3.7.1. Natural Occurrence and Physical Properties. Aluminum is a silvery-white, quite soft malleable metal that melts at 660
oC. Aluminum is the most abundant metal and the third most abundant element in the Earth's crust (after oxygen and silicon), occurring in nature in the form of various oxide, hydroxide, and silicate derivatives. Rubies and sapphires are Al
2O
3 colored by impurities of other metals. Beryl and some types of garnet are aluminum compounds. Feldspar rocks, the most common group of minerals in the Earth's crust, are composed of Al, Si, O, and an alkali (Na, K) or alkaline earth (Ca) metal.
3.7.2. Production and Uses of Aluminum. While there are many different aluminum minerals on Earth, only one group of them,
bauxites, is used to make aluminum metal. Making aluminum from other minerals would be less economical. To produce aluminum, pure aluminum oxide (Al
2O
3), also known as
alumina, is needed. The main components of bauxite, Al(OH)
3 and AlO(OH), could be quite easily converted to alumina by dehydration at heating. First, however, some iron and titanium impurities present in bauxites must be removed. Without going into details, the
Bayer alumina process furnishes pure Al
2O
3 suitable for making aluminum.
In Volume 2, it was mentioned that aluminum metal is made by the Hall-Héroult electrolytic process (section 2.8.1). In this highly energy demanding process, Al
2O
3 is electrolyzed to reduce Al
3+ to Al
0 at the cathode. The electrolysis is conducted in an Al
2O
3 solution in molten cryolite (Na
3AlF
6) at 950-1,000
oC. Note that pure Al
2O
3 melts at approximately 2,070
oC, too high a temperature for a large-scale operation. On passing electricity through a solution of alumina in molten cryolite, the aluminum ions move toward the cathode and the oxide ions toward the anode. Both electrodes are made of carbon, the anode of fused coke and the cathode of graphite. Figure 3-88 displays equations for the processes occurring at the anode and cathode in the electrolysis of Al
2O
3.