Chlorine-39 is a radioisotope of the chemical element chlorine, which, in addition to the element-specific 17 protons, has 22 neutrons in the atomic nucleus, resulting in the mass number 39. The very short-lived, unstable and therefore radioactive nuclide has no practical significance from a technical point of view.
39Cl is one of the cosmogenic nuclides that are continuously formed in the atmosphere by solar and cosmic radiation: The chlorine isotope is created by the interaction of slow negative muons μ- of cosmic rays with Argon-40 in the lower air layers. The trace radioisotope chlorine-39, which decays quickly into the stable isotope Ar-39, can be detected in small quantities in rainwater samples [2].
See also: list of Chlorine isotopes.
Half-life T½ = 56.2(6) min (minutes) respectively 3.372 × 103 seconds s.
Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
---|---|---|---|---|
β- | 39Ar | 100 % | 3.44197 MeV |
Direct parent isotope is: 39S.
Z | Isotone N = 22 | Isobar A = 39 |
---|---|---|
9 | 31F | |
10 | 32Ne | |
11 | 33Na | 39Na |
12 | 34Mg | 39Mg |
13 | 35Al | 39Al |
14 | 36Si | 39Si |
15 | 37P | 39P |
16 | 38S | 39S |
17 | 39Cl | 39Cl |
18 | 40Ar | 39Ar |
19 | 41K | 39K |
20 | 42Ca | 39Ca |
21 | 43Sc | 39Sc |
22 | 44Ti | 39Ti |
23 | 45V | |
24 | 46Cr | |
25 | 47Mn | |
26 | 48Fe | |
27 | 49Co | |
28 | 50Ni |
[1] - R. N. H. Haslam, L. Katz, H. E. Johns, H. J. Moody:
Confirmation of 39Cl Activity.
In: Physical Review, 76, 704, (1949), DOI 10.1103/PhysRev.76.704.
[2] - C. Papastefanou:
Chlorine-39 in rainfall at a temperate latitude (40°N).
In: Journal of Environmental Radioactivity, (2007), DOI 10.1016/j.jenvrad.2006.11.005.
Last update: 2023-10-09
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