Difference between revisions of "Texture"
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'''Texture''' in [http://en.wikipedia.org/wiki/Materials_science Materials Science] is the distribution of crystallographic orientations of a [http://en.wikipedia.org/wiki/Polycrystalline polycrystalline sample]. A sample in which these orientations are fully [[random]] is said to have no texture. If the crystallographic orientations are not random, but have some preferred orientation, then the sample has a weak, moderate or strong texture. The degree is dependent on the percentage of crystals having the preferred orientation. Texture is seen in almost all engineered [[material]]s, and can have a great [[influence]] on [[material]] properties. Also, geologic rocks show texture due to their thermo-[[Mechanism|mechanic]] history of formation [[processes]]. | '''Texture''' in [http://en.wikipedia.org/wiki/Materials_science Materials Science] is the distribution of crystallographic orientations of a [http://en.wikipedia.org/wiki/Polycrystalline polycrystalline sample]. A sample in which these orientations are fully [[random]] is said to have no texture. If the crystallographic orientations are not random, but have some preferred orientation, then the sample has a weak, moderate or strong texture. The degree is dependent on the percentage of crystals having the preferred orientation. Texture is seen in almost all engineered [[material]]s, and can have a great [[influence]] on [[material]] properties. Also, geologic rocks show texture due to their thermo-[[Mechanism|mechanic]] history of formation [[processes]]. |
Revision as of 17:11, 26 December 2009
Texture in Materials Science is the distribution of crystallographic orientations of a polycrystalline sample. A sample in which these orientations are fully random is said to have no texture. If the crystallographic orientations are not random, but have some preferred orientation, then the sample has a weak, moderate or strong texture. The degree is dependent on the percentage of crystals having the preferred orientation. Texture is seen in almost all engineered materials, and can have a great influence on material properties. Also, geologic rocks show texture due to their thermo-mechanic history of formation processes.
One extreme case is a complete lack of texture: a solid with perfectly random crystallite orientation will have isotropic properties at length scales sufficiently larger than the size of the crystallites. The opposite extreme is a perfect single crystal, which has anisotropic properties by geometric necessity.[1]