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单词 glass
释义
glass

Physics
  • An amorphous solid in which the atoms form a random network. Glasses do not have the rigidity of crystals and have a viscosity that increases as the temperature is lowered. At very low temperatures, when the viscosity is very large, glasses can become elastic and brittle. Because the simplifications that can be applied to a periodic system are not applicable it is more difficult to construct theories relating to the properties of glasses than it is for regular crystals and crystals with isolated defects. At the present, a fully quantitative theory of the properties of glasses, particularly those properties that are distinct from the properties of crystals, does not exist. Because glasses consist of a random network it is usually necessary to use statistical methods to discuss their properties. Experimentally, a glass is a disordered solid with nonzero shear (rigidity) modulus and a viscosity greater than 1013 poise.


Chemistry
  • Any noncrystalline solid; i.e. a solid in which the atoms are random and have no long-range ordered pattern. Glasses are often regarded as supercooled liquids. Characteristically they have no definite melting point, but soften over a range of temperatures.

    The common glass used in windows, bottles, etc., is soda glass, which is made by heating a mixture of lime (calcium oxide), soda (sodium carbonate), and sand (silicon(IV) oxide). It is a form of calcium silicate. Borosilicate glasses (e.g. Pyrex) are made by incorporating some boron oxide, so that silicon atoms are replaced by boron atoms. They are tougher than soda glass and more resistant to temperature changes, hence their use in cooking utensils and laboratory apparatus. Glasses for special purposes (e.g. optical glass) have other elements added (e.g. barium, lead). It has proved very difficult to get a good quantitative theoretical description of glasses. One reason for this is that glasses are associated with broken ergodicity. Although glass does not have long-range order, it does have a considerable amount of short-range order due to chemical bonding. In so-called metallic glasses, atoms are close packed but (unlike crystals) with a certain amount of randomness. In glass with covalent bonds there are networks of atoms that are not densely packed. Glass has been investigated using various diffraction techniques and computer simulations. Zachariasen’s rules and topology have been used to discuss the structure of glass. See also spin glass.


Geology and Earth Sciences
  • An amorphous, metastable solid with the atomic structure of a silicate liquid. Glass can be formed by quenching a silicate melt, the short timescale for cooling or pressure reduction preventing the reorganization of the random liquid structure into an ordered crystalline structure. Since cohesion between atoms in the liquid silicate increases with increasing silica content, melts with high silicate contents are most likely to form glasses. Natural igneous glasses of rhyolite composition (70% SiO2) are termed ‘obsidians’. A wide variety of glasses, formed by meteoritic impact into the lunar regolith, exist on the lunar surface. Shapes include spheres averaging 100 μ‎m in diameter, tear-drops, dumb-bells, etc., typical of rotational shapes assumed by splashed liquids. They do not resemble meteoritic chondrules. Volcanic glasses, formed by fire fountains during eruption of mare basalts, also occur locally on the Moon. Their compositions match those of local surface rocks, soils, or minerals. No tektite compositions are found.


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