Argon-36 is a naturally occurring, stable isotope of the chemical element argon, which has 18 neutrons in its atomic nucleus in addition to the element-specific 18 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 36.
The first mass spectroscopic detection and thus the discovery of Argon-36 was reported in 1920 [1].
See also: List of individual Argon isotopes (and general data sources).
Argon is a stable isotope! Theoretically, the nuclide could undergo neutrinoless double beta decay (0νββ); however, this has not yet been experimentally proven.
Half-life T½ = stable.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| 0νββ ? |
Direct parent isotopes are: 37Ca, 36K, 36Cl, 40Sc.
| Atomic Mass ma | Quantity | Half-life | Spin | |
|---|---|---|---|---|
| Argon Isotopic mixture | 39.88 u | 100 % | ||
| Isotope 36Ar | 35.967545106(29) u | 0.3336(210) % | stable | 0+ |
| Isotope 38Ar | 37.96273210(21) u | 0.0629(70) % | stable | 0+ |
| Isotope 39Ar | 38.964313(5) u | [trace] | 268(8) a | 7/2- |
| Isotope 40Ar | 39.962383120(23) u | 99.6035(250) % | stable | 0+ |
| Isotope 42Ar | 41.963046(6) u | [trace] | 32.9(11) a | 0+ |
| Z | Isotone N = 18 | Isobar A = 36 |
|---|---|---|
| 7 | 25N | |
| 8 | 26O | |
| 9 | 27F | |
| 10 | 28Ne | |
| 11 | 29Na | 36Na |
| 12 | 30Mg | 36Mg |
| 13 | 31Al | 36Al |
| 14 | 32Si | 36Si |
| 15 | 33P | 36P |
| 16 | 34S | 36S |
| 17 | 35Cl | 36Cl |
| 18 | 36Ar | 36Ar |
| 19 | 37K | 36K |
| 20 | 38Ca | 36Ca |
| 21 | 39Sc | 36Sc |
| 22 | 40Ti | |
| 23 | 41V | |
| 24 | 42Cr | |
| 25 | 43Mn |
[1] - F. W. Aston:
The Constitution of the Elements.
In: Nature, 105, 8, (1920), DOI 10.1038/105008a0.
[2] - GERDA Collaboration:
An improved limit on the neutrinoless double-electron capture of 36Ar with GERDA.
In: The European Physical Journal C, 84, 34, (2024), DOI 10.1140/epjc/s10052-023-12280-6.
Last update: 2026-01-05
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