What is Sulfur?
Sulfur (symbol S) is element 16 on the periodic table, a nonmetal in period 3, group 16. Yellow, brittle, and responsible for the smell of struck matches, rotten eggs and volcanic vents. At room temperature it is a solid.
Structure
Not a diagram of dots on rings — a Monte-Carlo sample of the actual probability density |ψ|² for each occupied subshell. Drag to rotate. Blue and violet mark opposite signs of the wavefunction, which is what makes bonding possible.
Measured values
Every bar shows where sulfur sits among all 118 elements for that property.
Sources: IUPAC 2021 standard atomic weights · CRC Handbook of Chemistry and Physics · NIST. Values marked ~ are predicted rather than measured.
Size, to scale
Radius 105 pm — that is 0.105 nm, so about 4762 million of them side by side would span a millimetre.
Thermal range
Sulfur is liquid over a 329 K window, from 388 K to 718 K.
The story
Yellow solid with distinctive smell. Essential for proteins.
Sulfur holds the distinction of being one of the few elements known to ancient civilizations in its pure form. Chinese alchemists around 500 BCE called it "liu huang" (flowing yellow) and used it in early gunpowder formulations. The ancient Egyptians employed sulfur for mummification and medicine, while Greek philosopher Pliny the Elder (23-79 CE) documented its use for fumigation and medicinal purposes in his "Natural History."
The element's name derives from the Latin "sulfurium," related to "sulfur" meaning "to burn." Ancient Romans knew it as "sulphur" and associated it with volcanic activity, particularly around Mount Vesuvius and the volcanic islands of Sicily.
Jabir ibn Hayyan (721-815 CE), the father of chemistry, identified sulfur as one of the fundamental principles of matter in his sulfur-mercury theory. This Persian polymath proposed that all metals contained varying proportions of sulfur and mercury, a theory that dominated alchemical thinking for centuries. His work "Kitab al-Khawass al-kabir" described sulfur's properties and purification methods.
The modern understanding of sulfur began with Antoine Laurent Lavoisier (1743-1794), who definitively proved sulfur was an element in his groundbreaking 1777 experiments. Working in his laboratory at the Paris Arsenal, Lavoisier demonstrated that sulfur could not be decomposed into simpler substances and included it in his famous 1789 list of 33 elements in "Traité Élémentaire de Chimie."
Lavoisier's student Joseph Louis Gay-Lussac (1778-1850) and colleague Louis Jacques Thénard (1777-1857) further confirmed sulfur's elemental nature in 1809 by showing that hydrogen sulfide contained only hydrogen and sulfur, with no hidden components.
The industrial significance of sulfur exploded during the 19th century. Peregrine Phillips, a British vinegar manufacturer, patented the Contact Process for sulfuric acid production on October 15, 1831. His method used platinum catalysts to efficiently convert sulfur dioxide to sulfur trioxide, revolutionizing chemical manufacturing.
Nicolas Leblanc (1742-1806) had earlier developed the Leblanc process in 1791, which required enormous quantities of sulfuric acid for sodium carbonate production, driving demand for sulfur worldwide.
German-American chemist Herman Frasch (1851-1914) solved the challenge of extracting sulfur from underground deposits with his ingenious process patented in 1894. Working for Union Sulfur Company in Louisiana, Frasch developed a method using superheated water (160°C) to melt underground sulfur and compressed air to force it to the surface.
On December 26, 1894, at Sulphur Mine, Louisiana, the first Frasch well produced molten sulfur, transforming the global sulfur industry. By 1900, American sulfur production had increased 100-fold, making the United States the world's leading sulfur producer.
Eilhard Mitscherlich (1794-1863) discovered sulfur's allotropic forms in 1823, identifying rhombic and monoclinic crystals. Swedish chemist Jöns Jacob Berzelius (1779-1848) determined sulfur's atomic weight as 32.07 in 1818, remarkably close to today's accepted value of 32.065.
The 20th century brought understanding of sulfur's role in biochemistry, with Frederick Gowland Hopkins discovering the sulfur-containing amino acids cysteine and methionine, earning him the 1929 Nobel Prize in Physiology.
Applications
Sulfur is primarily converted to sulfuric acid (H₂SO₄) through the Contact Process, invented by Peregrine Phillips in 1831. This three-stage process involves:
Modern plants produce up to 3,000 tons per day, with 99.5% conversion efficiency. The largest producers include Mosaic Company (Florida) and Nutrien (Canada).
