Protactinium-231
Th | → | Th | ← | Th | → | Th | (White actinides: t½<27d) | |||||||
↓ | ↓ | |||||||||||||
Pa | → | Pa | ← | Pa | → | Pa | (Colored : t½>68y) | |||||||
↑ | ↓ | ↓ | ↓ | |||||||||||
U | ← | U | ↔ | U | ↔ | U | ↔ | U | ↔ | U | → | U | ||
↓ | ↓ | ↓ | ↓ | |||||||||||
(Fission products with t½<90y or t½>200ky) | Np |
Protactinium-231 is the longest-lived isotope of protactinium, with a half-life of 32,760 years. In nature, it is found in trace amounts as part of the actinium series which starts with the primordial isotope uranium-235; the equilibrium concentration in uranium ore is 46.55 231Pa per million 235U.
In nuclear reactors, it is one of the few long-lived radioactive actinides produced as a byproduct of the projected thorium fuel cycle, as a result of (n,2n) reactions where a fast neutron removes a neutron from 232Th or 232U, and can also be destroyed by neutron capture though the cross section for this reaction is also low.
binding energy: 1759860 keV
beta decay energy: -382 keV
spin: 3/2-
mode of decay: alpha to 227Ac, also others
possible parent nuclides: beta from 231Th, EC from 231U, alpha from 235Np.
Read more about this topic: Isotopes Of Protactinium