta = \gamma  = \delta = \epsilon = 90 ^\circ, \zeta = 120 ^\circ

8 Ditetragonal Diclinic: a = d \ne b = c, \alpha = \zeta = 90 ^\circ, \beta = \epsilon \ne 90 ^\circ, \gamma \ne  90 ^\circ, \delta = 180 ^\circ - \gamma

9 Ditrigonal (Dihexagonal) Diclinic: a = d \ne b = c, \alpha = \zeta = 120 ^\circ, \beta = \epsilon \ne 90 ^\circ, \gamma \ne \delta \ne 90 ^\circ, cos \delta = cos \beta - cos \gamma

10 Tetragonal Orthogonal: a\ne b = c \ne d, \alpha = \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

11 Hexagonal Orthogonal: a\ne b = c \ne d, \alpha = \beta = \gamma  = \delta = \epsilon = 90 ^\circ, \zeta = 120 ^\circ

12 Ditetragonal Monoclinic: a = d \ne b = c, \alpha = \gamma = \delta = \zeta = 90 ^\circ, \beta = \epsilon \ne 90 ^\circ

13 Ditrigonal (Dihexagonal) Monoclinic: a = d \ne b = c, \alpha = \zeta = 120 ^\circ, \beta = \epsilon \ne 90 ^\circ, \gamma = \delta \ne 90 ^\circ, cos \gamma = -\color{Black}\tfrac{1}{2} cos \beta

14 Ditetragonal Orthogonal: a = d \ne b = c, \alpha = \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

15 Hexagonal Tetragonal: a = d \ne b = c, \alpha = \beta = \gamma  = \delta = \epsilon = 90 ^\circ, \zeta = 120 ^\circ

16 Dihexagonal Orthogonal: a = d \ne b = c, \alpha = \zeta = 120 ^\circ, \beta = \gamma  = \delta = \epsilon = 90 ^\circ,

17 Cubic Orthogonal: a = b = c \ne d, \alpha = \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

18 Octagonal: a = b = c = d, \alpha = \gamma = \zeta \ne 90 ^\circ, \beta = \epsilon = 90 ^\circ, \delta = 180 ^\circ - \alpha

19 Decagonal: a = b = c = d, \alpha = \gamma = \zeta \ne \beta = \delta = \epsilon, cos \beta = -0.5 - cos \alpha

20 Dodecagonal: a = b = c = d, \alpha = \zeta = 90 ^\circ, \beta = \epsilon = 120 ^\circ, \gamma = \delta \ne 90 ^\circ

21 Di-isohexagonal Orthogonal: a = b = c = d, \alpha  = \zeta = 120 ^\circ, \beta = \gamma = \delta = \epsilon = 90 ^\circ

22 Icosagonal (Icosahedral): a = b = c = d, \alpha = \beta = \gamma  = \delta = \epsilon = \zeta, cos \alpha = -\color{Black}\tfrac{1}{4}

23 Hypercubic: a = b = c = d, \alpha = \beta = \gamma  = \delta = \epsilon = \zeta = 90 ^\circ

The names here are given according to Whittaker.[3] They are almost the same as in Brown et al,[4] with exception for names of the crystal families 9, 13, and 22. The names for these three families according to Brown et al are given in parenthesis.


The relation between four-dimensional crystal families, crystal systems, and lattice systems is shown in the following table.[3][4] Enantiomorphic systems are marked with asterisk. The number of enantiomorphic pairs are given in parentheses. Here the term "enantiomorphic" has different meaning than in table for three-dimensional crystal classes. The latter means, that enantiomorphic point groups describe chiral (enantiomorphic) structures. In the current table, "enantiomorphic" means, that group itself (considered as geometric object) is enantiomorphic, like enantiomorphic pairs of three-dimensional space groups P31 and P32, P4122 and P4322. Starting from four-dimensional space, point groups also can be enantiomorphic in this sense.

