Cluster decay

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Cluster decay is a type of nuclear decay in which a radioactive atom emits a cluster of neutrons and protons heavier than an alpha particle. This type of decay happens only in nuclides which decay predominatly by alpha decay, and occurs only a small percentage of the time in all cases. Cluster decay is limited to heavy atoms which have enough nuclear energy to expel a portion of its nucleus.


Cluster decay was discovered in 1987 when researchers at Oxford University detected that 223Ra emits one 14C nucleus for every billion (109) alpha decays.[1]


Cluster decay has an intermediate position between alpha decay (in which a nucleus spits out a 4He nucleus) and spontaneous fission in which a heavy nucleus splits into two large fragments and a variable number of neutrons. In cluster decay the emitted particle is a light nucleus and the decay always emits the same particle. More than 20 nuclei have been found which occasionally decay by emitting clusters.[1]

Tritons and deuterons are also known as radioactive decay products. Helium-6 occasionally decays via deuteron emission and Helium-8 decays a small part of the time with a triton emission. It is possible that other exotic isotopes decay in these methods as helium is studied in particle accelerators to a great degree.

The known cluster emissions are as follows:

Isotope Particle emission Branching ratio
221Fr 14C 9×10-15
221Ra 14C 1×10-14
222Ra 14C 3.0×10-10
223Ra 14C 8.9×10-10
224Ra 14C 4.0×10-11
226Ra 14C 3.2×10-11
225Ac 14C 6×10-12
228Th 20O 1×10-13
228Th Ne  ?
232U Ne 9×10-12
233U Ne 7×10-13
234U Mg

Ne

1×10-13

9×10-14

235U Ne

28Mg

8×10-12

8×10-12

236U 30Mg  ?
242Cm 34Si 1×10-16


References

External links

National Nuclear Data Center

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