Americium Oxidation States

Reference for Americium (Am, element 95) oxidation states — known states (+2 through +7), the dominant +3 state, and representative compounds.

Use the Americium Oxidation States

Am
Americium
Atomic number 95 · Period 7 · Actinide series
Radioactive

Americium (Am) is a synthetic actinide metal produced in nuclear reactors. All isotopes are radioactive. Unlike the preceding actinide actinium, americium exhibits multiple oxidation states — +2, +3, +4, +5, +6, and +7 — with +3 being the most stable in standard aqueous conditions. Am³⁺ is 5f⁶; the half-filled 5f⁷ configuration belongs to the much rarer Am²⁺ ion.

Oxidation States

State Status Notes
+3 Most stable Am³⁺; [Rn] 5f⁶; dominant in ordinary aqueous solution; colorless–pale pink in solution
+4 Confirmed Am⁴⁺; exists in solid AmO₂ and in strongly oxidizing fluoride media; pink color
+5 Confirmed AmO₂⁺ (americyl(V)); yellow-brown in solution; unstable toward disproportionation to Am³⁺ + Am(VI)
+6 Confirmed AmO₂²⁺ (americyl(VI)); strong oxidizer; prepared with persulfate or ozone; reverts to Am³⁺ in weakly acidic media
+7 Confirmed Observed in strongly alkaline solution (e.g., [AmO₆]⁵⁻) via ozone or persulfate oxidation; strong oxidizer
+2 Rare Am²⁺; [Rn] 5f⁷ half-filled subshell; observed in certain solid-state systems under extreme reducing conditions; very uncommon in water
+1, 0 Not observed No confirmed compounds; only element 0 is metallic Am

Why Is +3 the Most Stable State?

1
Electron configuration

Americium's ground-state configuration is [Rn] 5f⁷ 7s². Removing the two 7s electrons gives Am²⁺ with the half-filled configuration [Rn] 5f⁷; removing one more 5f electron gives Am³⁺ with configuration [Rn] 5f⁶.

2
Why half-filled Am²⁺ does not dominate in water

The half-filled 5f⁷ subshell provides real electronic stabilization to Am²⁺, but it is only one part of the free-energy balance. In ordinary aqueous solution, the stronger hydration of Am³⁺ and the unfavorable Am³⁺/Am²⁺ reduction energetics outweigh that shell benefit. Am²⁺ is therefore a powerful reductant that requires exceptional reducing conditions, while hydrated Am³⁺ is the prevalent state.

3
Contrast with early actinides

Early actinides (U, Np, Pu) readily form +5 and +6 because their 5f electrons are spatially more extended and energetically accessible for bonding. By the time you reach Am (5f⁷), the 5f orbitals are more contracted and lower in energy, reducing their participation in bonding — so +3 dominates, just as in the lanthanides.

Key Americium Compounds by Oxidation State

Am₂O₃
+3
Americium(III) oxide

Black solid; most common oxide. Adopts the Mn₂O₃ or La₂O₃ structure depending on temperature.

AmCl₃
+3
Americium(III) chloride

Pink crystalline solid; UCl₃-type structure. The pink color is characteristic of Am³⁺ in many solids.

AmO₂
+4
Americium(IV) oxide

Black solid with fluorite structure (same as UO₂, PuO₂). Stable in the solid state; Am⁴⁺ in solution is much harder to sustain.

AmO₂²⁺
+6
Americyl(VI) ion

Linear O=Am=O²⁺ dioxocation; analogous to UO₂²⁺. Formed by strong oxidizers (S₂O₈²⁻, O₃); rapidly reverts to Am³⁺ in dilute acid.

AmF₃ (pink), AmBr₃, and AmI₃ also confirm the +3 state. All halide salts are isostructural with the corresponding lanthanide halides.

Comparison to Europium (Eu)

Property Europium (Eu) Americium (Am)
Atomic number 63 95
Series Lanthanide Actinide
Electron config [Xe] 4f⁷ 6s² [Rn] 5f⁷ 7s²
f-shell in atom 4f⁷ (half-filled) 5f⁷ (half-filled)
Divalent ion Eu²⁺: 4f⁷ (half-filled) Am²⁺: 5f⁷ (half-filled)
Trivalent ion Eu³⁺: 4f⁶ Am³⁺: 5f⁶
Common oxidation states +2, +3 +2, +3, +4, +5, +6, +7
Most stable state +3 +3
Radioactive? No (stable isotopes exist) Yes (all isotopes)

Neutral Eu and Am both have f⁷s² ground-state patterns, and their divalent ions retain half-filled f⁷ subshells. Their prevalent trivalent ions are instead f⁶. Americium extends to higher states (+4 through +7) because 5f orbitals are more spatially extended than 4f and can participate in bonding more readily.

Radioactivity and Practical Occurrence

All americium isotopes are radioactive; the element does not occur in nature. ²⁴¹Am (half-life 432.2 years, alpha emitter) is the most widely encountered isotope — it is found in household ionization smoke detectors, where a small amount of Am is used in an ionization chamber. ²⁴³Am (half-life 7,370 years) is longer-lived and used in research. Americium is produced in nuclear reactors by successive neutron captures on 239Pu. Despite its radioactivity, the oxidation chemistry of americium is well established — the ionic state does not depend on which isotope is present.

Summary

Reference for Americium (Am, element 95) oxidation states — known states (+2 through +7), the dominant +3 state, and representative compounds.

How it works

  1. Locate the oxidation states table to see confirmed states for americium (+2 through +7) and their stability.
  2. Read the electron configuration section to compare half-filled 5f⁷ Am²⁺ with the aqueous-dominant 5f⁶ Am³⁺ state.
  3. Review the compounds list (AmO₂, AmF₃, AmCl₃, AmO₂⁺) to see each oxidation state in real chemistry.
  4. Check the europium comparison to understand the lanthanide–actinide relationship at element 63/95.

Use cases

  • Looking up americium oxidation states for a nuclear chemistry or radiochemistry problem.
  • Understanding why Am³⁺ dominates aqueous chemistry even though Am²⁺ has a half-filled 5f⁷ subshell.
  • Writing balanced equations for americium compounds such as Am₂O₃ or AmO₂.
  • Comparing americium to europium as f-block homologs whose uncommon +2 ions have half-filled f⁷ subshells.
  • Studying actinide chemistry and the variable oxidation states that distinguish early from late actinides.

Frequently Asked Questions

Last updated: 2026-09-13 · Reviewed by Nham Vu