The few fissile nuclei found in nature belong to heavy atoms, all possessing high atomic masses. On the map of observed nuclei, they are located near uranium at the upper end of the stability line (*). The most notable are uranium 233, uranium 235, plutonium 239 and plutonium 241. Less known are protactinium 230, neptunium 235 and americium 242. Most of them have very long lifetimes of several thousands or millions of years with a radioactive alpha decay
The size of fissile nuclei approaches the maximum allowed for a nucleus. All are unstable, but most of them have very long lifetimes of several thousands or millions of years with a radioactive alpha decay. More than their instability, the remarkable feature of these nuclei is their fragility when they capture an extra neutron.
They all have odd numbers of neutrons, with the lightest possessing 91 protons and 129 neutrons. The number of protons is even for the 4 main fissile nuclei (uranium 92 and plutonium 94) and odd for the other three.
These 7 fissile isotopes belong to the class of chemicals known as the 'actinides'.
Three of these have a practical use: uranium 233, uranium 235 and plutonium 239. Uranium 235 has the longest half-life of the three, with a period of 0.7 billion years. Now a extremely rare isotopes, it was 86 times more abundant at the time of the Earth's formation Plutonium 239 lives for only 24,000 years, but large quantities of it are regularly produced in uranium reactors. If thorium-based reactors become a reality, then the same will one day be true of uranium 233, whose half-life is 160,000 years.
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