Point group
A point group is a special type of symmetry group in Euclidean geometry that describes the symmetry of a finite body. All point groups are characterized by the fact that there is a point which is mapped back onto itself by all symmetry operations of the point group. Based on Neumann's principle , the point group determines the macroscopic properties of the body. Further statements can be obtained with the help of representation theory .
The point groups are used in molecular physics and crystallography , where the 32 crystallographic point groups are also called crystal classes. The point groups are designated in the Schoenflies notation . In crystallography, the Hermann Mauguin symbolism is now mainly used.
Mathematical basics
The symmetry of a body is mathematically described as the set of all possible symmetry operations ( symmetry group ). With symmetry operations are meant Euclidean movements that represent the body on itself. A distinction must be made here between even movements that maintain the orientation and odd movements that reverse the orientation, e.g. B. Reflections on planes.
Possible symmetry operations in point groups in three-dimensional Euclidean vector space, the symmetry operations, which have a fixed point at least: identity mapping , point reflection on a center of inversion , reflection on a mirror plane , rotation about an axis of rotation , as well as a combination thereof rotary reflection or the equivalent of rotary inversion . The translation , the screwing and the glide mirror cannot be elements of a point group because they do not have a fixed point.
If one understands the successive execution of symmetry operations as additive operation, one recognizes that a set of symmetry operations is a (usually non- commutative ) group .
There are both discrete and continuous point groups. The discrete point groups can be divided into two different types:
- Point groups with a maximum of one axis of rotation with a count greater than two,
- Point groups with at least two axes of rotation with a count greater than two.
The discrete point groups with a maximum of one marked -numerous axis of rotation can also be combined with mirror planes and twofold axes of rotation. There are a total of the following options:
group | Group symbol (Schönflies) | Explanation |
---|---|---|
Turning group | C n | An n-fold axis of rotation |
C nv | 1 C n axis + n mirror planes that contain this axis (v: vertical mirror plane) | |
C nh | 1 C n -axis + 1 mirror plane perpendicular to this axis (h: horizontal mirror plane) | |
Dihedral group | D n | 1 C n axis + n C 2 axes perpendicular to it |
D nd | 1 D n axis + n mirror planes that contain the D n axis and an angle bisector of the C 2 axes (d: diagonal mirror plane) | |
D nh | 1 D n axis + 1 mirror plane perpendicular to it | |
Rotating mirror group | S n | 1 n-fold rotating mirror axis |
There are special names for individual groups:
- ( Reflection)
- ( Inversion, i.e. point reflection)
The point groups which have at least two axes of rotation with a number greater than two correspond to the symmetry groups of the Platonic solids .
- The tetrahedral groups : . This corresponds to the full symmetry of a tetrahedron .
- The Oktaedergruppen : . This corresponds to the full symmetry of an octahedron or hexahedron .
- The Ikosaedergruppen : . This corresponds to the full symmetry of an icosahedron or dodecahedron .
The continuous point groups are also called Curie groups . They consist of the cylinder groups (with an infinite axis of rotation) and the spherical groups (with two infinite axes of rotation).
Point groups in crystallography
The complete possible symmetry of a crystal structure is described with the 230 crystallographic space groups . In addition to the symmetry operations of the point groups, there are also translations in the form of screws and sliding reflections as symmetry operations. To describe the symmetry of a macroscopic single crystal, on the other hand, the point groups are sufficient, since crystals are always convex polyhedra and possible internal translations in the structure cannot be macroscopically recognized.
If you delete all translations in a space group and additionally replace the screw axes and glide mirror planes with corresponding axes of rotation and mirror planes, you get the so-called geometric crystal class or point group of the crystal. Only point groups whose symmetry is compatible with an infinitely extended lattice can therefore be considered as crystal classes. In a crystal, only 6-, 4-, 3-, 2-way axes of rotation are possible (rotations by 60, 90, 120 or 180 and multiples thereof). The three-dimensional point groups in which no or only 2, 3, 4 and / or 6-fold axes of rotation occur are therefore called crystallographic point groups. There are a total of 32 crystallographic point groups, which are also referred to as crystal classes.
