Chlorine-32 is a radioisotope of the chemical element chlorine, which has 15 neutrons in its atomic nucleus in addition to the element-specific 17 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 32. The very short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 32Cl is exclusively for academic purposes.
The isotope chlorine was first produced by the charge exchange reaction 32S(p,n)32Cl during the irradiation of natural S samples with protons accelerated to 20 MeV [1, (1953)].
See also: List of individual Chlorine isotopes (and general data sources).
Half-life T½ = 298(1) ms respectively 2.98 × 10-1 seconds s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| EC/β+ | 32S | 99.92 % | 12.6808(6) MeV | |
| β+ p | 31P | 0.26(5) % | 3.822 MeV | |
| β+ α | 28Si | 0.054(8) % | 5,738 MeV |
Direct parent isotope is: 32Ar.
| Z | Isotone N = 15 | Isobar A = 32 |
|---|---|---|
| 5 | 20B | |
| 6 | 21C | |
| 7 | 22N | |
| 8 | 23O | |
| 9 | 24F | |
| 10 | 25Ne | 32Ne |
| 11 | 26Na | 32Na |
| 12 | 27Mg | 32Mg |
| 13 | 28Al | 32Al |
| 14 | 29Si | 32Si |
| 15 | 30P | 32P |
| 16 | 31S | 32S |
| 17 | 32Cl | 32Cl |
| 18 | 33Ar | 32Ar |
| 19 | 34K | 32K |
| 20 | 35Ca | |
| 21 | 36Sc |
[1] - Neel W. Glass, Louis K. Jensen, J. Reginald Richardson:
The Short-Lived Radioisotopes P28 and Cl32.
In: Physical Review, 90, 320, (1953), DOI 10.1103/PhysRev.90.320.2.
[2] - S. W. Breckon, A. Henrikson, J. S. Foster, W. M. Martin:
The Radioactive Isotopes Al24, P28, Cl32.
In: Canadian Journal of Physics, 32, 3, (1954), DOI 10.1139/p54-020.
[3] - W. F. Rogers et al.:
Ground-state magnetic moment of the T=1 nucleus 32Cl using on-line β-NMR spectroscopy.
In: Physical Review C, 62, 044312, (2000), DOI 10.1103/PhysRevC.62.044312.
Last update: 2026-01-01
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