(crystallography) A crystal, usually grown artificially, in which all parts have the same crystallographic orientation.
| Sci-Tech Dictionary: single crystal |
(crystallography) A crystal, usually grown artificially, in which all parts have the same crystallographic orientation.
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| Sci-Tech Encyclopedia: Single crystal |
In crystalline solids the atoms or molecules are stacked in a regular manner, forming a three-dimensional pattern which may be obtained by a three-dimensional repetition of a certain pattern unit called a unit cell. When the periodicity of the pattern extends throughout a certain piece of material, one speaks of a single crystal. A single crystal is formed by the growth of a crystal nucleus without secondary nucleation or impingement on other crystals. See also Crystal structure; Crystallography.
When grown from a melt, single crystals usually take the form of their container. Crystals grown from solution (gas, liquid, or solid) often have a well-defined form which reflects the symmetry of the unit cell. See also Crystal growth; Crystallization; Zone refining.
Ideally, single crystals are free from internal boundaries. They give rise to a characteristic x-ray diffraction pattern.
Many types of single crystal exhibit anisotropy, that is, a variation of some of their physical properties according to the direction along which they are measured. For example, the electrical resistivity of a randomly oriented aggregate of graphite crystallites is the same in all directions. This anisotropy exists both for structure-sensitive properties, which are strongly affected by crystal imperfections (such as cleavage and crystal growth rate), and for structure-insensitive properties, which are not affected by imperfections (such as elastic coefficients).
The structure-sensitive properties of crystals (for example, strength and diffusion coefficients) seem governed by internal defects, often on an atomic scale. See also Crystal defects.
| Wikipedia: Single crystal |
A single crystal usually refers to a grain boundary free monocrystalline solid
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A single crystal solid is a material in which the crystal lattice of the entire sample is continuous and unbroken to the edges of the sample, with no grain boundaries. The opposite of a single crystal sample is an amorphous structure where the atomic position is limited to short range order only. In between the two extremes exist polycrystalline and paracrystalline phases, which are made up of a number of smaller crystals known as crystallites.
Because of a variety of entropic effects on the microstructure of solids, including the distorting effects of impurities and the mobility of crystallographic defects and dislocations, single crystals of meaningful size are exceedingly rare in nature, and are also difficult to produce in the laboratory, though can be made - under controlled conditions (see also recrystallisation).
Because grain boundaries can have significant effects on the physical and electrical properties of a material, single crystals are of interest to industry, and have important industrial applications.
One notable use of these is the use of single crystal silicon in the fabrication of semiconductors. On the quantum scale that microprocessors operate on, the presence of grain boundaries would have a significant impact on the functionality of field effect transistors by altering local electrical properties. Therefore, microprocessor fabricators have invested heavily in facilities to produce large single crystals of silicon.
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Another application of single crystal solids is in materials science - in the production of high strength materials, e.g. turbine blades;[1] here, the absence of grain boundaries gives a significant increase in physical strength.
Single crystal copper has better conductivity than polycrystalline copper - As of 2009 no single crystal copper is manufactured industrially, but methods of producing very large individual crystal sizes for copper conductors are exploited for high performance electrical applications. These can be considered meta-single crystals with only a few crystals per metre of length.
The detailed study of the Crystal structure of a material by Bragg diffraction techniques is much easier with monocrystals. They may be grown for this purpose, even when the material is otherwise only needed in polycrystalline form.
In the case of silicon and metal single crystal fabrication the techniques used involved high controlled and therfore relatively slow crystallization.
Specific techniques to produce large single crystals (aka boules) include the Czochralski process and the Bridgeman technique). Other less exotic methods of crystallization may be used, depending on the physical properties of the substance - including hydrothermal synthesis, sublimation, or simply solvent based crystallization.
A different technology to create single crystalline materials is called epitaxy. As of 2009 this process is used to deposit very thin (micrometre to nanometer scale) layers of the same or different materials on the surface of an existing single crystal. Applications of this technique lie in the areas of semiconductor production, with potential uses in other nanotechnological fields and catalysis.
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
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