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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 are in the same crystal system if they have similar symmetries, although 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 seven crystal systems according to their point groups, and into seven 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.
A lattice system is a class of lattices with the same set of lattice point groups, which are subgroups of the arithmetic crystal classes. The 14 Bravais lattices are grouped into seven lattice systems: triclinic, monoclinic, orthorhombic, tetragonal, rhombohedral, hexagonal, and cubic.
In a crystal system, a set of point groups and their corresponding space groups are assigned to a lattice system. Of the 32 point groups that exist in three dimensions, most are assigned to only one lattice system, in which case both the crystal and lattice systems have the same name. However, five point groups are assigned to two lattice systems, rhombohedral and hexagonal, because both exhibit threefold rotational symmetry. These point groups are assigned to the trigonal crystal system. In total there are seven crystal systems: triclinic, monoclinic, orthorhombic, tetragonal, trigonal, hexagonal, and cubic.
A crystal family is determined by lattices and point groups. It is formed by combining crystal systems which have space groups assigned to a common lattice system. In three dimensions, the crystal families and systems are identical, except the hexagonal and trigonal crystal systems, which are combined into one hexagonal crystal family. In total there are six crystal families: triclinic, monoclinic, orthorhombic, tetragonal, hexagonal, and cubic.
Spaces with less than three dimensions have the same number of crystal systems, crystal families and lattice systems. In one-dimensional space, there is one crystal system. In 2D space, there are four crystal systems: 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 (6)||Crystal system (7)||Required symmetries of point group||Point groups||Space groups||Bravais lattices||Lattice system|
|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 2 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|
|Hexagonal||1 sixfold axis of rotation||7||27|
|Cubic||3 fourfold axes of rotation||5||36||3||Cubic|
The 7 crystal systems consist of 32 crystal classes (corresponding to the 32 crystallographic point groups) as shown in the following table below:
|Crystal family||Crystal system||Point group / Crystal class||Schönflies||Hermann–Mauguin||Orbifold||Coxeter||Point symmetry||Order||Abstract group|
|triclinic||pedial||C1||1||11||[ ]+||enantiomorphic polar||1||trivial|
|domatic||Cs (C1h)||m||*11||[ ]||polar||2||cyclic|
|orthorhombic||rhombic-disphenoidal||D2 (V)||222||222||[2,2]+||enantiomorphic||4||Klein four|
|tetragonal-scalenohedral||D2d (Vd)||42m or 4m2||2*2||[2+,4]||non-centrosymmetric||8||dihedral|
|trigonal-trapezohedral||D3||32 or 321 or 312||322||[3,2]+||enantiomorphic||6||dihedral|
|ditrigonal-pyramidal||C3v||3m or 3m1 or 31m||*33||||polar||6||dihedral|
|ditrigonal-scalenohedral||D3d||3m or 3m1 or 31m||2*3||[2+,6]||centrosymmetric||12||dihedral|
|ditrigonal-dipyramidal||D3h||6m2 or 62m||*322||[2,3]||non-centrosymmetric||12||dihedral|
The point symmetry of a structure can be further described as follows. Consider the points that make up the structure, and reflect 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 in the non-centrosymmetric case, the inverted structure can in some cases be rotated to align with the original structure. This is a non-centrosymmetric achiral structure. If the inverted structure cannot be rotated to align with the original structure, then the structure is chiral or enantiomorphic and its symmetry group is enantiomorphic.
A direction (meaning a line without an arrow) is called polar if its two directional senses are geometrically or physically different. A symmetry direction of a crystal that is polar is called a polar axis.Groups containing a polar axis are called polar . A polar crystal possesses a unique polar axis (more precisely, all polar axes are parallel). Some geometrical or physical property is different at the two ends of this axis: for example, there might develop a dielectric polarization as in pyroelectric crystals. A polar axis can occur only in non-centrosymmetric structures. There cannot be a mirror plane or twofold axis perpendicular to the polar axis, because they would make the two directions of the axis equivalent.
The crystal structures of chiral biological molecules (such as protein structures) can only occur in the 65 enantiomorphic space groups (biological molecules are usually chiral).
There are seven different kinds of crystal systems, and each kind of crystal system has four different kinds of centerings (primitive, base-centered, body-centered, face-centered). However, not all of the combinations are unique; some of the combinations are equivalent while other combinations are not possible due to symmetry reasons. This reduces the number of unique lattices to the 14 Bravais lattices.
The distribution of the 14 Bravais lattices into lattice systems and crystal families is given in the following table.
|Crystal family||Lattice system||Schönflies||14 Bravais lattices|
In geometry and crystallography, a Bravais lattice is a category of translative symmetry groups (also known as lattices) in three directions.
Such symmetry groups consist of translations by vectors of the form
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 the space group of the lattice itself, viewed as a collection of points; there are 14 Bravais lattices in three dimensions; each belongs to one lattice system only. They[ clarification needed ] represent the maximum symmetry a structure with the given translational symmetry can have.
