Aluminium-30 is a radioisotope of the chemical element aluminium, which has 17 neutrons in its atomic nucleus in addition to the element-specific 13 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 30.
The radioactive isotope was first described in 1961 [1]; according to this, 30Al was observed during the irradiation of a Si template in a cyclotron with deuterons (hydrogen-2 nuclei) with an energy of 8.8 MeV; the nuclide was formed by a charge exchange reaction of silicon-30:
30Si(n,p)30Al.The very short-lived, neutron-rich, unstable and thus radioactive nuclide has no practical significance; the study of 30Al serves exclusively academic purposes.
See also: List of individual Aluminium isotopes (and general data sources).
Half-life T½ = 3.62(6) s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| β- | 30Si | 100 % | 8.5688(19) MeV | 2.23523(2) MeV [65(1) %] 1.26313(3) MeV [40.6(14 %] |
Direct parent isotope is: 30Mg.
| Z | Isotone N = 17 | Isobar A = 30 |
|---|---|---|
| 7 | 24N | |
| 8 | 25O | |
| 9 | 26F | 30F |
| 10 | 27Ne | 30Ne |
| 11 | 28Na | 30Na |
| 12 | 29Mg | 30Mg |
| 13 | 30Al | 30Al |
| 14 | 31Si | 30Si |
| 15 | 32P | 30P |
| 16 | 33S | 30S |
| 17 | 34Cl | 30Cl |
| 18 | 35Ar | 30Ar |
| 19 | 36K | |
| 20 | 37Ca | |
| 21 | 38Sc | |
| 22 | 39Ti | |
| 23 | 40V | |
| 24 | 41Cr | |
| 25 | 42Mn |
[1] - E. L. Robinson, O. E. Johnson:
New Isotope, Al30.
In: Physical Review, 123, 1349, (1961), DOI 10.1103/PhysRev.123.1349.
Last update: 2024-11-24
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