Magnesium

Magnesium is a chemical element in the periodic table that has the symbol Mg and atomic number 12. Magnesium is the eighth most abundant element and constitutes about 2% of the Earth's crust, and it is the third most plentiful element dissolved in seawater. This alkaline earth metal is primarily used as an alloying agent to make aluminium-magnesium alloys.

Table of contents

1 Notable Characteristics
2 Uses
3 History
4 Sources
5 Compounds
6 Isotopes
7 Precautions
8 External Links

Notable Characteristics

Magnesium is a fairly strong, silvery-white, light-weight metal (one third lighter than aluminium) that slightly tarnishes when exposed to air. In a powder, this metal heats and ignites when exposed to air and burns with a white flame. It is difficult to ignite in bulk, though it is easy to light if it is shaved in to thin strips.

Uses

Magnesium compounds, primarily magnesium oxide, are used mainly as refractory material in furnace linings for producing iron and steel, nonferrous metals, glass, and cement. Magnesium oxide and other compounds also are used in agricultural, chemical, and construction industries. This element's principal use is as an alloying additive to aluminium with these aluminium-magnesium alloys being used mainly for beverage cans. Magnesium alloys also are used as structural components of automobiles and machinery. Another use of this metal is to aid the removal of sulfur from iron and steel.

Other uses include:

Magnesium, like aluminium, is strong and light, so it is often used in high grade car wheels, called "mag wheels."
Combined in alloys this metal is essential for airplane and missile construction.
When used as an alloying agent, this metal improves the mechanical, fabrication, and welding characteristics of aluminium.
Additive agent for conventional propellants and used in producing nodular graphite in cast iron.
Reducing agent for the production of pure uranium and other metals from their salts.
Its hydroxide is used in milk of magnesia, its chloride and sulfate in Epsom salts, and its citratess are used in medicine.
Dead-burned magnesite is used for refractory purposes such as brick and liners in furnaces and converters.
Magnesium is also flammable, burning at a temperature of (4000^oF?).
The extremely high temperature at which magnesium burns makes it a handy tool for starting emergency fires during outdoor recreation.
Magnesium carbonate (MgCO₃) powder is also used by athletes, such as gymnasts and weightlifters, to improve the grip on objects -- the apparatus or lifting bar.
Other uses include flashlight photography, flares, and pyrotechnics, including incendiary bombs.

History

The name originates from the Greek word for a district in Thessaly called Magnesia. Joseph Black in England recognized magnesium as being an element in 1755, Sir Humphrey Davey electrolytically isolated pure magnesium metal in 1808 from a mix of magnesia and Hg O and AA Bussy prepared it in coherent form in 1831. Magnesium is the eighth most abundant element in the earth's crust. It is a alkaline earth element and therefore does not occur uncombined with other elements. It is found in large deposits of magnesite, dolomite, and other minerals.

Sources

In the United States this metal is principally obtained by electrolysis of fused magnesium chloride from brines, wells, and sea water. Although magnesium is found in over 60 minerals, only dolomite, magnesite, brucite, carnallite, and olivine are of commercial importance.
Isolation (* follow):
cathode: Mg²⁺* + 2e^- --> Mg
anode: Cl^-* �Cl₂ (gas) + e^-

Compounds

Organic magnesium is important in both plant and animal life. Chlorophylls are magnesium-centered porphyrins. The adult daily nutritional requirement, which is affected by various factors include weight and size, is about 300 mg/day.

Isotopes

Magnesium-26 is a stable isotope that has found application in isotopic geology, similar to that of aluminium. Mg-26 is a radiogenic daughter product of Al-26 (half -life = 0.72x106 yr). Large enrichments of stable Mg-26 have been observed in the Ca-Al-rich inclusions of some carbonaceous chondrite meteorites. The anomalous abundance of Mg-26 is attributed to the decay of its parent Al-26 in the inclusions. Therefore, the meteorite must have formed in ation sources and external links: the solar nebula before the Al-26 had decayed. Hence, these fragments are among the oldest objects in the solar system and have preserved information about its earliest history.

It is conventional to plot Mg-26/Mg-24 against an Al/Mg ratio. In an isochron plot, the Al/Mg ratio plotted is Al-27/Mg-24. The slope of the isochron has no age significance, but indicates the initial Al-26/Al-27 ratio in the sample at the time when the systems were separated from a common reservoir.

Precautions

Magnesium metal is highly flammable in its pure form, especially when it is a powder.
Magnesium metal quickly reacts exothermically upon contact with air or water and should be handeld with care. Water should not be used to extinguish magnesium fires.