No. of </br >Crystal family Crystal family Crystal system No. of </br>Crystal system Point groups Space groups Bravais lattices Lattice system
I Hexaclinic 1 2 2 1 Hexaclinic P
II Triclinic 2 3 13 2 Triclinic P, S
III Diclinic 3 2 12 3 Diclinic P, S, D
IV Monoclinic 4 4 207 6 Monoclinic P, S, S, I, D, F
V Orthogonal Non-axial Orthogonal 5 2 2 1 Orthogonal KU
112 8 Orthogonal P, S, I, Z, D, F, G, U
Axial Orthogonal 6 3 887
VI Tetragonal Monoclinic 7 7 88 2 Tetragonal Monoclinic P, I
VII Hexagonal Monoclinic Trigonal Monoclinic 8 5 9 1 Hexagonal Monoclinic R
15 1 Hexagonal Monoclinic P
Hexagonal Monoclinic 9 7 25
VIII Ditetragonal Diclinic* 10 1 (+1) 1 (+1) 1 (+1) Ditetragonal Diclinic P*
IX Ditrigonal Diclinic* 11 2 (+2) 2 (+2) 1 (+1) Ditrigonal Diclinic P*
X Tetragonal Orthogonal Inverse Tetragonal Orthogonal 12 5 7 1 Tetragonal Orthogonal KG
351 5 Tetragonal Orthogonal P, S, I, Z, G
Proper Tetragonal Orthogonal 13 10 1312
XI Hexagonal Orthogonal Trigonal Orthogonal 14 10 81 2 Hexagonal Orthogonal R, RS
150 2 Hexagonal Orthogonal P, S
Hexagonal Orthogonal 15 12 240
XII Ditetragonal Monoclinic* 16 1 (+1) 6 (+6) 3 (+3) Ditetragonal Monoclinic P*, S*, D*
XIII Ditrigonal Monoclinic* 17 2 (+2) 5 (+5) 2 (+2) Ditrigonal Monoclinic P*, RR*
XIV Ditetragonal Orthogonal Crypto-Ditetragonal Orthogonal 18 5 10 1 Ditetragonal Orthogonal D
165 (+2) 2 Ditetragonal Orthogonal P, Z
Ditetragonal Orthogonal 19 6 127
XV Hexagonal Tetragonal 20 22 108 1 Hexagonal Tetragonal P
XVI Dihexagonal Orthogonal Crypto-Ditrigonal Orthogonal* 21 4 (+4) 5 (+5) 1 (+1) Dihexagonal Orthogonal G*
5 (+5) 1 Dihexagonal Orthogonal P
Dihexagonal Orthogonal 23 11 20
Ditrigonal Orthogonal 22 11 41
16 1 Dihexagonal Orthogonal RR
XVII Cubic Orthogonal Simple Cubic Orthogonal 24 5 9 1 Cubic Orthogonal KU
96 5 Cubic Orthogonal P, I, Z, F, U
Complex Cubic Orthogonal 25 11 366
XVIII Octagonal* 26 2 (+2) 3 (+3) 1 (+1) Octagonal P*
XIX Decagonal 27 4 5 1 Decagonal P
XX Dodecagonal* 28 2 (+2) 2 (+2) 1 (+1) Dodecagonal P*
XXI Di-isohexagonal Orthogonal Simple Di-isohexagonal Orthogonal 29 9 (+2) 19 (+5) 1 Di-isohexagonal Orthogonal RR
19 (+3) 1 Di-isohexagonal Orthogonal P
Complex Di-isohexagonal Orthogonal 30 13 (+8) 15 (+9)
XXII Icosagonal 31 7 20 2 Icosagonal P, SN
XXIII Hypercubic Octagonal Hypercubic32 21 (+8) 73 (+15) 1 Hypercubic P
107 (+28) 1 Hypercubic Z
Dodecagonal Hypercubic 33 16 (+12) 25 (+20)
Total: 23 (+6) 33 (+7) 227 (+44) 4783 (+111) 64 (+10) 33 (+7)

See alsoEdit

NotesEdit

  1. Template:Cite journal
  2. E. Koch , W. Fischer , U. Müller , in ‘International Tables for Crystallography, Vol. A, Space-Group Symmetry’, 5th edn., Ed. T. Hahn, Kluwer Academic Publishers, Dordrecht, 2002, Chapt. 10, p. 804.
  3. 3.0 3.1 E. J. W. Whittaker, An atlas of hyperstereograms of the four-dimensional crystal classes. Clarendon Press (Oxford Oxfordshire and New York) 1985.
  4. 4.0 4.1 H. Brown, R. Bülow, J. Neubüser, H. Wondratschek and H. Zassenhaus, Crystallographic Groups of Four-Dimensional Space. Wiley, NY, 1978.

ReferencesEdit

External linksEdit

Template:Crystal systems Template:Mineral identificationru:Сингония sh:Kristalni sustav

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