What Is a Metalloid and Where Are They Found?

Metalloids represent the small but significant group of elements on the periodic table that serve as a bridge between the distinct properties of metals and nonmetals. These elements possess a unique blend of characteristics, making them indispensable to modern technology and industry.

Defining the Metalloid Category

Metalloids, also referred to as semimetals, are elements that exhibit properties intermediate between those of highly conductive metals and generally insulating nonmetals. They are typically identified by their position on the periodic table, situated along the “stair-step line” that diagonally separates the metals on the left from the nonmetals on the right.

The six elements most commonly accepted as metalloids are Boron (B), Silicon (Si), Germanium (Ge), Arsenic (As), Antimony (Sb), and Tellurium (Te). The classification of Astatine (At) and Polonium (Po) is less consistent among chemists due to their highly radioactive and unstable nature.

Physically, metalloids appear as shiny solids, similar to metals, but they are often brittle and lack malleability. Their chemical behavior tends to lean toward that of nonmetals, such as their tendency to form covalent bonds. This dual nature allows them to sometimes react like a nonmetal and at other times display metallic behaviors, depending on the chemical environment.

Unique Characteristics and Semiconductor Behavior

The most defining and technologically significant property of metalloids is their unique electrical conductivity, which categorizes them as intrinsic semiconductors. Unlike metals, which conduct electricity easily, and nonmetals, which are insulators, metalloids have a conductivity level that falls in between. This intermediate conductivity can be precisely controlled, which forms the foundation of the electronics industry.

The effect of temperature demonstrates this control. A metal’s conductivity decreases as temperature rises because thermal energy causes atoms to vibrate more, which impedes the flow of electrons. Conversely, a metalloid’s conductivity increases with rising temperature because the added thermal energy excites more electrons, allowing them to carry a current.

The primary method for tuning a metalloid’s conductivity is a process called “doping,” which involves intentionally introducing trace amounts of impurities into the pure material. Doping with a Group 15 element, such as Phosphorus or Arsenic, which has five valence electrons, creates an N-type semiconductor. These extra electrons become free charge carriers, increasing the material’s negative charge conductivity.

Alternatively, doping with a Group 13 element, such as Boron, which has only three valence electrons, creates a P-type semiconductor. The missing electron in the crystal lattice creates a “hole,” which acts as a positive charge carrier. The combination of N-type and P-type materials forms a p-n junction, the basic building block of diodes, transistors, and virtually all modern electronic devices.

Where Metalloids Are Found and Used

Metalloids are not typically found in their pure, elemental form in nature. Instead, they are chemically bound within various mineral ores in the Earth’s crust. Silicon, the second most abundant element in the crust, is primarily found in compounds like silicon dioxide (silica), the main component of sand.

The unique properties of metalloids translate directly into their widespread and diverse industrial applications. Silicon’s precise semiconducting ability makes it the dominant material for the microchips and integrated circuits that power computers and smartphones. Silicon is also the foundation of most solar cells, where its ability to create p-n junctions allows it to convert sunlight directly into electricity through the photovoltaic effect.

Boron is incorporated into high-strength, lightweight composite materials, such as boron fibers, used in advanced aerospace structures. It is also used in the manufacturing of borosilicate glass, known for its high resistance to thermal shock.

Germanium is a less common element, often recovered as a byproduct of zinc and copper ore refinement. Its transparency to infrared light makes it a preferred material for lenses and windows in thermal imaging and night vision devices. Germanium is also added to the glass core of fiber-optic cables to precisely control the refractive index, maximizing speed and minimizing signal loss of data transmission.