Sodium Chloride

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Sodium Chloride

Halite (sodium chloride) comes from the Greek halos, meaning "salt" and lithos meaning "rock," and is in fact, better known as rock salt. Halite is called an evaporate because it is formed by the evaporation of saline water in partially enclosed basins. It is very common worldwide, deposited in solid underground masses, and as a dissolved solution in oceans and many arid-region inland lakes.  has lots of salt; it contains an average of 2.6% (by weight) NaCl, or 26 million metric tons per cubic kilometre.

Whenever seawater evaporates, several different minerals come out of solution, starting with the carbonate mineral calcite, then gypsum, then halite. In places where evaporation happens repeatedly, halite beds can be 1,000 meters thick.

Halite is a soft mineral that flows easily under pressure. At depths of as little as 3 kilometres, it begins to rise through the rocks above it in cylindrical plugs called salt domes.

Every day, each of the earth's 5.9 billion inhabitants uses salt. Annual salt production has increased over the past century from 10 million tons to over 200 million tons today. Nearly 100 nations have salt producing facilities ranging from primitive solar evaporation to advanced, multi-stage evaporation in salt refineries.

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Structure

This structure shows the halite, or rock-salt structure. The white spheres represent the larger chloride ions and the smaller red spheres represent the sodium ions. In this structure the chloride ions form a face-centred cubic array, with the sodium ions residing inside the octahedral holes.

Sodium chloride  are . It consists of  tightly  through ionic bonding of the  and chloride ions.  The  is often used as an  of crystalline structure.  It can be . It varies in colour from colourless, when pure, to white, grey or brownish, typical of rock salt (halite). Chemically, it is ...

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