Phosphorus-33 is a radioisotope of the chemical element phosphorus, which has 18 neutrons in its atomic nucleus in addition to the element-specific 15 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 33. The short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 33P is exclusively for academic purposes.
A report on the discovery of the nuclide appeared in 1951 [1]. According to this report, phosphorus-33 could be produced and detected by irradiating elemental sulfur, sodium sulfide, and lithium chloride with gamma rays of an energy of 48 MeV; the isotope was formed by the following photonuclear reactions:
34S(γ,p)33P,
35Cl(γ,2p)33P,
37Cl(γ,α)33P.
See also: List of individual Phosphorus isotopes (and general data sources).
Half-life T½ = 25.38(6) d respectively 2.192832 × 106 seconds s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| β- | 33S | 100 % | 0.2485(11) MeV |
Direct parent isotope is: 33Si.
| Z | Isotone N = 18 | Isobar A = 33 |
|---|---|---|
| 7 | 25N | |
| 8 | 26O | |
| 9 | 27F | |
| 10 | 28Ne | 33Ne |
| 11 | 29Na | 33Na |
| 12 | 30Mg | 33Mg |
| 13 | 31Al | 33Al |
| 14 | 32Si | 33Si |
| 15 | 33P | 33P |
| 16 | 34S | 33S |
| 17 | 35Cl | 33Cl |
| 18 | 36Ar | 33Ar |
| 19 | 37K | 33K |
| 20 | 38Ca | |
| 21 | 39Sc | |
| 22 | 40Ti | |
| 23 | 41V | |
| 24 | 42Cr | |
| 25 | 43Mn |
[1] - Raymond K. Sheline, Richard B. Holtzman, Chang-Yun Fan:
The Nuclide P33 and the P32 Spectrum.
In: Physical Review, 83, 919, (1951), DOI 10.1103/PhysRev.83.919.
Last update: 2025-12-29
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