All crystalline materials (not including quasicrystals) must, by definition, fit into one of these arrangements.
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 in 1842, who found that there were 15 Bravais lattices. This was corrected to 14 by A. Bravais in 1848.
The four-dimensional unit cell is defined by four edge lengths (a, b, c, d) and six interaxial angles (α, β, γ, δ, ε, ζ). The following conditions for the lattice parameters define 23 crystal families
|No.||Family||Edge lengths||Interaxial angles|
|1||Hexaclinic||a ≠ b ≠ c ≠ d||α ≠ β ≠ γ ≠ δ ≠ ε ≠ ζ ≠ 90°|
|2||Triclinic||a ≠ b ≠ c ≠ d||α ≠ β ≠ γ ≠ 90°|
δ = ε = ζ = 90°
|3||Diclinic||a ≠ b ≠ c ≠ d||α ≠ 90°|
β = γ = δ = ε = 90°
ζ ≠ 90°
|4||Monoclinic||a ≠ b ≠ c ≠ d||α ≠ 90°|
β = γ = δ = ε = ζ = 90°
|5||Orthogonal||a ≠ b ≠ c ≠ d||α = β = γ = δ = ε = ζ = 90°|
|6||Tetragonal monoclinic||a ≠ b = c ≠ d||α ≠ 90°|
β = γ = δ = ε = ζ = 90°
|7||Hexagonal monoclinic||a ≠ b = c ≠ d||α ≠ 90°|
β = γ = δ = ε = 90°
ζ = 120°
|8||Ditetragonal diclinic||a = d ≠ b = c||α = ζ = 90°|
β = ε ≠ 90°
γ ≠ 90°
δ = 180° − γ
|9||Ditrigonal (dihexagonal) diclinic||a = d ≠ b = c||α = ζ = 120°|
β = ε ≠ 90°
γ ≠ δ ≠ 90°
cos δ = cos β − cos γ
|10||Tetragonal orthogonal||a ≠ b = c ≠ d||α = β = γ = δ = ε = ζ = 90°|
|11||Hexagonal orthogonal||a ≠ b = c ≠ d||α = β = γ = δ = ε = 90°, ζ = 120°|
|12||Ditetragonal monoclinic||a = d ≠ b = c||α = γ = δ = ζ = 90°|
β = ε ≠ 90°
|13||Ditrigonal (dihexagonal) monoclinic||a = d ≠ b = c||α = ζ = 120°|
β = ε ≠ 90°
γ = δ ≠ 90°
cos γ = −1/cos β
|14||Ditetragonal orthogonal||a = d ≠ b = c||α = β = γ = δ = ε = ζ = 90°|
|15||Hexagonal tetragonal||a = d ≠ b = c||α = β = γ = δ = ε = 90°|
ζ = 120°
|16||Dihexagonal orthogonal||a = d ≠ b = c||α = ζ = 120°|
β = γ = δ = ε = 90°
|17||Cubic orthogonal||a = b = c ≠ d||α = β = γ = δ = ε = ζ = 90°|
|18||Octagonal||a = b = c = d||α = γ = ζ ≠ 90°|
β = ε = 90°
δ = 180° − α
|19||Decagonal||a = b = c = d||α = γ = ζ ≠ β = δ = ε|
cos β = −1/ − cos α
|20||Dodecagonal||a = b = c = d||α = ζ = 90°|
β = ε = 120°
γ = δ ≠ 90°
|21||Diisohexagonal orthogonal||a = b = c = d||α = ζ = 120°|
β = γ = δ = ε = 90°
|22||Icosagonal (icosahedral)||a = b = c = d||α = β = γ = δ = ε = ζ|
cos α = −1/
|23||Hypercubic||a = b = c = d||α = β = γ = δ = ε = ζ = 90°|
The names here are given according to Whittaker.They are almost the same as in Brown et al, 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.Enantiomorphic systems are marked with an asterisk. The number of enantiomorphic pairs are given in parentheses. Here the term "enantiomorphic" has a different meaning than in the table for three-dimensional crystal classes. The latter means, that enantiomorphic point groups describe chiral (enantiomorphic) structures. In the current table, "enantiomorphic" means that a group itself (considered as a 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 |
|Crystal family||Crystal system||No. of |
|Point groups||Space groups||Bravais lattices||Lattice system|
|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|
|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|
|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|
|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|
|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|
|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*|
|XX||Dodecagonal*||28||2 (+2)||2 (+2)||1 (+1)||Dodecagonal P*|
|XXI||Diisohexagonal orthogonal||Simple diisohexagonal orthogonal||29||9 (+2)||19 (+5)||1||Diisohexagonal orthogonal RR|
|19 (+3)||1||Diisohexagonal orthogonal P|
|Complex diisohexagonal orthogonal||30||13 (+8)||15 (+9)|
|XXII||Icosagonal||31||7||20||2||Icosagonal P, SN|
|XXIII||Hypercubic||Octagonal hypercubic||32||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)|
In crystallography, crystal structure is a description of the ordered arrangement of atoms, ions or molecules in a crystalline material. Ordered structures occur from the intrinsic nature of the constituent particles to form symmetric patterns that repeat along the principal directions of three-dimensional space in matter.