The 32 crystallographic point groups (crystal classes)
Point group (crystal class) | Physical Properties | Examples | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
No. | Crystal system | Surname | Schoenflies icon | International symbol ( Hermann-Mauguin ) |
Tepid class | Associated room groups ( no.) |
Enantiomorphism | Optical activity | Pyroelectricity | Piezoelectricity ; SHG effect | ||
Full | Short | |||||||||||
1 | triclinic | triklin-pedial | C 1 | 1 | 1 | 1 | 1 | + | + | + [ uvw ] | + |
Abelsonite axinite |
2 | triclinic-pinacoidal | C i ( S 2 ) | 1 | 1 | 2 | - | - | - | - |
Albite anorthite |
||
3 | monoclinic | monoclinic-sphenoid | C 2 | 121 (or 112) | 2 | 2 / m | 3-5 | + | + | + [010] (or [001]) | + |
Uranophane halotrichite |
4th | monoclinic | C s ( C 1 h ) | 1 m 1 (or 11 m ) | m | 6-9 | - | + | + [ u 0 w ] (or [ uv 0]) | + |
Soda Skolezite |
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5 | monoclinic prismatic | C 2 h | 12 / m 1 (or 112 / m ) | 2 / m | 10-15 | - | - | - | - |
Gypsum cryolite |
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6th | orthorhombic | orthorhombic-disphenoidal | D 2 ( V ) | 222 | 222 | mmm | 16-24 | + | + | - | + |
Austinite epsomite |
7th | orthorhombic-pyramidal | C 2 v | mm 2 | mm 2 | 25-46 | - | + | + [001] | + |
Hemimorphite struvite |
||
8th | orthorhombic-dipyramidal | D 2 h ( V h ) | 2 / m 2 / m 2 / m | mmm | 47-74 | - | - | - | - |
Topaz anhydrite |
||
9 | tetragonal | tetragonal-pyramidal | C 4 | 4th | 4th | 4 / m | 75-80 | + | + | + [001] | + |
Pinnoit Percleveit- (Ce) |
10 | tetragonal-disphenoidal | S 4 | 4th | 4th | 81-82 | - | + | - | + |
Clerk's seat Cahnit |
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11 | tetragonal-dipyramidal | C 4 h | 4 / m | 4 / m | 83-88 | - | - | - | - |
Scheelite baotite |
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12 | tetragonal-trapezoidal | D 4 | 422 | 422 | 4 / mmm | 89-98 | + | + | - | + |
Cristobalite maucherite |
|
13 | ditetragonal-pyramidal | C 4 v | 4 mm | 4 mm | 99-110 | - | - | + [001] | + |
Lenait Diaboleit |
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14th | tetragonal-scalenohedral | D 2 d ( V d ) | 4 2 m or 4 m 2 | 4 2 m | 111-122 | - | + | - | + |
Chalcopyrite stannite |
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15th | ditetragonal-dipyramidal | D 4 h | 4 / m 2 / m 2 / m | 4 / mmm | 123-142 | - | - | - | - |
Rutile zircon |
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16 | trigonal | trigonal-pyramidal | C 3 | 3 | 3 | 3 | 143-146 | + | + | + [001] | + |
Carlinite gratonite |
17th | rhombohedral | C 3 i ( S 6 ) | 3 | 3 | 147-148 | - | - | - | - |
Dolomite Dioptas |
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18th | trigonal-trapezoidal | D 3 | 321 or 312 | 32 | 3 m | 149-155 | + | + | - | + |
Quartz tellurium |
|
19th | ditrigonal-pyramidal | C 3 v | 3 m 1 or 31 m | 3 m | 156-161 | - | - | + [001] | + |
Tourmaline pyrargyrite |
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20th | ditrigonal-scalenohedral | D 3 d | 3 2 / m 1 or 3 12 / m | 3 m | 162-167 | - | - | - | - |
Calcite corundum |
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21st | hexagonal | hexagonal-pyramidal | C 6 | 6th | 6th | 6 / m | 168-173 | + | + | + [001] | + |
Nepheline zinkenite |
22nd | trigonal-dipyramidal | C 3 h | 6th | 6th | 174 | - | - | - | + |
Penfieldite Laurelite |
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23 | hexagonal-dipyramidal | C 6 h | 6 / m | 6 / m | 175-176 | - | - | - | - |
Apatite zemannite |
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24 | hexagonal-trapezoidal | D 6 | 622 | 622 | 6 / mmm | 177-182 | + | + | - | + |
High quartz pseudorutile |
|
