Spontaneous fission (SF) is a form of radioactive decay in which a heavy atomic nucleus splits into two or more lighter nuclei. In contrast to induced fission, there is no inciting particle to trigger the decay; it is a purely probabilistic process.
Spontaneous fission is a dominant decay mode for superheavy elements, with nuclear stability generally falling as nuclear mass increases. It thus forms a practical limit to heavy element nucleon number. Heavier nuclides may be created instantaneously by physical processes, both natural (via the r-process) and artificial, though rapidly decay to more stable nuclides. As such, apart from minor decay branches in primordial radionuclides, spontaneous fission is not observed in nature.
Observed fission half-lives range from 60 nanoseconds () to greater than the current age of the universe ().
History
Following the discovery of induced fission by Otto Hahn and Fritz Strassmann in 1938, Soviet physicists Georgy Flyorov and Konstantin Petrzhak began conducting experiments to explore the effects of incident neutron energy on uranium nuclei. Their equipment recorded fission fragments even when no neutrons were present to induce the decay, and the effect persisted even after the equipment was moved 60 meters underground into the tunnels of the Moscow Metro's Dinamo station in an effort to insulate it from the effects of cosmic rays. The discovery of induced fission itself had come as a surprise, and no other mechanism was known that could account for the observed decays. Such an effect could only be explained by spontaneous fission of the uranium nuclei without external influence.
Mechanism
Spontaneous fission arises as a result of competition between the attractive properties of the strong nuclear force and the mutual coulombic repulsion of the constituent protons. Nuclear binding energy increases in proportion to atomic mass number (A), while coulombic repulsion increases with the square of the proton number (Z). Thus, at high mass and proton numbers, coulombic repulsion overpowers the nuclear binding forces, and the nucleus is energetically more stable as two separate fragments than as a single bound system.
Spontaneous fission is usually a slow process, as the nucleus cannot simply jump to the lower energy (divided) state. Instead it must tunnel through a potential barrier, with a probability determined by the height of the barrier. Such a barrier is energetically possible for all A ≥ 93, though its height generally decreases with increasing Z,
The stability of a nuclide against fission is expressed as the ratio of the Coulomb energy to the surface energy, which can be empirically estimated as the fissility parameter, x:
<math display=block>x \approx \frac{Z^2}{50.88A(1-\eta I^2)}</math>
with <math>I = \tfrac{N-Z}{A}</math> and <math>\eta \approx 1.78</math>. For light nuclei, x is small and a sizeable fission barrier exists. As nuclear mass increases, so too does the fissility parameter, eventually approaching and exceeding unity, where stability against fission is lost altogether.
Shell effects and nucleon pairing effects may further affect observed half-lives. Decays of odd-A nuclides are hindered by 3–5 orders of magnitude compared to even–even nuclides. The barrier to fission is expected to be zero around A = 300, though an island of stability may exist centred around Z = 114, N = 184.
Products
Fission fragments are usually neutron-rich and always generated in excited states. Ternary products are usually alpha-particles, though can be as massive as oxygen nuclei. Prompt gamma emission constitutes a further 8 MeV, while beta decay and delayed-gammas contribute a further and respectively.
Applications
The most common application for spontaneous fission is as neutron source for further use. These neutrons may be used for applications such as neutron imaging, or may drive additional nuclear reactions, including initiating induced fission of a target as is common in nuclear reactors and nuclear weapons. On the other hand, nuclear weapons based on plutonium-239 can fail due to the presence of spontaneous fission neutrons if they contain too much plutonium-240. The resulting "fizzle" is caused by the premature initiation of the nuclear chain reaction.
In crystals containing high proportions of uranium, fission products generated via spontaneous fission produce damage trails as the fragments recoil through the crystal structure. The number of trails, or fission tracks, may be used to estimate the age of a sample via fission track dating.
Spontaneous fission rates
thumb|upright=1.9|Spontaneous fission half-life of various nuclides depending on their Z/A ratio. Nuclides of the same element are linked with a red line. The green line shows the upper limit of half-life. Data taken from [[:fr:Fission spontanée#Noyaux décroissant par fission spontanée|French Wikipedia.]]
{| class="wikitable"
|+ Spontaneous fission rates
|-
! rowspan="2" | Nuclide
! rowspan="2" | Half-life<br/>(yrs)
! rowspan="2" | Fission branching ratio<br/>(% of decays)
! colspan="2" | Neutrons per
! rowspan="2" | Spontaneous<br/>half-life (yrs)
! rowspan="2" |
|-
! Fission
! Gram-sec
|-
| style="text-align:center;" |
| 7.04·10
| 2.0·10
| 1.86
| 0.0003
| 3.5·10
| 36.0
|-
| style="text-align:center;" |
| 4.47·10
| 5.4·10
| 2.07
| 0.0136
| 8.4·10
| 35.6
|-
| style="text-align:center;" |
| 24100
| 4.4·10
| 2.16
| 0.022
| 5.5·10
| 37.0
|-
| style="text-align:center;" |
| 6569
| 5.0·10
| 2.21
| 920
| 1.16·10
| 36.8
|-
| style="text-align:center;" |
| 8300
| 74
| 3.31
| 1.6·10
| 1.12·10
| 36.9
|-
| style="text-align:center;" |
| 2.6468
| 3.09
| 3.73
| 2.3·10
| 85.7
| 38.1
|}
See also
- Nuclear fission
- Natural nuclear fission reactor
- Alpha decay
- Cluster decay
Notes
External links
- File:Ndslivechart.png The LIVEChart of Nuclides at IAEA, with filter on spontaneous fission decay
<!--Categories-->