A lattice constant or lattice parameter is one of the physical dimensions and angles that determine the geometry of the unit cells in a crystal lattice, and is proportional to the distance between atoms in the crystal. A simple cubic crystal has only one lattice constant, the distance between atoms, but in general lattices in three dimensions have six lattice constants: the lengths a, b, and c of the three cell edges meeting at a vertex, and the angles α, β, and γ between those edges.
The crystal lattice parameters a, b, and c have the dimension of length. The three numbers represent the size of the unit cell, that is, the distance from a given atom to an identical atom in the same position and orientation in a neighboring cell (except for very simple crystal structures, this will not necessarily be distance to the nearest neighbor). Their SI unit is the meter, and they are traditionally specified in angstroms (Å); an angstrom being 0.1 nanometer (nm), or 100 picometres (pm). Typical values start at a few angstroms. The angles α, β, and γ are usually specified in degrees.
A chemical substance in the solid state may form crystals in which the atoms, molecules, or ions are arranged in space according to one of a small finite number of possible crystal systems (lattice types), each with fairly well defined set of lattice parameters that are characteristic of the substance. These parameters typically depend on the temperature, pressure (or, more generally, the local state of mechanical stress within the crystal), [2] electric and magnetic fields, and its isotopic composition. [3] The lattice is usually distorted near impurities, crystal defects, and the crystal's surface. Parameter values quoted in manuals should specify those environment variables, and are usually averages affected by measurement errors.
Depending on the crystal system, some or all of the lengths may be equal, and some of the angles may have fixed values. In those systems, only some of the six parameters need to be specified. For example, in the cubic system, all of the lengths are equal and all the angles are 90°, so only the a length needs to be given. This is the case of diamond, which has a = 3.57 Å = 357 pm at 300 K. Similarly, in hexagonal system, the a and b constants are equal, and the angles are 60°, 90°, and 90°, so the geometry is determined by the a and c constants alone.
The lattice parameters of a crystalline substance can be determined using techniques such as X-ray diffraction or with an atomic force microscope. They can be used as a natural length standard of nanometer range. [4] [5] In the epitaxial growth of a crystal layer over a substrate of different composition, the lattice parameters must be matched in order to reduce strain and crystal defects.
The volume of the unit cell can be calculated from the lattice constant lengths and angles. If the unit cell sides are represented as vectors, then the volume is the scalar triple product of the vectors. The volume is represented by the letter V. For the general unit cell
For monoclinic lattices with α = 90°, γ = 90°, this simplifies to
For orthorhombic, tetragonal and cubic lattices with β = 90° as well, then [6]
Matching of lattice structures between two different semiconductor materials allows a region of band gap change to be formed in a material without introducing a change in crystal structure. This allows construction of advanced light-emitting diodes and diode lasers.
For example, gallium arsenide, aluminium gallium arsenide, and aluminium arsenide have almost equal lattice constants, making it possible to grow almost arbitrarily thick layers of one on the other one.
Typically, films of different materials grown on the previous film or substrate are chosen to match the lattice constant of the prior layer to minimize film stress.
An alternative method is to grade the lattice constant from one value to another by a controlled altering of the alloy ratio during film growth. The beginning of the grading layer will have a ratio to match the underlying lattice and the alloy at the end of the layer growth will match the desired final lattice for the following layer to be deposited.
The rate of change in the alloy must be determined by weighing the penalty of layer strain, and hence defect density, against the cost of the time in the epitaxy tool.
For example, indium gallium phosphide layers with a band gap above 1.9 eV can be grown on gallium arsenide wafers with index grading.
