Chlorine-33 is a radioisotope of the chemical element chlorine, which has 16 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 33. The very short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 33Cl is exclusively for academic purposes and experimental research.
The isotope was first observed when highly purified sulfur templates were irradiated with deuterons (hydrogen-2 nuclei) of an energy of 8 MeV [1, (1940)]:
32S(d,n)33Cl.
Chlorine-33 can also be produced by irradiating sulfur-32 with helium-3 nuclei of an energy of 9.68 MeV according to the following proton transfer reaction [2]:
32S(3He, d)33Cl.
See also: List of individual Chlorine isotopes (and general data sources).
Half-life T½ = 2.5059(23) s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| EC/β+ | 33S | 100 % | 5.5825(4) MeV |
Direct parent isotopes are: 33Ar, 35Ca.
| Z | Isotone N = 16 | Isobar A = 33 |
|---|---|---|
| 5 | 21B | |
| 6 | 22C | |
| 7 | 23N | |
| 8 | 24O | |
| 9 | 25F | |
| 10 | 26Ne | 33Ne |
| 11 | 27Na | 33Na |
| 12 | 28Mg | 33Mg |
| 13 | 29Al | 33Al |
| 14 | 30Si | 33Si |
| 15 | 31P | 33P |
| 16 | 32S | 33S |
| 17 | 33Cl | 33Cl |
| 18 | 34Ar | 33Ar |
| 19 | 35K | 33K |
| 20 | 36Ca | |
| 21 | 37Sc | |
| 22 | 38Ti |
[1] - J. Barton Hoag:
The Production and Half-Life of Chlorine 33.
In: Physical Review, 57, 937, (1940), DOI 10.1103/PhysRev.57.937.2.
[2] - I. Lombardo et al.:
Study of the 33Cl spectroscopic factors via the 32S(3He, d)33Cl one-proton transfer reaction.
In: Journal of Physics G, 48, 065101, (2021), DOI 10.1088/1361-6471/abdee4.
Last update: 2026-01-01
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