
Every smartphone, every laptop, every solar panel runs on a single element. That element is silicon — the semiconductor that reshaped civilization. Its atom holds 14 electrons. Sounds modest, but this exact structure lets engineers control electric current inside microchips.
Silicon is the second most abundant element in Earth's crust, right after oxygen. It hides in plain sight: beach sand, granite cliffs, window glass. Every grain of sand is silicon dioxide, SiO₂. And yes — Silicon Valley was literally named after this element.
In pure form, silicon is a hard, brittle crystal with a metallic luster. But its real power lies in semiconducting. Add a tiny trace of boron or phosphorus, and silicon conducts current exactly as needed. Every transistor on the planet works on this principle.
Today silicon drives the green energy revolution. Over 95% of solar panels worldwide are made from it. Silicon also forms the core of fiber optic cables — the backbone of the internet. From chips to clean energy, this element shapes the modern world.
Pure silicon is mostly harmless. You can hold a chunk of crystalline silicon in your hand. But silicon dioxide dust (SiO₂) is a serious hazard. Prolonged inhalation of quartz dust causes silicosis — an incurable lung disease. The IARC classifies crystalline SiO₂ as a Group 1 carcinogen. When cutting stone or concrete, respirators and dust extraction are mandatory.
Silicon Valley in California was named after silicon. Mass production of silicon transistors started there in the 1950s, launching the tech revolution.
Ordinary beach sand is silicon dioxide. For microchips, it must be purified to 99.9999999% (nine nines). That's like finding one wrong grain among a billion.
Over 95% of the world's solar panels are made from silicon. A single square meter can produce up to 200 watts of electricity.
Silicon makes up 27.7% of Earth's crust. Only oxygen is more common. Every granite rock, every clay brick contains silicon.
Amethyst, opal, agate, jasper — all are varieties of silicon dioxide SiO₂. Their colors come from microscopic traces of other elements.
Swedish chemist Jons Jacob Berzelius isolated silicon in 1824. He reduced potassium fluorosilicate and got a dark brown powder.
| Isotope | Mass (u) | Abundance | Half-life | Decay |
|---|---|---|---|---|
28Si | 27.976927 | 92.22% | stable | — |
29Si | 28.976495 | 4.68% | stable | — |
30Si | 29.973770 | 3.09% | stable | — |
Reduction of potassium fluorosilicate