Cluster decay

Cluster decay, also known as heavy particle radioactivity, is a rare type of radioactive decay in which an unstable atomic nucleus emits a small cluster of protons and neutrons, that is to say an atomic nucleus. The emitted nucleus (cluster) is larger than an alpha particle (a 4
2
He
nucleus) which has two protons and two neutrons), but is smaller than the typical fragments produced in spontaneous fission. In a nuclear fission process, the masses of the two nuclei that emerge are usually relatively close to one another.

The cluster decay process is a way for a heavy, unstable atom to become more stable. For example, an atom of 223
88
Ra
can emit a 14
6
C
nucleus (which contains 6 protons and 8 neutrons) and transform into a more stable 209
82
Pb
atom.

Cluster decay was theoretically predicted in 1980 by Aureliu Săndulescu, Dorin N. Poenaru, and Walter Greiner, and was first experimentally confirmed in 1984 by H. J. Rose and G. A. Jones.