by Chris Woodford. Last updated: February 18, 2016.
Hard, shiny, and tough—metals are the macho poster boys of the material world. Learning how to extract these substances from the Earth and turn them into all kinds of useful materials was one of the most important developments in human civilization, spawning tools, jewelry, engines, machines, and giant static constructions like bridges and skyscrapers. Having said that, "metal" is an almost impossibly broad term that takes in everything from lead (a super-heavy metal) and aluminum (a super-light one) to mercury (a metal that's normally a liquid) and sodium (a metal soft enough to cut like cheese that, fused with chlorine, you can sprinkle on your food—as salt!). What exactly are metals and what makes them so useful? Let's take a closer look!
What are metals?
You might think Earth is a big lump of rock, hard on the outside and soft in the middle—but quite a lot of it is actually metal. What exactly is metal? Over three quarters of the chemical elements that occur naturally on our planet are metals, so it's almost easier to say what metal isn't.
When we talk about metals, we're usually referring to chemical elements that are solid (with relatively high melting points), hard, strong, durable, shiny, silvery gray in color, good conductors of electricity and heat, and easy to work into various different shapes and forms (such as thin sheets and wires). The word metal is quite a broad and vague term, and not something you can define precisely.
When we talk about nonmetals, it ought to mean everything else—although things are a bit more complex than that. Sometimes you'll hear people refer to semimetals or metalloids, which are elements whose physical properties (whether they're hard and soft, how they carry electricity and heat) and chemical properties (how they behave when they meet other elements in chemical reactions) are somewhere in between those of metals and nonmetals. Semimetals include such elements as silicon and germanium—semiconductors (materials that conduct electricity only under special conditions) used to make integrated circuits in computer chips and solar cells. Other semimetals include arsenic, boron, and antimony (all of which have been used in the preparation—"doping"— of semiconductors).
Take a look at the periodic table (the way we draw the elements in a chart so ones with similar physical and chemical properties line up together) and you'll see two types of metal get special treatment. The middle of the table is dominated by a large group of elements called the transition metals (or transition elements); most of the familiar metals (including iron, copper, silver, and gold) live here, along with less well known metals such as zirconium, osmium, and tantalum. The other group, called the rare-earth metals, is often printed separately from the main periodic table and includes the fifteen elements from lanthanum to lutetium plus scandium and yttrium. They're called "rare earth" metals for the rather obvious reason that they were originally believed to exist in extremely scarce deposits in Earth, though some are now known to be relatively common. Like many conventional metals, the rare-earths don't occur naturally in their pure form, but only as metal oxides.
When is a metal not a metal? Look at a car, plane, or motorcycle and you see lots of metal—or do you? Quite a lot of the metal-like materials around us are actually alloys: metals that have been mixed with other materials (metals or nonmetals) to make them stronger, harder, lighter, or superior in some other way. Steel is an alloy of iron, for example, that contains a small amount of carbon (different types of steel contain more or less carbon). Bronze is an alloy of copper and tin, while brass is the alloy you get when you mix copper and zinc.
Photo: Metal or alloy? Screws like this are usually made from steel, an alloy of iron (a metal) and carbon (a nonmetal).
How are metals made?
Whether you're assembling airplanes or building batteries, you need metals—and lots of them. The snag is that metals generally don't occur in the ground in exactly the way that we'd like to find them, in their pure form and in deposits large enough to make it worth our while to extract them. Often they're buried in rock with deposits of other metals and they exist not as pure elements but oxides (metals fused with oxygen atoms) and other compounds. Producing large quantities of a metal like iron, aluminum, or copper therefore involves two distinct operations: extracting an ore (a deposit consisting usually of a huge amount of useless rock and smaller amounts of useful metals) from a mine or quarry and then refining the ore to get the metals away from their oxides (or other compounds) into the pure form that we need.
Exactly how this is done varies from metal to metal and from place to place, but usually involves a mixture of mechanical processing (such as grinding, filtering, or using water to wash away unwanted materials), chemical treatment (using acids, perhaps), heating (smelting iron ore, for example, involves roasting it in air to remove the impurities), and electrical treatment (such as electrolysis—separating a chemical solution into its constituent elements by passing an electric current through it).
Photo: Metals are buried inside Earth, usually mixed in with useless rock. Extracting them is often difficult, dangerous, and expensive. Photo by David Parsons courtesy of US DOE/NREL (US Department of Energy/National Renewable Energy Laboratory).
What are metals like?
With so many chemical elements classified as metals, you might think it would be difficult to generalize about them. But that problem is true of pretty much any generalization: every house is different, but we can still say that houses tend to have doors, walls, windows, and a roof and provide shelter from the weather—and we can all sketch one on paper.
The generalizations we make about metals are that they are mostly solid (at everyday temperatures), crystalline (their atoms are stacked up in orderly patterns like cans in a supermarket), hard, strong, and dense (most metals will sink if you drop them in water, for example). Metals are malleable (relatively easy to work into new shapes and forms) and ductile (with the right equipment, you can tease them out into long, thin wires). Even so, they don't wear out quickly or break easily, though they can and do snap eventually through repeated stresses and strains because of metal fatigue (a gradually developing weakness). Most metals are opaque (unless extremely thin) and shiny and silvery gray in color (because they tend to reflect all wavelengths of light to the same extent). Some metals are colored (because they reflect certain light wavelengths better than others); the best-known examples are probably gold (a yellowish color) and copper (normally reddish, though it turns blue after exposure to air converts it into copper oxide). Most metals conduct electricity well (they have a low electrical resistance, in other words) and feel instantly cold to the touch (because they conduct heat well too, carrying heat energy quickly away from your body).
Photo: Metals are generally colorless, but they do glow with characteristic (and different) colors when you hold them in a flame—a technique called a flame test. This greenish-blue flame is being produced by a pipe made from copper and nickel. Photo by Adam York courtesy of US Navy.