Chlorine-38 is a radioisotope of the chemical element chlorine, which has 21 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 38. The short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 38Cl is exclusively for academic purposes and experimental research.
A report on the discovery of the isotope during the irradiation of chlorine-containing templates with neutrons was published in 1940 [1].
See also: List of individual Chlorine isotopes (and general data sources).
Half-life T½ = 37.230(14) min (minutes) respectively 2.2338 × 103 seconds s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| β- | 38Ar | 100 % | 4.91671(22) MeV | 1.64268(2) MeV [32.9(5) %] 2.167400(9) MeV [44.0(6) %] |
Direct parent isotope is: 38S.
Nuclear isomers or excited states with the activation energy in keV related to the ground state.
| Nuclear Isomer | Excitation Energy | Half-life | Spin |
|---|---|---|---|
| 38mCl | 671.365(8) keV | 715(3) ms | 5- |
| Z | Isotone N = 21 | Isobar A = 38 |
|---|---|---|
| 9 | 30F | |
| 10 | 31Ne | |
| 11 | 32Na | 38Na |
| 12 | 33Mg | 38Mg |
| 13 | 34Al | 38Al |
| 14 | 35Si | 38Si |
| 15 | 36P | 38P |
| 16 | 37S | 38S |
| 17 | 38Cl | 38Cl |
| 18 | 39Ar | 38Ar |
| 19 | 40K | 38K |
| 20 | 41Ca | 38Ca |
| 21 | 42Sc | 38Sc |
| 22 | 43Ti | 38Ti |
| 23 | 44V | |
| 24 | 45Cr | |
| 25 | 46Mn | |
| 26 | 47Fe | |
| 27 | 48Co | |
| 28 | 49Ni |
[1] - J. W. Kennedy, G. T. Seaborg:
Isotopic Identification of Induced Radioactivity by Bombardment of Separated Isotopes; 37-Minute Cl38.
In: Physical Review, 57, 843, (1940), DOI 10.1103/PhysRev.57.843.2.
Last update: 2026-01-02
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