
Rotten eggs, blue volcanic flames, and gunpowder that changed the course of wars — all thanks to sulfur. Ancient civilizations called it "brimstone" and linked it to the underworld. In reality, this bright yellow nonmetal is one of the most essential elements for life and industry.
Sulfur is part of the amino acids cysteine and methionine. Without them, proteins could not exist. Sulfuric acid (H₂SO₄) is the world's most produced chemical by volume. It goes into fertilizers, oil refining, and metallurgy. And vulcanizing rubber with sulfur gave humanity car tires.
Every year, humanity produces over 80 million tons of sulfur. Most of it comes as a byproduct of oil and gas refining. That is actually good news: factories used to release SO₂ into the air, but now they capture sulfur and put it to use.
Sulfur springs have been prized for healing since ancient times. Sulfur helps treat skin conditions. In agriculture, sulfur-based fertilizers boost crop yields. And in winemaking, sulfur dioxide (SO₂) acts as a preservative that keeps wine fresh.
Pure sulfur has low toxicity. But its compounds are treacherous. Hydrogen sulfide (H₂S) at 100 ppm paralyzes your sense of smell — you stop detecting the gas and assume the danger is gone. At 500 ppm, death comes within minutes. Sulfur dioxide (SO₂) irritates the airways. Sulfuric acid causes severe chemical burns on contact. Working with sulfur requires ventilation and safety goggles.
Sulfur burns with a blue flame. Ancients thought it was hellfire. The blue glow actually comes from excited SO₂ molecules.
Sulfuric acid is the most produced chemical on Earth. Over 260 million tons of H₂SO₄ are made every year.
Gunpowder — the first explosive in history — contains 10–15% sulfur. It was invented in China back in the 9th century.
No sulfur means no proteins. The amino acids cysteine and methionine contain sulfur atoms that hold protein molecules in shape.
Indonesia's Kawah Ijen volcano has a turquoise lake colored by dissolved sulfuric acid. Miners still extract sulfur there by hand.
| Isotope | Mass (u) | Abundance | Half-life | Decay |
|---|---|---|---|---|
32S | 31.972071 | 94.93% | stable | — |
33S | 32.971459 | 0.76% | stable | — |
34S | 33.967867 | 4.29% | stable | — |
36S | 35.967081 | 0.02% | stable | — |
Known since antiquity