Aluminium

Aluminium, Al, is a metallic element found in Group IIIb of the periodic table. Aluminium is the most abundant metal in the world (approximately 8.1% by weight)

Discovery

Aluminium in the form of its oxide was shown as being different from Lime, Ca(OH)2, by A S Marggraf in 1754AD. Aluminium was isolated, as a gray metallic powder, by F Wohler in 1827AD, after he heated Anhydrous Aluminium Chloride, AlCl3, with Potassium metal.

Occurrence

Aluminium is highly reactive and does not occur in the free state. However, it is widely distributed and it is third in abundance on earth after Oxygen and Silicon.
Aluminium exists primarily as Alumino-Silicates (i.e. as Felspar, NaAlSi3O8, or KAlSi3O8, or CaAl2Si2O8), in igneous rocks and as Clays, H4Al2Si2O9, in sedimentary rocks.
Aluminium has three principal ores Aluminium also occurs in the form of its Aluminium Oxide, Al2O3, in the semiprecious stones. The colouration in these gems is caused by trace quantities of impurities :

Manufacture

Aluminium is manufactured by the electrolysis of fused mixture of Bauxite, Al2O3.2H2O, and Cryolite, AlF3.3HF.

Properties


Uses

The typical metallic properties of aluminium cause it to be used

Reactions

Aluminium reacts rapidly with the Oxygen in air to form Aluminium Oxide, Al2O3, which forms a tough layer on the surface of the metal, thereby preventing any further reaction. This aluminium oxide layer can be thickened by a process known as anodising, which involves using the aluminium object as the anode in an electrolytic cell.

Detection and Analysis

Aluminium is usually identified by the gelatinous precipitate of its hydroxide which forms when alkali is added to a solution of its salts.


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