Americium is a radioactive transuranic chemical element with symbol Am and atomic number 95. This member of the actinide series is located in the periodic table under the lanthanide element europium, and thus by analogy was named after the Americas. Americium was first produced in 1944 by the group of Glenn T.Seaborg from Berkeley, California, at the metallurgical laboratory of University of Chicago.
Americium has seven outer electrons ([Rn] 5f⁷ 7s²) and shows states from +2 to +6, with +3 the most stable in solution. Its electronegativity is very low (1.13) and it is dense, malleable, and radioactive: it heats its compounds and oxidizes in air. Its half-filled 5f shell makes it the actinide most similar to europium; Am-241 emits steady alphas for centuries.
4 Am + 3 O₂ → 2 Am₂O₃
In air it tarnishes rapidly to the dark dioxide, the ceramic form used in detectors and sources. Fine powder can burn spontaneously.
2 Am + 6 HCl → 2 AmCl₃ + 3 H₂
It dissolves in acids to give pink americium(III) salts. The chloride is the route for purifying Am-241 from aged plutonium.
AmO₂ + 4 HF → AmF₄ + 2 H₂O
The dioxide converts to the tetrafluoride, the precursor of the metal by reduction with barium and of targets for berkelium.
²⁴¹Am → ²³⁷Np + α
Am-241 decays emitting 5.5 MeV alphas that ionize the air inside detectors and, with beryllium, produce neutrons.
| Compound | Formula | Use or importance |
|---|---|---|
| Americium-241 dioxide | ²⁴¹AmO₂ | Smoke detectors and sources |
| Am-Be source | Am-Be | Neutrons for prospecting |
| Americium tetrafluoride | AmF₄ | Metal production |
| Americium oxalate | Am₂(C₂O₄)₃ | Radiochemical purification |
| Am-243 target | ²⁴³Am | Superheavy element synthesis |
No americium isotope is stable. Americium-241 (²⁴¹Am, 432 years) dominates detectors and sources and is bred from Pu-241. Americium-243 (²⁴³Am, 7,370 years) is a target for curium and berkelium. Americium-242m is one of the most potent fissile isotopes known.
It does not occur in nature in appreciable amounts: only traces from neutron capture in uranium. All americium is bred in reactors, when Pu-239 captures neutrons up to Pu-241, which decays into Am-241. It is extracted from spent fuel or aged plutonium by advanced PUREX.
Glenn Seaborg and his team synthesized it in 1944 by bombarding plutonium with neutrons in Chicago and named it americium, after America: europium's twin on the other side of the Atlantic. It was announced in 1945 on a children's radio program. Smoke detectors carried it into every home.
As Am-241 in ceramic pellets it ionizes the smoke detectors in every house and, with beryllium, generates neutrons for oil exploration and soils. As Am-243 it serves as a target to create berkelium and superheavy elements.
The sealed dioxide measures thickness and density in factories; Am-Be mixtures calibrate reactors and start-up sources. Oxalates purify the isotope in hot cells.
It has no biological function and is highly radiotoxic: inhaled it accumulates in bone and liver for decades. The dose in an intact detector is lower than annual natural radiation.
It is handled only in nuclear facilities, sealed in steel and ceramic. If a detector breaks, do not touch it: ventilate and call radiation protection. It must never be opened or drilled.
Retired detectors are collected as low-level radioactive waste with full traceability. Am-241 decays into extremely long-lived Np-237, which shapes geological repositories.
Americium-241 emits alpha particles that ionize the air inside a sealed chamber. That ionization allows a very small electric current to flow between two electrodes. When smoke enters, its particles attach to the ions and reduce the current flow; the circuit detects that drop and triggers the alarm. The amount of americium is tiny and is encapsulated in layers of metal and ceramic.
Besides smoke detectors, americium-241 is used in thickness, density, and liquid or solid level gauges. It is also combined with beryllium to produce neutron sources used in oil prospecting, soil moisture measurement, and materials analysis. These applications take advantage of its stable alpha emission and long half-life to obtain reliable measurements for years.
Americium is used as starting material to synthesize heavier elements in particle accelerators. By bombarding americium atoms with heavy ions, scientists can create nuclei of superheavy elements that do not occur naturally. These syntheses require tiny amounts of material and high-energy facilities. Americium is therefore a stepping stone in the search for new elements of the periodic table.
If the sealed source is damaged, there is a risk of contamination from americium-241 particles, especially if they are inhaled. For this reason the detector must not be opened, drilled, or dismantled to extract the material. In case of accidental breakage, it is recommended not to touch the debris, ventilate the area, and contact the radiation protection authorities or the manufacturer for safe disposal.
The ionization detector uses americium-241 to create an electric current and responds quickly to the very small particles produced by fast-flaming fires. The photoelectric detector uses a light beam and a sensor: when smoke scatters the light, it triggers the alarm. Ionization detectors are therefore usually more sensitive to fast-burning fires, while photoelectric ones respond better to the dense smoke of slow-burning fires.
Americium-241 decays by alpha emission and transforms into neptunium-237, an element with a half-life of about 2.14 million years. This process is very slow: americium's half-life is about 432 years, so the amount of neptunium produced in a household detector is insignificant. The transformation is part of a broader radioactive chain within the actinides.
When the alpha particles from americium-241 hit light atoms such as beryllium, they can trigger nuclear reactions that release neutrons. This combination makes it possible to build compact neutron sources for prospecting, industrial control, and materials analysis. Americium's advantage is its long half-life and steady emission, which guarantee a constant neutron flux for many years without a reactor.
Main sources consulted: PubChem, Royal Society of Chemistry, NIST, IUPAC. Last revision: November 2026.