Any of a group of techniques used to purify an element or a compound or to control its composition by melting a short region (called a zone) and causing this liquid zone to travel slowly through a relatively long ingot, or charge, of the solid. In zone refining, the most important of the zone-melting techniques, a solid is refined by multiple molten zones being passed through it in one direction. Each zone carries a fraction of the impurities to the end of the solid charge, thereby purifying the remainder. Zone refining is particularly important as a method of purifying crystals, especially for use in semiconductor devices.
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Temperature at which the solid and liquid states of a pure substance can exist in equilibrium. As heat is applied to a solid, its temperature increases until it reaches the melting point. At this temperature, additional heat converts the solid into a liquid without a change in temperature. The melting point of solid water (ice) is 32°F (0°C). Though the melting point of a solid is generally considered to be the same as the freezing point of the corresponding liquid, they may differ because a liquid may freeze into different crystal systems and impurities can lower the freezing point.
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The melting point of a substance is a characteristic property. The melting point may not be equal to the freezing point. This is evident in the phenomenon known as supercooling. In the case of water, ice crystals typically require a seed on which to begin formation. Water on a very clean glass surface will often supercool several degrees below the melting point without freezing. Fine emulsions of pure water have been cooled to -38 degrees celsius without the nucleation of ice taking place. For this reason, melting point is a characteristic property of a substance while freezing point is not.
The "","", and "" in the above are respectively the temperature at the melting point, change of entropy of melting, and the change of enthalpy of melting.
Melting of (Mg,Fe)SiO3-perovskite to 625 kilobars: indication of a high melting temperature in the lower mantle.
Oct 22, 1993; The interpretation and understanding of geochemical differentiation of the Earth, geodynamics, rheology, and, more recently,...
Amplicon melting analysis with labeled primers: A closed-tube method for differentiating homozygotes and heterozygotes
Mar 01, 2003; Background: Common methods for identification of DNA sequence variants use gel electrophoresis or column separation after PCR....