Crystallinity refers to the degree of structural order in a solid. In a crystal, the atoms or molecules are arranged in a regular, periodic manner. The degree of crystallinity has a large influence on hardness, density, transparency and diffusion. In an ideal gas, the relative positions of the atoms or molecules are completely random. Amorphous materials, such as liquids and , represent an intermediate case, having order over short distances (a few atomic or molecular spacings) but not over longer distances.
Many materials, such as and some , can be prepared in such a way as to produce a mixture of crystalline and Amorphous solid regions. In such cases, crystallinity is usually specified as a percentage of the volume of the material that is crystalline. Even within materials that are completely crystalline, however, the degree of structural perfection can vary.
For instance, most metallic are crystalline, but they usually comprise many independent crystalline regions (grains or ) in various orientations separated by grain boundary; furthermore, they contain other crystallographic defects (notably ) that reduce the degree of structural perfection. The most highly perfect crystals are silicon boules produced for semiconductor electronics; these are large (so they have no grain boundaries), are nearly free of dislocations, and have precisely controlled concentrations of defect atoms.
Crystallinity can be measured using x-ray diffraction, but calorimetric techniques are also commonly used.
Use in geochemistry
In geochemistry, mineral crystallinity plays a pivotal role in regulating water-rock interactions, particularly during the early stages of mineral crystallization. For example, in the case of goethite, dissolved lithium can be taken up by poorly crystallized goethite, whereas little sorption occurs in well-crystallized goethite.
Additionally, lithium isotope fractionation during low-temperature water-rock interactions is controlled by reactions occurring at defect sites in poorly crystallized minerals, such as hectorite
and goethite.
Rock crystallinity
Geologists describe four qualitative levels of crystallinity:
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holocrystalline rocks are completely crystalline;
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hypocrystalline rocks are partially crystalline, with crystals embedded in an amorphous or glassy matrix;
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hypohyaline rocks are partially glassy;
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holohyaline rocks (such as obsidian) are completely glassy.
Further reading