Pleochroism is an optical phenomenon in which a substance has different colors when observed at different angles, especially with polarized light.
In crystallography, the tetragonal crystal system is one of the 7 crystal systems. Tetragonal crystal lattices result from stretching a cubic lattice along one of its lattice vectors, so that the cube becomes a rectangular prism with a square base and height.
In mathematics, physics and chemistry, a space group is the symmetry group of a configuration in space, usually in three dimensions. In three dimensions, there are 219 distinct types, or 230 if chiral copies are considered distinct. Space groups are also studied in dimensions other than 3 where they are sometimes called Bieberbach groups, and are discrete cocompact groups of isometries of an oriented Euclidean space.
In physics, a ferromagnetic material is said to have magnetocrystalline anisotropy if it takes more energy to magnetize it in certain directions than in others. These directions are usually related to the principal axes of its crystal lattice. It is a special case of magnetic anisotropy.
In crystallography, the monoclinic crystal system is one of the seven crystal systems. A crystal system is described by three vectors. In the monoclinic system, the crystal is described by vectors of unequal lengths, as in the orthorhombic system. They form a rectangular prism with a parallelogram as its base. Hence two pairs of vectors are perpendicular, while the third pair makes an angle other than 90°.
In crystallography, the orthorhombic crystal system is one of the 7 crystal systems. Orthorhombic lattices result from stretching a cubic lattice along two of its orthogonal pairs by two different factors, resulting in a rectangular prism with a rectangular base and height (c), such that a, b, and c are distinct. All three bases intersect at 90° angles, so the three lattice vectors remain mutually orthogonal.
In geometry and crystallography, a Bravais lattice, named after Auguste Bravais (1850), is an infinite array of discrete points generated by a set of discrete translation operations described in three dimensional space by:
In crystallography, a crystallographic point group is a set of symmetry operations, corresponding to one of the point groups in three dimensions, such that each operation would leave the structure of a crystal unchanged i.e. the same kinds of atoms would be placed in similar positions as before the transformation. For example, in a primitive cubic crystal system, a rotation of the unit cell by 90 degree around an axis that is perpendicular to two parallel faces of the cube, intersecting at its center, is a symmetry operation that projects each atom to the location of one of its neighbor leaving the overall structure of the crystal unaffected.
In crystallography, the tricliniccrystal system is one of the 7 crystal systems. A crystal system is described by three basis vectors. In the triclinic system, the crystal is described by vectors of unequal length, as in the orthorhombic system. In addition, the angles between these vectors must all be different and may not include 90°.
In crystallography, the cubiccrystal 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.
Crystal twinning occurs when two separate crystals share some of the same crystal lattice points in a symmetrical manner. The result is an intergrowth of two separate crystals in a variety of specific configurations. The surface along which the lattice points are shared in twinned crystals is called a composition surface or twin plane.
Vauxite is a phosphate mineral with the chemical formula Fe2+Al2(PO4)2(OH)2·6(H2O). It belongs to the laueite – paravauxite group, paravauxite subgroup, although Mindat puts it as a member of the vantasselite Al4(PO4)3(OH)3·9H2O group. There is no similarity in structure between vauxite and paravauxite Fe2+Al2(PO4)2(OH)2·8H2O or metavauxite Fe3+Al2(PO4)2(OH)2·8H2O, even though they are closely similar chemically, and all minerals occur together as secondary minerals. Vauxite was named in 1922 for George Vaux Junior (1863–1927), an American attorney and mineral collector.
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In geometry, Hermann–Mauguin notation is used to represent the symmetry elements in point groups, plane groups and space groups. It is named after the German crystallographer Carl Hermann and the French mineralogist Charles-Victor Mauguin. This notation is sometimes called international notation, because it was adopted as standard by the International Tables For Crystallography since their first edition in 1935.
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Stibarsen or allemontite is a natural form of arsenic antimonide (AsSb) or antimony arsenide (SbAs). The name stibarsen is derived from Latin stibium (antimony) and arsenic, whereas allemonite refers to the locality Allemont in France where the mineral was discovered. It is found in veins at Allemont, Isère, France; Valtellina, Italy; and the Comstock Lode, Nevada; and in a lithium pegmatites at Varuträsk, Sweden. Stibarsen is often mixed with pure arsenic or antimony, and the original description in 1941 proposed to use stibarsen for AsSb and allemontite for the mixtures. Since 1982, the International Mineralogical Association considers stibarsen as the correct mineral name.
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