Silicon-28 is a naturally occurring, stable isotope of the chemical element silicon, which has 14 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 28.
Silicon-28 was first identified as a distinct isotope in 1920 by measuring its mass spectrum [1].
See also: List of individual Silicon isotopes (and general data sources).
Direct parent isotopes are: 28P, 28Al, 29S, 31Ar, 32Cl.
Silicon-28 is produced in stars through the so-called alpha process and the oxygen-burning process; at the same time, the nuclide drives the silicon-burning process in massive stars shortly before their supernova explosion. High-purity Si-28 – such as that used in quantum computers – can be obtained by various methods, as the review article [2] shows.
| Atomic Mass ma | Quantity | Half-life | Spin | |
|---|---|---|---|---|
| Silicon Isotopic mixture | 28.085 u | 100 % | ||
| Isotope 28Si | 27.9769265344(6) u | 92.254 % [92.191 - 92.318 %] | stable | 0+ |
| Isotope 29Si | 28.9764946643(6) u | 4.673 % [4.645 - 4.699 %] | stable | 1/2+ |
| Isotope 30Si | 29.973770137(23) u | 3.073 % [3.037 - 3.110 %] | stable | 0+ |
| Z | Isotone N = 14 | Isobar A = 28 |
|---|---|---|
| 5 | 19B | |
| 6 | 20C | |
| 7 | 21N | |
| 8 | 22O | 28O |
| 9 | 23F | 28F |
| 10 | 24Ne | 28Ne |
| 11 | 25Na | 28Na |
| 12 | 26Mg | 28Mg |
| 13 | 27Al | 28Al |
| 14 | 28Si | 28Si |
| 15 | 29P | 28P |
| 16 | 30S | 28S |
| 17 | 31Cl | 28Cl |
| 18 | 32Ar | |
| 19 | 33K | |
| 20 | 34Ca |
[1] - F. W. Aston:
The Constitution of the Elements.
In: Nature, 105, 547, (1920), DOI 10.1038/105547a0.
[2] - Ravi Acharya et al.:
Highly 28Si enriched silicon by localised focused ion beam implantation.
In: Communications Materials, 5, 57, (2024), DOI 10.1038/s43246-024-00498-0.
Last update: 2025-12-24
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