Sulfur

REACTIVE NONMETAL · GROUP 16 · PERIOD 3
16
S
Sulfur
32.06

Atomic Data

Atomic Number16
SymbolS
Atomic Weight32.06 u
Density (STP)2.067 g/cm³
Melting Point115.21 °C (388.36 K)
Boiling Point444.6 °C (717.75 K)
Electronegativity2.58 (Pauling)
Electron Config.1s2 2s2 2p6 3s2 3p4
Oxidation States−2, +2, +4, +6
Phase at STPSolid
CategoryReactive Nonmetal
Period / Group3 / 16
CAS Number7704-34-9

Electron Configuration

K L M S

[Ne] 3s2 3p4

Shell n Subshell Electrons Cumulative
K11s22
L22s24
L22p610
M33s212
M33p416
Total 16 16

Isotopes of Sulfur

Sulfur has four naturally occurring stable isotopes. The most abundant is ³²S, comprising 94.99% of all naturally occurring Sulfur.

Isotope Symbol Protons Neutrons Abundance Stability
Sulfur-32³²S161694.99Stable
Sulfur-33³³S16170.75Stable
Sulfur-34³⁴S16184.25Stable
Sulfur-36³⁶S16200.01Stable

Abundance & Occurrence

Sulfur is present in Earth's crust at approximately 350 ppm by mass and at approximately 440 ppm by mass throughout the universe.

Earth's Crust (ppm by mass)

Sulfur
350 ppm
Silicon (ref.)
277,000 ppm
Oxygen (ref.)
461,000 ppm

Universe (ppm by mass)

Sulfur
440 ppm
Helium (ref.)
230,000 ppm
Hydrogen (ref.)
739,000 ppm

Discovery & History

antiquity
Known since antiquity — Sulfur (brimstone) occurs naturally near volcanic vents and was known to ancient civilisations; it is referenced in the Hebrew Bible, the Iliad, and Roman texts as a fumigant, bleaching agent, and incendiary material.
1777
Antoine Lavoisier — Lavoisier argued convincingly that sulfur is a simple substance and not a compound, listing it in his 1789 table of elements — cementing its recognition as a true chemical element.
1839
Charles Goodyear — Goodyear discovered that heating natural rubber with sulfur (vulcanisation) dramatically increases its strength and elasticity — an industrial application that launched the rubber industry and remains in use in every tyre produced today.

Safety & Handling

  • Sulfur dioxide toxicity: Burning sulfur or sulfur-containing materials produces sulfur dioxide (SO2), an acrid, toxic gas that irritates the respiratory tract; high concentrations cause pulmonary oedema and can be fatal.
  • Hydrogen sulfide hazard: H2S, produced when sulfur compounds react with acids or in anaerobic decomposition, is highly toxic — comparable to hydrogen cyanide — and dangerously desensitises the sense of smell at moderate concentrations.
  • Dust and fire: Sulfur dust forms explosive mixtures with air; bulk sulfur can ignite if subjected to friction or spark, especially in the presence of oxidising agents.
  • Skin and eye irritation: Direct contact with sulfur dust causes mild irritation; sulfuric acid, the industrial derivative, is severely corrosive and one of the most hazardous bulk chemicals in industrial use.

Real-World Uses

  • Sulfuric acid production — More sulfuric acid is produced annually than any other industrial chemical; it is used in fertiliser manufacture, petroleum refining, metal ore processing, battery electrolyte, and chemical synthesis.
  • Rubber vulcanisation — Elemental sulfur cross-links natural and synthetic rubber polymer chains during vulcanisation, converting soft, tacky latex into the durable, elastic rubber used in tyres, seals, and hoses.
  • Fungicides and pesticides — Elemental sulfur and sulfur-containing compounds are among the oldest and most widely used agricultural fungicides, effective against powdery mildew, black spot, and mite infestations in vineyards and orchards.
  • Pharmaceuticals and personal care — Sulfur compounds appear in antibiotics (sulfonamides), diuretics, anti-inflammatory drugs, and in acne treatments and medicated shampoos that exploit sulfur's keratolytic and antimicrobial properties.
  • Paper and pulp (kraft process) — The sulfate/kraft pulping process uses sodium sulfide and sodium hydroxide to dissolve lignin from wood chips, producing the strong chemical pulp used in most paper and cardboard production.
  • Gunpowder — Traditional black powder consists of potassium nitrate, charcoal, and sulfur; sulfur lowers the ignition temperature and helps sustain combustion, making it a historical propellant and pyrotechnic ingredient.

Downloadable Resources

Free periodic table reference sheets for classrooms, study sessions, and laboratory use.

Frequently Asked Questions

What is sulfur used for?

Sulfur's most important use is in the production of sulfuric acid, the world's most produced industrial chemical, used in fertilisers, petroleum refining, battery electrolyte, and chemical synthesis. Sulfur is also used to vulcanise rubber, as an agricultural fungicide and pesticide, in pharmaceuticals, in the kraft paper-pulping process, and historically in gunpowder.

What does sulfur smell like?

Pure elemental sulfur is actually odourless. The distinctive rotten-egg smell commonly associated with sulfur is caused by hydrogen sulfide (H₂S), a toxic gas produced by the bacterial breakdown of sulfur-containing proteins and by volcanic activity. Other pungent sulfur compounds include sulfur dioxide (SO₂, the acrid smell of burning sulfur matches) and thiols (the mercaptans added to odourless natural gas as a safety odorant).

Is sulfur essential for life?

Yes, sulfur is an essential element for all living organisms. It is present in the amino acids cysteine and methionine, which are components of proteins. Disulfide bonds (S–S) between cysteine residues help maintain the three-dimensional structure of proteins and enzymes. Sulfur is also part of important coenzymes, including coenzyme A, biotin, and thiamine (vitamin B₁), and is a key component of the iron-sulfur clusters in many electron-transfer enzymes.

Where does sulfur come from?

Most commercial sulfur is recovered as a by-product of oil and gas processing: the hydrodesulfurisation process removes sulfur from petroleum and natural gas to produce clean fuels, and the elemental sulfur is captured rather than emitted as SO₂. Additional sulfur comes from smelting of sulfide ores (pyrite, chalcopyrite, sphalerite). Natural deposits of elemental sulfur occur around volcanic vents and salt dome cap rocks, where it was deposited by bacterial reduction of calcium sulfate.