Gadolinium-136 is a radioisotope of the chemical element gadolinium, which has 72 neutrons in its atomic nucleus in addition to the element-specific 64 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 136. The very short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 136Gd is exclusively for academic purposes.
Gd-136 was first mentioned in a conference report from 2000; according to this, the isotope was observed as a fragmentation product during the irradiation of a zirconium-90 target with gold-197 (30 MeV per nucleon) [1]. A more recent report, published in 2026, describes the production and identification of gadolinium-136 during the irradiation of a 1 mm thick beryllium target with uranium-238 particles (345 MeV/nucleon) [2].
See also: List of individual Gadolinium isotopes (and general data sources).
Half-life T½ = > 310 ns respectively 3.1 × 10-7 seconds s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| EC β+ | 136Eu | ? | 7.154(358) MeV | |
| β+, p ? | 135Sm |
| Z | Isotone N = 72 | Isobar A = 136 |
|---|---|---|
| 39 | 111Y | |
| 40 | 112Zr | |
| 41 | 113Nb | |
| 42 | 114Mo | |
| 43 | 115Tc | |
| 44 | 116Ru | |
| 45 | 117Rh | |
| 46 | 118Pd | |
| 47 | 119Ag | |
| 48 | 120Cd | |
| 49 | 121In | 136In |
| 50 | 122Sn | 136Sn |
| 51 | 123Sb | 136Sb |
| 52 | 124Te | 136Te |
| 53 | 125I | 136I |
| 54 | 126Xe | 136Xe |
| 55 | 127Cs | 136Cs |
| 56 | 128Ba | 136Ba |
| 57 | 129La | 136La |
| 58 | 130Ce | 136Ce |
| 59 | 131Pr | 136Pr |
| 60 | 132Nd | 136Nd |
| 61 | 133Pm | 136Pm |
| 62 | 134Sm | 136Sm |
| 63 | 135Eu | 136Eu |
| 64 | 136Gd | 136Gd |
| 65 | 137Tb | 136Tb |
| 66 | 138Dy |
[1] - G. A. Souliotis:
Formation and studies of new proton emitters via intermediate-energy fragmentation of heavy-element beams.
In: Physica Scripta, 153, (2000), DOI 10.1238/Physica.Topical.088a00153.
[2] - H. Suzuki, N. Fukuda, H. Takeda et al.:
Discovery of Proton-Rich Radioactive Isotopes in the Z = 63-70 Region Produced by the Projectile Fragmentation of a 345-MeV/Nucleon 238U Beam.
In: Progress of Theoretical and Experimental Physics, 2, 023D02, (2026), DOI 10.1093/ptep/ptaf190.
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