Aluminum
Aluminium is the most abundant metal in the Earth's crust and the most widely used metal after iron and steel. It is light, strong, rust-resistant and endlessly recyclable. Chances are there is aluminium in your kitchen, your phone, your school bag and your bicycle.
- Atomic Number1313 protons, 13 electrons
- Atomic Mass26.981538 uAbout 27× heavier than hydrogen
- State at Room TempSolidlight, strong solid
- Density2.70 g/cm³One third the density of iron
- Melting / Boiling660.3°C / 2518.8°CMelts at 660°C
- DiscoveredAncientHans Christian Ørsted, 1825
How does aluminium compare to other structural metals?
Aluminium's combination of low density and good strength makes it the go-to metal for transport.
Aluminium (2.70 g/cm³) is about one third as dense as iron and less than a quarter as dense as lead. That is why a jet aircraft can be 80% aluminium and still fly.
What is aluminium?
Aluminium is a post-transition metal in Group 13 of the periodic table. It has 13 protons and three electrons in its outer shell. Although aluminium is highly reactive chemically, it instantly forms a thin, tough layer of aluminium oxide on its surface when exposed to air. That oxide skin protects the metal beneath from further corrosion, which is why aluminium objects do not visibly rust the way iron does.
Aluminium gets its name from alum, a crystalline salt (potassium aluminium sulfate) used since antiquity for dyeing cloth and treating wounds. The name alum comes from the Latin alumen. The British chemist Humphry Davy originally proposed the name alumium, then aluminium. Americans later shortened it to aluminum. Both spellings are in use today, this article uses the British spelling.
Where you find aluminium
In space
Aluminium is the most abundant metal in the Earth's crust. The Moon's highland regions are rich in aluminium silicate minerals, lunar rock samples brought back by Apollo astronauts contain significant amounts. Rocks from Mars also contain aluminium compounds.
On Earth
Aluminium makes up approx. 8% of the Earth's crust by mass, third overall after oxygen and silicon. But because it bonds so readily with other elements, it is never found as a free metal, it must always be extracted from its minerals.
- Bauxite. Bauxite is the ore from which aluminium is extracted. It is a mixture of aluminium hydroxides formed by intense tropical weathering of rocks. Australia, Guinea and Brazil are among the world's largest producers.
- Feldspar and clay. These widespread minerals contain aluminium silicates, but the aluminium is too difficult to extract economically from them.
- Corundum. Pure aluminium oxide forms the mineral corundum. With traces of chromium it becomes a ruby; with iron and titanium, a blue sapphire.
How we use aluminium
- Drink cans and packaging. Aluminium is used for billions of drinks cans and food trays every year. It is light, does not corrode and can be recycled repeatedly without losing quality.
- Aircraft and vehicles. Aluminium alloys are the main structural material in aircraft. A modern passenger jet is approx. 80% aluminium by weight. Cars, trains and buses also use aluminium to save weight.
- Construction. Window frames, cladding panels, roofing and structural supports are made from aluminium because it does not rust and lasts for decades.
- Electrical cables. Aluminium conducts electricity well and weighs far less than copper. High-voltage power lines strung between pylons are almost always aluminium.
How it was discovered
Aluminium was first isolated in 1825 by the Danish physicist Hans Christian Ørsted, who reduced aluminium chloride with potassium amalgam to produce small amounts of impure metal. Friedrich Wöhler produced purer samples in 1827. For decades, producing aluminium was so difficult and expensive that it truly was more valuable than gold.
Everything changed in 1886 when Charles Martin Hall in the USA and Paul Héroult in France independently invented the same electrolytic process to smelt aluminium cheaply from bauxite, on the same day, without knowing about each other. Their process: the Hall-Héroult process, is still used to produce all aluminium today.
Deeper dive: the Hall-Héroult process and the aluminium oxide layer
The Hall-Héroult process dissolves aluminium oxide (Al₂O₃) from processed bauxite in molten cryolite (sodium aluminium fluoride) at approx. 960°C. An electric current is passed through the melt, causing aluminium to deposit at the cathode (bottom) and oxygen to be released at the carbon anodes. The process uses enormous amounts of electricity, approx. 13,000 kilowatt-hours per tonne, which is why aluminium smelters are built next to hydroelectric dams or other cheap power sources.
When aluminium is exposed to air, it immediately forms a layer of aluminium oxide just nanometres thick. This layer is impermeable and extremely hard, protecting the metal beneath. "Anodising" makes this oxide layer much thicker artificially, giving aluminium extra protection and making it easier to colour with dyes, which is why anodised aluminium comes in so many colours.
Aluminium is almost perfectly recyclable: it can be melted and reformed any number of times without losing properties. The global aluminium recycling rate is around 76%, making it one of the most recycled materials in the world. As pressure to reduce carbon footprints grows, the low energy cost of recycled aluminium makes it increasingly valuable.
Aluminium is the metal of the modern world, light, strong, recyclable and everywhere. Moving along the periodic table to 14 protons brings us to silicon, the element inside every computer chip.