25th | dihexagonal-pyramidal | C 6 v | 6 mm | 6 mm | 183-186 | - | - | + [001] | + |
Wurtzit Zinkit |
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26th | ditrigonal-dipyramidal | D 3 h | 6 m 2 or 6 2 m | 6 m 2 | 187-190 | - | - | - | + |
Bastnasite benitoite |
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27 | dihexagonal-dipyramidal | D 6 h | 6 / m 2 / m 2 / m | 6 / mmm | 191-194 | - | - | - | - |
Graphite magnesium |
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28 | cubic | tetrahedral-pentagon-dodecahedral | T | 23 | 23 | m 3 | 195-199 | + | + | - | + |
Ullmannit sodium bromate |
29 | disdodecahedral | T h | 2 / m 3 | m 3 | 200-206 | - | - | - | - |
Pyrite Potash Alum |
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30th | pentagon-icositetrahedral | O | 432 | 432 | m 3 m | 207-214 | + | + | - | - |
Maghemite Petzit |
|
31 | hexakistrahedral | T d | 4 3 m | 4 3 m | 215-220 | - | - | - | + |
Sphalerite sodalite |
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32 | hexakisoctahedral | O h | 4 / m 3 2 / m | m 3 m | 221-230 | - | - | - | - |
Diamond copper |
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|
Remarks
The relationship between the space group and the point group of a crystal results as follows: The set of all translations of a space group form a normal divisor of . The point group of the crystal is the point group that is isomorphic to the factor group . The point group describes the symmetry of a crystal at the gamma point, i.e. its macroscopic properties. At other points in the Brillouin zone , the symmetry of the crystal is described by the star group of the corresponding wave vector . These are usually different for room groups that belong to the same point group.
The "prohibition" of 5-, 7- and higher-number axes of rotation only applies to three-dimensional periodic crystals. Such axes of rotation occur both in molecules and in solids in the quasicrystals . Until the discovery of quasicrystals and the subsequent redefinition of the term crystal , the prohibition on crystals was accepted as universally valid.
According to Friedel's law, the diffraction pattern of crystals in structural analyzes using X-ray diffraction always contains an inversion center in the absence of anomalous scattering . Therefore, crystals from the diffraction data cannot be assigned directly to one of the 32 crystal classes, but only to one of the 11 centrosymmetric crystallographic point groups, which are also referred to as Lau groups . Through the identification of the Lau group, the affiliation of the crystal to one of the seven crystal systems is clarified.
Point groups in molecular physics
Schoenflies | H. / M. | Symmetry elements | Molecular examples |
---|---|---|---|
Point groups of low symmetry | |||
C 1 | I / E = C 1 | CHFClBr | |
C s ≡ S 1 | σ ≡ S 1 | BFClBr, SOBrCl | |
C i ≡ S 2 | i ≡ S 2 | 1,2-dibromo-1,2-dichloroethane, meso- tartaric acid | |
flat turning groups SO (2) | |||
C 2 | C 2 | H 2 O 2 , S 2 Cl 2 | |
C 3 | C 3 | Triphenylmethane , N (GeH 3 ) 3 | |
C 4 | C 4 | ||
C 5 | C 5 | 15-crown-5 | |
C 6 | C 6 | α-cyclodextrin | |
Turning groups with vertical mirror planes | |||
C 2v ≡ D 1h | C 2 , 2σ v | H 2 O , SO 2 Cl 2 , o- / m- dichlorobenzene | |
C 3v | C 3 , 3σ v | NH 3 , CHCl 3 , CH 3 Cl , POCl 3 | |
C 4v | C 4 , 4σ v | SF 5 Cl, XeOF 4 | |
C 5v | - | C 5 , 5σ v | Corannulene , C 5 H 5 In |
C 6v | C 6 , 6σ v | Benzene-hexamethylbenzene-chromium (0) | |
C ∞v | - | C ∞ , ∞σ v | linear molecules like HCN , COS |
Turning groups with horizontal mirror planes | |||
C 2h ≡ D 1d ≡ S 2v | C 2 , σ h , i | Oxalic acid , trans -butene | |
C 3h ≡ S 3 | C 3 , σ h | Boric acid | |
C 4h | C 4 , σ h , i | Polycycloalkane C 12 H 20 | |
