Photodisintegration
Photodisintegration is a nuclear process in which an atomic nucleus absorbs a high-energy gamma ray, enters an excited state, and immediately decays by emitting a subatomic particle. The incoming gamma ray effectively knocks one or more neutrons, protons, or an alpha particle out of the nucleus. The reactions are called,, and, respectively.
Photodisintegration is endothermic for atomic nuclei lighter than iron and sometimes exothermic for atomic nuclei heavier than iron. Photodisintegration is responsible for the nucleosynthesis of at least some heavy, proton-rich elements via the p-process in supernovae of type Ib, Ic, or II.
This causes the iron to further fuse into the heavier elements.
Photodisintegration of deuterium
A photon carrying 2.22 MeV or more energy can photodisintegrate an atom of deuterium:James Chadwick and Maurice Goldhaber used this reaction to measure the proton-neutron mass difference. This experiment proves that a neutron is not a bound state of a proton and an electron, as had been proposed by Ernest Rutherford.
Photodisintegration of beryllium
A photon carrying 1.67 MeV or more energy can photodisintegrate an atom of beryllium-9 :Antimony-124 is assembled with beryllium to make laboratory neutron sources and startup neutron sources. Antimony-124 emits β− and 1.690 MeV gamma rays, yielding stable tellurium-124. Gamma rays from antimony-124 split beryllium-9 into two alpha particles and a neutron with an average kinetic energy of 24 keV :
Other isotopes have higher thresholds for photoneutron production, as high as 18.72 MeV, for carbon-12.