**Unit cell**

The defining property of a crystal is its inherent symmetry, by which we mean that under certain

*operations*the crystal remains unchanged. For example, rotating the crystal 180 degrees about a certain axis may result in an atomic configuration which is identical to the original configuration. The crystal is then said to have a twofold rotational symmetry about this axis. In addition to rotational symmetries like this, a crystal may have symmetries in the form of mirror planes and translational symmetries, and also the so-called

*compound symmetries*which are a combination of translation and rotation/mirror symmetries. A full classification of a crystal is achieved when all of these inherent symmetries of the crystal are identified.

**Classification of crystals by symmetry**

The crystal systems are a grouping of crystal structures according to the axial system used to describe their lattice. Each crystal system consists of a set of three axes in a particular geometrical arrangement. There are seven unique crystal systems. The simplest and most symmetric, the cubic (or isometric) system, has the symmetry of a cube, that is, it exhibits four threefold rotational axes oriented at 109.5 degrees (the tetrahedral angle) with respect to each other. These threefold axes lie along the body diagonals of the cube. This definition of a cubic is correct, although many textbooks incorrectly state that a cube is defined by three mutually perpendicular axes of equal length – if this were true there would be far more than 14 Bravais lattices. The other six systems, in order of decreasing symmetry, are hexagonal, tetragonal, rhombohedral (also known as trigonal), orthorhombic, monoclinic and triclinic. Some crystallographers consider the hexagonal crystal system not to be its own crystal system, but instead a part of the trigonal crystal system. The crystal system and Bravais lattice of a crystal describe the (purely) translational symmetry of the crystal.

**Crystal system**

When the crystal systems are combined with the various possible lattice centerings, we arrive at the Bravais lattices. They describe the geometric arrangement of the lattice points, and thereby the translational symmetry of the crystal. In three dimensions, there are 14 unique Bravais lattices which are distinct from one another in the translational symmetry they contain. All crystalline materials recognized until now (not including quasicrystals) fit in one of these arrangements. The fourteen three-dimensional lattices, classified by crystal system, are shown to the right. The Bravais lattices are sometimes referred to as

*space lattices*.

The crystal structure consists of the same group of atoms, the

*basis*, positioned around each and every lattice point. This group of atoms therefore repeats indefinitely in three dimensions according to the arrangement of one of the 14 Bravais lattices. The characteristic rotation and mirror symmetries of the group of atoms, or unit cell, is described by its crystallographic point group.

**The Bravais lattices**

The crystallographic point group or

*crystal class*is the mathematical group comprising the symmetry operations that leave at least one point unmoved and that leave the appearance of the crystal structure unchanged. These symmetry operations can include

*reflection*, which reflects the structure across a

*reflection plane*,

*rotation*, which rotates the structure a specified portion of a circle about a

*rotation axis*,

*inversion*which changes the sign of the coordinate of each point with respect to a

*center of symmetry*or

*inversion point*and

*improper rotation*, which consists of a rotation about an axis followed by an inversion. Rotation axes (proper and improper), reflection planes, and centers of symmetry are collectively called

*symmetry elements*. There are 32 possible crystal classes. Each one can be classified into one of the seven crystal systems.

The space group of the crystal structure is composed of the translational symmetry operations in addition to the operations of the point group. These include pure

*translations*which move a point along a vector,

*screw axis*, which rotate a point around an axis while translating parallel to the axis, and

*glide planes*, which reflect a point through a plane while translating it parallel to the plane. There are 230 distinct space groups.

**Point and space groups**

**Physical properties**

Real crystals feature defects or irregularities in the ideal arrangements described above and it is these defects that critically determine many of the electrical and mechanical properties of real materials. In particular dislocations in the crystal lattice allow shear at much lower stress than that needed for a perfect crystal structure.

**Crystal symmetry and physical properties**

*For more detailed information in specific technology applications see materials science, ceramic, or metallurgy.*

Cleavage (crystal)

Crystal

Crystal engineering

Crystallography

Crystallographic point group

Crystallographic defect

Crystal growth

Liquid crystal

Miller Index

Patterson function

Quasicrystals

Seed crystal

## 0 件のコメント:

コメントを投稿