C 6h | C 6 , σ h , i | Hexa-2-propenyl-benzene | |
Rotating mirror groups | |||
S 4 | S 4 | 12-crown-4, tetraphenylmethane , Si (OCH 3 ) 4 | |
S 6 ≡ C 3i | S 6 | 18-crown-6, hexacyclopropylethane | |
Dihedral groups | |||
D 2 ≡ S 1v | 3C 2 | Twistan | |
D 3 | C 3 , 3C 2 | Tris-chelate complexes | |
D 4 | C 4 , 4C 2 | - | |
D 6 | C 6 , 6C 2 | Hexaphenylbenzene | |
Dieder groups with horizontal mirror planes | |||
D 2h | S 2 , 3C 2 , 2σ v , σ h , i | Ethene , p- dichlorobenzene | |
D 3h | S 3 , C 3 , 3C 2 , 3σ v , σ h | BF 3 , PCl 5 | |
D 4h | S 4 , C 4 , 4C 2 , 4σ v , σ h , i | XeF 4 | |
D 5h | - | S 5 , C 5 , 5C 2 , 5σ v , σ h | IF 7 |
D 6h | S 6 , C 6 , 6C 2 , 6σ v , σ h , i | benzene | |
D h | - | S 2 , C ∞ , ∞C 2, ∞σ v, σh, i | linear molecules like carbon dioxide , ethyne |
Dieder groups with diagonal mirror planes | |||
D 2d ≡ S 4v | S 4 , 2C 2 , 2σ d | Propadiene , cyclooctatetraene , B 2 Cl 4 | |
D 3d ≡ S 6v | S 6 , C 3 , 3C 2 , 3σ d , i | Cyclohexane | |
D 4d ≡ S 8v | - | S 8 , C 4 , 4C 2 , 4σ d | Cyclo- sulfur (S 8 ) |
D 5d ≡ S 10v | - | S 10 , C 5 , 5C 2 , 5σ d | Ferrocene |
Tetrahedral groups | |||
T | 4C 3 , 3C 2 | Pt (PF 3 ) 4 | |
T h | 4S 6 , 4C 3 , 3C 2 , 3σ h , i | Fe (C 6 H 5 ) 6 | |
T d | 3S 4 , 4C 3 , 3C 2 , 6σ d | CH 4 , P 4 , adamantane | |
Octahedral groups | |||
O | 3C 4 , 4C 3 , 6C 2 | - | |
O h | 4S 6 , 3S 4 , 3C 4 , 4C 3 , 6C 2 , 3σ h , 6σ d , i | SF 6 , cubane | |
Icosahedral groups | |||
I. | - | 12S 10 , 10S 6 , 6C 5 , 10C 3 , 15C 2 | - |
I h | - | 12S 10 , 10S 6 , 6C 5 , 10C 3 , 15C 2 , 15σ v , i | Fullerene-C60 , fullerene-C20 ( pentagon dodecahedron ) |
spatial rotation groups SO (3) | |||
K h | - | ∞C ∞ , ∞σ, i | monatomic particles such as helium , elementary particles |
Applications
The properties of a crystal generally depend on the direction. Therefore, all material properties are described by a corresponding tensor . There is a fixed relationship between the point group of a crystal and the shape of the respective property tensor or the number of its independent components. Here are two examples:
In point groups with a center of inversion, all components of an odd tensor are identically zero. Therefore there is no pyro effect, no piezo effect and also no optical activity in these point groups.
The elastic constants are a 4th order tensor. This generally has 3 4 = 81 components. In the cubic crystal system there are only three independent components that differ from zero: C 1111 (= C 2222 = C 3333 ), C 1122 (= C 2233 = C 1133 ) and C 1212 (= C 1313 = C 2323 ). All other components are zero.
In molecular and solid-state physics, the symmetry of the molecule or crystal can be used to determine the number of infrared and Raman-active modes and their deflection patterns. An assignment of the measured frequencies to the respective modes is not possible with group theoretical methods. If this assignment can be carried out, the binding energies between the atoms can be calculated from the frequencies.
literature
- Wolfgang Demtröder: Molecular Physics . Oldenbourg, Munich 2003, ISBN 3-486-24974-6 .
- Will Kleber , Hans-Joachim Bautsch , Joachim Bohm , Detlef Klimm: Introduction to crystallography . 19th edition. Oldenbourg Wissenschaftsverlag, Munich 2010, ISBN 978-3-486-59075-3 .
- Hahn, Theo (Ed.): International Tables for Crystallography Vol. A D. Reidel publishing Company, Dordrecht 1983, ISBN 90-277-1445-2
- Hollas, J. Michael: The symmetry of molecules , Walter de Gruyter, Berlin 1975, ISBN 3-11-004637-7
Web links
- Definition of the point group (IUCr)
- Geometric crystal class (IUCr)
Individual evidence
- ^ The Nobel Prize in Chemistry 2011. In: Nobelprize.org. Retrieved October 21, 2011 .