Magnesium (Mg) is a light, silvery-white, moderately hard, metallic element which in ribbon or powder form burns with a brilliant white flame. Magnesium is the second lightest member of the alkaline earth metals (after beryllium). It can be combined with aluminum to give a structural alloy, and is also used in pyrotechnics. It was formerly used to make flash bulbs in photography. The most common isotope is ²⁴Mg (78.7%).

 

Earth's oceans contain an estimated trillion trillions tons of magnesium, and this is the source of much of the 300,000 tons produced annually.

 

Magnesium was recognized as an element by Joseph Black of Edinburgh in 1775 and first isolated as a metal by Humphry Davy in 1808. It is named after Magnesia, a district of Thessaly in Greece, where it was first found.

 

atomic number	12
relative atomic mass	24.305
electron configuration	1s22s22p63s2
melting point	651°C (1,204°F)
boiling point	1,107°C (2,205°F)
relative density	1.74
first ionization energy	737.1 kJ/mol
second ionization energy	1,451 kJ/mol
second ionization energy	1,451 kJ/mol
atomic radius	160 pm
ionic radius	66 pm

 

Chemistry of magnesium

Magnesium is one of the least reactive of the alkaline earth metals. If heated it will react with water to form magnesium hydroxide and hydrogen, but this reaction occurs very slowly. Magnesium ribbon burns in air with a brilliant white light to form magnesium oxide (Figure 1). It will also react with any of the halogens to form the corresponding magnesium halide, and will react with nitrogen to form magnesium nitride at high temperatures. When heated with sulfur, magnesium sulfide is formed. Magnesium reacts readily with acids and displaces the hydrogen from the acid as hydrogen.

Magnesium forms a wide range of ionic compounds. Some common magnesium compounds include milk of magnesia, which is a suspension of magnesium hydroxide and Epsom salts, which is magnesium sulfate hepahydrate. The ionic compounds of magnesium generally tend to be more soluble than the heavier members of the group. Magnesium can also form covalent bonds with carbon, an example of which is the Grignard reagent phenylmagnesium bromide.

 

Sources and production

The most important sources of magnesium are seawater and dolomite rock, a mixture of calcium and magnesium carbonates. It also occurs naturally as the minerals brucite and magnesite. Magnesium is generally obtained by the electrolysis of magnesium halides. In the production of magnesium from seawater the magnesium is precipitated as the hydroxide and converted to the chloride by reaction with hydrochloric acid. The magnesium chloride is recovered by evaporation of the solution, and magnesium metal is obtained by electrolysis of the molten salt. Magnesium isalso manufactured by the silicothermic process, in which mixed oxides, formed by the calcination of dolomite, are reduced at high temperature with ferrosilicon, forming magnesium crystals.

 

Brucite

Brucite is a mineral form of magnesium hydroxide (Mg₃(OH)₆), derived from periclase. The crystals are either glassy or waxy, can be white, pale green, gray, or blue, and occur in fibrous masses or plate aggregates (Figure 2). Brucite is found in serpentine, schists, and other metamorphic rocks. It is used to make magnesia refractory materials.

 

Magnesite

Magnesite is a carbonate mineral, magnesium carbonate (MgCO₃). It is an alteration product of calcite or dolomite in sedimentary rocks and is found in microcrystalline masses and hexagonal crystals like Iceland spar (Figure 3). Magnesite is white, with a glassy to dull texture. Hardness 3.5–5, relative density 3.1. Magnesite is used mainly for lining furnaces, since it decomposes to give magnesium oxide on heating.

 

Magnesium and life

Magnesium is an essential element for all terrestrial life. Humans take in approximately 250–350 milligrams each day (about 4 ounces a year), and we each have about 25 grams (just under an ounce) in our bodies, much of it in the bones and teeth. It is needed for the proper functioning of muscle and nervous tissue, and is required as a cofactor for approximately 90 enzymes. Chlorophyll, the compound responsible for the green color of leaves and for photosynthesis, is a coordination compound containing magnesium.

 

Dietary sources of magnesium include cereals (especially whole-grain), nuts, soya beans, milk, fish, and meat. Deficiency usually occurs as a result of severe kidney disease, alcohol dependence, an intestinal disorder that impairs the absorption of magnesium and calcium, or prolonged treatment with diuretic drugs or digitalis drugs. Symptoms of deficiency include anxiety, restlessness, tremors, palpitations, and depression. There may also be an increased risk of kidney stones.

 

Magnesium compounds

Magnesium hydroxide (Mg(OH)₂) occurs naturally as colorless hexagonal plates of brucite. It is formed as a gelatinous precipitate when an alkali is added to magnesium salts. It is a base and loses water when heated to 350°C. Magnesium hydroxide is used as an osmotic laxative to treat constipation, and is also combined with aluminum hydroxide in antacid preparations.

 

Magnesium oxide (MgO), or magnesia, is a white crystalline solid and also a base. Being highly refractory, it is used in furnace linings. When mixed with magnesium chloride solution, magnesia forms a durable cement used as a stucco finish on buildings.

 

Magnesium sulfate (MgSO₄), or Epsom salts, is a colorless crystalline solid. It is used in the form of mixtures or powders as an osmotic laxative for rapid evacuation of the bowel. It is also administered intravenously to treat magnesium deficiency and serious arrhythmias and to prevent the recurrence of convulsions in eclampsia.