Silicon-26 is a radioisotope of the chemical element silicon, which has 12 neutrons in its atomic nucleus in addition to the element-specific 14 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 26. The very short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 26Si is exclusively for academic purposes.
The first observation of the nuclide was reported in 1960 [1]; according to this, silicon-26 could be produced and identified by irradiating a magnesium-24 containing template with helium-3 ions of an energy of 8 MeV:
24Mg(3He,n)26Si.
See also: List of individual Silicon isotopes (and general data sources).
Half-life T½ = 2.2453(7) s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| EC/β+ | 26Al | 100 % | 5.06914(13) MeV |
Direct parent isotope is: 26P.
| Z | Isotone N = 12 | Isobar A = 26 |
|---|---|---|
| 4 | 16Be | |
| 5 | 17B | |
| 6 | 18C | |
| 7 | 19N | |
| 8 | 20O | 26O |
| 9 | 21F | 26F |
| 10 | 22Ne | 26Ne |
| 11 | 23Na | 26Na |
| 12 | 24Mg | 26Mg |
| 13 | 25Al | 26Al |
| 14 | 26Si | 26Si |
| 15 | 27P | 26P |
| 16 | 28S | 26S |
| 17 | 29Cl | |
| 18 | 30Ar | |
| 19 | 31K |
[1] - E. L. Robinson, O. E. Johnson:
Decay of Si26.
In: Physical Review, 120, 1321, (1960), DOI 10.1103/PhysRev.120.1321.
Last update: 2025-12-24
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