Material | Lattice constant (Å) | Crystal structure | Ref. |
---|---|---|---|
C (diamond) | 3.567 | Diamond (FCC) | [7] |
C (graphite) | a = 2.461 c = 6.708 | Hexagonal | |
Si | 5.431020511 | Diamond (FCC) | [8] [9] |
Ge | 5.658 | Diamond (FCC) | [8] |
AlAs | 5.6605 | Zinc blende (FCC) | [8] |
AlP | 5.4510 | Zinc blende (FCC) | [8] |
AlSb | 6.1355 | Zinc blende (FCC) | [8] |
GaP | 5.4505 | Zinc blende (FCC) | [8] |
GaAs | 5.653 | Zinc blende (FCC) | [8] |
GaSb | 6.0959 | Zinc blende (FCC) | [8] |
InP | 5.869 | Zinc blende (FCC) | [8] |
InAs | 6.0583 | Zinc blende (FCC) | [8] |
InSb | 6.479 | Zinc blende (FCC) | [8] |
MgO | 4.212 | Halite (FCC) | [10] |
SiC | a = 3.086 c = 10.053 | Wurtzite | [8] |
CdS | 5.8320 | Zinc blende (FCC) | [7] |
CdSe | 6.050 | Zinc blende (FCC) | [7] |
CdTe | 6.482 | Zinc blende (FCC) | [7] |
ZnO | a = 3.25 c = 5.2 | Wurtzite (HCP) | [11] |
ZnO | 4.580 | Halite (FCC) | [7] |
ZnS | 5.420 | Zinc blende (FCC) | [7] |
PbS | 5.9362 | Halite (FCC) | [7] |
PbTe | 6.4620 | Halite (FCC) | [7] |
BN | 3.6150 | Zinc blende (FCC) | [7] |
BP | 4.5380 | Zinc blende (FCC) | [7] |
CdS | a = 4.160 c = 6.756 | Wurtzite | [7] |
ZnS | a = 3.82 c = 6.26 | Wurtzite | [7] |
AlN | a = 3.112 c = 4.982 | Wurtzite | [8] |
GaN | a = 3.189 c = 5.185 | Wurtzite | [8] |
InN | a = 3.533 c = 5.693 | Wurtzite | [8] |
LiF | 4.03 | Halite | |
LiCl | 5.14 | Halite | |
LiBr | 5.50 | Halite | |
LiI | 6.01 | Halite | |
NaF | 4.63 | Halite | |
NaCl | 5.64 | Halite | |
NaBr | 5.97 | Halite | |
NaI | 6.47 | Halite | |
KF | 5.34 | Halite | |
KCl | 6.29 | Halite | |
KBr | 6.60 | Halite | |
KI | 7.07 | Halite | |
RbF | 5.65 | Halite | |
RbCl | 6.59 | Halite | |
RbBr | 6.89 | Halite | |
RbI | 7.35 | Halite | |
CsF | 6.02 | Halite | |
CsCl | 4.123 | Caesium chloride | |
CsBr | 4.291 | Caesium chloride | |
CsI | 4.567 | Caesium chloride | |
Al | 4.046 | FCC | [12] |
Fe | 2.856 | BCC | [12] |
Ni | 3.499 | FCC | [12] |
Cu | 3.597 | FCC | [12] |
Mo | 3.142 | BCC | [12] |
Pd | 3.859 | FCC | [12] |
Ag | 4.079 | FCC | [12] |
W | 3.155 | BCC | [12] |
Pt | 3.912 | FCC | [12] |
Au | 4.065 | FCC | [12] |
Pb | 4.920 | FCC | [12] |
V | 3.0399 | BCC | |
Nb | 3.3008 | BCC | |
Ta | 3.3058 | BCC | |
TiN | 4.249 | Halite | |
ZrN | 4.577 | Halite | |
HfN | 4.392 | Halite | |
VN | 4.136 | Halite | |
CrN | 4.149 | Halite | |
NbN | 4.392 | Halite | |
TiC | 4.328 | Halite | [13] |
ZrC0.97 | 4.698 | Halite | [13] |
HfC0.99 | 4.640 | Halite | [13] |
VC0.97 | 4.166 | Halite | [13] |
NbC0.99 | 4.470 | Halite | [13] |
TaC0.99 | 4.456 | Halite | [13] |
Cr3C2 | a = 11.47 b = 5.545 c = 2.830 | Orthorhombic | [13] |
WC | a = 2.906 c = 2.837 | Hexagonal | [13] |
ScN | 4.52 | Halite | [14] |
LiNbO3 | a = 5.1483 c = 13.8631 | Hexagonal | [15] |
KTaO3 | 3.9885 | Cubic perovskite | [15] |
BaTiO3 | a = 3.994 c = 4.034 | Tetragonal perovskite | [15] |
SrTiO3 | 3.98805 | Cubic perovskite | [15] |
CaTiO3 | a = 5.381 b = 5.443 c = 7.645 | Orthorhombic perovskite | [15] |
PbTiO3 | a = 3.904 c = 4.152 | Tetragonal perovskite | [15] |
EuTiO3 | 7.810 | Cubic perovskite | [15] |
SrVO3 | 3.838 | Cubic perovskite | [15] |
CaVO3 | 3.767 | Cubic perovskite | [15] |
BaMnO3 | a = 5.673 c = 4.71 | Hexagonal | [15] |
CaMnO3 | a = 5.27 b = 5.275 c = 7.464 | Orthorhombic perovskite | [15] |
SrRuO3 | a = 5.53 b = 5.57 c = 7.85 | Orthorhombic perovskite | [15] |
YAlO3 | a = 5.179 b = 5.329 c = 7.37 | Orthorhombic perovskite | [15] |
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.
In trigonometry, the law of sines, sine law, sine formula, or sine rule is an equation relating the lengths of the sides of any triangle to the sines of its angles. According to the law,
In solid-state physics and solid-state chemistry, a band gap, also called a bandgap or energy gap, is an energy range in a solid where no electronic states exist. In graphs of the electronic band structure of solids, the band gap refers to the energy difference between the top of the valence band and the bottom of the conduction band in insulators and semiconductors. It is the energy required to promote an electron from the valence band to the conduction band. The resulting conduction-band electron are free to move within the crystal lattice and serve as charge carriers to conduct electric current. It is closely related to the HOMO/LUMO gap in chemistry. If the valence band is completely full and the conduction band is completely empty, then electrons cannot move within the solid because there are no available states. If the electrons are not free to move within the crystal lattice, then there is no generated current due to no net charge carrier mobility. However, if some electrons transfer from the valence band to the conduction band, then current can flow. Therefore, the band gap is a major factor determining the electrical conductivity of a solid. Substances having large band gaps are generally insulators, those with small band gaps are semiconductor, and conductors either have very small band gaps or none, because the valence and conduction bands overlap to form a continuous band.