Sulfuric acid is essential for producing phosphate fertilizers like superphosphate and triple superphosphate. The reaction Ca₃(PO₄)₂ + 2H₂SO₄ → Ca(H₂PO₄)₂ + 2CaSO₄ creates water-soluble phosphorus. Cargill and CF Industries operate massive sulfur-to-fertilizer facilities across the American Midwest.
Sulfuric acid removes impurities in petroleum refining through alkylation processes. ExxonMobil and Chevron use 40-60% sulfuric acid to catalyze the combination of isobutane with alkenes, producing high-octane gasoline components. A single refinery consumes 200-500 tons of sulfuric acid daily.
Sulfuric acid leaches copper from low-grade ores through heap leaching. At Freeport-McMoRan's Arizona operations, crushed ore is irrigated with dilute sulfuric acid (pH 1.5-2.0), dissolving copper as copper sulfate. This process recovers 60-90% of copper from ores containing only 0.4-0.8% copper.
Sulfur compounds are crucial intermediates:
Charles Goodyear's 1839 discovery uses elemental sulfur to cross-link rubber polymers. Modern tire manufacturing at Bridgestone and Michelin uses 1-3% sulfur by weight, creating disulfide bonds between polymer chains. This process transforms soft rubber into durable, elastic material resistant to temperature extremes.
Where it comes from
350 mg/kg of Earth's crust · more abundant than 86% of elements
Sulfur ranks as the 10th most abundant element in the Earth's crust at 260 ppm, and the 5th most abundant in the human body. The element concentrates in specific geological environments due to its unique chemical properties and biological cycling.
Pure sulfur crystals form through several geological processes:
Over 200 sulfur-bearing minerals exist in nature:
Sulfur undergoes complex transformations through biological processes:
Sulfur forms through silicon burning in massive stars (>8 solar masses) at temperatures exceeding 3 billion Kelvin. The process: ²⁸Si + ⁴He → ³²S occurs during the final stages of stellar evolution. Sulfur-16 has a "magic number" of protons, making it unusually stable. Meteorites contain sulfur as troilite (FeS) and oldhamite (CaS), providing evidence of early solar system chemistry.
Seawater contains approximately 905 ppm sulfur as sulfate ions (SO₄²⁻), making it the second most abundant anion after chloride. Mid-ocean ridge hydrothermal vents deposit sulfur minerals from reaction of hot volcanic fluids with cold seawater, creating "black smoker" chimneys rich in copper, zinc, and lead sulfides.
Handling
Elemental sulfur has remarkably low toxicity with an oral LD50 of >5,000 mg/kg in rats, making it practically low-toxicity. However, sulfur compounds pose significant hazards:
Elemental sulfur: Store in cool, dry areas away from oxidizers. Sulfur dust can create explosion hazards - maintain humidity above 65% and use anti-static equipment. Ground all containers and avoid friction-generating activities.
Sulfuric acid: Store in double-walled containers, maintain temperature below 40°C. Always add acid to water, never water to acid. Provide emergency eyewash stations within 25 feet of storage areas.
Sulfur burns at 248°C producing toxic sulfur dioxide. Sulfur dust can form explosive mixtures in air (35-1400 g/m³). Use water spray to cool burning sulfur, never use CO₂ or dry chemical extinguishers on large sulfur fires.
Quick answers
Sulfur (symbol S) is element 16 on the periodic table, a nonmetal in period 3, group 16. Yellow, brittle, and responsible for the smell of struck matches, rotten eggs and volcanic vents. At room temperature it is a solid.
[Ne] 3s² 3p⁴, giving 3 occupied shells holding 2, 8, 6 electrons respectively. Its outer shell holds 6 electrons, which is what sets its bonding behaviour.Sulfur melts at 388.4 K (115.2 °C) and boils at 717.8 K (444.7 °C).
The standard atomic weight of Sulfur is 32.06 u. That is a weighted average across its naturally occurring isotopes, which is why it is rarely a whole number.
Sulfur has a density of 2.067 g/cm³. Water is 1.0 g/cm³, so a block of sulfur is about 2.1× heavier.
Sulfur has a Pauling electronegativity of 2.58. The scale runs from 0.70 (francium, the least greedy for electrons) to 3.98 (fluorine, the most). Values in this middle band tend to form covalent rather than strongly ionic bonds.
Sulfur has been known since antiquity — it occurs in a form usable without smelting, so no single person can be credited with its discovery. The name comes from sanskrit sulvere, via Latin sulphurium.
Sulfur makes up about 350 mg/kg of the Earth's crust — common enough to be mined at scale.