Gallium arsenide (GaAs) is a III-V direct band gap semiconductor with a zinc blende crystal structure.
Atomic force microscopy (AFM) or scanning force microscopy (SFM) is a very-high-resolution type of scanning probe microscopy (SPM), with demonstrated resolution on the order of fractions of a nanometer, more than 1000 times better than the optical diffraction limit.
Epitaxy refers to a type of crystal growth or material deposition in which new crystalline layers are formed with one or more well-defined orientations with respect to the crystalline seed layer. The deposited crystalline film is called an epitaxial film or epitaxial layer. The relative orientation(s) of the epitaxial layer to the seed layer is defined in terms of the orientation of the crystal lattice of each material. For most epitaxial growths, the new layer is usually crystalline and each crystallographic domain of the overlayer must have a well-defined orientation relative to the substrate crystal structure. Epitaxy can involve single-crystal structures, although grain-to-grain epitaxy has been observed in granular films. For most technological applications, single-domain epitaxy, which is the growth of an overlayer crystal with one well-defined orientation with respect to the substrate crystal, is preferred. Epitaxy can also play an important role while growing superlattice structures.
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 other words, the excess energy required to magnetize a specimen in a particular direction over that required to magnetize it along the easy direction is called crystalline anisotropy energy.
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 (a by b) 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, is an infinite array of discrete points generated by a set of discrete translation operations described in three dimensional space by
In crystallography, the diamond cubic crystal structure is a repeating pattern of 8 atoms that certain materials may adopt as they solidify. While the first known example was diamond, other elements in group 14 also adopt this structure, including α-tin, the semiconductors silicon and germanium, and silicon–germanium alloys in any proportion. There are also crystals, such as the high-temperature form of cristobalite, which have a similar structure, with one kind of atom at the positions of carbon atoms in diamond but with another kind of atom halfway between those.
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.
A crystallographic database is a database specifically designed to store information about the structure of molecules and crystals. Crystals are solids having, in all three dimensions of space, a regularly repeating arrangement of atoms, ions, or molecules. They are characterized by symmetry, morphology, and directionally dependent physical properties. A crystal structure describes the arrangement of atoms, ions, or molecules in a crystal.
The Pearson symbol, or Pearson notation, is used in crystallography as a means of describing a crystal structure, and was originated by W. B. Pearson. The symbol is made up of two letters followed by a number. For example:
In crystallography, a fractional coordinate system is a coordinate system in which basis vectors used to the describe the space are the lattice vectors of a crystal (periodic) pattern. The selection of an origin and a basis define a unit cell, a parallelotope defined by the lattice basis vectors where is the dimension of the space. These basis vectors are described by lattice parameters consisting of the lengths of the lattice basis vectors and the angles between them .
Solution of triangles is the main trigonometric problem of finding the characteristics of a triangle, when some of these are known. The triangle can be located on a plane or on a sphere. Applications requiring triangle solutions include geodesy, astronomy, construction, and navigation.
In crystallography, the hexagonal crystal family is one of the 6 crystal families, which includes two crystal systems and two lattice systems. While commonly confused, the trigonal crystal system and the rhombohedral lattice system are not equivalent. In particular, there are crystals that have trigonal symmetry but belong to the hexagonal lattice.
Metals, and specifically rare-earth elements, form numerous chemical complexes with boron. Their crystal structure and chemical bonding depend strongly on the metal element M and on its atomic ratio to boron. When B/M ratio exceeds 12, boron atoms form B12 icosahedra which are linked into a three-dimensional boron framework, and the metal atoms reside in the voids of this framework. Those icosahedra are basic structural units of most allotropes of boron and boron-rich rare-earth borides. In such borides, metal atoms donate electrons to the boron polyhedra, and thus these compounds are regarded as electron-deficient solids.
Zone axis, a term sometimes used to refer to "high-symmetry" orientations in a crystal, most generally refers to any direction referenced to the direct lattice of a crystal in three dimensions. It is therefore indexed with direct lattice indices, instead of with Miller indices.
Solid nitrogen is a number of solid forms of the element nitrogen, first observed in 1884. Solid nitrogen is mainly the subject of academic research, but low-temperature, low-pressure solid nitrogen is a substantial component of bodies in the outer Solar System and high-temperature, high-pressure solid nitrogen is a powerful explosive, with higher energy density than any other non-nuclear material.
Rhenium disulfide is an inorganic compound of rhenium and sulfur with the formula ReS2. It has a layered structure where atoms are strongly bonded within each layer. The layers are held together by weak Van der Waals bonds, and can be easily peeled off from the bulk material.